1000 Sentences With "alluvium" | Random Sentence Generator

NASA's photos showed well-preserved river channels, deltas and fan-shaped masses of material called alluvium that is carried and deposited by water.

After a heavy rainstorm in May 2001, flooding in Nahal Arugot, near Ein Gedi on the edge of the Dead Sea, destroyed a modern highway bridge that had been designed to withstand such weather and filled a canyon with stone and alluvium in quantities officials said had not been seen in 40 years.

The alluvium which is found in the Indo-Gangetic plain belongs to this era. It was eroded from the Himalayas by the rivers and the monsoons. These alluvial deposits consist of clay, loam, silt etc. and are divided into the older alluvium and the newer alluvium.

Alluvium specifically refers to the geomorphic processes involved with flowing water and so alluvium is generally fine-grained clay and silt material that has the capacity to be entrained in water currents and eventually deposited. For these same reasons, alluvium is also generally well sorted material while colluvium is not.

These are the subtropical dry forest on alluvium and other unconsolidated sediments, subtropical moist forest on alluvium and other unconsolidated sediments and subtropical rainforest on volcanic rock altered by hydrothermal vents.

The endangered Geometric tortoise is largely confined to Alluvium Fynbos. The Geometric tortoise used to be found primarily in Alluvium Fynbos. Now, with its habitat largely destroyed, it is also critically endangered. Harmony Flats Nature Reserve, which conserves Alluvium Fynbos, lost its last population of these tortoises which became extinct here in the 1980s.

Most of the till in the vicinity of the stream is expected to be more than thick. Near the stream's mouth and also a few areas in its middle reaches, there are areas of alluvium. In the valley of the stream, the alluvium is approximately . Nearer to the valley of Huntington Creek, the alluvium is thick or more.

Older alluvium with sandy soil with variegated clay and loose boulder deposits and artesian flows; lateritic formations on higher contours and newer Alluvium on southern parts with reissuing springs akin to artesian flows.

This clay is also found around the alluvium along the river.

Glacial till, alluvium, and wetlands can be found in its vicinity.

The definitions of colluvium and alluvium are interdependent and reliant on one another. Distinctions between the two are important in order to properly define the geomorphic processes that have occurred in a specific geological setting. Alluvium is sand, clay, or other similar detrital material deposited by running water. The distinction between colluvium and alluvium relates to the involvement of running water.

The unit can be divided into three sets of flows separated by alluvium in the southern San Luis Valley. The alluvium separating the upper two flows is a significant local aquifer known as the Agua Azul.

Saltwater streams cut across the shoal. A recent geological formation, Brosselard-Faidherbe (1982), p. 10. Carabane consists of a shoal and alluvium. The alluvium has developed because of the saltwater streams that cut across the shoal.

Wisconsinan Till, Wisconsinan Outwash, and alluvium can be found in its vicinity.

Alluvial floodplains have developed in the lower park on deposits of quaternary alluvium.

Geologically, the study area comprises of alluvium, sandy clay, silt and fluviomarine sediments.

However, there are large patches of wetland and smaller patches of bedrock and alluvium.

Taupo Formation alluvium is the top layer on which most of the peat bogs formed.

The surface geology in its vicinity consists of alluvium, alluvial fan, Wisconsinan Till, and bedrock.

The surficial geology in its vicinity consists of alluvium, Wisconsinan Outwash, Wisconsinan Till, and bedrock.

The surficial geology in the creek's vicinity includes Wisconsinan Till, alluvium, alluvial fan, and bedrock.

The surficial geology in the area mainly features Illinoian Till, Illinoian Leg, alluvium, colluvium, and bedrock.

The surficial geology in the vicinity of the stream's mouth includes alluvium, Wisconsinan Till, and bedrock.

Soda Lake, view to southeast The parent materials for soils in the Carrizo Plain are predominantly alluvium deposits. Alluvium is soil that has been deposited by rivers or flowing water. The Paso Robles formation is a Pleistocene aged alluvium deposit that reaches up to thick near the San Andreas fault and thins out towards the north and west. The Paso Robles formation is a well known aquifer that has been reliably productive for ground wells throughout the area.

The surficial geology in the area mainly consists of Illinoian Till, Illinoian Lag, alluvium, colluvium, and bedrock.

The surficial geology in its vicinity mainly consists of Wisconsinan Till, bedrock, Boulder Colluvium, alluvium, and wetlands.

In the early 1900s, the Glen Brook Water Company planned to construct a dam on the creek. The surficial geology in the vicinity of Pond Creek includes Wisconsinan Till, alluvium, boulder alluvium, alluvial fan, and bedrock consisting of sandstone and shale, as well as some patches of wetland.

Lourensford Alluvium Fynbos growing at Harmony Flats Nature Reserve in Cape Town. Lourensford Alluvium Fynbos is a critically endangered vegetation type that is endemic to Cape Town. Though closest to Fynbos, it has characteristics of both Fynbos and Renosterveld vegetation and is thus actually a unique hybrid vegetation type.

110 In certain places, the batholith is overlain by the El Vergel Beds, alluvium and other Quaternary deposits.

The surficial geology in its vicinity consists of Wisconsinan Till, alluvium, Wisconsinan Ice-Contact Stratified Drift, and wetlands.

The surficial geology in its vicinity consists of Wisconsinan Till, alluvium, and bedrock. It has one unnamed tributary.

Once the alluvium deposited in the valley has begun to erode and fill terraces form along the valley walls, cut terraces may also form below the fill terraces. As either a stream or river continues to incise into the material, multiple levels of terraces may form. The uppermost being the fill terraces and the remaining lower terraces are cut terraces. Nested fill terraces: Nested fill terraces are the result of the valley filling with alluvium, the alluvium being incised, and the valley filling again with material but to a lower level than before. The terrace that results for the second filling is a nested terrace because it has been “nested” into the original alluvium and created a terrace.

The surficial geology in the vicinity of the mouth of Marsh Creek consists of alluvium and Wisconsinan Ice-Contact Stratified Drift. Further upstream, the surficial geology consists of Wisconsinan Till and bedrock consisting of sandstone and shale, though there are some patches of alluvium, Wisconsinan Ice-Contact Stratified Drift, and wetlands.

Andrew Orlowski, February 24, 2003 In 2004, CodeCon 3 was broadcast live using Alluvium 2.0.Codecon 2004 Conference Website. Alluvium was further developed and incorporated into software developed at and named after ActLab.TV, a peercasted TV and radio service operated by the ActLab at the University of Texas at Austin.

However, the stream's lower reaches are on alluvium containing stratified silt, sand, and gravel. The alluvium is approximately thick. The stream also passes through a small patch of fill near its headwaters, where it crosses Pennsylvania Route 118. The Wisconsinan Till Moraine occurs a short distance north of its headwaters.

The surficial geology in the creek's vicinity consists of Wisconsinan Till, alluvium, bedrock, fill, peat bogs, lakes, and wetlands.

The surficial geology in the area consists mainly of bedrock, along with alluvium, colluvium, Illinoian Till, and Illinoain Lag.

Inland narrow bands of alluvium floor the narrow incised valleys with wider extents at Oxwich Bay and Llangennith Moors.

Red Rock Pass has a surface deposit of calcareous silty alluvium with topsoil of dark grayish brown silt loam.

Alluvium, sand, gravel, barrier islands and loess define most of the Quaternary deposition from the past 2.5 million years.

The surficial geology in its vicinity consists of Wisconsinan Till, a lake, and some alluvium in the lower reaches.

In river plains, due to alluvium and availability of water, the farmlands are fertile but the soils remain immature.

The surficial geology in its vicinity includes Wisconsinan Till, alluvium, Wisconsinan Ice-Contact Stratified Drift, bedrock, and a lake.

Upper Saddle River, NJ: Prentice Hall. Once this occurs benches composed completely of alluvium form on the sides of the valley. The upper most benches are the fill terraces. As it continues to cut down through the alluvium the fill terraces are left above the river channel (sometimes 100 m or more).

River terraces of Mirusha valley are mainly constructed from pieces of rounded quartzite, Palaeozoic Slate, Cretaceous limestone, sandstone, serpentinite, diabase and Gabrovo. These fluvial terraces are of diluvial origin. Alluvium is common on both sides of the river Mirusha. In general there is not a wide spread in the area of Alluvium.

The Pennsylvania Department of Transportation also has a permit to maintain a box culvert made of reinforced concrete on the stream. This culvert is long and high and is sunk into the streambed. Culley Run flows over alluvium in its lower reaches. This alluvium contains stratified sand, silt, gravel, and some boulders.

The surficial geology in its vicinity mainly consists of alluvium, Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, bedrock, and wetlands.

The Mackenzie delta formed as alluvium drowned valleys. Thermokarst and an ice-cored landscape took shape in the early Holocene.

The surficial geology in its vicinity consists of Wisconsinan Till, alluvium, alluvial fan, Wisconsinan Ice-Contact Stratified Drift, and bedrock.

The surficial geology in the vicinity of the creek mainly consists of bedrock, Wisconsinan Till, alluvium, fill, wetlands, and lakes.

The surficial geology in its vicinity consists of alluvium, alluvial fan, Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Till, and bedrock.

Alluvium (containing stratified sand, silt, and gravel), Wisconsinan Outwash, alluvial terrace, wetlands, fill, and lakes also occur in the area.

There are also areas of river alluvium consisting of clay, silt and sand deposited by the main rivers and streams.

Granite supplied thousands of tons of rock fill to stabilize the SP line crossing the saturated alluvium of Elkhorn Slough.

Close to the rivers is khadar land of new alluvium that is subject to flooding. Above the flood limit, bangar land is older alluvium deposited in the middle Pleistocene. The annual rainfall increases from west towards the east. The Lower Ganges Plains and the Assam Valley are more verdant than the middle Ganga plain.

The soil is sandy and instantial laterite, mostly Recent Alluvium. Geological formations are concealed by Recent alluvium, with little or no exposure of rocks, most formations being Archean and tertiary sediments. Alluvial deposits of thickness of 28 meters, can amplify ground shaking during Tremors. Muthapudupet is a predominantly Tamil speaking area with sizable Telugu speakers.

In the Sybertsville quadrangle, the surficial geology in the valley of Little Wapwallopen Creek mainly consists of alluvium, alluvial terrace, alluvial fan, Wisconsinan Ice-Contact Stratified Drift, and some small patches of Wisconsinan Till. The surficial geology on the valley slopes and uplands mainly consists of bedrock. In the quadrangle of Freeland, the surficial geology near Little Wapwallopen Creek mainly features Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, and alluvium. The surficial geology near the creek in the Wilkes-Barre West quadrangle mainly consists of Wisconsinan Till, with some scattered areas of bedrock and alluvium.

The surficial geology in its vicinity consists of colluvium, alluvium, Illinoian Till, Illinoian Lag, and bedrock consisting of sandstone and shale.

Chowk is situated in southern part of Allahabad Municipal council.1 It is part of the Ganges plain with alluvium soil.

The surficial geology in its vicinity mainly consists of alluvium, Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, alluvial terrace, and wetlands.

The elevation near the mouth of Bee Sellers Hollow is above sea level. The elevation of the stream's source is between above sea level. In the upper and middle reaches of Bee Sellers Hollow, the surficial geology consists of colluvium and alluvium along the valley floor. Alluvium contains stratified sand, silt, and gravel, along with some boulders.

The older alluvium is called Bhangar and is present in the ground above the flood level of the rivers. Khaddar or newer alluvium is confined to the river channels and their flood plains. This region has some of the most fertile soil found in the country as new silt is continually laid down by the rivers every year.

The elevation near the mouth of Oxbow Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology near the mouth of Oxbow Creek mainly consists of alluvium. Slightly further upstream, there is still some alluvium, but also a till known as Wisconsinan Till, and bedrock consisting of sandstone and shale.

Glacial till covers much of the river bottom in its headwaters. Further downstream there is stratified drift and alluvium in the sediments.

In Western Australia it is found along creeks and in other damp areas in the Kimberley region where it grows in alluvium.

The surficial geology in its vicinity consists of Wisconsinan Till, Wisconsinan Outwash, Wisconsinan Ice- Contact Stratified Drift, alluvium, alluvial fan, and bedrock.

The surficial geology in the vicinity of Monument Creek consists of bedrock, Wisconsinan Till, alluvium, Wisconsinan Ice-Contact Stratified Drift, and fill.

The surficial geology in the stream's vicinity consists of Wisconsinan Till, bedrock, Wisconsinan Ice Contact-Stratified Drift, alluvium, and sand and gravel pits.

Surficial geology in the area mainly consists of alluvium, Boulder Colluvium, Wisconsinan Till Moraine, Wisconsinan Till, and bedrock consisting of sandstone and shale.

Little Creek is designated as Class A Wild Trout Waters. The surficial geology in its vicinity mainly consists of Wisconsinan Till and alluvium.

The old alluvium is found in the north of the district where it consists of kankars (stone dust). The new alluvium is available in the south of the district and is composed of silt, clay and sand. The alluvial soil is supposed to be brought by the Ganges and its tributaries from the Himalayas and is very rich in fertilizing nutrients.

Part of Moneypenny Falls The elevation near the mouth of Moneypenny Creek is above sea level. The elevation of the creek's source is between . The surficial geology along the lowest reaches of Moneypenny Creek mainly consists of alluvium, although Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Till, and bedrock occur nearby. Slightly further upstream, the surficial geology mainly consists of alluvium and bedrock.

Alluvium was developed as part of the Tristero project, hosted at Sourceforge, by Brandon Wiley. The source code, still in beta, is available as part of the Tristero project at tristero.cvs.sourceforge.net Alluvium was unveiled at CodeCon 2 in February 2003, generating interest in the peer-to-peer, open source, and streaming radio communities.Swarm Radio- a cheaper, faster 'casting tech The Register.

The surficial geology in the area consists of Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, alluvium, bedrock, fill, sand and gravel pits, and wetlands.

Kimberley white gum is found along swampy river flats in forest and woodland throughout the western Kimberley region where it grows in sandy alluvium.

Calcareous shales from the Canberra Formation are overlain by Quaternary alluvium. This rock is the limestone of the original title of Canberra "Limestone Plains".

Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, alluvium, sandstone and shale pits, and bedrock consisting of sandstone and shale all occur in the watershed.

The surficial geology in the area mainly features bedrock consisting of sandstone and shale, as well as a small amount of Boulder Colluvium and alluvium.

A planned trail is in its vicinity. The surficial geology in the area consists of alluvium, bedrock, peat bogs, wetlands, Boulder Colluvium, and Wisconsinan Till.

Soils range from pure sand and gravel to rich alluvium of river banks; shisham can grow in slightly saline soils. Seedlings are intolerant of shade.

The type of soil is partly Alluvium in nature. Temperature : Maximum 35-38 degree Celsius in Summer and Minimum 8-10 degree Celsius in Winter.

The zone has mostly alluvia soils developed from recent and old alluvium of mixed origin as well as those developed on very old river terraces.

In the upper reaches, the surficial geology is mostly Wisconsinan Till, with some alluvium and wetland. Tinker Creek has been described as a small creek.

In the gorge, the creek flows through a ledge of tough rocks with few cracks or fissures. Most of the upper reaches of the watershed of Pond Creek are on a glacial or resedimented till known as Wisconsinan Till. However, outcroppings of bedrock consisting of sandstone and shale occur on Penobscot Mountain. Small patches of alluvium and boulder alluvium occur along the creek downstream of Lily Lake.

The elevation near the mouth of York Run is above sea level. The elevation of the stream's source is between above sea level. The surficial geology near the mouth of York Run mainly consists of alluvium, alluvial fan, and Wisconsinan Ice-Contact Stratified Drift. Further upstream, the surficial geology consists of Wisconsinan Till and alluvium, but bedrock consisting of sandstone and shale is also in the area.

The elevation near the mouth of Hettesheimer Run is above sea level. The elevation of the stream's source is between above sea level. The surficial geology in the vicinity of the mouth of Hettesheimer Run consists of alluvial fan, alluvial terrace, alluvium, and Wisconsinan Ice- Contact Stratified Drift. Further upstream, the surficial geology along the stream consists of alluvium, while Wisconsinan Till is also in the area.

1:250,000 Taupo Pumice Alluvium (Q1a) was deposited on the Hinuera Formation (Q2a) until about 15,000 years ago. Some of the alluvium has been dug for sand and gravel. The Hinuera formation is also sand and gravel, interbedded with silt and some peat. In the last 14,000 years the Waikato River has cut into these formations, forming a low terrace and then cutting deeper.

The elevation near the mouth of Leslie Creek is above sea level. The elevation near the creek's source is above sea level. The surficial geology at the mouth of Leslie Creek mainly consists of alluvial fan, with some alluvium. Further upstream, the surficial geology along the creek consists mainly of alluvium, but the sides of the valley have a till known as Wisconsinan Till.

The estuarine plain is level to nearly level and consists of fine fluvial-marine deposits over sandy layers with marine shells. The fluvial marine deposits are usually saline at depths of approximately and includes depresses areas along the Bicol River. The river floodplain is made up of mixed alluvium. The piedmont plain on the fringe of the Ragay Hills consists of fine alluvium clay and reworked colluviums.

The web server handles static files: content, and the playlist(s). The Alluvium playlist file is a text file, residing on the web server, written in the Alluvium playlist format, which is based on the RSS 1.0 news format. The playlist file specifies the play order of URLs that can be hosted anywhere on the web. All RSS tags used are standard tags from existing schemas.

Alluvium of the Red River system creates the central and south Red River Delta. Two banks of the rivers are protected by a great dyke system.

Aside from volcanic deposits there are also traces of glaciation which has smoothened the slopes of Uturuncu, as well as Pleistocene and Holocene alluvium and colluvium.

Panther Creek is considered to be Class A Wild Trout Waters. The surficial geology in its vicinity consists of alluvium, alluvial terrace, Wisconsinan Till, and bedrock.

Boulder Colluvium, alluvium, and bedrock consisting of sandstone and shale can be found in the vicinity of the stream. It is on Pennsylvania State Game Lands.

When describing recent alluvium, the material that has arrived through volcanic, glacial or fluvial action can be described as a veneer on the (older) country rock.

The surficial geology in its vicinity consists of alluvium, Wisconsinan Till, Wisconsinan Outwash, alluvial fan, Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Bouldery Till, wetlands, and peat bogs.

The river flows over several soil types including Loam, Sand and Alluvium. There are over of drainage ditches that feed into the river, but few natural tributaries.

The surficial geology in its vicinity consists mostly of alluvium, Wisconsinan Till, and other things. Its watershed is designated as a Coldwater Fishery and a Migratory Fishery.

There are extensive spreads of coastal and estuarine alluvium on the Thames Estuary coast, in the low ground surrounding the Isle of Thanet and across Romney Marsh. Alluvium also floors the valleys of the River Medway and Stour. 'Clay-with-flints' is a commonly occurring deposit across the North Downs which is a product of periglacial conditions during the last ice age. Loessic deposists, of aeolian origin i.e.

The elevation near the mouth of Obendoffers Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology in the vicinity of the mouth of Obendoffers Creek consists of alluvial fan and alluvium, both of which contain stratified sand, silt, and gravel. Further upstream, there is alluvium, Wisconsinan Ice-Contact Stratified Drift, and bedrock consisting of coal, conglomerate, sandstone, and shale.

The elevation near the mouth of Monroe Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology near the mouth of Monroe Creek mainly consists of alluvium and alluvial terrace. Further upstream, it consists of alluvium and a till known as Wisconsinan Till, although bedrock consisting of sandstone and shale occurs in the surficial geology on some nearby hills.

Alluvium, Wisconsinan Outwash, Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Bouldery Till, Wisconsinan Till Moraine, and bedrock consisting of shale and sandstone all occur near the creek.

Rowanty Creek flows its entire distance through Coastal Plain alluvium. However, the two runs that form the creek start in Petersburg Granite that is part of the Piedmont.

The surficial geology in its vicinity consists of alluvium, alluvial terrace, and Wisconsinan Till. Its watershed is designated as a High-Quality Coldwater Fishery and a Migratory Fishery.

In Western Australia it is much more restricted being found on floodplains and basalt hillslopes in the Kimberley and Pilbara regions where it grows in sandy rocky alluvium.

The site at Plasketlands seems typical of "a combination of arable, grazing, peat, alluvium and marine resources".Bewley (1993), ch. 4, p. 35, quoted by Barrowclough, p. 148.

Part of the Wey Valley in the west of the parish and the banks of a stream which joins it from the east are particularly formed from alluvium.

There are very thick layers of till on the north side and bedrock on the south side. The surficial geology along the lower reaches of Dundaff Creek mainly consists of alluvium, with some patches of wetland and Wisconsinan Outwash nearby and Wisconsinan Till on the side of the valley. Further upstream, the surficial geology along the creek is still predominantly alluvium, but the alluvium band is thinner, with Wisconsinan Till coming much closer to the creek. There are also patches of bedrock consisting of sandstone and shale nearby, as well as a patch of Wisconsinan Outwash, a patch of alluvial fan and a much smaller patch of Wisconsinan Ice-Contact Stratified Drift.

The stream is affected by sediment deposits and debris such as fallen trees. Wisconsinan Till, alluvium, wetlands, and bedrock consisting of shale and sandstone occur in the stream's vicinity.

However, a small patch of alluvium is also present in this reach. Keeler Creek is a small stream that in 1827 was described as being able to support mills.

There is a layer of clay, sand and gravel alluvium overlaying this in the river channel. The river is greatly affected by rainfall, raising levels and muddying the water.

The surficial geology in the vicinity of its lower reaches mostly consists of alluvium and Wisconsinan Till, but there are patches of alluvial fan and bedrock nearby as well.

Some of the volcanoes in the area are highly alkaline. Alluvium and lake sediments of Quaternary age occur in parts of the Western Rift and along rivers and lakes.

Sorber Run looking downstream in its upper reaches The elevation near the mouth of Sorber Run is above sea level. The elevation of the stream's source is between above sea level. For most of the length of Sorber Run, the surficial geology immediately next to it consists of alluvium. However, the surficial geology of alluvium does not extend very far from the stream before being replaced by a till known as Wisconsinan Till.

The whole park lies on the Kerri formation, of Tertiary age, which is composed of sandstone, silt stones, kaolinites and grits. Underneath this lies the Gombe formation, of Cretaceous age, composed of sandstones, silt stones, and ironstones. The valleys of the Gaji, Yashi and Yuli Rivers are filled with Alluvium of more recent age. Sandy loans and clayey soils of riverine alluvium occur in the valley of the Gaji Yashi and Yuli Rivers.

The elevation near the mouth of Field Brook is above sea level. The elevation of the stream's source is between above sea level. The surficial geology near the mouth of Field Brook consists mostly of alluvium, but there is some till known as Wisconsinan Till in this reach as well. In the stream's middle reaches, the surficial geology alongside it consists mostly of alluvium, while the rest of the valley is mostly Wisconsinan Till.

These basalt flows are part of Atherton basalt province, which extends over an area of . The southern Jarra Creek portion of the TTA is dominated by granitic mountain ranges, which gives way to river alluvium and freshwater swamps to the south. The valley area also includes isolated pockets of basalt. The Downey and Jarra Creek valleys contain deep alluvium soils, which have been deposited by both stream overflow and by slope wash.

Deakin Volcanics red-purple and green grey rhyodacite with spherulitic texture cover most of Rivett except for Laidlaw Volcanics grey tuff on the southernmost quarter. Quaternary alluvium covers the center.

The drift geology of the Midhurst area comprises alluvium following the course of the River Rother and its tributaries, together with associated river terrace deposits of gravels, sands and silts.

The present geomorphology is marked by deep valleys, eroded as a result of the regional uplift. Throughout the Quaternary deposition of alluvium and freshwater tufa occurred in the valley bottoms.

Sills and dikes of rather massive greenstone are very generally distributed along the creek. The alluvium includes pebbles derived from bed fock, light micaceous sands, and in some places quicksands.

The solid geology of Baptist Mills comprises Triassic Redcliffe Sandstone, which is overlain by superficial deposits of Quaternary alluvium in the floodplain of the Horfield Brook and the River Frome.

With a coastline about 20 kilometers long, Nga Sơn annually encroaches into the sea some 80-100 meters per year due to alluvium deposits from the Red and Day Rivers.

Tertiary and Pleistocene alluvium consisting of sand, gravel, pebbles, and cobbles has accumulated in Six Bit and Poor Man's Gulches in the northern and eastern portions of the Management Area.

Deakin Volcanics green-grey and purple rhyodacite underlies the whole suburb. Deakin Volcanics cream rhyolite occurs on the top of Farrer Ridge. Quaternary alluvium can be found in the valley bottom.

The surficial geology near its mouth consists of alluvium, Wisconsinan Outwash, and Wisconsinan Till. The creek is a High-Quality Coldwater Fishery, a Migratory Fishery, and Class A Wild Trout Waters.

The surficial geology in the vicinity of the stream consists of alluvium, alluvial terrace, and Wisconsinan Till. Its watershed is designated as a High-Quality Coldwater Fishery and a Migratory Fishery.

The surficial geology in its vicinity consists mainly of alluvium, Wisconsinan Till, bedrock, Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Outwash, and peat bogs. Several bridges have been constructed over the creek.

However, it is considered to be impaired by abandoned mine drainage. The surficial geology in the creek's vicinity consists of alluvium, fill, urban land, strip mining land, Wisconsinan Till, and bedrock.

In 1884 the stream ran at top of the terrace. 1939 photo by United States Geological Survey. Fill terraces: Fill terraces are the result of an existing valley being filled with alluvium. The valley may fill with alluvium for many different reasons including: an influx in bed load due to glaciation or change in stream power which causes the valley, that was down cut by either a stream or river, to be filled in with material (Easterbrook).

Plucking is common in jointed rocks, where this occurs. Alluvial channels are much more common and can be large or small. All large rivers, and most small ones, have channels that are usually lined with alluvium, sediment that was carried to that channel reach by the river and that eventually will be carried farther downstream. This lining of alluvium creates a protective shield over the bedrock, which means it takes a much greater stream power to carve the channel.

The formation consists principally of tholeiitic olivine basalt flows with interlayered beds of alluvium. The basalt is distinctive for its olivine content (typically altered to iddingsite) and its diktytaxitic texture, in which the basalt contains laths of plagioclase that are randomly oriented and have angular spaces between grains. Geologists have not reached consensus on whether the alluvium beds should be regarded as part of the formation. These are lithologically similar to nearby sedimentary units of the Santa Fe Group.

The surficial geology in the vicinity of the stream's lower reaches consists of Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, bedrock, and alluvium. A bridge carrying Pennsylvania Route 690 crosses the stream.

It will succeed in almost any soil but prefers a rich loam or > black alluvium, and, though naturally a plant of rather dry places, will do > well in moist land, if drained.

The surficial geology in its vicinity consists of Wisconsinan Outwash, alluvium, Wisconsinan Till, bedrock, and a lake. The stream's watershed is designated as a High-Quality Coldwater Fishery and a Migratory Fishery.

This is one of the few remaining spots of the critically endangered vegetation type Lourensford Alluvium Fynbos. Local volunteers and community organisations are now heavily involved in protecting and managing the reserve.

The geology of the area is very young alluvium surrounded by very old parent rock. These old rocks have weathered to clay, which is incorporated in the alluvial soils of the valley.

The surficial geology in the vicinity of Nine Partners Creek includes Wisconsinan Till, alluvium, bedrock, alluvial fan, and wetlands. The creek's drainage basin is designated as a Coldwater Fishery and a Migratory Fishery.

The two main geological formations are Antalo Limestone in most of the tabia, and Adigrat Sandstone on the slopes towards the river gorges. Quaternary alluvium and freshwater tufa occur in the valley bottoms.

Laidlaw Volcanics pale to dark grey dacitic tuff covers most of Chapman. Shale, sandstone, ashstone and tuff is found near the west end of Rafferty Street. Quaternary alluvium covers up the eastern valley.

It was noted that, "The deposit is probably of considerable extent, but its dimensions cannot be correctly ascertained on account of the bed-rock in the vicinity being hidden from view by alluvium".

In the interior, along the Congo River, most groundwater is stored in permeable unconsolidated Congo Basin alluvium, which can be up to thick. Small areas of this unconsolidated Quaternary alluvium are also found near the Atlantic coast. The Coastal basin aquifer is made up of Cenozoic clay-rich sands, dolomitic sandstones and dolomitic limestones with low hardness and a neutral pH but relatively high salinity and sulfide. The unit is known from exploratory wells drilled in search of potash, water and petroleum.

Until about 960, the Isle of Thanet was an island, separated by the Wantsum channel, formed around a deposit of chalk; over time, the channels silted up with alluvium. Similarly Romney Marsh and Dungeness have been formed by accumulation of alluvium. Kent's principal river, the River Medway, rises near East Grinstead in Sussex and flows eastwards to Maidstone. Here it turns north and breaks through the North Downs at Rochester, then joins the estuary of the River Thames near Sheerness.

The greater portion of the district consists of a rolling country covered by laterite and alluvium. While metamorphic or gneissose rocks are found to the extreme west, to the east there is a wide plain of recent alluvium. Strong massive runs of hornblendic varieties stretch across the region in tolerably continuous lines, the general strike being nearly east and west. The most characteristic geological feature of the district is the area of laterite and associated rocks of sand and gravel.

The elevation near the mouth of Taques Creek is above sea level. The elevation near the source of the creek is above sea level. The surficial geology near the mouth of Taques Creek mainly consists of a till known as Wisconsinan Till and bedrock consisting of sandstone and shale, though there is some fill and alluvium at the mouth. Further upstream, the surficial geology along the creek itself mainly consists of alluvium, though most of the rest of the valley is Wisconsinan Till.

Further upstream, the surficial geology in the area mostly consists of Wisconsinan Till, but there are large patches of bedrock consisting of sandstone and shale, smaller patches of alluvium and wetland, and a lake.

The surficial geology in its vicinity consists mainly of Wisconsinan Till, alluvium, with some lakes, wetlands, bedrock, and alluvial fan. The stream's drainage basin is classified as a Coldwater Fishery and a Migratory Fishery.

However, small patches of alluvium, Boulder Colluvium (which contains numerous quartz, sandstone, and shale boulders), and wetlands are also present. A hill known as Pinnacle Hill is in the watershed of Plank Bridge Creek.

The tract is considered as an area of jungle- covered of old alluvium. It is an elevated plateau, with hillocks of varying heights, ranging from 30 to 60 feet. There are also cultivated valleys.

The surficial geology near the creek features alluvium, Wisconsinan Till, Wisconsinan Boulder Till, a peat bog, and bedrock consisting of sandstone and shale. Bear Hollow is listed on the Luzerne County Natural Areas Inventory.

Quaternary sediments include raised beach deposits which are extensive across the island and incorporating areas of alluvium locally. There are considerable areas of blown sand in the west and behind the major bays elsewhere.

Part of the river with its alluvium and surroundings is a unique environment with a fragile nature balance. In an otherwise industrialized and densely populated region, it is quite special, and hence is protected.

The Yogyakarta depression area is mostly covered by alluvium and the volcanic deposit of Mount Merapi. The Yogyakarta depression area is located between the volcanic arc of the Central Java and the Java Trench.

On sandy podzols (Wilde et al. 1949), it is usually a minor species (Nienstaedt and Zasada 1990). Good development occurs on moist alluvium (Seeley, cited by Nienstaedt 1957; Jeffrey 1961, 1964; Lacate et al.

The Gondwana system is represented in the northern portion of the district, south of the Damodar, between Mejia and Biharinath Hill. The beds covered with alluvium contains seams of coal belonging to the Raniganj system.

The Santa Teresa Formation conformably overlies the San Juan de Río Seco Formation and is covered by subrecent alluvium. The formation is part of the sequence after the Eocene unconformity.Lamus Ochoa et al., 2013, p.

Deakin Volcanics red-purple and green grey rhyodacite with spherulitic texture cover most of Stirling except for Laidlaw Volcanics pale to dark grey tuff on the southernmost quarter. Quaternary Alluvium covers the south west quarter.

Calcareous shales from the Canberra Formation are overlain by Quaternary alluvium. This rock is the limestone of the original title of Canberra "Limestone Plains". Several fault lines pass through Turner including the inactive Acton Fault.

Width 1–2 mm, and of the paratype: Height 3–1 mm. Width 1–0 mm. Type locality:. Gurmat Ali, right bank, 56 ft below surface of Alluvium holotype; Recent, Madras, M. D. Crichton leg.

It flows through a lake known as Tingley Lake in its upper reaches. The surficial geology in the vicinity of Leslie Creek mainly includes Wisconsinan Till and alluvium, with some alluvial fan, wetlands, and lakes.

Moneypenny Creek has experienced flash flooding. The surficial geology in its vicinity consists of Wisconsinan Till, bedrock, alluvium, and Wisconsinan Ice-Contact Stratified Drift. The creek's watershed is a Coldwater Fishery and a Migratory Fishery.

Mount House box is found along watercourses and on plains where it grows in alluvium and heavy clay soils. Populations are found in the Kimberley region of Western Australia, the Northern Territory and northern Queensland.

Yanal Bog is a calcicolous lowland mire. Underlying the site are gravels and clay alluvium. Above this sits a layer of peat. This results in a high water table, creating a distinct domed landscape feature.

The soil consists mainly of recent sediments (Alluvium, Teri’s, Brown sands etc.). Hydromorphic saline soils are also found in the areas surrounding the backwaters. The major rock types are Archaean-basic dykes, Charnockites and Gneisses.

The stream has one unnamed tributary. Many reaches of the stream have been affected by mining and abandoned mines. The surficial geology in its vicinity features alluvium, coal dumps, surface mining land, and Wisconsinan Till.

Initially these are mainly the Late Quaternary Piako Subgroup, which includes Late Pleistocene alluvium, and minor fan deposits of unconsolidated to very soft, thinly to thickly bedded, yellow- grey to orange-brown, pumiceous mud, silt, sandy mud and gravel, with local muddy peat. Finally, the river flows mostly over the Holocene floodplain, where the alluvium and colluvium consist of variously coloured, unconsolidated sand, silt, mud, clay, local gravel and thin intercalated (a form of interbedding, where distinct deposits in close proximity migrate back and forth) peat beds.

The elevation near the mouth of Willow Brook is above sea level. The elevation near the stream's source is above sea level. The surficial geology near the mouth of Willow Brook includes alluvium (which contains stratified silt, sand, and gravel), a till known as Wisconsinan Till, and bedrock consisting of sandstone and shale. In the vicinity of the lower reaches of the stream, there are patches of alluvium and wetlands, as well much Wisconsinan Till, all typically having thicknesses of or more in the general area.

Pliocene rocks include 30 meters of marl in the Yafo Formation and marl, conglomerate and sandstone 20 meters thick in the Bira, Gesher and Pleshet formations. Conglomerate and volcanic rocks mark the transition to the Quaternary. During the last 2.5 million years, sandstone, mudstone, oolitic limestone, conglomerate, gypsum and aragonite varves were deposited as well as travertine, calcareous sandstone, red sand loam and alluvium. Recent sands and alluvium dominates most river valleys and coastal areas, while conglomerate, gravel and playa deposits are more common in the south.

These hills are consist of a narrow belt of folded neogene molasse type sediments (siwaliks). Southward, the folded siwaliks sequence is covered by Indo-Gangetic Plain alluvium. An acute fault is "Himalayan front fault" cut the alluvium in foothill region, this fault is a series of en-echelon faults which are parallel to the strike of the hills between Punjab and Assam. Northward, this sequence is terminated by MBT, which is a set of north dipping faults and forms the boundary between Southern Himalayas and Lesser Himalayas.

The geology of the commune is limestone from the Jurassic period, part of the Aquitaine Basin as with all the northern half of Charente. The commune is on an Upper Jurassic area, specifically the Kimmeridgian. A small area of sandy soil dating from the Quaternary period covers the plateau in the south-west of the commune and alluvium (silt and clay) cover the Aume Valley on the north-eastern border. The oldest alluvium has accumulated in terraces mainly in the north of the commune.

The drainage basin of Partners Creek is classified as a Coldwater Fishery and a Migratory Fishery. The surficial geology in the vicinity of the creek consists of Wisconsinan Till, alluvium, bedrock, wetlands, lakes, and alluvial fan.

The underlying geology is chalk, which outcrops in places along the east side of the valley. The subsoil is predominantly a stiff reddish clay-with-flints; in the valley itself the chalk is overlain with alluvium.

The geology of Israel includes igneous and metamorphic crystalline basement rocks from the Precambrian overlain by a lengthy sequence of sedimentary rocks extending up to the Pleistocene and overlain with alluvium, sand dunes and playa deposits.

Further upstream, alluvium and Wisconsinan Till are also prevalent. However, there is also a patch of Wisconsinan Ice-Contact Stratified Drift, another patch of Wisconsinan Bouldery Till, and a few patches of wetlands and peat bogs.

The surficial geology in the vicinity of Brish Run mostly consists of Wisconsinan Till, but there is alluvium near its mouth and also bedrock in the area. The stream is being considered for wild trout designation.

It is named after marshes, which can be found in the vicinity of the stream. Alluvium and Wisconsinian Outwash area also present, as is bedrock consisting of sandstone and shale. The stream has one unnamed tributary.

Glacial activity occurred near the stream during the Wisconsinan Glaciation. Wisconsinan Ice-Contract Stratified Drift, Wisconsinan Bouldery Till, Wisconsinan Till, and alluvium can be found near the stream. A bridge was constructed over it in 2000.

The area has a diversity of soil types, mostly calcareous sediments mixed with alluvium and clay. Some of the most acclaimed vineyards in the region are found on some of the scattered limestone deposits in the area.

The soil of Magor Marsh is mostly peat with a depth of around . Beneath this is alluvium laid down by the Severn Estuary. The level of water must be kept near the surface to preserve the peat.

Wild trout inhabit Paint Spring Run. Wisconsinan Till, Wisconsinan Bouldery Till, Wisconsinan Ice- Contact Stratified Drift, alluvium, peat bogs, wetlands, and bedrock consisting of sandstone and shale all occur in the surficial geology in the stream's vicinity.

The plain in the south of Jalpaiguri, Alipurduar and Cooch Behar district is also made of new alluvium deposited by numerous rivers like the Teesta, Torsa, Raidak, Jaldhaka, Sankosh, Balason, Punarbhaba, Atrai and several other small rivulets.

The Terai is crossed by the large perennial Himalayan rivers Yamuna, Ganges, Sarda, Karnali, Narayani and Kosi that have each built alluvial fans covering thousands of square kilometres below their exits from the hills. Medium rivers such as the Rapti rise in the Mahabharat Range. The geological structure of the region consists of old and new alluvium, both of which constitute alluvial deposits of mainly sand, clay, silt, gravels and coarse fragments. The new alluvium is renewed every year by fresh deposits brought down by active streams, which engage themselves in fluvial action.

Alluvium is open source peercasting software developed by the Foundation for Decentralization Research, first released in 2003. It comprises three components, Core, Media Player, and Server. Alluvium allows video and audio programming to be broadcast over the Internet using swarming technology. It is powered by Onion Networks' Swarmcast, and is notable for its incorporation of server-side time-based playlists, and client software which examines those playlists and begins streaming content from the server(and available peers) per that schedule, simplifying the creation of continuous-broadcast video and audio.

The surficial geology along the stream in its lower reaches mainly consists of alluvium, surface mining land, coal dumps, and fill. There are also areas of a glacial or resedimented till known as Wisconsinan Till nearby, and also bedrock consisting of sandstone and shale. Further upstream, the surficial geology in the stream's vicinity mainly consists of Wisconsinan Till, but there are patches of alluvium and peat bogs near the Brace Brook Reservoir. Bedrock consisting of sandstone and shale lines the sides of the stream's valley in its middle reaches.

Further upstream, the surficial geology along the creek continues to consist mainly of alluvium, but there are several patches of Wisconsinan Ice-Contact Stratified Drift nearby, as well as one small patch of alluvial fan. Wisconsinan Till continues to line the sides of the valley and bedrock is present on nearby hills. In the upper reaches, the surficial geology along the creek mainly includes Wisconsinan Till, but there are patches of alluvial fan, alluvium, and wetlands. At the headwaters, there is Butler Lake and patches of wetlands and peat bogs.

However, there are some areas containing bedrock consisting of sandstone, shale, conglomerate, and coal. The same is true in the lower reaches of the watershed, but there are also areas of alluvium along the creek near its mouth.

Currently the San Jorge is one of the rivers with fish wealth, but its high pollution and deterioration was due largely to fishing with explosives and obtaining gold alluvium of its waters by the method of flotation mercury.

It has an alkalinity concentration of 2 milligrams per liter, but is slightly acidic. The surficial geology in its vicinity mainly consists of alluvium, Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, and bedrock consisting of sandstone and shale.

The solid geology is macroporphyritic basalt with carboniferous limestone at the Middleton Quarry site and these are both overlain by low river terrace and lake alluvium. A whinstone crag and old quarry site sit close to Lochend Farm.

View of Methow River from Goat Wall, Prime Rib, overlooking the Methow Valley. Soils are characteristically Leiko stony ashy sandy loam. Rock types in surrounding areas include Cretaceous Andesite, and Quaternary Alluvium which is mostly in the valley.

The site lies to the north-west of Cricklade near the county boundary, and consists of three meadows which have been managed for hay followed by grazing. The meadows overlie the alluvium and gravels of the Thames floodplain.

Quaternary and Tertiary sediments and sedimentary rocks are the formations in the lake basin and environs. The Quaternary sediments are of marine and fluvial alluvium of recent age. Tertiary sediments comprise laterite, sandstones and clays of Warkalai formation.

In the vicinity of the creek's upper reaches, the surficial geology mainly consists of Wisconsinan Till, although there is some alluvium and a patch of Wisconsinan Ice-Contact Stratified Drift near the confluence of the tributary Horton Creek.

The surficial geology in the vicinity of Field Brook consists of alluvium, Wisconsinan Till, alluvial terrace, alluvial fan, bedrock, wetlands, and a lake. The watershed of the stream is designated as a Coldwater Fishery and a Migratory Fishery.

There are also patches of alluvial fan, alluvial terrace, and bedrock consisting of sandstone and shale. In the upper reaches, the surficial geology is mostly Wisconsinan Till, but there is a patch of alluvium, wetlands, and a lake.

Part of the Olza River with its alluvium and surroundings from Dětmarovice to Bohumín (especially in Věřňovice) is an environment with fragile nature balance. In otherwise industrialized and densely populated area it is quite special, and hence is protected.

On a permeable basic rock such as chalk, the catena may consist of thick brown earths on the flatter facets, with thin rendzinas on the steeper slopes, while the valley bottom may include alkaline fen peat or river alluvium.

Aerial view from north east. Mount Ainslie is to the left. Calcareous shales from the Canberra Formation from the Silurian period is overlain by Quaternary alluvium. This rock is the limestone of the original title of Canberra "Limestone Plains".

Trees were cleared, the river diverted and dams and ponds built before the alluvium deposits were processed. Bucketwheel excavator dredges extracted material rich in cassiterite, which was pumped through pipes to floating processing plants that separated the tin ore.

There are deposits of alluvium - river laid sand, silt and gravel - along the floors of most of the larger valleys though these are typically narrow and discontinuous in their extent. At their seaward ends they merge with estuarine deposits.

Numerous bridges have been constructed across the creek. The surficial geology in its vicinity consists of alluvium, alluvial terrace, alluvial fan, Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Till, and wetlands. Numerous bridges have also been constructed across the creek.

An example is soil along the slopes of the Himalayan mountains. In river plains, particularly in flood-plain areas, new alluvium is deposited every year. The time for soil formation remains inadequate. Hence, flood plain soils also remain immature.

At least one bridge crosses the creek and the community of Broadway and several wetlands are in the watershed. The surficial geology in the creek's vicinity consists of Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, alluvium, wetlands, and bedrock.

205 though in many parts of the Tremp Basin the formation is exposed and covered by alluvium. The formation comprises several different lithologies, as sandstones, shales, limestones, marls, lignites, gypsum beds, conglomerates and siltstones have been registered.Arribas et al.

Lake Run is considered to be Class A Wild Trout Waters. The surficial geology in its vicinity consists of Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Till, Boulder Colluvium, alluvium, bedrock, sand and gravel pits, fill, wetlands, peat bogs, and a lake.

Overlies Biloxi Formation. Age is late Pleistocene. Gulfport Formation is limited to a 1- to 3-km-wide discontinuous barrier ridge belt that borders the Gulf mainland shore. Commonly overlies Prairie Formation (alluvium) landward and Biloxi Formation (shelf deposits) near shore.

Calcareous shales from the Canberra Formation is overlain by Quaternary alluvium. This rock is the limestone of the original title of Canberra "Limestone Plains".Henderson G A M and Matveev G, Geology of Canberra, Queanbeyan and Environs 1:50000 1980.

The types of rock about Ilaiyangudi are approximately 60 percent sedimentary rock and 40 percent igneous rock. There is sandstone, laterite, charnockite, gneiss and granite covered by thick alluvium.[environmentclearance.nic.in/writereaddata/.../06052017X0QV7Y9XSivagangai.pdf Sivagangai District Profile] Environment clearance. Government of India.

Further upstream, the surficial geology along the creek consists almost entirely of alluvium. However, large patches of Wisconsinan Till and bedrock, as well as smaller patches of Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Outwash, and peat bogs occur in close proximity.

However, there is also alluvium, Wisconsinan Till, and Wisconsinan Ice-Contact Stratified Dirft in the area. Further upstream, the surficial geology in the stream's vicinity consists of Wisconsinan Bouldery Till, but there is bedrock and Wisconsinan Till in the area.

Further upstream, the surficial geology near the creek mainly consists of a till known as Wisconsinan Till, with bedrock consisting of sandstone and shale on nearby hills, a patch of alluvium, a small patch of fill, and a couple of lakes.

The total area of Dhamrai Upazila is 307.4 km². It has 57,297 units of households. The Upazila consists of one municipality (Pouroshova), 16 unions and 398 villages. Dhamrai Upazila is composed of the alluvium soil of the Bongshi and Dholesshori rivers.

Phase I Environmental Site Assessment,301 West Lake Street, Mount Shasta, California, Earth Metrics Incorporated, San Mateo, California, Report Number 10363, December 18, 1989 The settlement is on the distal gently sloping southwest flanks of Mount Shasta, with the chief surficial soils being Quaternary alluvium. This alluvium is adjacent to and probably underlain by volcanic clastic rock deposited by Mount Shasta in the course of its development. Groundwater elevation is approximately at the elevation of the underlying native black peat soil. Where it occurs this peat, of approximately two feet thickness, is underlain by stream deposit sands and gravels.

As well as clay soils, the Bracklesham Beds result in some bands of sandy soil to the north of West End, and podzol soils around the M27 motorway west of Hedge End and on small areas of the gravels on top of the beds themselves. However most of the soil over the beds is more fertile brown earth. In the north of the borough, small pockets of valley gravels, London clay, Brickearth and Alluvium can be found, although these have mainly been built over with the exception of the Alluvium, which forms peaty soils around the floodplain of the River Itchen.

Deakin Volcanics green grey and purple rhyodacite underlies the suburb. These rocks are from the Silurian period. But it is overlaid by alluvium in the low- lying parts.Henderson G A M and Matveev G, Geology of Canberra, Queanbeyan and Environs 1:50000 1980.

Holocene alluvium and Quaternary sediments is a largely unconsolidated unit and is composed mostly of gravel and floodplain sediments. The sediments that mark the top of the basin can be found in modern streams/rivers and at the base of the foothills.

It is found in the IBRA regions of the Central Kimberley, the Gascoyne, the Gibson Desert, the Great Sandy Desert, the Little Sandy Desert, and the Pilbara, growing on sandplains, sand ridges, and drainage lines, on red sand, sandy gravel, and alluvium.

This melaleuca is widespread in Queensland north of about Bundaberg, in the Northern Territory and the northern Kimberley in Western Australia. It occurs in a wide range of habitats including alluvium, sandy soils, along watercourses, in damp depressions and red sand dunes.

However, patches of alluvium, wetlands, and lakes occur along some areas of the creek and the surficial geology on some nearby hills include bedrock consisting of sandstone and shale. There is also a patch of alluvial fan near the mouth of the creek.

Its major tributaries are the Assa and Argun. With a turbidity of , it carries 12.2 million tons of alluvium per year. It is used for irrigation. Cities that lie on the Sunzha include Nazran, Karabulak, Grozny (the capital of Chechnya), and Gudermes.

The newer alluvium, called khandar, forming the lowlands between the Ganga and Bhangar, is light coloured, poor in calcareous contain and composed of lenticular beds of sand, gravel and clays. The economic minerals found in the district are kankar, reh and sand.

Calcareous shales from the Canberra Formation is overlain in places by Quaternary alluvium. This rock includes the limestone of the original title of Canberra "Limestone Plains".Henderson G A M and Matveev G, Geology of Canberra, Queanbeyan and Environs 1:50000 1980.

The creek is crossed by a pipeline and a bridge carrying Pennsylvania Route 118. Wisconsinan Ice-Intact Stratified Drift, alluvium, Wisconsinan Till, Wisconsinan Bouldery Till, and bedrock consisting of sandstone and shale all occur in the surficial geology in the creek's vicinity.

Hall, Henry R. and Woolley, C. Leonard. 1927. Al-'Ubaid. Ur Excavations 1. Oxford: Oxford University Press. In South Mesopotamia the period is the earliest known period on the alluvial plain although it is likely earlier periods exist obscured under the alluvium.

There are some patches of peat bogs, wetlands, and lakes near the creek, but the surficial geology in the upper reaches mostly consists of alluvium and Wisconsinan Till, with some bedrock further away. Bear Swamp is not designated as an impaired waterbody.

Before the creation of Uttarakhand on 9 November 2000,Uttarakhand Govt. of India, Official website. Roorkee was a part of the state of Uttar Pradesh. The city is located in the Roorkee plain which is composed of recent alluvium with a gentle slope.

Bhavnagar District covers an area of over 8334 km2. The coastal area is mostly alluvium. Bhavnagar borders with Ahmedabad District to the northeast, Botad District to the northwest, the Gulf of Cambay to the east and south and Amreli District to the west.

Hall, Henry R. and Woolley, C. Leonard. 1927. Al-'Ubaid. Ur Excavations 1. Oxford: Oxford University Press. In South Mesopotamia the period is the earliest known period on the alluvial plain although it is likely earlier periods exist obscured under the alluvium.

It is native to an area of the Kimberley region of Western Australia. The shrub grows in sandy alluvium especially along watercourses in remote areas from around the Gibb River to around Karungie Station as a part of open Eucalyptus savannah communities.

It is endemic to an area in the Kimberley region of Western Australia where it is found on seasonally inundated flats with shallow skeletal alluvium overlying sandstone and dissected by outcropping sandstone ridges or in sandy soil around quartzite rocks alongside watercourses.

Quaternary alluvium is found in south and center of Gordon. Deakin Volcanics rhyodacitic crystal tuff from the Silurian age is on the surface in the north of the suburb.Henderson G A M and Matveev G, Geology of Canberra, Queanbeyan and Environs 1:50000 1980.

The orange garnets result from sodium-rich pegmatites. Spessartines are found in bedrock in the highlands in the Sahatany valley. Those in alluvium are generally found in southern Madagascar or in the Maevatanana region. Spessartine forms a solid solution series with the garnet species almandine.

Calcareous shales from the Canberra Formation is overlain by Quaternary alluvium. This rock is the limestone of the original title of Canberra "Limestone Plains". The higher parts of O'Connor in the west are different. Towards the south near Black Mountain is the Black Mountain Sandstone.

It is a member of the matlockite group. It was first described in 1935 from alluvium near bismuth-bearing pegmatites in South Africa. It has been found in association with granite pegmatite and in greisen. Associated minerals include bismutite, mica, jarosite, alunite, cerussite, atacamite, connellite.

The species is found on hillsides and in creek beds along the south coast in the Great Southern and Goldfields- Esperance region of Western Australia between Albany and Hopetoun, particularly in the Ravensthorpe Range, where it grows in loamy alluvium soils over granite or laterite.

The surficial geology in its vicinity consists of alluvium, Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Till, and Wisconsinan Bouldery Till. The stream is classified as Class A Wild Trout Waters and its watershed is designated as a High-Quality Coldwater Fishery and a Migratory Fishery.

Drew Conway is an American data scientist known for his venn diagram definition of data science as well as applying data science to study terrorism. He is currently the founder and CEO at technology startup Alluvium, as well as advisor at multiple technology startups.

Coal in Barakar formation is found in Barjora CD block. In Barjora coalfield a major part of the coal seams are covered with alluvium and laterite up to 35 m thick. As per the Geological Survey of India, proved reserve is 12 million tonnes.

These chloritic rocks acted as a lubricated sheet, effectively sliding off the batholith and tilting to the northwest during the Tertiary extension event. To the south, grabens that formed by normal faulting during crustal extension, are filled by the alluvium from the subsequent erosion.

The average annual rainfall in the area is . Much of the rainfall occurs from June to September when the snow melts and monsoons tend to start. The Ganga River tends to flow beyond capacity causing flooding and deposition of alluvium in the adjoining area.

Elevation map of south CaloocanElevation map of north Caloocan The geologic formation of the two portions of Caloocan City varies in type and characteristics. and are specifically classified as quaternary alluvium, tuff and tuffaceous sediment, pyroclastic flow deposit, and conglomerates. The formation on the eastern half of Metropolitan Manila extending to the coastline of Manila Bay and including a greater part of South Caloocan, is the quaternary alluvium - consisting of unconsolidated stream‐deposited sediments that includes sand, silt, clay or gravel. Eastward of South Caloocan, large areas consisting of tuff and tuffaceous sediment can be traced, spreading towards the whole eastern side of Metropolitan Manila.

Tees at Cliffe bordered by vegetation over alluvium The subsoil is magnesian limestone and recent alluvium by the Tees; the soil is a strong clay on a gravelly and sandy subsoil. In 1914 the chief crops raised were wheat, oats and turnips, the occupation of the people being mainly agricultural. In 1868 the land was "divided between arable and meadow, with about 80 acres of woodland". In 2007 the population for the whole of the Richmondshire 001D area, which includes Manfield, Aldbrough St John and Melsonby, was 1,447 residents and 619 dwellings; however Cliffe is much smaller than the other villages in the 001D area.

Silt and sand formed loess and dunes. During the last 11,000 years of the Holocene, Arkansas has experienced additional deposition of alluvium due to Mississippi River floods. Sand dikes formed due to significant seismic activity in northeast Arkansas in the vicinity of the New Madrid Seismic Zone.

Alluvium and alluvial fan occur near its mouth. The sides of the stream's valley contain bedrock consisting of sandstone and shale. The terminus of the glaciers during the late Wisconsinan glaciation bulged out in a small lobe near where the headwaters of Laurel Run are currently located.

The surficial geology along the lower reaches of the stream mainly features bedrock consisting of sandstone and shale. However, there is alluvial fan and alluvium near the mouth. There are a number of cascades on Cherry Run. The stream also flows through a glen at one point.

The shallow reservoir covers and is mostly hosted in porous Quaternary alluvium. Its basement is Himalayan granite and tuff. The water is a mixture of cold groundwater and deep thermal water. The deep reservoir was thought to have an area of below , contained in fractured bedrock.

For a significant portion of its length, Wasp Branch is on a glacial till known as Wisconsinan Till. However, Wisconsinan Ice-Contact Stratified Drift and alluvium are also found along portions of the stream. There is also bedrock made of sandstone and shale in its vicinity.

Superficial deposits of various kinds have accumulated during the Quaternary period. Narrow strips of alluvium i.e. accumulations of clay, silt, sand and gravel, occur along the valley floors Fragmentary rock material, the product of weathering, known as head is recorded. Peat of variable depth is extensive.

Bangaon subdivision is part of the Ichhamati-Raimangal Plain, one of the three physiographic regions in the district located in the lower Ganges Delta. It contains soil of mature black or brownish loam to recent alluvium. The Ichhamati flows through the eastern part of the district.

Basirhat subdivision is part of the Ichhamati-Raimangal Plain, one of the three physiographic regions in the district located in the lower Ganges Delta. It contains soil of mature black or brownish loam to recent alluvium. The Ichhamati flows through the eastern part of the district.

Isaacs and environs, taken from Isaacs Ridge Isaacs is built on Silurian age Deakin Volcanics. These are green-grey and purple coloured rhyodacite. The lower lying parts of the suburb are covered with Quaternary alluvium on top. Isaacs ridge has the same outcrops as the rest of the suburb.

Deakin Volcanics green grey and purple rhyodacite are in the west. Deakin Volcanics cream rhyolite is in high south east parts. Quaternary alluvium is in the north lower parts, washed off the surrounding slopes.Henderson G A M and Matveev G, Geology of Canberra, Queanbeyan and Environs 1:50000 1980.

Geologically in the Shan Hills and their southern subranges, layers of alluvium are superimposed on hard rock.Geology of Thailand - Ministry of Natural Resources and Environment, Bangkok Karstic ranges are common, for large tracts of the hills are limestone. The Shan Hills are an important silver and ruby mining area.

Streambed topography is the primary factor in creating rapids, and is generally consistent over time. Increased flow, as during a flood or high-rainfall season, can make permanent changes to the streambed by displacing rocks and boulders, by deposition of alluvium, or by creating new channels for flowing water.

Beth Run is a tributary of Bowman Creek in Luzerne County, Pennsylvania, in the United States. It is approximately long and flows through Ross Township and Lake Township. The watershed of the stream has an area of . The surficial geology along it consists of Wisconsinan Till and alluvium.

The Casa Grande series consists of very deep, well-drained, saline-sodic soils on fan terraces and relict basin floors. These soils formed in alluvium derived from granite, rhyolite, andesite, quartzite, and some limestone and basalt. Slopes generally are 0 to 5 percent. The climate is hot and arid.

The river measures from source to Redesmouth and drains an area of . In the upper reaches, the catchment is mostly upland and is partly in the Kielder Forest Park. In the lower reaches, the landscape changes slightly to grassland and upland heath with underlying boulder clay, alluvium and peat.

Wolf Run is a tributary of Bowman Creek in Luzerne County, Pennsylvania, in the United States. It is approximately long and flows through Ross Township. The watershed of the stream has an area of . The surficial geology in its vicinity consists of Wisconsinan Till, alluvium, alluvial fan, and bedrock.

Glacial lake outburst floods occurred during the melt outflow.University of Wisconsin Aquatic Sciences Center 2008 Flooding disturbed archaeological layers of lithics and ceramics in the alluvium of the south branch of the Potomac at the Romney bridge replacement archaeological site.GAI Consultants, Inc. (GAI) (2003) CWVA (retrieved 25 Nov 2010).

The Tura sandstone is a very thick unit, formed during the early and middle Cenozoic. It is named after the Tura range in the Tura district. Very little of the sandstone is visible at the surface. It forms three small hills at Takerghat, although these are blanketed in alluvium.

Stotts Island is composed of alluvium deposited from the Pleistocene to the present. It is prone to flooding, during which times silt and weed material accumulate on the island. The island is continuously being reshaped by erosion. The reserve contains an intact segment of lowland sub-tropical rainforest.

In the Pleistocene period, of 12.9 k a to 11.6 k a, the rivers re-formed into single channels, and meanders were formed. These became very distorted above the constrictions of the gorges. Down cutting occurred, exposing previous layers, creating terraces that were covered with silty clay alluvium.

It is endemic arid to semi-arid areas in the Mid West and western Goldfields regions of Western Australia, it occurs in watercourses, on floodplains, on flats, in low-lying areas and alongside rivers goring in red clay or loamy soils or on alluvium and stony red earth.

Rack Marsh is an old wet meadow. A thick layer of peat has developed on top of the deposits of alluvium and gravel which the river has spread over the chalk. The river Lambourn flows through the meadow. Aerial view of Rack Marsh, Bagnor, as seen in winter.

The elevation near the mouth of Mill Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology near the mouth of Mill Creek mainly consists of alluvium and Wisconsinan Ice-Contact Stratified Drift. However, slightly further upstream, Wisconsinan Till dominates.

Rhodamnia argentea is a rainforest tree of eastern Australia. Commonly known as malletwood, white myrtle, silver leaf, silver malletwood and white turpentine. The natural habitat is a variety of different rain forests, at sea level or in the adjacent ranges. Growing on sand, alluvium and volcanic based soils.

The height of the land gradually increases from the east to the west. The southern part of the upazila is composed of the alluvium soil of the Bangshi and Dhalashwari rivers. Main rivers are Bangshi, Turag, Buriganga and Karnatali. The Bangshi River has become polluted due to industrial.

The elevation near the mouth of Horton Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology along the lower reaches of Horton Creek mainly consists of alluvium. However, a till known as Wisconsinan Till lines the creek's valley.

The elevation near the mouth of Buck Run is above sea level. The elevation of the stream's source is above sea level. The surficial geology at the mouth of Buck Run consists of alluvium. However, most of the stream's valley has surficial geology featuring Illinoian Till and Illinoian Lag.

The soils consists mainly of recent sediments (Alluvium, Teri's, Brown sand etc.). Red colored sticky soil is also found in these areas. The climate is generally tropical, heavy rains from the southwest and northeast monsoon are common from June through September. The average annual rainfall is about 350 cm.

In 1972, BHP Deposit 20 located near the central southern boundary of the licence (E47/2855), was mapped however, no drilling was conducted. BHP identified haematite-goethite mineralization assigned to the Dales Gorge Member of the Brockman Iron Formation on the southern margin of the ranges. There still exists a large proportion of the rest of the licence area that is masked by Quaternary alluvium, in particular the central and northern blocks. Potential for both bedded (BID) and channel/detrital (CID/DID) iron deposits situated below recent alluvium tested has not been fully tested by historical exploration, whilst the priority target is the iron mineralization associated with the identified BHP Deposit 20.

Geologically the district forms part of the vast Indo-Gangetic alluvial tract, of which the origin is attributed to a sag in the earth's crust, formed, in the upper eocene times, between the northwardly drifting Gondwanaland and the rising Himalayan belt, and gradually filled in by sediments so as to constitute a level plane with a very gentle seaward slope. The alluvium formation of the district, comprising sand, silt & clay with occasional gravel, is of the early quaternary to sub-recent age. The older alluvium called bhangar, forms slightly elevated terraces usually above the flood levels. It is rather dark in colour generally rich in concretions and nodules of impure calcium carbonate, locally known as kankar.

In its lower reaches, the valley of the creek mostly contains alluvium and Wisconsinan Ice-Contact Stratified Drift. Wisconsinan Ice-Contact Stratified Drift consists of stratified sand and gravel, as well as some boulders. Bedrock consisting of sandstone and shale surrounds the valley and an alluvial fan occurs at its mouth.

The block was formed during the Eburnian orogeny, with the crystalline basement dated at 1,835 Ma, implying last Eburnian magmatism. Post-Eburnian sediments include the Mporokoso Group, the Kasama Formation, the Luitikila and Luapula Beds, and Cenozoic alluvium from the Chambeshi River and the Kalungu, Lower Chambeshi and Lake Bangweulu Basins.

Yogo sapphires were ultimately traced from the alluvium to their source. In February 1896, a sheepherder named Jim Ettien found the sapphire mother lode: the Yogo dike. Ettien was prospecting for gold, and found sapphires after washing gravel he found in a fissure within a limestone outcrop. Ettien staked two claims.

It is endemic to tropical areas in the Northern Territory where it is usually situated along creeks, in gullies or on sandstone hills where it is often found in colonies growing in alluvium or stony sandy soils as a part of shrubland, savannah grassland, Eucalyptus woodland or wet forest communities.

Furthermore, Justice Stevens concluded that "the very existence of words like 'alluvium' and 'silt' in our language" disproved Justice Scalia's assertion that material does not normally wash downstream.Rapanos, 547 U.S. at 807 (Stevens, J., dissenting) (citing Congress, Office of Technology Assessment, Wetlands: Their Use and Regulation , OTA-206, p. 48 (Mar.

A Camissonia resembling either of the two species on serpentine stream terraces outside of serpentine masses or mixed alluvium stream terraces could be either C. contorta or C. benitensis. C. strigulosa is the common Camissonia species found growing on nonserpentine alluvial stream and river deposits within the range of C. benitensis.

The lower ground in the west is largely covered by glacial till whilst higher ground in the east is free of superficial deposits. A small area of glacio-fluvial sands and gravels is mapped in the centre of the parish. A narrow strip of alluvium is associated with Salter's Brook.

Above the Buttermilk Falls, Buttermilk Creek flows over glacial drift. The creek is a relatively small stream with headwaters in a mountain lake. The surficial geology along most of Buttermilk Creek consists of alluvium. However, in the creek's upper reaches, Wisconinan Till makes up all the surficial geology along it.

Boulder clay is to the south and west, and first and second terrace river gravel to the east. Alluvium borders the Great Ouse. Underlying these superficial deposits is Oxford clay and Kellaways beds. Around the village the soil has low fertility, is freely draining and slightly acid with a loamy texture.

Bell Creek is a tributary of Tunkhannock Creek in Susquehanna County, Pennsylvania, in the United States. It is approximately long and flows through Gibson Township. The watershed of the creek has an area of . The surficial geology the creek's vicinity includes Wisconsinan Till, alluvium, bedrock, wetlands, lakes, and alluvial fan.

The elevation near the mouth of Bell Creek is above sea level. The elevation near the creek's source is above sea level. The surficial geology alongside Bell Creek at its mouth consists of alluvial fan. Further upstream, there is alluvium and a patch of bedrock consisting of sandstone and shale.

The elevation near the mouth of Thurston Hollow is above sea level. The elevation of the stream's source is between above sea level. The surficial geology along the lower reaches of Thurston Hollow mainly consists of alluvium. To the east, the surficial geology consists of bedrock and some Wisconsinan Till.

This range has a densely forested skirt of coarse alluvium called the bhabhar. Below the bhabhar, finer, less permeable sediments force groundwater to the surface in a zone of springs and marshes. In Persian, terai refers to wet or marshy ground. Before the use of DDT this was dangerously malarial.

W.B. Clarke first found traces of Alluvium gold in Dignams Creek in 1852. Gold mining then became a common activity in the area. A significant amount of gold was found in deposits along streams coming from Mount Gulaga's slopes. Between 1878 and 1920 approximately of gold was found in its slopes.

The concentration of alkalinity in the waters of Crooked Creek is 7 milligrams per liter. The elevation near the mouth of Crooked Creek is above sea level. The elevation of the creek's source is between . For much of its length, Crooked Creek flows through Wisconsinan Till, Wisconsinan Outwash, and alluvium.

It is a raised alluvium area along the Hooghly, which forms the western boundary of the district. Habra II CD Block has an area of 112.67 km2. It has 1 panchayat samity, 8 gram panchayats, 106 gram sansads (village councils), 78 mouzas and 78 inhabited villages.Ashoknagar police station serves this block.

The Tajo Basin received continental deposits from the end of Oligocene to the end of Miocene This basin is drained by the Tajo River to the Atlantic past Lisbon. The As Pontes Basin in the far northwest of Iberia filled with alluvium and lacustrine deposits from late Oligocene to early Miocene.

It contains soil of mature black or brownish loam to recent alluvium. The Ichhamati flows through the eastern part of the district. The Bidyadhari flows along the south-western border of the CD Block separating it from Haroa CD Block. Basirhat II CD Block has an area of 127.42 km2.

Alluvium is a technology for low-cost streaming media broadcasts. It differs in method from server-to-client streaming servers such as icecast, Real Server, and QuickTime Streaming Server. It requires only a standard web server and client software. No additional modules or CGI scripts are required for its operation.

The soil is composed of different varieties of alluvium. The main rivers are: Nagar, Mahananda, Kulik, Gamari, Chhiramati (Srimati) and Tangon. The rivers have little water in the dry season but with heavy rains, during monsoon, overflow the banks. The Mahananda river flows along the western boundary of Itahar CD Block.

The surficial geology in its vicinity consists of Wisconsinan Till, alluvium, bedrock, and fill. A number of bridges have been constructed over Kennedy Creek. The watershed of the creek is designated as a Coldwater Fishery and a Migratory Fishery. The creek flows through Lackawanna State Park in its lower reaches.

Deakin Volcanics green-grey and purple rhyodacite is under the suburb, but only exposed in the south east quarter. The rest is covered by Quaternary alluvium. The south west has Deakin Volcanics green grey, purple and cream rhyolite with the corner topped off with Deakin Volcanics red-purple and green grey rhyodacite.

Deakin Volcanics green-grey and purple rhyodacite is in the northern half and under Quaternary alluvium in the south. In the upper parts of the suburb are two patches of Deakin Volcanics green grey, purple and cream rhyolite. Further up Mount Taylor are Deakin Volcanics red-purple and green grey rhyodacite and porphyry.

Quaternary alluvium covers the whole suburb. This would have formed by erosion of the surrounding Deakin Volcanics in Chisholm and the hills to the east. Deep underneath are volcanic rocks from the Silurian age at 414 Mya.Henderson G A M and Matveev G, Geology of Canberra, Queanbeyan and Environs 1:50000 1980.

Alluvium contains stratified sand, silt, and gravel, as well as some boulders. Boulder Colluvium mainly contains boulders made of quartz, sandstone, or conglomerate. The Pennsylvania Game Commission has a permit to maintain a bridge over Deep Hollow. The bridge has a span of and the waterway opening underneath has an area of .

The elevation near the mouth of York Hollow is above sea level. The elevation of the stream's source is between above sea level. The surficial geology in the vicinity of York Hollow mainly consists of alluvium and colluvium. However, there is also Illinoian Till and Illinoian Lag present, as well as bedrock.

The surficial geology in its vicinity includes Wisconsinan Till, alluvium, wetlands, lakes, bedrock, and alluvial fan. The dominant land uses in the creek's watershed include forested land and agricultural land. A number of bridges have been constructed over the creek. Its drainage basin is designated as a Coldwater Fishery and a Migratory Fishery.

Elson, page 8. It is located atop the northernmost of the three ridges allowing for views of the central valley and portions of the Ocotlán alluvium. The site is extensively terraced but there is no evidence of irrigation canals, indicating that food was grown on the valley floor below.Elson, pages 8–9.

The soils of Stellenbosch range from dark alluvium to clay. This, combined with the well-drained, hilly terrain and Mediterranean climate, prove excellent for viticulture. Summers are dry and warm to hot, with some February and March days rising to over . Winters are cool, rainy and sometimes quite windy, with daytime temperatures averaging .

The elevation near the mouth of Horton Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology near the mouth of Horton Creek mainly consists of alluvium and a till known as Wisconsinan Till. However, there is also an area of Wisconsinan Outwash nearby.

Particulates on the river side of the soil interface may be periodically scoured away by turbulent flow. Wastewater percolation ponds may require maintenance to break up or remove a scum layer (Schmutzdecke) forming at the bottom of the pond. Biological filtration remains effective unless organic loading causes anaerobic conditions within the riverbed alluvium.

Silurian calcareous shales from the Canberra Formation is overlain by Quaternary alluvium. This rock is the limestone of the original title of Canberra "Limestone Plains". Greywacke from the Ordovician age Pittman Formation is in the north west.Henderson G A M and Matveev G, Geology of Canberra, Queanbeyan and Environs 1:50000 1980.

The geology of Husborne Crawley is made up of greensand sandstone, although there are areas of mudstone layered within the sandstone which is part of the Oxford Clay Formation. The soil is therefore mostly sandy and partially clay, with some smaller areas of mixed soil including; sand, alluvium, gravel, clay and silt.

York Run is a tributary of Bowman Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Noxen Township. The watershed of the creek has an area of . The surficial geology in its vicinity consists of alluvium, Wisconsinan Till, alluvial fan, and Wisconsinan Ice-Contact Stratified Drift.

The elevation near the mouth of Pikes Creek is between above sea level. The elevation of the creek's source is approximately above sea level. Pikes Creek flows through a manmade concrete flume for part of its length. A layer of alluvium with a thickness of occurs in the valley of Pikes Creek.

Broad Hollow Run is a tributary of Bowman Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Noxen Township. The watershed of the stream has an area of . The surficial geology in the vicinity of the stream consists of alluvium, alluvial fan, and Wisconsinan Till.

The elevation near the mouth of Utley Brook is above sea level. The elevation of the stream's source is between above sea level. The surficial geology in the valley of Utley Brook mostly consists of alluvium and a till known as Wisconsinan Till. However, there are also wetlands and lakes in the valley.

A few other small patches of it are located near the creek. Alluvium occurs along the creek in some places and there is a patch of sandstone and shale pits. A feature identified by the Federal Emergency Management Agency as an obstruction occurs on Browns Creek in Jackson Township, near a private road.

The elevation near the mouth of South Run is above sea level. The elevation of the stream's source is between above sea level. The surficial geology of the land adjacent to South Run mainly consists of alluvium. However, large areas of a till known as Wisconsinan Till also occur in the stream's watershed.

The soil is composed of different varieties of alluvium. The main rivers are: Nagar, Mahananda, Kulik, Gamari, Chhiramati (Srimati) and Tangon. The rivers have little water in the dry season but with heavy rains, during monsoon, overflow the banks. The Kulik river flows through a portion of the boundary with Raiganj CD Block.

The elevation near the mouth of Gardner Creek is above sea level. The elevation of the creek's source is between above sea level. For most of the length of Gardner Creek, the surficial geology on the floor of its valley consists mainly of alluvium. However, alluvial terrace is present in the lower reaches.

The alluvium is "10 feet (3 m) or more thick in the lower reaches of the Plunketts Creek valley", but only "6 feet (2 m) thick in headward tributary valleys". The outwash is described as "stratified sand and gravel that form terrace remnants along the flanks of Loyalsock Creek and Plunketts Creek valleys".

It is designated as a High-Quality Coldwater Fishery and a Migratory Fishery and the stream is Class A Wild Trout Waters. The surficial geology in its vicinity consists of alluvium, alluvial terrace, alluvial fan, bedrock, Wisconsinan Till, and Wisconsinan Ice-Contact Stratified Drift. A bridge carrying Pennsylvania Route 29 crosses the stream.

However, The Hindu reported that the state government is yet to take any concrete steps in this regard. Soil consists of sediments such as alluvium, teris, brown sands, etc. Hydromorphic saline soils are also found in the areas surrounding the backwaters. Predominant rock types found here are Archaean-basic dykes, Charnockites and Gneisses.

The elevation near the mouth of Newton Run is above sea level. The elevation of the stream's source is between above sea level. The surficial geology along the lower reaches of Newton Run consists of alluvium. Further away from the stream, this is flanked Wisconsinan Till and a patch of alluvial fan.

Calcareous shales from the Canberra Formation dates from the Silurian period. This rock is the limestone of the original title of Canberra "Limestone Plains". Quaternary alluvium lies on top of the shale in the flatter parts of Dickson.Henderson G A M and Matveev G, Geology of Canberra, Queanbeyan and Environs 1:50000 1980.

Marston lies west of the Peak District on the Cheshire Plain. Superficial Alluvium deposits on the West side of Marston has produced higher, fluctuating topography in this area as well as Glaciofluvial deposits on the South side producing a ridge by Wincham Brook. The surrounding flat areas are composed of Devensian Till.

The plain is bound on the north by the Himalayas, which feed its numerous rivers and are the source of the fertile alluvium deposited across the region by the two river systems. The southern edge of the plain is marked by the Chota Nagpur Plateau. On the west rises the Iranian Plateau.

The west dam rises to above the valley floor. It spans over a nearly flat alluvial valley floor between bedrock abutment ridges. About 65% of the dam's foundation area is founded on quartzite and phyllite bedrock. The remainder is founded on dense alluvium that fills three buried channels, which are up to deep.

The Kern River Beds Formation crops out in a roughly crescent-shaped belt, about wide at its widest, from Caliente Creek on the south to the Terra Bella vicinity on the north, a length of around . It ranges from in thickness. Where it does not outcrop, it is overlaid by Pleistocene Period alluvium.

Glaciofluvial deposits from the late stages of the ice age and post-glacial alluvium are also widespread. Beautifully coloured agates, which formed over millions of years in cavities (originally gas bubbles) in the volcanic lava which formed the hills, are occasionally to be found weathered out of the rock in the surrounding fields.

The elevation near the mouth of Rock Creek is above sea level. The elevation near the creek's source is above sea level. Rock Creek has been described as a small creek. The surficial geology near the lower reaches of Rock Creek mainly consists of alluvial terrace and alluvial fan, with some alluvium.

The elevation near the mouth of Tinker Hollow is above sea level. The elevation near the stream's source is above sea level. The surficial geology alongside Tinker Hollow in its lower and middle reaches mainly consists of alluvium. However, in its upper reaches, it mostly consists of a till known as Wisconsinan Till.

Culley Run (also known as Cully Run or Colley Run) is a tributary of Fishing Creek in Columbia County, Pennsylvania, in the United States. It is approximately long and flows through Benton Township. The stream's watershed has an area of . Shale, sandstone, alluvium, and glacial till can be found in the watershed.

Glacial sands and gravels occur in places along the eastern margin of the Wolds. There are extensive spreads of river, estuarine and coastal alluvium along the North Sea Coast and around the Wash as far inland as Crowland in the south and roughly along the line of the South Forty-Foot Drain. Alluvium also covers the flat floors of the Trent, Witham and Ancholme rivers whilst river terrace sands and gravels are widespread around Woodhall Spa, in the Trent valley and towards Lincoln, along the course of the River Slea and south of Sleaford through Bourne to Market Deeping. Areas of blown sand occur at Donna Nook and inland across an area centred upon Scunthorpe but extending southeast beyond Market Rasen and west to the Yorkshire border.

There is a bridge carrying Pennsylvania Route 309 across the creek. Wisconsinan Till, alluvium, and bedrock consisting of sandstone, shale, conglomerate, and coal occur in the watershed. Several volatile organic compounds have been detected in small amounts in surface water in the watershed. The creek occasionally floods, but such flooding typically causes little damage.

Sources include Australia, Myanmar, India, Afghanistan, Israel, Madagascar, Namibia, Nigeria, Mozambique, Tanzania and the United States. Spessartine of an orange-yellow has been called Mandarin garnet and is found in Madagascar. Violet-red spessartines are found in rhyolites in Colorado and Maine. In Madagascar, spessartines are exploited either in their bedrock or in alluvium.

Hallmann, Robert. (2006). Canvey Island, A History. Phillimore. . An unsuccessful search for coal beneath the island in 1953 revealed that the alluvium rests upon layers of London Clay, Lower London Tertiaries, Chalk, Lower Greensand and Gault Clay, with the basement rocks at a depth of consisting of hard Old Red Sandstone of Devonian age.

The flowering glumes are 4–6 mm long. The male spikelets are ovate and 4–8 mm long, with six tepals, three stamens and a minute pistillode. The female spikelets are ovate to elliptic and 8.5–9.3 mm long, with four tepals and two staminodes. It is found on alluvium in swamps and depressions.

Some springs are also seen in the hilly tract of the district. Geologically the area in comprised with Archean Granites and Gneisses. In the uplands considerable thickness of late-rite of Pleistocene age is found in the Granite and Gneisses tracts. Alluvium of recent to sub-recent age is found in the river valleys.

The soil is composed of different varieties of alluvium. The main rivers are: Nagar, Mahananda, Kulik, Gamari, Chhiramati (Srimati) and Tangon. The rivers have little water in the dry season but with heavy rains, during monsoon, overflow the banks. The Tangon river flows through the upper portion of western part of Kaliaganj CD Block.

Some Wisconsinan Lag is present at the top of the valley. The surficial geology near the lower reaches of the stream mainly consists of alluvium, bedrock, alluvial terrace, Illinoian Lag, and a small patch of Illinoian Flow-Till. In the valley of Davis Hollow, the Wisconsinan glacial terminus descends over the course of ( per mile).

In addition, techniques for gold mining have been described as resulting in both a major environmental and public health problem. Most gold miners use liquid mercury to extract gold particles from the alluvium. They often handle the toxic liquid mercury with their bare hands. To purify the gold particles, the mercury is burned off.

Typically, soils are formed from alluvium deposited by the rivers as either sandy clay in light colors or sand clay with gray or yellow colors. Upland soils derive from granitic, schistose, or sandstone parent rocks more acidic and less fertile. Southern Laos has areas of laterite soils, and basaltic soils in the Bolovens Plateau.

The surficial geology in the vicinity of Billings Mill Brook mainly consists of Wisconsinan Till, alluvium, and several others. A lake known as Lake Carey is in the stream's watershed. A number of bridges have also been constructed over Billings Mill Brook. The stream's watershed is designated as a Coldwater Fishery and a Migratory Fishery.

Patches of glacial till originating in the last ice age (Devensian) are common in many of the valleys. Around Clun itself is a substantial morainic deposit. Landslips have occurred in places, notably that beneath Caer-din Ring. The floor of the Clun valley is formed from alluvium whilst there is evidence of three river terraces.

It is a relatively small stream with a deep valley. In its upper reaches it is approximately wide. The surficial geology in the creek's vicinity mainly consists of Wisconsinan Till, alluvium, bedrock, and wetlands. The watershed of Hop Bottom Creek is relatively long in a north-south direction and narrow in an east-west direction.

At the outlet of Heart Lake, the creek's channel is wide and deep. The headwaters of Hop Bottom Creek are in a beaded valley, with alternating broad and narrow segments. Wetlands or lakes sometimes occur in the broad parts. The surficial geology along the lower reaches of Hop Bottom Creek mainly consists of alluvium.

An unconformity occurs before late Miocene sequences including the Dupi Tila sandstone and claystone, with another unconformity between the Dupi Tila units and Pliocene Dihing claysone and silty sandstone. Pleistocene St. Martin's limestone and Madhapur clay are separated from Pliocene units by an unconformity as well from Holocene sand, silt, clay, peat and coral alluvium.

The Ken valley separates the Rewa Plateau from the Satna Plateau. Because of the flatness they can also be called high plains. Only the southern part of the Rewa Plateau is hilly. The Rewa plateau from Rehli in the southwest to Satna in the northeast is covered with alluvium of the Pleistocene and recent periods.

The elevation near the mouth of Sugar Run is above sea level. The elevation of the stream's source is between above sea level. The surficial geology at the mouth of Sugar Run mainly consists of alluvium and Wisconsinan Ice-Contact Stratified Drift. There are also patches of these materials in the stream's upper reaches.

Lower down on the flood plain, the nature of the underlying ground is Magnesian Limestone over alluvium and terrace drift deposits. On top of this is a combination of slowly permeable and well drained fine loam over clay. Where the river passes through the Nidd Gorge, Carboniferous (Namurian) and Upper Permian rock is exposed.

In the upper reaches, the surficial geology along the creek mainly consists of Wisconsinan Till, but there is some alluvium, wetlands, and lakes. Leslie Creek has been described as a "small creek". It passes through a lake known as Tingley Lake in its upper reaches. Leslie Creek is not designated as an impaired waterbody.

The surficial geology in its vicinity mainly consists of alluvial terrace, alluvium, Wisconsinan Till, and bedrock. However, Wisconsinan Ice-Contact Stratified Drift, fill, alluvial fan, peat, and wetlands also occur. The creek is the main source of flooding in Ransom Township. The area at the mouth of Gardner Creek was settled as early as 1769.

Iron sand is also plentiful on the west coast from Taranaki to Auckland. Jade (Pounamu in Māori) from South Island ophiolites continues to be extracted, mostly from alluvium, and worked for sale. Groundwater reservoirs are extracted throughout the country, but are particularly valuable in the dryer eastern regions of both the North and South Islands.

The elevation near the mouth of Martin Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology along most of the length of Martin Creek features Wisconsinan Till. However, patches of alluvium and Wisconsinan Ice-Contact Stratified Drift occur in the creek's vicinity as well.

Elevation Blunham is between and above sea level, with the whole parish relatively flat. Geology and soil type The village lies on first, second and third terrace river gravel or boulder clay. Alluvium borders the Great Ouse and Ivel rivers. The soil has low fertility, is freely draining and slightly acid with a loamy texture.

To the north of the village are freely draining, slightly acid loamy soils. The village centre and areas to the south and east have lime-rich loamy and clayey soils with impeded drainage. The geology of the south-west of the parish and around Potton Brook is alluvium. Western and northern areas are Lower Greensand.

The entire part of North and South Dinajpur is silt laden plain. Mahananda River divides the district of Malda into two parts. The eastern part consists of undulating plains and some tilas and is made up of old alluvium and is a part of the Ganges delta. It is also known as Barind or Barendrabhumi.

Buck Run is a tributary of Little Muncy Creek in Lycoming County, Pennsylvania, in the United States. It is approximately long and flows through Jordan Township. The watershed of the stream has an area of . The surficial geology near the stream mostly consists of Illinoian Till and Illinoian Lag, with some alluvium and bedrock.

The District forms a part of the basin lying between Rajmahal hills on the east. The older alluvium is estimated to be Pleistocene age. Uttar Dinajpur is bestowed with a very fertile soil. The soil is very rich in nature due to the alluvial deposition which helps to grow Paddy, Jute, Mesta and Sugarcane etc.

Urbani & Mendi, 2010, p.17 The Castillo Formation is overlain by Quaternary alluvium and in places by the Capadare Formation.Urbani & Mendi, 2010, p.19 The formation, deposited in a calm near- shore lagoonal brackish environment, with possibly fluvial influence, has provided a rich assemblage of fossil crocodylians, turtles, giant sloths and various types of fish.

Khangabok represents the features of flat plain topography. The soil is of the type alluvium and contains small rock fragments, sand and sandy clay. The vegetation consists of a large variety of plants ranging from short and tall grasses, reeds and bamboos to trees of various species. Arundo Donax (yengtou), Leihao, Bamboo, Cane, Eucalyptus etc.

These terraces are depositional in origin and may be able to be identified by a sudden change in alluvium characteristics such as finer material. Strath terraces: Strath terraces are the result of either a stream or river downcutting through bedrock. As the flow continues to downcut, a period of valley widening may occur and expand the valley width.

However, alluvium is present along the creek in its middle and upper reaches and there are some patches of Wisconsinan Ice-Contact Drift in the watershed, as well as a few patches of bedrock consisting of conglomeratic sandstone, sandstone, and shale. There are also wetlands in the creek's headwaters and two patches of fill near the creek.

Within the lake area, the ground area is made up of a thick mantle of soil, blown sand and alluvium. Forest denudation, particularly in the hilly areas, has caused soil erosion, compounded by wind and water action. Due to these human factors silt built-up in the lake raises the bed level of the lake annually by many centimetres.

The elevation near the mouth of Deep Hollow is above sea level. The elevation near the stream's source is just over above sea level. Nearly all of the surficial geology in the valley of Deep Hollow is on bedrock consisting of sandstone and shale. However, near its mouth, there is an area of alluvium and Boulder Colluvium.

The elevation near the mouth of Little Nescopeck Creek is above sea level. The elevation of the creek's source is between above sea level. In its lower reaches, the surficial geology along Little Nescopeck Creek mainly consists of alluvium. There is also a glacial or resedimented till known as Wisconsinan Till in the vicinity of the creek.

Some patches of Wisconsinan Ice-Contact Stratified Drift and bedrock consisting of sandstone and shale are present as well, as are a few small patches of fill. In the upper reaches of the creek, the surficial geology features some alluvium and some bedrock. There is also Wisconsinan Till in the area and several wetlands and lakes near its headwaters.

These waterfowl feed heavily on the crops grown on the Stuttgart soils. Stuttgart soils have been mapped on about in Arkansas. The Stuttgart series consists of very deep, moderately well drained or somewhat poorly drained soils formed in silty and clayey alluvium. These level to gently sloping soils are on the Grand Prairie in the Lower Mississippi Valley.

The terrain consists mainly of Miocene volcaniclastic rocks with a single outcrop of Ordovician granodiorite. Parts of the area are covered by Quaternary alluvium and conglomerates. The basement rocks are influenced by normal faulting. The volcanism in the field has been explained by lithospheric delamination, a process by which part of the lower lithosphere founders into the mantle.

Artisanal mining, often associated with rebels involved in the Kivu conflict has arisen to meet international demand. DRC also has large diamond deposits, mainly extracted through artisanal mining of alluvium near Mbuji-Mayi in Kasai Province, although many of these reserves are becoming depleted. One third of the DRC's diamonds are smuggled out of the country every year.

Part of it is overlaid with alluvium, and in the west it is overlaid with the igneous rocks of the Deccan Traps. The climate is hot and semi-arid. The natural vegetation is dry monsoon forest, or monsoon scrub forest. Large parts of it are still forest, and it contains several national parks, including tiger populations.

The soil is composed of different varieties of alluvium. The main rivers are: Nagar, Mahananda, Kulik, Gamari, Chhiramati (Srimati) and Tangon. The rivers have little water in the dry season but with heavy rains, during monsoon, overflow the banks. The Pitana river flows along the eastern boundary of the Goalpokhar II CD Block with Goalpokhar I CD Block.

The confluence of Tryall Creek and Cooks Branch is in the Piedmont of Virginia in mafic and felsic metavolcanic rocks. Both tributaries arise in granite (Tryall Creek) or granite gneiss (Cooks Branch). Three Creek flows into the Coastal Plain in the Bacon Castle Formation and then for most of its length, especially the swampy areas it is in alluvium.

In case of the lake terraces of ancient ice-walled lakes, some proglacial lakes, and alluvium-dammed (slackwater) lakes, they often represent the relict bottom of these lakes.Shaw. E.D., 1915, "Newly discovered beds of extinct lakes in southern and western Illinois and adjacent states". Bulletin no. 20, Illinois State Geological Survey, Champaign, Illinois, p. 139-157.

The elevation near the mouth of Karnes Hollow is above sea level. The elevation of the stream's source is between above sea level. Along most of the length of Karnes Hollow, the surficial geology features colluvium. However, alluvium (which contains stratified sand, silt, and gravel, as well as some boulders), is present near the mouth of the stream.

Davis Hollow is a tributary of Fishing Creek in Columbia County, Pennsylvania, in the United States. It is approximately long and flows through Benton Township. The watershed of the stream has an area of . The surficial geology in its vicinity mainly consists of alluvium, alluvial terrace, Wisconsinan Till, Wisconsinan Lag, Illinoian Flow-Till, and Illinoian Lag.

Düsseldorf is built entirely on alluvium, mud, sand, clay and occasionally gravel. The highest point in Düsseldorf is the top of Sandberg in the far eastern part of the city (Hubbelrath borough) at . The lowest point is at the far northern end in Wittlaer borough where the Schwarzbach enters the Rhine, with an average elevation of .

Cherry Run is a tributary of South Branch Bowman Creek in Luzerne County, Pennsylvania, in the United States. It is approximately long and flows through Fairmount Township and Ross Township. The watershed of the stream has an area of . The surficial geology in its vicinity consists of alluvial fan, alluvium, bedrock, Wisconsinan Till, wetlands, and a peat bog.

The monument in the 2nd century AD was abandoned and completely buried by alluvium. The excavations that ultimately discovered the site were conducted in several phases: in 1857 and 1858, by the Bourbons, in 1871-72, out of interest of the Province, and in 1959 and subsequent years through the intervention of the Archaeological Superintendent of Molise.

The floors of the main river valleys are formed by alluvium, sand, silts and gravel laid down by rivers and streams. River terraces are evident along the Tyne valley and three terraces are developed along that of the River Tweed. Terraces are also developed along the course of the Till, Aln, Coquet, Font, Wansbeck and Breamish.

Kasganj is located at . It has an average elevation of 177 metres (580 feet). Situated on the banks of river Kali, the town is in proximity of the Himalayan foothills. It is located in the Doab, the area between the holy rivers Ganges and Yamuna and the alluvium soil makes the land one of the most fertile regions.

The elevation near the mouth of Billings Mill Brook is above sea level. The elevation of the stream's source is between above sea level. A large mass of partially quarried sand and gravel occurs at the mouth of Billings Mill Brook. The surficial geology along the lower and middle reaches of the stream mainly consists of alluvium.

An enormous scar on the valley side to the left of the foot of the lake shows the source of the landslide, and another landslide a few miles downstream caused the River Dysynni to divert into the adjoining valley to the north. The upper end of the lake is becoming shallower as a result of the deposition of alluvium.

Grapes are seeded in all districts of Ticino. The soil varies from acid soil in the northern part to limestone in the southern part, with some local geographical variation because of moraines, alluvium, etc. The region is very wet, but with few rainy days and many sunny days, so normally the vineyards are grassy, which limits erosion.

Plates in the crust of the earth, according to the plate tectonics theory The geology of India is diverse. Different regions of India contain rocks belonging to different geologic periods, dating as far back as the Eoarchean Era. Some of the rocks are very deformed and altered. Other deposits include recently deposited alluvium that has yet to undergo diagenesis.

Rattlesnake Creek is inhabited by wild trout and part of it is considered to be Class A Wild Trout Waters. A dammed lake known as Maple Lake is located near its headwaters. The surficial geology in the area mainly consists of Wisconsinan Till and bedrock, with some alluvium, Wisconsinan Ice-Contact Stratified Drift, wetlands, and peat bogs.

These old rocks lie beneath sea-level and are invisible beneath drift made up of glacial till deposits and post-glacial colluvium and alluvium deposits; there is a smaller amount of peat. Poulton has a generally temperate maritime climate like much of the British Isles, with cool summers and mild winters. There is an annual average rainfall of .

The shrub is widely distributed through arid and semi-arid inland areas of Western Australia, South Australia, the Northern Territory and Queensland where it is often found growing on stony hillsides and in a variety soil types especially coarse textured alluvium and is often a part of mulga woodland communities on plains with sandy to loamy soils.

On 1 April 2019 the parish was merged with Barnham to form "Barnham and Eastergate". Roman remains have been found near St George's Church, although until the 20th century the village remained a small one. The area, being on alluvium, was principally used for market gardens. Subsequent house building has resulted in a large increase in population.

A number of different plant communities were found near Fiddens Wharf. The early logging occurred in the Sydney Sandstone Gully Forest and Sydney Blue Gum High Forest. Soils in these forests are derived from Ashfield Shale and Hawkesbury Sandstone from the Triassic. In the Fiddens Wharf area Eocene alluvium and relatively high rainfall enabled large trees to grow.

The north and west boundaries of the desert are delineated by the fluvial systems Wadi Batha and Wadi Andam.Alsharhan, xii. Beneath the surface sands are an older layer of cemented carbonate sand. Alluvium deposits believed to have originated from the Wadi Batha during the Paleolithic era have been disclosed in the central desert beneath the interdune surface.

The elevation near the mouth of East Branch Martins Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology near the mouth of East Branch Martins Creek mainly consists of alluvium and a till known as Wisconsinan Till. However, there is a patch of alluvial fan at the creek's mouth.

The elevation near the mouth of Dry Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology in the valley of Dry Creek consists mostly of a till known as Wisconsinan Till, although large patches of alluvium also occur. Additionally, there is a small patch of peat bog.

Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, alluvium, sandstone and shale pits, and bedrock consisting of sandstone and shale all occur in the watershed. A 2-billion gallon reservoir known as the Huntsville Reservoir is situated on the creek. The reservoir supplies water to 30,000 people. The creek has one named tributary, which is known as Browns Creek.

The elevation near the mouth of Trout Creek is above sea level. The elevation of the creek's source is between above sea level. In the lower reaches of Trout Creek, the surficial geology along the valley floor consists of alluvium. The sides of the valley mainly have surficial geology containing bedrock consisting of conglomerate, sandstone, and shale.

In the east calcareous Shales from the Canberra Formation is overlain by Quaternary alluvium. This rock is the limestone in the original name of Canberra "Limestone Plains". The Narrabundah Ashstone is part of this formation and can be seen in the easternmost corner. In the higher west including Mount Pleasant is grey quartz andesite from the Ainslie Volcanics.

Until they either died or were overwhelmed by the accumulating sediments, these trees would likely continue to regenerate by adding height and new roots with each increment of sediment, eventually leaving several meters of former "trunk" buried underground as sediments accumulated.Gastaldo, R.A., 1992, Regenerative growth in fossil horsetails (Calamites) following burial by alluvium. Historical Biology, 6(3):203-220.

Mill Creek is a tributary of Whitelock Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Northmoreland Township and Exeter Township. The watershed of the creek has an area of . The surficial geology in its vicinity consists mainly of alluvium, Wisconsinan Till, bedrock, Wisconsinan Ice-Contact Stratified Drift, and loess.

The elevation near the mouth of Roaring Run is above sea level. The elevation of the stream's source is between above sea level. In its lower reaches, Roaring Run flows through a band where the surficial geology consists of alluvium. This area is flanked by areas with a surficial geology consisting of alluvial terrace and alluvial fan.

The three sandstone beds are informally called the red, green, and white sandstone beds (Gazin, 1934). The Hagerman Fossil Beds National Monument reopened the Horse Quarry during the summer of 1997. The only sandstone now exposed within the monument is the white sandstone. The red and green sandstone remain covered by alluvium (Richmond and others, 2002).

The elevation near the mouth of Beaver Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology along the lower reaches of Beaver Creek mainly consists of alluvium, although Wisconsinan Till also occurs in the area. There are also a few small patches of Wisconsinan Outwash and alluvial fan.

Melaleuca dissitiflora is found in the drier parts of inland Australia such as Flinders Ranges in South Australia. It is also found in the Northern Territory and western Queensland and there is a disjunct population in the Rawlinson Range in Western Australia near its border with the Northern Territory. It grows in rocky places, in ephemeral watercourses and alluvium.

In the eastern part the eye constantly rests on wide expanses of rice fields, green in the rains but parched and dry in summer. The Gondwana system is represented in the northern portion of the district, south of the Damodar, between Mejia and Biharinath Hill. The beds covered with alluvium contains seams of coal belonging to the Raniganj system.

The soils are loamy with little clay and lime content but with a high content of magnesia. Chemical fertilization, green manure and legume is used before cultivation .There is sufficient organic matter and nitrogen content in the alluvium because of plant residue, crops stubble, natural vegetation and animal excretion. Soils types include Gurti (clay), Bahil (Loam) and Sekil (Sandy).

The elevation near the mouth of Brish Run is above sea level. The elevation of the stream's source is above sea level. The surficial geology in the vicinity of the mouth of Brish Run consists of alluvium. The rest of the stream flows through land with surficial geology consisting of a till known as Wisconsinan Till.

Claire Étienne-Steiner, Frédéric Saunier, Le Havre a port with new towns, Paris, éditions du patrimoine, 2005, p. 21 The soil consists of several metres of alluvium or silt deposited by the Seine. The city centre was rebuilt after the Second World War using a metre of flattened rubble as a foundation.C. Étienne-Steiner, Le Havre.

The soils of Builsa North District are developed from different geological formations namely Granite, Birimian rocks, Voltaian shale, recent and old Alluvium of mixed origin and very old river terraces. Out of these, the dominant soil groups in the district are of granite origin and cover over 70 percent (approximately 153,300ha) of the district‟s land area.

The site is set back from the Donets River itself, on the terrace supporting a strip of flood lakes about 50 meters above sea level. In the 1990s the lakes in the middle of the reserve were frequently connected to the river by flooding. The soils are chernozym (black soils) on 15-20 meters of alluvium and limestone rocks.

Some areas near the creek are on Wisconsinan Till. Most of the till in the vicinity of the creek is expected to be more than thick. Wisconsinan Ice-Contact Stratified Drift and alluvium are also found along parts of the stream, especially in its middle and upper reaches. Additionally, an alluvial fan is present in the creek's upper reaches.

Part of the stream is considered to be Class A Wild Trout Waters for brook trout, which inhabit the entire stream. Alluvium and glacial till can be found near it, as can bedrock made of sandstone and shale. There are at least two bridges crossing the stream and a sawmill was built on it in the early 1800s.

The alluvium is thick and contains some boulders, especially closer to its headwaters. Under it lie unconsolidated glacial deposits. Wisconsinan Ice-Contact Stratified Drift occurs in the stream's lower reaches and in a small patch in its middle reaches. Wisconsinan Till, a glacial till, surrounds the stream, which flows through the till in its upper reaches.

The long East Dam, constructed by a Kiewit-led joint venture, is the longest of the three dams. It measures wide at the base and wide at the top. Before embankment of the dam could begin, more than of alluvium had to be excavated to reach a solid bedrock foundation. The embankment required of crushed rock.

Alluvium borders the Great Ouse. Underlying these superficial deposits and also in part at the surface is Oxford clay and Kellaways beds. Around the hamlet the soil has low fertility, is freely draining and slightly acid with a loamy texture. The eastern part of the parish has highly fertile, lime-rich loamy and clayey soils with impeded drainage.

This swarming architecture offers savings in bandwidth and processor usage. Because most transfers happen between listeners, the source server has much less load. Also, unlike icecast, servers which serve files for Alluvium stations do not decode the files, so broadcasts can be done from low-cost, obsolete hardware with sufficiently fast I/O and network speeds.

In the south sections of the county, Permian Garber Sandstone is commonly found with some Hennessey Group shale. Area creeks including East Cache Creek and West Cache Creek contain deposits of Quaternary alluvium. To the northwest, the Wichita Mountains consist primarily of Wichita Granite Group from the Cambrian Period. There are three cities in Comanche County.

It is deep- to medium-black coastal alluvium, due to its proximity to the sea, long shoreline, and nearby mountain ridge. Because of many fault lines in the vicinity, Junagadh is in a seismically active zone. Junagadh lies in a Seismic Zone III region, which means earthquakes up to magnitude 6.5 on the Richter-scale may be expected.

It drains a portion of the Moosic Mountains. The surficial geology in its vicinity consists of alluvium, surface mining land, coal dumps, fill, Wisconsinan Till, and bedrock containing sandstone and shale. A reservoir known as the Brace Brook Reservoir is in the watershed. The stream's drainage basin is designated as a Coldwater Fishery and a Migratory Fishery.

The surficial geology along much of Kennedy Creek consists of alluvium. However, the surficial geology in the creek's valley as a whole consists mostly of a till known as Wisconsinan Till. There is also a patch of bedrock consisting of sandstone and shale at the creek's mouth and a patch of fill where the creek crosses Interstate 81.

The investigation of Mummy Cave was led by Robert Edgar from 1963 to 1965. The alcove was marked out into a grid, with a permanent reference mark for elevation marked on the wall. Initial investigation focused on establishing stratigraphy. Once the layers of alluvium in the cave floor were established, the excavation proceeded layer by layer.

Borehole and magnetic data surveys show that the alluvium and lahar deposits at the Bantul graben are thick and at places over 200 meters, and the water table is below ground level. Most liquefaction events took place near the wide Opak Fault zone. Sand boils, lateral spreading, settling, and slides led to some tilting and collapse of buildings.

There are also patches of alluvial terrace and Wisconsinan Ice-Contact Stratified Drift near its mouth. In the creek's upper reaches, the surficial geology immediately adjacent to the creek is also alluvium, while the surficial geology in most of the rest of the valley is Wisconsinan Till. There are also two wetland patches near the creek in this reach.

However, due to the semi-arid > climate it only fills intermittently with water. The main land formations > are saline flats that contain shallow soils overlying gypsum, dune fields > that contain relics of Pleistocence sand ridges, and floodplains that are > formed of a quarterly alluvium. The biosphere reserve was established in 1981 and is managed by Parks Victoria.

The slope of Marsh Creek near Silo Road ranges from 0.0011 to 0.0037. Upstream of Silo Road, the streambed of Marsh Creek mainly consists of fine sand. Downstream of that road, the streambed consists of coarse gravel, with an average particle size of . The surficial geology along the creek in its lower reaches mainly consists of alluvium.

Darwin box occurs across northern Australia from near Broome in Western Australia to Darwin in the Northern Territory, then as far east as near Normanton in Queensland and on some islands in the Gulf of Carpentaria. It is found on hillsides and along creeks in woodland, where it grows in skeletal sandy alluvium over quartzite, sandstone or basalt.

Most of the till in the vicinity of the stream is expected to be more than thick. However, the stream's lower reaches are on alluvium and Wisconsinan Outwash. The former contains stratified sand, silt, and gravel, while the latter contains stratified sand and gravel. Bedrock consisting of sandstone and shale is also present in the vicinity of the stream.

The floors of the main river valleys are formed by alluvium, sand, silts and gravel laid down by rivers and streams. River terraces are evident along the Tyne valley and three terraces are developed along that of the River Tweed. Terraces are also developed along the course of the Till, Aln, Coquet, Font, Wansbeck and Breamish.

The topography of the district is a typical representative of an alluvial plain. It owes its origin to the aggravation work of the Satluj River. The alluvium deposited by the river has been worked over by the wind, which gave rise to a number of small dunes and sand mounds. Most of these dunes have been leveled by farmers.

The elevation near the mouth of Elk Run is above sea level. The elevation of the stream's source is between . Elk Run has a high gradient and is a clearwater creek. The valley of Elk Run is mostly in the vicinity of Wisconsinan Ice-Contract Stratified Drift, a glacial till known as Wisconsinan Bouldery Till, and alluvium.

Cambodia has few natural resources, mainly gold and some non-metallic minerals. Artisanal mining often extracts gold bearing alluvium, which originated from quartz veins in different rocks. Gold was found at Suptrup in 1877 and mined until 1940. Bauxite, iron ore, tin, greisen and aplite are also known, although only bauxite appears to be economically valuable.

The bulk of the population is situated from around Collinsville in the north down to around Crows Nest in south and out to the west as far as around Tambo. It is found on stony hillsides as a part of open Eucalyptus woodland communities where it grows in shallow sandy soils or sometimes in deep alluvium.

Nijhum Dwip () is a small island under Hatiya upazila. It is situated in Noakhali District in Bangladesh. Once it was called Char Osmani, Baluar Char, Golden Island A cluster of islands (mainly, Ballar Char, Kamlar Char, Char Osman and Char Muri) emerged in the early 1950s as an alluvium in the shallow estuary of the Bay of Bengal on the south of Noakhali. These new sandbanks first drew the notice of a group of fishermen, who named it Baular Char (literally, the alluvium of sand) later transformed into Ballar Char. Occupying an area of , the island is situated between 21 0 1 / to 22 0 6 /North latitude and 90 0 3 / to 91 0 4 / East longitude Migratory Birds in Nijhum Dwip: During winter, thousands of migratory birds flock in to island.

The basement consists mainly of Precambrian-Paleozoic metamorphic rocks with intruded granitic, mafic and ultramafic rocks of Paleozoic age; these metamorphic rocks are also known as the Puncoviscana Formation. There are Paleogene-Neogene continental sequences. It is mostly buried beneath Quaternary sediments; outcrops have characteristic dark colours. The Quaternary sediments in turn contain both aeolian, colluvium and alluvium-derived sediments.

Within the Upper Coal Measures of the outlying 'Avonmouth Basin' are the Avonmouth No 1 and No 2 coals. This is sometimes known as the Severn Coalfield. It lies several miles to the west of the main Bristol Coalfield and extends under the Severn Estuary as far as Portskewett. It is also largely obscured by thick deposits of estuarine alluvium.

Little Nescopeck Creek is designated as a Coldwater Fishery and Class A Wild Trout Waters. It is one of the main sources of flooding in Dennison Township. The surficial geology in the vicinity of the creek mainly features alluvium, Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, bedrock, and fill. Little Nescopeck Creek shares its name with another river in southern Luzerne county.

The entire district is a part of the Deccan Traps flood basalts of the Cretaceous-Paleocene. Alluvium of the recent period is, however, found along the river Parbati in a narrow strip. The district has deep black and shallow black brown and alluvial soils of the northern region. Shajapur is a part of central Madhya Pradesh plateau and Ratlam plateau.

The surficial geology in the vicinity of Rock Bottom Creek mainly consists of a glacial or resedimented till known as Wisconsinan Till. However, there are also large patches of bedrock consisting of conglomeratic sandstone, sandstone, and shale. There are smaller patches of wetlands, peat bogs, lakes and fill. There is also an area of alluvium at the mouth of the creek.

The slip-off slope of an entrenched meander is a gently sloping bedrock surface that rises from the inside, concave bank of an asymmetrically entrenched river. A thin, discontinuous layer of alluvium often covers this gently sloping bedrock surface. This type of slip-off slope is formed by the contemporaneous migration of a meander as a river cuts downward into bedrock.Davis, W.M., 1913.

The general slope of the district descends to the southeast. Geologically, the district is mainly covered by Chhota Nagpur granite gneiss of Archean age with patches of alluvium, sandstone, and shale of Gondwana formations. Important rivers flowing in the district include the Ajay and the Paltro. These rivers gather a large number of tributaries that form the landscape full of Tanrs and Dons.

The most important mineral of the district is bauxite. Other minerals which are found in the district are feldspar, fire clay and china clay and have less economic importance. The major part of the district is covered with Golden Alluvium, Red and Sandy and Red and Gravelly soils. Laterite and Red and Yellow soils are also found elsewhere in the district.

Stony Creek flows from the Piedmont to the Coastal Plain of Virginia. The forming confluence is at the edge of mafic and felsic rocks metavolcanic rocks and the Petersburg Granite. Petersburg Granite underlies most of the course and once in the Coastal Plain, it flows a short distance through the Windsor Formation and then through alluvium to the Nottoway River.

When the deposition is in an estuary, the sediments are known as bay mud. Outwash plains and valley trains are usually accompanied by basins known as "kettles". These are small lakes formed when large ice blocks that are trapped in alluvium melt and produce water-filled depressions. Kettle diameters range from 5 m to 13 km, with depths of up to 45 meters.

The elevation near the mouth of Beth Run is above sea level. The elevation of the stream's source between above sea level. The surficial geology along most of the length of Beth Run consists of a till known as Wisconsinan Till. In the stream's upper reaches, alluvium is present as well and some of the Wisconsinan Till is underlain by glacial lake clays.

To the northwest, where the fault cuts the base of the Serranía del Darién, the scarp and the contact between the Atrato alluvium and Tertiary rocks are sinuous. To the north of Unguía, the fault strikes north through the Bajo Atrato Valley, probably extending either into the Gulf of Urabá or to the northwest into the Caribbean Sea.Paris et al., 2000, p.

Geology and soil type The village lies mainly on first and second terrace river gravel. Alluvium borders the Great Ouse and Ivel rivers. There are patches of boulder clay, and the eastern and northern parts of the parish are on Oxford clay overlying Kellaways beds. Around the village the soil has low fertility, is freely draining and slightly acid with a loamy texture.

The Seitz soil series consists of very deep, well drained, slowly permeable soils that formed in colluvium or slope alluvium derived from igneous, sedimentary, and volcanic rocks. Seitz soils are located on mountains, mainly in southwestern and central Colorado. These soils are well suited to outdoor recreation and the growth of forest-related products in moderately steep or more gently sloping areas.

Neighboring districts are (from the north clockwise) Mueang Sa Kaeo, Watthana Nakhon, Khlong Hat, and Wang Nam Yen of Sa Kaeo Province, and Tha Takiap of Chachoengsao Province. The district is named after the hills of Khao Chakan, a group of limestone hills rising out of the valley alluvium. In the hills are several caves, including the cave temple Wat Tham Khao Chakan.

The elevation near the mouth of Bean Run is above sea level. The elevation of the stream's source is between above sea level. The surficial geology near the mouth of Bean Run consists of alluvium, Wisconsinan Ice-Contact Stratified Drift, and fill. Further upstream, there is mostly Wisconsinan Till, but also patches of Wisconsinan Bouldery Till and bedrock consisting of sandstone and shale.

Since it lies within the Indo- Gangetic Plain area, and hence "The Gangetic Alluvium" soil is found in this area which is very fertile. Because the land here is very fertile, people grow four crops a year. Almost anything grows at a rapid rate because of the rich soil. The most common are rice, wheat, maize, arhar, and several vegetables.

The elevation near the mouth of Swale Brook is above sea level. The elevation of the stream's source is between above sea level. The stream has been described as "small enough to step across". The surficial geology in the vicinity of the lower and middle reaches of Swale Brook consists of alluvium, Wisconsinan Outwash, Wisconsinan Ice-Contact Stratified Drift, and alluvial terrace.

The surficial geology immediately adjacent to the creek mostly consists of alluvium. However, much of the rest of the valley has surficial geology consisting of Wisconsinan Till. There are also a few patches of alluvial terrace, alluvial fan, wetlands, peat bogs, and bedrock consisting of sandstone and shale. There are also two small sandstone quarry dump patches, consisting of chunks of broken sandstone.

Altitude The hamlet is above sea level. The land rises to in the north of the parish towards Topler's Hill. Geology and soil type Land north of the main road through the hamlet is arable farmland and lies on boulder clay. To the south are pastures on largely grey and grey-blue clay but by the River Ivel is alluvium and river gravel.

The East canal, the Nizampatnam canal and the West canal flow through the city, which originates from Krishna River. The region around the city forms a part of Western Delta System of Krishna river. The area is covered by Alluvium and the main soil varieties are Red and Black. Climate Tenali has a tropical wet and dry climate (Köppen Aw).

The surficial geology in its vicinity includes alluvial fan, alluvial terrace, alluvium, Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, fill, wetlands, and bedrock. Beaver Run is a source of flooding in Lake Township, Luzerne County. A number of bridges have also been constructed over Beaver Run. The watershed of the stream is designated as a High Quality Coldwater Fishery and a Migratory Fishery.

The elevation near the mouth of Stone Run is above sea level. The elevation of the stream's source is between above sea level. The surficial geology along the lower reaches of Stone Run mainly consists of alluvium, while Wisconsinan Ice-Contact Stratified Drift occurs in the vicinity. However, further upstream, the surficial geology consists of Wisconsinan Till and Wisconsinan Bouldery Till.

Sorber Run is a tributary of Bowman Creek in Luzerne County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through Lake Township in Luzerne County and Noxen Township in Wyoming County. The watershed of the stream has an area of . The surficial geology in the stream's vicinity consists of alluvium and Wisconsinan Till.

For most of its length, the surficial geology in the vicinity of Fades Creek consists of alluvium, Wisconsinan Ice-Intact Stratified Drift, and resedimented or glacial tills such as Wisconsinan Till and Wisconsinan Bouldery Till. However, bedrock consisting of sandstone and shale also occurs in the surficial geology in the creek's vicinity, as do a few small patches of wetland.

Yanam's soil is alluvium consisting of sand clay and gravel. It is grey black and clay-like in composition. A few thin layers of sandy clay or sand approximating 0.3 metres in thickness, are intercalated with the clay soil. The river sand on the bank of Gauthami, Godavari consist of quartz, felspar and mica, with monazite found in the black streaks.

The Geological Society, London. p442 The late Devensian glaciation resulted in the North Sea icesheet impinging upon the north coast of Norfolk. Of more recent origin are alluvial deposits which extend across the floors of the main river valleys and widely across the flats of the Broads. Coastal alluvium is also present along the north coast from Holme-next-the-Sea to Brancaster.

The elevation near the mouth of Sugar Hollow Creek is above sea level. The elevation of the creek's source is between above sea level. Sugar Hollow Creek flows through a valley known as Sugar Hollow. Near the mouth of Sugar Hollow Creek, the surficial geology mainly consists of Wisconsinan Outwash, but there is a thin strip of alluvium along the creek itself.

The surficial geology near the creek includes Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, alluvium, coal dumps, and bedrock consisting of sandstone and shale. On July 3, 2011, Coal Creek flooded when of rain fell in the watershed in less than 90 minutes. The flood caused $5 million in damage. The creek is designated as a Coldwater Fishery and a Migratory Fishery.

West Tilbury lies in the extreme south of Essex, fronting the Thames. About half of its land surface is Thames alluvium (clay), the inland portion rising as a dramatic gravel ridge (about 30 metres OD). Upon its northward border with Mucking parish there are limited sandy loams. The substratum is of Thanet Sands, which in turn overlie a considerable depth of chalk.

Sugar Run is a tributary of Bowman Creek in Luzerne County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through Lake Township in Luzerne County and Noxen Township in Wyoming County. The watershed of the stream has an area of . The surficial geology in its vicinity consists of alluvium, alluvial fan, Wisconsinan Till, and bedrock.

The elevation near the mouth of Sugar Run is above sea level. The elevation of the stream's source is between above sea level. The surficial geology in the vicinity of the mouth of Sugar Run consists of alluvium and alluvial fan. Slightly further upstream, there is a till known as Wisconsinan Till, which is underlain with glacial lake clays in some reaches.

The surficial geology in its vicinity consists of Wisconsinan Till, alluvium, Wisconsinan Ice-Contact Stratified Drift, alluvial fan, alluvial terrace, bedrock, and sand and gravel pits. Major land uses in the watershed of Leonard Creek include forested land and agricultural land. The creek is one of the more significant tributaries of Bowman Creek. Leonard Creek has at times been impacted by flooding.

Only a pond remained at the top of the gully. The soils of the forest at the Vorskla developed on different parent materials, especially on the loam, which is found in the eastern half of the forest. In the northwestern part of the forest, old alluvium sands play a role. They are distributed on the river terraces of Gotnja and Loknja.

The surficial geology in the vicinity of Whitelock Creek mainly consists of alluvium, Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Till, bedrock, and alluvial terrace. Major land uses in the watershed of Whitelock Creek include forested land and agricultural land. A number of bridges have been constructed over the creek. Its watershed is designated as a Coldwater Fishery and a Migratory Fishery.

The elevation near the mouth of Whitelock Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology along the lower reaches of Whitelock Creek mainly consists of alluvium. The sides of its valley have surficial geology featuring Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Till, and bedrock consisting of coal, conglomeratic sandstone, sandstone, and shale.

Alluvium again occurs along the creek in its middle and upper reaches, although larger Wisconsinan Till and bedrock consisting of sandstone and shale occur nearby. There are also a few patches of loess, which contains silt and fine sand. There is a pipeline in the watershed of Mill Creek. In 2013, this pipeline was found to violate the Clean Streams Law.

Roundness is an important indicator of the genetic affiliation of a clastic rock. The degree of roundness points to the range and mode of transport of clastic material, and can also serve as a search criterion in mineral exploration, especially for placer deposits. Alluvial debris in major rivers tend to exhibit a high degree of roundness. Alluvium from small rivers is less rounded.

The soil in the area is a light gravel or sand laid over Keuper marl with some lower lias and alluvium also present. The 1881 UK Census recorded the population at 380. According to the 2011 UK Census, the population was 962 living in 388 dwellings, of which 763 were over sixteen years old, and of those 507 were in employment.

A typical streetscape in Fyshwick Most of the north of Fyshwick is underlain by Canberra Formation, calcareous shale. On top of this to the east and west of Jerrabomberra creek are Tertiary pebble gravels, and also quaternary alluvium. There are two andesite dykes intruded across Gladstone Street. South of the South Fyshwick fault is the dacitic andesite of the Ainslie Volcanics.

The stock generated the porphyry copper deposits, gold-bearing veins, and gold placers. There are about 26 major veins forming a radial pattern from the stock. The Golddust Camp placer deposits are found in the alluvium of the dry gulches radiating off Copper Flat and the andesite flows. The fissure veins produced 51,000 ounces of gold, while the placer deposits produced 110,000 ounces.

South Branch Roaring Run is a tributary of Roaring Run in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Noxen Township and Forkston Township. The watershed of the stream has an area of . The surficial geology in its vicinity consists of bedrock, Wisconsinan Till, Wisconsinan Bouldery Till, Wisconsinan Ice-Contact Stratified Drift, and alluvium.

This alluvium builds up to form the river delta. When the flow enters the standing water, it is no longer confined to its channel and expands in width. This flow expansion results in a decrease in the flow velocity, which diminishes the ability of the flow to transport sediment. As a result, sediment drops out of the flow and deposits.

The Kavik River is an river in the North Slope region of Alaska. It is swift- flowing and is braided. In winter, parts of the Kavik (and the nearby Canning River) are covered with extensive ice sheets known as aufeis. The Kavik runs in a wide, flat alluvium-filled valley and is bordered by terraces at a number of levels.

The watershed is separated from Lake Winola by a wall of glacial drift with a height of . Rock types in the vicinity of Mill Run include green and greenish-gray sandstone, red shale, and others. The surficial geology in the vicinity of the lower reaches of Mill Run mainly consists of Wisconsinan Till. However, there is alluvium and fill near its mouth.

Some of the tributaries on this middle section are similar to those on the upper section, but others are lowland streams, where the underlying geology is alluvium and clays, and which flow more slowly. The Bevern Stream and Northend Stream both originate in the chalk uplands of the South Downs, but traverse greensand and clay before they reach the Ouse.

Chordifex hookeri is a native herb commonly found in infertile poorly-drained acid peaty soil, which are thin or skeletal. It grows on a range of substrates, including dolerite, basalt, alluvium and quartzite gravels, but most commonly on siliceous substrates. It is limited by nutrients and frequent fires control the vegetation. This inhibits larger scrubs and forest to grow and prolongs succession.

A small waterfall on Maple Run The concentration of alkalinity in the waters of Maple Run is 5 milligrams per liter. The elevation near the mouth of Maple Run is above sea level. The elevation of the stream's source is between above sea level. For a significant portion of its length, Maple Run flows over alluvium, mostly in its middle reaches.

Rice fields in Bagaya The village is located in the alluvium of the Casamance River. Most families produce rice, peanuts, mangos, cashew nuts, millet, maniok, oil palm of coconut for private or local consumption. Animals like chicken, goat and cow are much elevated. Milk is not used for human consumption because there is no cooling infrastructure, and because of the lack of transportation.

Alluvium is materials that are deposited by floodwaters from engorged bodies of water—chiefly streams and rivers. Organic deposits are largely the result of decomposing plant material.See also: Salisbury, Rollin D. The Glacial Geology of New Jersey, Volume V of the Final Report of the State Geologist. (Trenton, New Jersey: Geological Survey of New Jersey, 1902); Volkert, Richard A., and Scott Stanford.

The solid geology of St Werburghs comprises Triassic Redcliffe Sandstone to the south-east of Glenfrome Road, and Triassic mudstone and halite-stone of the Mercia Mudstone Group to the north. The solid geology in the Mina Road Park area and in the valleys of the River Frome and Horfield Brook is overlain by superficial deposits of Quaternary alluvium., Geology of Britain Viewer.

The Wisconsinian Till is a glacial till that is more than thick. The Wisconsinian Outwash consists of stratified sand and gravel and ranges from to more than thick. The alluvium contains stratified silt, sand, and gravel, and is typically more than thick. Bedrock made of shale and sandstone can also be found in the vicinity of the creek in its lower reaches.

While Gobardanga municipality is in the north, Baduria and Basirhat municipalities are in the south. Baduria CD Block is part of the Ichhamati-Raimangal Plain, one of the three physiographic regions in the district located in the lower Ganges Delta. It contains soil of mature black or brownish loam to recent alluvium. The Ichhamati flows through the eastern part of the district.

It is a raised alluvium area along the Hooghly, which forms the western boundary of the district. Barrackpore II CD Block has an area of 40.74 km2. It has 1 panchayat samity, 6 gram panchayats, 104 gram sansads (village councils), 21 mouzas and 21 inhabited villages, as per the District Statistical Handbook: North 24 Parganas. Khardaha police station serves this block.

It is a raised alluvium area along the Hooghly, which forms the western boundary of the district. Barrackpore I CD Block has an area of 95.44 km2. It has 1 panchayat samity, 8 gram panchayats, 120 gram sansads (village councils), 39 mouzas and 38 inhabited villages, as per the District Statistical Handbook: North 24 Parganas. Naihati police station serves this block.

The geological setting of Broadstreet Hollow Creek is similar to Bushnellsville Creek. The surficial geology consists of glacial and alluvial deposits. The exposed sediments are primarily glacial till and alluvium although lacustrine clay has been observed in the banks and the bed. The bedrock consists of red beds including shales and mudstones as well as grey sandstones and grey shales.

It is not designated as an impaired waterbody. The surficial geology in its vicinity mostly consists of Wisconsinan Till, alluvium, Wisconsinan Ice-Contact Stratified Drift, and bedrock. The area near the mouth of Oxbow Creek was settled before 1800 and some mills were constructed on it in the 19th century. A number of bridges have also been constructed across the creek.

Oguta Lake is a lean 'finger lake' formed by the damming of the lower Njaba River with alluvium. It is the largest natural lake in Imo State, Southeastern Nigeria; within the equatorial rainforest region of Niger Delta. Oguta Lake's catchment area comprises the drainage area of the Njaba River and a part of the River Niger floodplain in the region south of Onitsha.

The elevation near the mouth of Little Creek is above sea level. The elevation near the creek's source is above sea level. The surficial geology along the lower reaches of Little Creek mainly consists of alluvium, though there is a till known as Wisconsinan Till in the surrounding valley. Along the upper reaches of the creek, the surficial geology is mostly Wisconsinan Till.

The elevation near the mouth of Oxbow Inlet is above sea level. The elevation of the stream's source is between above sea level. Oxbow Inlet is the inlet to Oxbow Lake, which does not appear to have any springs in its vicinity. The surficial geology in the immediate vicinity of the lower reaches of Oxbow Inlet mainly consists of alluvium.

The elevation near the mouth of Black Ash Creek is above sea level. The elevation near the source of the creek is between above sea level. The surficial geology near the mouth of Black Ash Creek mainly consists of alluvium, which contains stratified gravel, sand, and silt, along with some boulders. A patch of Wisconsinan Outwash is also present nearby.

The surficial geology in the vicinity of West Branch Little Muncy Creek includes alluvium, bedrock, fill, Wisconsinan and Reworked Illinoian Till, Wisconsinan Till, Wisconsinan Flow-Till, Wisconsinan Till Moraine, and Boulder Colluvium. The creek designated as a Coldwater Fishery and a Migratory Fishery and is being considered for addition to the wild trout waters list of the Pennsylvania Fish and Boat Commission.

The elevation near the mouth of Little Butler Creek is above sea level. The elevation near the creek's source is above sea level. The surficial geology along the lower and upper reaches of Little Butler Creek consists of a till known as Wisconsinan Till. However, in the middle reaches, there is a large area of alluvium and a small patch of alluvial fan.

The bedrock of Wamdeo town is formed by basement granite. The Stratigraphy unit is overlain by widespread eluvium deposit and minor deposit of alluvium. Basement Complex Most of the basement complex of the area is dominated by biotitic granite which is light gray, very coarse grained and occasionally pegmatitic and aplitic. Porphoric feldspar is occasionally present and sometimes shows a general parallel alignment.

Ron Ward's Meadow With Tadley Pastures covers an area of 11.3 hectares. The SSSI is an area of unimproved meadows which is managed for hay production. The main part of the site is meadows which are on a south-facing hillside sloping down towards Honeywell Brook. The meadows sit on a mixture of Bracklesham Beds, Lower Bagshot sands and alluvium.

The Treasure Valley ecoregion (named for the Treasure Valley) is an unglaciated rolling valley containing many canals and incised rivers. Elevation varies from 2,000 to 2,800 feet (640 to 853 m). The valley is underlain by Quaternary alluvium, loess, lacustrine, and alluvial fan deposits. Soils have an aridic moisture regime, and they originally supported sagebrush-grassland before the valley was converted to agriculture.

The Dissected Plateaus and Teton Basin ecoregion is characterized by dissected plateaus, alluvial fans, low terraces, bottomlands, outwash plains, and nearly flat, poorly drained basins. Elevation varies from 4,700 to 6,300 feet (1,443 to 1,920 m). Mollisols developed in thick loess deposits or alluvium and are subject to wind erosion. Loess is far more extensive than in the Upper Snake River Plain subregion.

Another ridge lies between the stream and West Branch Fishing Creek. Sandstone of the Pocono Formation occurs near the headwaters of Painter Run. In most of the stream's valley, alluvium, alluvial terrace, alluvial fan, and a glacial till known as the Wisconsinan Till can be found. The Wisconsinan Bouldery Till occurs on the eastern side of the stream's valley in its lower reaches.

Echaurren et al., 2016, p.103 of the El Mirador Formation,Echaurren et al., 2016, p.102 and Quaternary alluvium overly the Collón Curá Formation in the Cañadón Asfalto Basin.Echaurren et al., 2016, p.105Echaurren, 2017, p.102 In the Collón Curá valley, the formation covers Paleogene sediments of the Huitrera and Cerro Petiso Formations and in places overlying crystalline basement.

Sutton Creek is located a few miles upriver of the Wyoming Valley. The surficial geology in its watershed consists of alluvium, Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, and bedrock, while the bedrock geology consists of sandstone. Major land uses in the watershed of Sutton Creek include forested land and agricultural land. Lakes in the creek's watershed include Lake Louise and Cummings Pond.

Lampblack Creek (also known as Lamp Black Creek) is a tributary of Gardner Creek in Luzerne County, Pennsylvania, in the United States. It is approximately long and flows through Jenkins Township. The watershed of the creek has an area of . The surficial geology in the area mainly consists of bedrock consisting of sandstone and shale, shale and sandstone pits, urban land, alluvium, Wisconsinan Till, and coal dumps.

The elevation near the mouth of Lampblack Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology of Lampblack Creek mainly features bedrock consisting of sandstone and shale, as well as shale and sandstone pits. There are also some patches of urban land, alluvium, a glacial or resedimented till known as Wisconsinan Till, and coal dumps.

Turtle Creek (also known as Turtle Run) is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States. It is approximately long and flows through Conyngham Township. The watershed of the creek has an area of . Wisconsinan Bouldery Till, Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Outwash, alluvium, alluvial terrace, fill, and coal dumps all occur in the vicinity of the creek.

The elevation near the mouth of Bear Brook is above sea level. The elevation of the stream's source is between above sea level. The surficial geology in the vicinity of Bear Brook in its lower reaches mainly consists of Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Till, and bedrock consisting of conglomeratic sandstone, sandstone, and shale. However, there are also a few patches of alluvium.

The total length of the district from east to west is approximately 75 km and the breadth from north to south is about 42 km. The district of Ambedkar Nagar forms a part of the central Ganga basin. The soils of the Ambedkar Nagar district are alluvium. The Sarayu River is the main river and is located at the northern boundary of the district.

The Kole Wetlands acts as natural drainage system for Thrissur city and Thrissur district through a network of canals and ponds which connects different parts of Kole Wastelands to Enamavu river{one of the smallest River in Kerala,Canoli Canal,Chettuva River and then to the Arabian sea. It is fertile with Alluvium soil which is deposited Kechery and Karuvannoor river in the monsoon.

Upstream of Long Iram (upstream part of Mahakam river basin) the river is flowing in tertiary rocks (Voss, 1983).Voss, F.: Kalimantan Timur, Atlas. HWWA Institute, Hamburg, 1983. Between Long Iram and Muara Kaman (middle Mahakam area) the river is flowing in quaternary alluvium, while in the downstream area between Muara Kaman and the coast including the Mahakam delta, tertiary rocks are again present.

Willow Brook is a tributary of Utley Brook in Susquehanna County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through Lenox Township in Susquehanna County and Nicholson Township in Wyoming County. The surfcial geology in the vicinity of the stream consists mainly of Wisconsinan Till, bedrock, alluvium, wetlands, and a lake. A number of bridges have been constructed across it.

Islampur is located at . Uttar Dinajpur district has a flat topography and slopes gently from north to south. All rivers flow in that direction. Except for the eastern fringes of Chopra CD Block, most of the district is a part of the catchment area of the Mahanada and also a part of the larger Barind Tract The soil is composed of different varieties of alluvium.

Salt-loving plants then take root in the mud, and the salting is established. The plants trap sediments, and the surface rises until it remains above the level of most tides. Inning occurs when a sea wall is built around the edge of the salting, after which rain washes the salt downwards. The alluvium which forms the soil is highly fertile once freshwater plants start to grow.

Shoalwater Bay Military Training Area is approximately , north-west of Byfield. The main geomorphic units comprise hilly to mountainous terrain, aeolian sand dunes, undulating and rolling terrain and flat areas of riverine alluvium. The permutations of geomorphological, pedological and microclimatic environments support diverse vegetation types, for which 58 floristic communities have been recognised within 13 structural forms. Rainfall decreases markedly westwards and sharp vegetational gradients exist.

The elevation near the mouth of Partners Creek is above sea level. The elevation near the creek's source is above sea level. The surficial geology at the mouth of Partners Creek consists of alluvial fan. Further upstream, the surficial geology mainly consists of a till known as Wisconsinan Till, but there are large patches of alluvium and bedrock consisting of sandstone and shale in the area.

After the drainage of the lake the lakefloor was eroded by streams, which redeposited its sediments, and soils formed. The lake would have been replaced by dry lakes and anastomosing stream networks. Creeks cut into the lake floor, forming valleys that later filled with alluvium. The Alamosa Formation, a geological formation, fills the basin of Lake Alamosa; it represents the deep water deposits of Lake Alamosa.

Madre de Dios depends heavily on natural products and raw materials for its economy. There is virtually no manufacturing industry. The main agricultural products are: #Cotton #Coffee #Sugarcane #Cacao beans #Brazil nuts #Palm oil Gold mining is the only other large industry of the region, confined mainly to alluvium adjacent to the Inambari and Madre de Dios rivers. Significant deforestation has resulted due to this activity.

The fault is prominent on satellite images and topographic maps. The irregular boundary between the Serranía del Darién and the Atrato Valley suggests that the fault is a thrust fault that dips northwest. Along its southern extent, the fault forms a scarp that faces east and is a few tens of meters high. The fault separates alluvium of the Atrato and Tuira Rivers from Tertiary strata.

There are eleven meadows which are on alluvium and Lower Lias clays near the confluence of the Rivers Eye and Dikler. The citation states they are one of the richest and largest traditional meadow systems remaining in the Cotswolds. The meadows are divided by well developed ancient hedges and there are occasional hedgerow trees. The meadows which make up the SSSI support a wide range of species.

Laurel Run is a tributary of West Branch Fishing Creek in Sullivan County, Pennsylvania, in the United States. It is approximately long and flows through Davidson Township. The stream is in the United States Geological Survey quadrangle of Elk Grove. Wisconsinan Flow-Till, Boulder Colluvium, Wisconsinan Till Moraine, alluvium, and alluvial fan occur in the vicinity of the stream, as does bedrock consisting of sandstone and shale.

The elevation near the mouth of North Branch Bowman Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology in the vicinity of the lower reaches of North Branch Bowman Creek consists of alluvial fan and alluvium. Further upstream, in the creek's valley, there is Boulder Colluvium, which is rich in boulders made of quartz, sandstone, or conglomerate.

The elevation near the mouth of Wolf Run is above sea level. The elevation of the stream's source is just over above sea level. The surficial geology near the mouth of Wolf Run consists of alluvium and alluvial fan, which both contain stratified sand, silt, and gravel, as well as some boulders. Further upstream, the surficial geology consists of a till known as Wisconsinan Till.

Geologically Aureille belongs to the Crau plain: its soil consists of Alluvium and pebbles. This type of soil is found throughout the Aureille plateau, to the point where it descends sharply at Mouriès. The soil composition is then modified, consisting of sloping deposits. The peaks north of Aureille, including the Tour des Opies, are very different from what is usually found in the Alpilles mountains.

The elevation near the mouth of Panther Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology along the lower reaches of Panther Creek consists of alluvium and alluvial terrace. Bedrock containing conglomeratic sandstone, sandstone, and shale is present slightly further from the creek, as is a glacial or resedimented till known as Wisconsinan Till.

East of the San Joaquin Fault there is a flow pattern of alluvium reported as a mud flow.C.Michael Hogan, Marc Papineau, Ballard George, et al., Environmental Assessment for the Proposed Residential and Commercial Development at the Westley Interchange, Earth Metrics Inc., Report 10529C, California State Environmental Clearinghouse, Sacramento, Ca., July, 1990 This flow pattern was deposited in the early Holocene period or the late Pleistocene.

Further upstream, the surficial geology immediately adjacent to the creek consists of alluvium, but it eventually switches to Wisconsinan Till, which also makes up most of the surficial geology elsewhere in the watershed. However, there are a few large patches of bedrock and a few small patches of Wisconsinan Ice-Contact Stratified Drift. Additionally, there are several patches of wetlands and peat bogs, especially near the headwaters.

The southern part of Acton has a complicated arrangement of sediments that include the Pittman Formation greywacke and the black coloured Acton Shale Member from the Ordovician age. Then from the Silurian age there is mudstone, State Circle Shale, and Camp Hill Sandstone. Some limestone is found near the National Museum of Australia. Calcareous shales from the Canberra Formation are overlain by Quaternary alluvium on the north.

A meteorite was recovered here on July 10, 1977. The meteorite was discovered in alluvium approximately 200,000 years old.Weathering-Induced Re-crystallisation of Kamacite, Grokhovsky, V.A. 60th Annual Meteoritical Society Meeting It weighed and was classified by the Natural History Museum as a medium Octahedrite,Natural History Museum Catlogue containing (mineral composition determined by X-ray spectral microanalysis): 9.25% nickel, 0.42% cobalt, and 0.30% phosphorus.

The channels run southwest to a group of channels at the headwaters of Paint Spring Run and Pikes Creek. These channels are lower than those that run to Huntington Creek, but higher than those running to Bear Hollow. The channels are in a large area of Wisconsinan Ice-Contact Stratified Drift. The surficial geology along Paint Spring Run features alluvium for most of its length.

The surficial geology in the vicinity of Bear Hollow Creek features alluvium in its lower and upper reaches. Glacial or resedimented tills such as Wisconsinan Till and Wisconsinan Bouldery Till occur in the creek's valley and bedrock consisting of sandstone and shale occurs in the surficial geology on the slopes of the valley. A patch of peat bog is situated in the creek's middle reaches.

It consists of Sonipat tehsil lying to the west of the Khadar, and is the most extensive of the three regions: The Upland Plain is covered with old alluvium, which if properly irrigated, is highly productive. There is extensive Farming of crops, oil seeds, horticultural plants, vegetables and flowers in this region. The ridges in Gohana tehsil represent the northernmost extension of the Aravallis.

The tree is endemic to the Pilbara and northern parts of the Mid West regions of Western Australia, it occurs along creeks and rivers in the semi-arid land north of Carnarvon and Meekatharra where it is often situated in rocky river and creek beds, on stony plains and on rocky ridges growing in stony loam or clay loam, alluvium or red sandy soils.

Cascades of water flowed over a dam while waterfalls migrated up-river along it. Most lava dams lasted for around 10,000 to 20,000 years. However others have proposed that the lava dams were much more ephemeral and failed catastrophically before overtopping. In this model dams would fail due to fluid flow through fractures in the dams and around dam abutments, through permeable river deposits and alluvium.

There were also reports of wells that dried up, and a crack in a deep alluvium north of Massena Center oozed water and sand. Damage to the city of Cornwall, Ontario, was heavier due to a denser population and its geological location; many structures' foundations were built on sand. Cornwall Collegiate and Vocational School received heavy damage from masonry work falling through the roof of the gymnasium.

Lansium parasiticum is grown from low grounds up to heights of above sea level, in areas with an average rainfall of a year. The plant can grow and blossom in latosol, yellow podzol, and alluvium. The plant prefers slightly acidic soil with good drainage and rich in mulch. The langsat variant is hardier, and can weather dry seasons with a little shade and water.

Upputeru tidal creek, 15 km in length, and Isakapalli lagoon, separated from the Bay of Bengal by the Isakapalli barrier island, 180 m long and up to 3 m high, form the main coastal wetlands. The upper basin of the Penna is largely made up of ancient Archean rocks, principally granite and schist. The lower basin is made up of young sediments, including laterite and recent alluvium.

The elevation near the mouth of Leonard Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology along a significant portion of the length of Leonard Creek consists of alluvium. In the lower reaches of the creek, this is bordered by alluvial terrace, Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, bedrock consisting of sandstone and shale, and fill.

Quaternary deposits include glacial till and peat alongside some small patches of alluvium (clay, silt, sand and gravel) which occupy lower ground. Around the margins of Lismore are modern beach deposits and raised marine deposits of clay, silt and sand, the latter being a product of varying relative sea-levels during the Holocene epoch. The whole of Scotland was subjected to glaciation during the Pleistocene epoch.

Degradation of Precambrian rock has effected in the creation of a mature mantled and undulating peneplain, disturbed by many prominent remnants of erosion (rock outcrops) and ridges. Imposing topographic feature is the long range of rocky mountains of the south-west of the park. The geographical regime includes alluvium deposits and Miocene limestone. The major soil type is the relatively fertile but easily eroded red earth.

The San Joaquin Fault is a seismically active geological structure in the California Central Valley.U.S. government map of the San Joaquin Fault East of the San Joaquin fault there is a flow pattern of alluvium that has been reported to be a mud flow.C.Michael Hogan, Marc Papineau, Ballard George, et al., Environmental Assessment for the Proposed Residential and Commercial Development at the Westley Interchange, Earth Metrics Inc.

The Northern Backswamps ecoregion is made up of low-lying overflow areas on floodplains, and includes poorly drained flats and swales. Water often collects in its marshes, swamps, oxbow lakes, ponds, and low gradient streams. Soils developed from clayey alluvium including overbank and slack-water deposits; they commonly have a high shrink-swell potential and are locally rich in organic material. Water levels are seasonally variable.

There is also a patch of alluvial terrace near the creek's mouth. The surficial geology further upstream is fairly similar except that there is little Wisconsinan Ice-Contact Stratified Drift or alluvium at the headwaters and that the bedrock consists only of sandstone and shale. There are at least of pipeline in the watershed of Whitelock Creek. This pipeline crosses a number of streams.

Primary deposits are found in the hills of the Serra da Madeira and alluvium deposits have been washed down into the forested valleys. The alluvial deposits, now exhausted, consisted of greisens associated with the Água Boa biotite granite and the Madeira niobium-tantalum- tin deposit. The coarse-grained porphyritic albite granite has intruding paleoproterozoic acid volcanic and pyroclastic rocks. It includes Rapakivi granite and Biotite granite.

The first generator was commissioned on 8 January 1955, the second and last on 1 April 1955. On 1 July 1955 the entire project was complete. The Great Alaska earthquake in March 1964 caused significant damage to the dam, particularly the water intake for the power plant. The intake shifted towards the lake and frozen alluvium beneath and near the dam's spillway densified, creating voids.

In the case of placer mining, unconsolidated gravel, or alluvium, is fed into machinery consisting of a hopper and a shaking screen or trommel which frees the desired minerals from the waste gravel. The minerals are then concentrated using sluices or jigs. Large drills are used to sink shafts, excavate stopes, and obtain samples for analysis. Trams are used to transport miners, minerals and waste.

The northern salmon gum is found in the north of Western Australia and the Northern Territory. In Western Australia it occurs along watercourses and low-lying flats in the Kimberley region where it grows in alluvium or sandy soils. In the Northern Territory it is found across the Top End, including the Tiwi Islands, the Cobourg Peninsula and as far south as Daly Waters.

The elevation near the mouth of Fitch Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology near the mouth of Fitch Creek mainly consists of alluvium, Wisconsinan Outwash, and sand and gravel pits. Further upstream, Wisconsinan Till is most prevalent, but there are also a few patches of Wisconsinan Ice-Contact Stratified Drift, bedrock, and lakes.

The elevation near the mouth of Bear Swamp Creek is above sea level. The elevation near the creek's source is above sea level. The surficial geology near the mouth of Bear Swamp Creek mainly consists of a till known as Wisconsinan Till, plus some patches of alluvium. However, the nearby Carey Hill has surficial geology consisting almost entirely of bedrock consisting of sandstone and shale.

Much of the country is covered with jungles. The western part of the district has poor, ferruginous soil and hard beds of laterite with scrub jungles and sal woods. Long broken ridges with irregular patches of more recent alluvium have marks of seasonal cultivation. During the long dry season large extents of red soil with hardly any trees lend the country a scorched and dreary appearance.

The region north of the city consists of the Wichita Mountains, including Mount Scott and Mount Pinchot, the area's highest peaks. The area consists mostly of Permian Post Oak Conglomerate limestone on the northern sections of the city. In the south sections of the city, Permian Garber sandstone is commonly found with some Hennessey Group shale. Area creeks including East Cache Creek contain deposits of Quaternary alluvium.

The clay soil settled farther away from the rivers and being less stable, it slumped to muddy back-swamps.See soil surveys of the various parishes. The plantations in the vicinity of St. Francisville, Louisiana, are on a high bluff on the east side of the Mississippi River with loess soil, which was not as fertile as the river alluvium, but was relatively well-suited to plantation agriculture.

Cleome oxalidea is a species of plant in the Cleomaceae family and is found in Western Australia. The annual or ephemeral herb has a rosetted habit and typically grows to a height of . It blooms between January and September producing blue-pink-purple flowers. It is found in the Kimberley, Pilbara, Goldfields-Esperance and Mid West regions of Western Australia growing in stony sandy-loam alluvium.

Trumao is the name of a soil of the Andosol order found in southern and central Chile. Trumaos are formed from young volcanic ash, by volcanic ash redeposited by aeolian processes or by volcanic ash mobilized as alluvium. Trumaos are characterized by containing the following minerals: allophane, imogolite plus a series of paracrystalline and non-crystalline clays. These soils have high porosity and low bulk density.

Goalpokhar is located at . Uttar Dinajpur district has a flat topography and slopes gently from north to south. All rivers flow in that direction. Except for the eastern fringes of Chopra CD Block, most of the district is a part of the catchment area of the Mahanada and also a part of the larger Barind Tract The soil is composed of different varieties of alluvium.

It contains soil of mature black or brownish loam to recent alluvium. The Ichhamati flows through the eastern part of the district. The Ichhamati flows in from the north-western part of the CD Block, cuts across the northern part of the CD Block and then flows along the eastern international boundary with Bangladesh. Basirhat I CD Block has an area of 111.84 km2.

Even more geologically recent gravel, alluvium and fen deposits are found in the valley of the River Great Ouse at the eastern end of the village; they merge into the extensive flat tracts of The Fens which stretch north-north-west towards The Wash. Holme at nine feet () below sea-level is East Cambridgeshire's (and the United Kingdom's) lowest point, and is north-west.

The site is important for protection being one of the few remaining ham meadows which are traditionally managed. It is sited on the alluvium of the Severn Vale and is a flooded area in the winter months. It is neutral grassland and mostly only semi-improved. There are specific requirements in respect of fertilisers for the site to ensure the protection of the wide-ranging flora.

It is a raised alluvium area along the Hooghly, which forms the western boundary of the district. Barasat I CD Block has an area of 104.97 km2. It has 1 panchayat samity, 9 gram panchayats, 152 gram sansads (village councils), 81 mouzas and 81 inhabited villages, as per the District Statistical Handbook: North 24 Parganas.Duttapukur police station has jurisdiction over Barasat I CD Block.

The park's geologic record preserves three different groups of rock and sediment. The oldest rocks are Early to Middle Proterozoic gneiss and schist, including the Ute Canyon Stock. Overlying these, and separated by an angular unconformity, are mostly horizontally bedded Mesozoic sedimentary rocks, including the cliff-forming Wingate Sandstone. Overlying these are various types of Quaternary unconsolidated deposits such as alluvium, colluvium, and dunes.

Savar is located at . It has 66,956 units of household and a total area of . It is bounded by Kaliakair and Gazipur Sadar upazilas on the north, Keraniganj upazila on the south, Mirpur, Mohammadpur, Pallabi and Uttara thanas of Dhaka City on the east, and Dhamrai and Singair upazilas on the west. The land of the upazila is composed of alluvium soil of the Pleistocene period.

The elevation near the mouth of Little Indian Run is above sea level. The elevation near the stream's source is above sea level. The surficial geology along the middle reaches of the valley floor of Little Indian Run mainly consists of alluvium. However, bedrock consisting of sandstone and shale makes up the surficial geology on the sides of the stream's valley in this reach.

The elevation near the mouth of West Branch Little Muncy Creek is above sea level. The elevation of the creek's source is above sea level. The surficial geology alongside West Branch Little Muncy Creek in its lower reaches mainly consists of alluvium. However, there is a patch of fill at the mouth and bedrock consisting of sandstone and shale occurs on the sides of the creek's valley.

Corymbia aspera grows in low, open woodland on hills, ridges and plateaus as well as on floodplains in red sand, alluvium and skeletal soils. Its range extends from the Pilbara and Kimberley regions of Western Australia east through the Roper and McArthur River catchments in the Northern Territory and into Queensland as far east as the Selwyn Range to the south east of Cloncurry.

However, near the mouth of the stream, there is alluvium containing stratified silt, sand, and gravel, as well as some boulders. Additionally, a colluvium known as Boulder Colluvium occurs near the stream's mouth and also in the higher portions of the watershed, above the stream's valley. In these areas, the majority of the surface is covered in boulders and cobbles consisting of quartz, sandstone, or conglomerate.

Additionally, many areas have surficial geology featuring bedrock made of coal, conglomeratic sandstone, sandstone, and shale. The surficial geology alongside the creek continues to feature alluvium as far upstream as Lake Louise. However, in the watershed's upper reaches, Wisconsinan Till and bedrock consisting of sandstone and shale are more common. There is also a patch of Wisconsinan Ice- Contact Stratified Drift near the creek's headwaters.

Dredging to clear the active channel of the Yuba River was done periodically, but a vast majority of dredging was done away from the active channel, with the purpose of recovering gold from the river sediments. This off-channel gold dredging accounts for the vast majority of land dredged, and is what created the linear gravel piles, called tailing windrows, now visible in aerial photos. And while historic upstream hydraulic mining did result in the deposition of of hydraulic mining debris (slickens) in the area of the Hammonton dredge field, these slickens were considered uneconomical at the time (because they had already been processed for gold once), and the primary target of gold dredging was the native river sediments (alluvium) of the Yuba River. To that point, a vast majority of the more than one billion cubic yards of material dredged was native alluvium, not hydraulic mining debris.

Importantly, all six ecological life zones identified in Puerto Rico are represented in a region just 13 miles (21 km) long, formed by the Northeast Ecological Corridor, Las Cabezas de San Juan Nature Reserve and El Yunque National Forest. Changes in precipitation, temperature and elevation are observed in the whole area constitute one of the most pronounced environmental gradients across the Caribbean. Three geoclimatic zones have been identified within the NEC: these are the subtropical dry forest on alluvium soil and other unconsolidated sediments, subtropical moist forest on alluvium and other unconsolidated sediments and subtropical rainforest on volcanic rock that has been altered hydrothermically. According to the descriptions in Lugo, A. E., 2005, in the NEC there are four forest types: coastal dry forest on volcanic substrate, wet and dry forest in alluvial valleys, coastal rain forest on sandy substrate and lowland rainforest on the volcanic substrate.

Aerial view from east In the east, Fadden is built on Alluvium. The west of Fadden consists of Deakin Volcanics rhyolite. The rhyolite can be coloured green-grey, purple or cream, and dates from the Silurian age at 414±9 My. A fault heads north-north-west from Macarthur Hill with a quartz outcrop.Henderson G A M and Matveev G, Geology of Canberra, Queanbeyan and Environs 1:50000 1980.

These intrusions were likely the necks of volcanoes that erupted the other tuff and dacite in the area. A Cenozoic age dyke of teschenite intrudes the Laidlaw ignimbrite in the Kambah Pool and Red Rocks Gorge area. Quaternary alluvium covers the ground around the upper reaches of Village Creek, around Drakeford Drive. A fault runs from the north-west in Allchin Circuit to the south-east under Urambi primary school.

The Ballona Wetlands, is a habitat of a marine estuary alongside grassland, woodland, sand dune, and freshwater wetland ecosystems. Historically the outlet-mouth of the Los Angeles River switched, between San Pedro Bay and the Ballona creek watercourse to Santa Monica Bay, several times in the early 19th century only. It last came through Ballona in the early 19th century. The alluvium it left makes up the soils below.

There is a large patch of Wisconsinan Ice-Contact Stratified Drift in the stream's lower reaches and a much smaller patch of alluvium near its headwaters. There is also a sand and gravel pit along the creek. This pit is the only such pit in the United States Geological Survey quadrangle of Sweet Valley. Roaring Brook is in the Susquehanna Valley Section of the ridge and valley physiographic province.

Although meteorites fall uniformly across the globe they do not typically remain on the surface in areas with a large amount of yearly rainfall. If a newly fallen meteorite is not recovered within a few months it is likely to be buried with alluvium or covered by plant growth. Some arctic and desert regions have proven to be well-suited to preserving meteorites, and can provide excellent surfaces for hunting visually.

The elevation near the mouth of White Oak Run is above sea level. The elevation near the source of the stream is between . The surficial geology in the vicinity of the lower reaches of White Oak Run consists of alluvium. Slightly further from the stream, there are areas of a glacial or resedimented till known as Wisconsinan Till, as well as bedrock containing conglomeratic sandstone, sandstone, and shale.

The 1854 North Fork Diversion ditch provided water for Avery's Pond and water from the pond became a reliable year-around water source for Avery's extensive orchards. Avery used to supply lumber, fruit, and sheep to the gold miners in the area. His ranch consisted of about 117 acres, of which 40 acres had 1,500 fruit trees (pears, persimmons, cherries). The pond is lined with fine-grained alluvium.

Calcareous shales from the Canberra Formation is overlain by Quaternary alluvium. This rock is the limestone of the original title of Canberra "Limestone Plains". The higher eastern side of Hackett is on top of the lowest layer of the Ainslie Volcanics, a grey Dacite and other erupted particles such as agglomerate and tuff.Henderson G A M and Matveev G, Geology of Canberra, Queanbeyan and Environs 1:50000 1980.

There are a number of arcuate till ridges in the vicinity of Slip Run. Conglomerate erratics also occur to the west of the stream's valley. The surficial geology at the mouth of Slip Run consists of alluvium and Boulder Colluvium, which contains numerous boulders made of sandstone, conglomerate, and quartz. Further upstream, the surficial geology features bedrock consisting of sandstone and shale, with Boulder Colluvium occurring on a nearby upland.

The elevation near the mouth of Kingsbury Brook is above sea level. The elevation near the stream's source is between above sea level. The surficial geology along Kingsbury Brook in its lower reaches mainly features alluvium, which contains stratified sand, silt, gravel, and some boulders. Some Wisconsinan Ice-Contact Stratified Drift, which contains stratified sand and gravel along with some boulders, is present along the sides of the stream's valley.

The elevation near the mouth of Conety Run is above sea level. The elevation near the stream's source is between above sea level. The surficial geology along the lower reaches of Conety Run mainly consists of alluvium. However, bedrock consisting of sandstone and shale, a glacial or resedimented till known as Wisconsinan Till, and a small patch of Wisconsinan Ice-Contact Stratified Drift are also present in the stream's vicinity.

Further upstream the surficial geology is similar, but with two more alluvial fan patches and a wetland patch. Along the uppermost reaches of the creek, includes Wisconsinan Till (especially at the headwaters) and alluvium, as well as small patches of alluvial fan and wetland. Nine Partners Creek has been described as a "small creek". Some sources describe the creek as flowing into Leslie Creek, which is one of its tributaries.

The elevation near the mouth of Tower Branch is above sea level. The elevation near the stream's source is above sea level. The surficial geology near the mouth of Tower Branch mainly consists of alluvial fan. Most of the area in stream's vicinity has its surficial geology dominated by a till known as Wisconsinan Till, but there are patches of alluvium and smaller patches of lakes and wetlands.

The elevation near the mouth of Davis Hollow is above sea level. The elevation of the stream's source is between above sea level. There are two patches of alluvium, which contains stratified silt, sand, and gravel, near the upper reaches of Davis Hollow. However, the surficial geology in the area mainly consists of bedrock made of sandstone and shale as well as a glacial or resedimented till known as Wisconsinan Till.

The Ubehebe Craters formed within sedimentary rocks, which crop out in the craters. Conglomerates and sandstones form a sequence under Ubehebe Crater; they are part of the so-called Navadu Formation. Beyond this mostly Miocene formation are Paleozoic carbonates. The Cottonwood Mountains consist of Paleozoic, Mesozoic, and in part Tertiary sedimentary rocks; most of the terrain west and north of the Ubehebe Craters is covered by modern alluvium.

Sapphires were first discovered in Montana in 1865, in alluvium along the Missouri River. Finds in other locations in the western half of the state occurred in 1889, 1892, and 1894. The Rock Creek location, near Phillipsburg, is the most productive site in Montana, and its gems inspired the name of the nearby Sapphire Mountains. In 1969, the sapphire was co-designated along with the agate as Montana's state gemstones.

The surficial geology in its vicinity includes Wisconsinan Till, alluvial fan, Boulder Colluvium, alluvium, bedrock, and a peat bog. The creek is mostly in Pennsylvania State Game Lands and Ricketts Glen State Park. The drainage basin of North Branch Bowman Creek is designated as a High-Quality Coldwater Fishery and a Migratory Fishery. The creek has been stocked with fish in the past, but also has wild trout.

The elevation near the mouth of South Branch Bowman Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology in the lower reaches of the valley of South Branch Bowman Creek mainly consists of alluvium, alluvial fan, Wisconsinan Ice-Stratified Drift, and a lake. However, there is also fill and Boulder Colluvium, which is rich in boulders containing quartz, sandstone, or conglomerate.

Heritable property is capable of acceding to other heritable property, known as alluvio after the Roman law method of acquisition of the same name. This primarily operates by rivers or other moving-waters such as the tide depositing sediment, or alluvium, deposited by a river. It should not be confused with avulsion, which occurs when there is a deposit of sediment after a heavy storm or other weather event.

Shallow black soil, medium black soil, Deep to very black soil, mixed red & black soil, red loamy soil, which cover large tracts of land and the other two lateritic and alluvium soils are local in nature. _About the Transportation_ Hukkeri has a wide range of road networks. Adjacent cities can be reached through state highways and villages have proper roadways as well. A National Highway(NH4) connects to Belagavi City.

The Kumbhi River rises near Gaganbavada And flows north-eastwards for about fifteen miles up to Kirwai. From there it flows eastwards with a winding course and receives an important tributary Dhamani, near Chaugalewadi. It then develops wide basin underlain by alluvium. North-east of Sangrul it has a sharp bend eastwards after which it meets the united Tulsi and Bhogavati river near Bahireshwar about eight miles south-west of Kolhapur.

The geology of the site is alluvium underlain by river terrace gravels and in turn overlying the London Clay formation. The reservoir is formed by a continuous earthen embankment that encloses the basin. The embankments consist of a central puddle clay core with a selected material adjacent to the core forming a filter. The core is a maximum of wide at the base and tapers to wide at the crest.

The San Pedro Valley is a site for Holocene mammal fossils because of the riparian environment. In recent decades, the Arizona Geological Society has focused on the region, as well as researchers. Development pressures, recreation, and groundwater harvesting have led to recent concerns of protecting the region. A recent floodplain study focused on the Holocene floodplain alluvium and its history, over a stretch of the river to understand subground waterflow resources.

The surficial geology near it consists of alluvium, alluvial terrace, Wisconsinan Outwash, Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, fill, and a wetland. There are several road crossings and a railroad bridge crossing over Swale Brook. A number of industries also historically operated near the stream. The stream's watershed is designated as a Coldwater Fishery and a Migratory Fishery and the stream itself has a high level of fish diversity.

The leaves are long and wide and has beaked fruit that persists year round. The species was first described by botanists Alfred James Ewart and O.B.Davies in 1917 in The Flora of the Northern Territory. It is found on flat to slightly undulating places in swampy areas and on basaltic plains in the Kimberley region of Western Australia, the Northern Territory and Queensland growing in alluvium and heavy soils.

The catchment area has an average rainfall of per annum and an evaporation rate of per annum. The landscape is a mixture of saline and fresh lakes and swamps with lunettes, dunes and swales on aeolian and lacustrine deposits and alluvium over granite based rocks. The lake is situated on major ancient drainage lines. The lake was once a freshwater source but land clearing has led to salinity.

After the junction with Aliso Canyon Road, the highway leaves Aliso Creek and crosses a ridge to Kentucky Springs Canyon. The straight-away section on alluvium, approaching the Mt. Emma Road and the Angeles National Forest boundary, goes through pinyon pine and California juniper woodland. In the springtime, flannelbush and goldenbush bloom in this area. After the boundary sign, the pinyon pines disappear and Great Basin sagebrush becomes more dominant.

The species occurs in all states of Australia, New ZealandBodmin, K.A., Champion, P.D., James, T., Burton, T. (2015) New Zealand Rushes: Juncus factsheets. Hamilton: NIWA Southern Africa and South America. Juncus kraussii is salt tolerant and favours a damp environment and is most often found in areas such as swamps and brackish estuaries. The plant is able to grow in a range of soils from sands to alluvium.

Beaver Run looking upstream near its mouth The elevation near the mouth of Beaver Run is above sea level. The elevation of the stream's source is between above sea level. The surficial geology near the mouth of Beaver Run mainly consists of alluvial terrace, alluvium, and a till known as Wisconsinan Till. The latter two types of surficial geology are also common further upstream, as is Wisconsinan Ice-Contact Stratified Drift.

Lower Caldecote stands on first and second terrace river gravel while alluvium is by the Ivel. The soil is of low fertility, freely draining and slightly acid with a loamy texture. Lynton Cottages (built 1902) and York House (1904) directly front the A1 northbound carriageway but the remainder of the hamlet was bypassed in 1960/61. Housing on The Grange was developed in the mid to late 1990s.

The elevation near the mouth of Cider Run is above sea level. The elevation of the stream's source is between above sea level. The surficial geology in the vicinity of Cider Run mainly consists of alluvium, except in its upper reaches, where it consists of a till known as Wisconsinan Till. Wisconsinan Till occurs along the stream's valley throughout its length and is underlain by glacial lake clays in some reaches.

This is a linear village arranged in a north-west to south-east alignment on the A67 road where it crosses the Motorway A1, west of the edge of Darlington. Although the A1 is part of the landscape, there is no access to it from the A67. The underlying geology is glacial clay with areas of gravel, sand, peat and alluvium, and outcrops of dolomite and carboniferous limestone.

The pattern of shaking intensity was somewhat variable, with a large region with an intensity of VII (Very strong) containing localized areas of intensity VIII (Severe). These variations generally relate closely to the underlying geology, with higher intensities recorded where there was either artificial fill or alluvium, although there were some exceptions. The observed pattern of intensities was very similar to those from the 1949 Olympia and 2001 Nisqually earthquakes.

Covered completely by a thick mantle of alluvium of variable thickness, the lie of the region is flat having a gentle slope towards the Bay of Bengal in the east. It is limited on the north by the Nandalar and on the south-east by the Vettar. The group of rocks known as Cuddalore formations is met with in the area contiguous to Karaikal region in Nagappattinam District.

Near the culvert, Benson Hollow has a streambed made of gravel with an average grain size of . The stream is a Rosgen C Type stream and does not have large loads of debris. The surficial geology along the lower reaches of the stream, but alluvium and a lake occur in the upper reaches. The stream's valley is flanked by Wisconsinan Till and bedrock consisting of sandstone and shale.

The East Cliff runs for several miles from Pool Valley towards Rottingdean and Saltdean, reaching above sea level. The soil beneath it, a mixture of alluvium and clay with some flint and chalk rubble, has experienced erosion for many years. The cliff itself, like the rest of Brighton's soil, is chalk. Below this are thin layers of Upper and Lower Greensand separated by a thicker band of Gault clay.

Since Roman times and perhaps earlier, the isostatic rebound from the weight of previous ice sheets, and its interplay with the eustatic change in sea level, have resulted in the old valley of the River Brent, together with that of the Thames, silting up again. Thus, along much of the Brent's present-day course, one can make out the water-meadows of rich alluvium, which is augmented by frequent floods.

Utley Brook is a tributary of Tunkhannock Creek in Susquehanna County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through Lenox Township in Susquehanna County and Nicholson Township in Wyoming County. The stream is in the United States Geological Survey quadrangles of Hop Bottom and Lenoxville. The surficial geology in its vicinity consists of Wisconsinan Till, alluvium, bedrock, wetlands, and lakes.

The elevation near the mouth of Monument Creek is above sea level. The elevation near the source of the creek is between above sea level. The surficial geology in the vicinity of the lower reaches of Monument Creek mainly consists of alluvium and Wisconsinan Ice-Contact Stratified Drift. However, a glacial or resedimented till known as Wisconsinan Till is also present, as is bedrock consisting of conglomerate, sandstone, and shale.

The elevation near the mouth of Falls Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology along the lower reaches of Falls Creek mainly consists of Wisconsinan Till, although there is alluvium (consisting of stratified sand and gravel) and Wisconsinan Outwash near its mouth. There are also patches of Wisconsinan Ice-Contact Stratified Drift and bedrock in some places.

Further east, forming a rather unstable base to the Cotswold escarpment, are the sands and clays of the Upper Lias. Superficial deposits are widespread. Floodplain alluvium accompanies the course of the Severn itself as well as tributaries such as the Leadon, Chelt, Frome and Cam. Ancient terraces of former, more elevated floodplains mark the position of the major rivers through various glacial and inter-glacial periods in the last Ice Age.

Two miners in Kilo-Moto c. 1941 At the end of 1919 Louis Franck, the Minister of the Colonies, gave Moulaert responsibility for the state mines at Kilo and Moto. These were located in largely hostile territory, with no communications and very primitive operations. Moulaert tackled improvements to roads, transport, medical support, supplies and crops, as well as mining installations, exploitation of alluvium and eluvium deposits, prospecting and research.

Geocene 6, 12–-17. Originally, the crater floor was filled with a lava lake, the western half collapsed slightly and became a freshwater lake which later turned into a swamp and slowly filled up with alluvium and sediment, before being drained by Europeans for use as playing fields and parkland. These origins are still somewhat visible in that the Duck Ponds are freshwater-fed from the drainage of the crater.

It is native to southern Angola, southern DRC, Zambia, southern Tanzania, Malawi, Mozambique, Namibia, Botswana, Zimbabwe, South Africa and Swaziland. It occupies any arid to moist, and relatively open savanna woodlands, especially where Acacia trees are present. They frequent the edges of miombo woodland, and occur commonly along water courses, dry riparian forest and in Acacia woodland on alluvium. It also occurs commonly on farms and in suburban gardens and parks.

The town sits on flat ground consisting mostly of clay with soil that is sand and alluvium. To the west of the village is Westfield Beck. The nearby town of Haxby now merges with Wigginton though the old Parish Boundary map still shows the dividing line. This runs east to west along the back of the houses on Wheatfield Drive on its southern edge as far as Barley Drive.

The southern boundary is formed by Ganga which separates it from the district of Fatehpur. On the west lies the Bighapur and Purwa tehsil of Unnao. The district forms a part of the Gangetic plan which is of recent origin according to geological chronology and reveal ordinary Gangetic alluvium. The district being a part of the alluvial plain conforms to the same geological sequence as the plain itself.

From the northeast, the Kanak Vrindavan valley, where a temple complex sits, the hills slope gently towards the lake edge. Within the lake area, the ground area is made up of a thick mantle of soil, blown sand, and alluvium. Forest denudation, particularly in the hilly areas, has caused soil erosion, compounded by wind and water action. As a result, silt built up in the lake incrementally raises the lake bed.

Within water transported parent material there are several important types. Parent material transported by streams is called alluvium of which there are three main types. Floodplains are the parts of river valleys that are covered with water during floods. Due to their seasonal nature, floods create stratified layers in which larger particles tend to settle nearer the channel and smaller particles settle nearer the edges of the flooding area.

Except for the eastern fringes of Chopra CD Block, most of the district is a part of the catchment area of the Mahanada and also a part of the larger Barind Tract. The soil is composed of different varieties of alluvium. The main rivers are: Nagar, Mahananda, Kulik, Gamari, Chhiramati (Srimati) and Tangon. The rivers have little water in the dry season but with heavy rains, during monsoon, overflow the banks.

Sedimentary rock such as alluvium, clay, limestone, and sandstone forms the greatest share of the Far North's geology. These deposits follow the province's rivers, such as the Logone and Mayo Tsanaga, as they empty into Lake Chad to the north. At the province's south, a band of granite separates the sedimentary area from a zone of metamorphic rock to the southwest. This latter region includes deposits of gneiss, mica, and schists.

The Arkansas River Floodplain ecoregion is characteristically veneered with Holocene alluvium and includes natural levees, meander scars, oxbow lakes, point bars, swales, and backswamps. It is lithologically and physiographically distinct from the surrounding uplands of the Arkansas Valley. Mollisols, Entisols, Alfisols, and Inceptisols are common; the soil mosaic sharply contrasts with nearby, higher elevation ecoregions where Ultisols developed under upland oaks, hickory, and pine. Potential natural vegetation is southern floodplain forest.

In contrast to the eastern part, the western part is made up of new alluvium and in this part River Kalindi joins the Mahananda River. The part of Malda lying to the north of river Kalindi is known as tal. This is a lowland and covered with swamps and beels (small water bodies). Whereas the area south of the Kalindi is a very fertile land and is known as diara.

The major rivers of this system are the Ganga and the Indus along with their tributaries; Beas, Yamuna, Gomti, Ravi, Chambal, Sutlej and Chenab. The Indus-Ganga belt is the world's most extensive expanse of uninterrupted alluvium formed by the deposition of silt by the numerous rivers. The plains are flat and mostly treeless, making it conducive for irrigation through canals. The area is also rich in ground water sources.

Glacial till, alluvium, sandstone, and shale can be found in its vicinity. Its course has been altered by glaciation and it is in the vicinity of North Mountain. At least one bridge has been built over the creek and a number of hunting cabins and cottages existed in the area. The creek's discharge has a 10 percent chance of reaching 915 cubic feet per second in any given year.

The more than 100 trackways, made up of more than 1500 individual footprints, were made by both biped and quadruped dinosaurs. The tracks occur in limestone of the Jurassic Morrison Formation. The site formed along the shore of a large freshwater lake at the time the tracks were made. A previously unmapped region was discovered in 2012, where removal of alluvium revealed 90 new trackways, showing parallel prints.

The Lea and Hackney Marshes are underlain by alluvium soils; and the higher ground between Homerton and Stamford Hill is formed on a widening bed of London Clay. Brickearth deposits are within tongues of clay extending beneath Clapton Common, Stamford Hill and Stoke Newington High Street. The centre and south western districts lie on river terrace deposits of Taplow Gravel. Victoria Park and Well Street Common lie on flood plain gravel.

Except for the eastern fringes of Chopra CD Block, most of the district is a part of the catchment area of the Mahanada and also a part of the larger Barind Tract. The soil is composed of different varieties of alluvium. The main rivers are: Nagar, Mahananda, Kulik, Gamari, Chhiramati (Srimati) and Tangon. The rivers have little water in the dry season but with heavy rains, during monsoon, overflow the banks.

The lowland valleys of the Albane and Bèze consist of recent carbonate alluvium in the Bèze basin but clayey-silty soil in the Albane basin. The upstream part of the Bèze basin is fed by an important karst network replenished in part by losses from the Tille and the Venelle rivers. Some rainwater supplies these aquifers. The source of the Bèze is the outlet of this important network.

The modern Egyptian fellahin calculate the agricultural seasons, with the months still bearing their ancient names, in much the same manner. The importance of the Nile in Egyptian life, ancient and modern, cannot be overemphasized. The rich alluvium carried by the Nile inundation was the basis of Egypt's formation as a society and a state. Regular inundations were a cause for celebration; low waters often meant famine and starvation.

According to the United States Geological Survey, Brownsville's soils are primarily alluvium and windblown deposits. The majority of the city's soil is made of floodplain deposits from the Rio Grande river; it consists of clay, sand, silt, gravel and organic matter. Windblown deposits are made up of "active dunes and dune complexes" that contain mostly clay and silt near the coastal region and combination of clay, sand and silt inland.

Little Wapwallopen Creek in its upper reaches looking upstream The elevation near the mouth of Little Wapwallopen Creek is above sea level. The elevation of the creek's source is approximately above sea level. The course of the creek is tortuous. Alluvium, which consists of stratified sand, silt, and gravel, as well as some boulders, occurs in the valley of Little Wapwallopen Creek to a depth of or more.

The site is between the River Churn and the disused Thames and Severn Canal. It is on the alluvium and gravels of the Thames floodplain. It is made-up of a number of ancient, unimproved meadows and the old ridge and furrow remains visible. This is one of the largest remaining examples of its type in south- east Gloucestershire, and has been traditionally managed by hay cutting and grazing of stock.

Wet tropical forests in North America span from sea level to an altitude of . They have particular geologic, topographic and soil conditions that characterize them. These characteristics influence biotic structures and relationships and have contributed to the high biodiversity of the ecoregion. The geology of these forests is primarily composed of folded and metamorphic hills, which are covered by a thin layer of alluvium (loose sediments and soil).

The Magic Valley ecoregion, named for the irrigation canals of the Magic Valley that "magically" transformed the region in the early 1900s, is an agricultural valley underlain by alluvium, loess, and basalt flows. Elevation varies from 3,200 to 4,500 feet (975 to 1,372 m). The aridic soils require irrigation to grow commercial crops. Many canals, reservoirs, and diversions supply water to the region's pastureland, cropland, and residential, commercial, and industrial developments.

The surficial geology near Shickshinny Creek mainly consists of urban land, fill, alluvium, alluvial terrace, alluvial fan, Wisconsinan Ice- Contact Stratified Drift, Wisconsinan Ice-Contact Delta, Wisconsinan Bouldery Till, Wisconsinan Till, lakes, and wetlands. The lower reaches of the creek are in a water gap between Huntington Mountain and Shickshinny Mountain. A lake known as Shickshinny Lake is in the watershed and is dammed by the Shickshinny Lake Dam.

In the middle reaches of the creek, the surficial geology mainly features bedrock consisting of sandstone and shale, alluvium, and a glacial or resedimented till known as Wisconsinan Till. Some Wisconsinan Outwash and alluvial terrace is also present near Koonsville. Some patches of Wisconsinan Bouldery Till and wetlands are also present. In its upper reaches, the creek is almost entirely dominated by Wisconsinan Till, bedrock, and some lakes.

The creek is located roughly upriver of the Wyoming Valley. All of the bedrock in the watershed of Sutton Creek is made of sandstone. The surficial geology along the floor of the valley of Sutton Creek in its lower reaches mainly consists of alluvium. However, Wisconsinan Ice- Contact Stratified Drift occurs near the creek's mouth and some patches of a till known as Wisconsinan Till occur further upstream.

It is also reported that the sanctuary has been subjected to deforestation due to anthropogenic pressures; with the mining activities permitted after de-notification causing considerable stress on the sanctuary. ;Geology Geological formations in the sanctuary area primarily consist of basaltic rocks on the eastern part, tertiary formation in the central part comprising numimulistic limestone and shale bordering the basaltic rocks in south and up to Lakhpat, recent alluvium in a belt of along the coast and scattered coastal sand dunes are on the western boundary. The area is rich in minerals such as limestone in belt (assessed as 1270 million tonnes) extends from the south Saran Nani village to Lakhpat), lignite in a belt of (15 million tonnes) and bentonite; lignite and bentonite are being mined close to Panandhro and Saran villages, while the mining of limestone is yet to begin. Sandy alluvium, clay and black loam are the soil types identified in the sanctuary area.

After 3.5 ka, however, the delta had built out beyond the embayment and became subject to wave action and marine currents. These deflected deposition south-eastwards in the direction of the Cà Mau Peninsula, which is one of the most recent features of the delta. For much of its length the Mekong flows through bedrock channels, i.e., channels that are confined or constrained by bedrock or old alluvium in the bed and riverbanks.

The two types of rocks found in Santa Cruz are alluvium and clastic rocks. Clastic rocks are located at the eastern portion of the municipality specifically in Barangay Alipit, San Jose, Oogong, Jasaan, San Juan, Palasan, and portions of Barangays Pagsawitan, Patimbao, Bubukal, Labuin and Malinao. These rocks consist of inter-bedded shale and sandstone with occasional thin lenses of limestone, tuff, and reworked sandy tuffs, calcareous sandstone and partly tuffaceous shale.

Karur District is a part of cauvery delta region and utilization of land area in the district is up to 44.59%. 4.76% of the land area remains as uncultivated land, and th e rest 2.74% is forest area in Karur district. Black soil is the predominant soil type in this district accounting for 35.51% followed by laterite soil for 23.85% of the total soil cover. The remaining 20.31% is sandy, coastal and alluvium soil.

Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.

Purba Medinipur district is part of the lower Indo- Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.

Geology of Rajasthan, Geological Society of india, Bangalore. According to Heron (1953), the eastern pediplain, occurring between the Vindhyan plateau and the Aravalli hill range, contains a thin veneer of Quaternary sediments, reworked soil and river channel fills. At least two erosional surfaces can be recognised within the pediplain are the Tertiary age. The Vindhyan upland, the adjoining Chambal valley and the Indo-Gangetic alluvial tract (older alluvium) are of Pleistocene to Sub-recent age.

The soil is composed of different varieties of alluvium. The main rivers are: Nagar, Mahananda, Kulik, Gamari, Chhiramati (Srimati) and Tangon. The rivers have little water in the dry season but with heavy rains, during monsoon, overflow the banks. The Nagar River flows in the eastern part of the CD Block and Kulik river flows along the western boundary eastern boundary with Hemtabad CD Block and then though the Raiganj CD Block.

The elevation near the mouth of Nine Partners Creek is above sea level. The elevation near the creek's source is above sea level. The surficial geology inside the valley of Nine Partners Creek in its lower reaches mainly consists of alluvium and fill, although there is a small patch of alluvial fan. The sides of the valley have surficial geology containing a till known as Wisconsinan Till and bedrock consisting of sandstone and shale.

Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.

While regolith refers to all unconsolidated earth materials above the solid bed rock, including transported sediments such as sand or alluvium, residuum is strictly a non transported parent material. However, parent materials formed in place or "in-situ" can further be classified as saprolite or residuum. Residuum differs from saprolite through its structure and degree of weathering. Saprolite is commonly referring to weathered material retaining details or structural features of the bedrock.

Purba Medinipur district is part of the upper Indo- Gangetic Plain and Eastern coastal plains. Topographically, the university can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.

South Branch Bowman Creek (also known as Cherry Run) is a tributary of Bowman Creek in Luzerne County, Pennsylvania, in the United States. It is approximately long and flows through Fairmount Township and Ross Township. The watershed of the creek has an area of . The surficial geology in its vicinity consists of alluvial fan, alluvium, Wisconsinan Ice-Contact Sratified Drift, fill, lakes, Boulder Colluvium, Wisconsinan Till, Wisconsinan Bouldery Till, wetlands, and bedrock.

Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 meters above the mean sea level.

Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.

There are two main types of channels, bedrock and alluvial, which are present no matter the sub-classification. Bedrock channels are composed entirely of compacted rock, with only patches of alluvium scattered throughout. Because the bedrock is constantly exposed it takes much less stream power to carve the channel. The hydraulic force of flowing water can push and pull detached joint blocks out of their initial position and roll or drag them downstream.

It is believed that earlier than 11,000 years ago, alluvium or unconsolidated soil accumulated along a gully. In one area of uneven distribution, dark silt of the lower Domebo Formation also accumulated. Stratigraphic evidence such as two colored clay deposits suggests that the bone bed was disturbed by erosion at least twice before its discovery. It is here that the bones of a mammoth along with projectile points were found buried beneath these deposits.

The first constituted exclusively by alluvium deposits and surface runoff, including lahars, in the form of conglomerates and loamy coarse particulates, such as those in Bom Despacho Velho and Alto do Poente, as well as between Feteiras and Poço Grande. Marine sediments are confined to the older beaches, such as Ponta dos Matos, Ponta da Rocha or Ponta do Castelo. Some, like in Ponta do Castelo, are composed of calcrious fossils dating to the Pliocene.

The elevation near the mouth of Rattlesnake Creek is above sea level. The elevation near the source of the creek is between above sea level. The surficial geology along Rattlesnake Creek near its mouth mainly consists of alluvium. However, some patches of Wisconsinan Ice-Contact Stratified Drift and alluvial fan are present, as are larger areas of a glacial or resedimented till known as Wisconsinan Till and bedrock consisting of conglomerate, sandstone, and shale.

The ecoregion is underlain by unconsolidated glaciofluvial deposits, silty alluvium, silty and clayey marine sediments and glacial till. Bedrock outcrops of Mesozoic and Palaeozoic origin form rolling hills up to about 310 metres above sea level. The Fraser River dominates this lowland. Gleysols, Mesisols, and Humisols are the dominant wetland soils in the region, while Eutric and Dystric Brunisols and some Podzols have developed on sandy to loamy outwash and glacial till in the uplands.

The elevation near the mouth of East Branch Field Brook is above sea level. The elevation of the stream's source is between above sea level. The surficial geology along the lower and middle reaches of East Branch Field Brook mainly consists of alluvium, while the rest of the stream's valley has surficial geology consisting of a till known as Wisconsinan Till. However, near the mouth of the stream, there is a patch of alluvial terrace.

Prior to the excavation of Bhirrana, no Hakra Wares culture, predating the Early Harappan had been exposed in any Indian site. According to the ASI, for the first time, the remains of this culture have been exposed at Bhirrana. This culture is characterised by structures in the form of subterranean dwelling pits, cut into the natural soil. The walls and floor of these pits were plastered with the yellowish alluvium of the Saraswati valley.

Glenelly at PlumbridgeGlenelly River is a river in County Tyrone, Northern Ireland. It flows westwards along the long linear Glenelly Valley to the south of Sawel Mountain, following one of the principal fault-lines in the Sperrin Mountains. The river meanders across a complex, undulating floodplain of alluvium and glacial moraine. The channel has often carved deep ridges within these soft deposits, creating steep, irregular mounds and pockets of peaty marsh on the valley floor.

The lake is part of the Bow River sub-catchment and the Kent River catchment. The surrounding landscape is composed of lakes and swamps with lunettes situated over tertiary alluvium, colluvium and sand with underlying laterite also present. Quaternary swamp and lake deposits are also found within the Frankland district. Small amounts of brackish water can be received from the south western flanks of the Stirling Range that can flow into the lake.

The base of the Kilmersdon Valley is of alluvium deposits. Above this on both sides of all of the valleys is a band of shales and clays from the Penarth Group. These rocks are from the Triassic period. The majority of the remaining upland in this area is Lias Limestone (white and blue) while the very highest part above 130 m, south of Haydon, is a small outcrop of Inferior Oolitic Limestone.

It lies on the north bank of the River Yeo, from which it gets its name, opposite Limington. The parish is largely flat, lying mostly between and above sea level, on the alluvium of the Yeo and Cam valleys and partly on clay loam on the Lower Lias. Below are the average maximum and minimum temperatures, average rainfall, rain days and sunshine recorded between 1981 and 2010 at the Met Office weather station in Yeovilton.

Hoggett, The Archaeology of the East Anglian Conversion, pp. 1–2. Erosion on the eastern border and deposition on the north coast altered the East Anglian coastline in Roman and Anglo-Saxon times (and continues to do so). In the latter, the sea flooded the low-lying Fens. As sea levels fell alluvium was deposited near major river estuaries and the "Great Estuary" near Burgh Castle became closed off by a large spit of land.

It is native to the Pilbara, southern Kimberley and far northern Goldfields regions of Western Australia where it is found growing in stony soils and gritty alluvium and is often found along creek beds and on rocky hills. The disjunct distribution extends into the top end of the Northern Territory to around the Hooker Creek area where it is often situated on sand plains or rocky slopes as a part of spinifex communities.

The repetition of alluvial deposition (during periods of Quaternary glaciation) and overdeepening (during interglacial periods), known as a fluvioglacial system, led to the formation of several stepped terraces in the lower Isère valley, like the one on which Saint-Marcel-lès-Valence is built. This occurred through the massive accumulation of alluvium from the Isère on top of a bed of Miocene molasse. Today, these terraces still define the geography of the Plain of Valence.

However, it can experience short, high-rate floods on occasion. The surficial geology in the vicinity of the lower reaches of Wadham Creek consists largely of alluvium, with some fill. The surficial geology near the creek's middle reaches consists mainly of alluvial fan and Wisconsinan Ice-Contact Stratified Drift. The surficial geology in the creek's upper reaches features land where coal was once surface mined, with large pits and piles of rock waste.

A 1978 inspection judged the dam to be in good condition. Most of the surficial geology in the vicinity of Huntsville Creek features a glacial or resedimented till known as Wisconsinan Till and bedrock consisting of sandstone and shale. However, Wisconsinan Ice-Contact Stratified Drift occurs in some parts of the watershed, especially in its lower reaches. Alluvium is also found in some areas and there is one patch of sandstone and shale pits.

Further upstream, the surficial geology consists almost entirely of Wisconsinan Till and bedrock, but some fill is present as well. Near the headwaters, there are also small patches of alluvium and Wisconsinan Ice-Contact Stratified Drift, as well as one lake. At one point, Monument Creek flows through an embankment with a depth of approximately . A 36-inch (0.9-meter) water main has crossed Monument Creek, elevated at a height of above the creek.

The sedimentary and metamorphic rocks that are present in the city are alluvium, fluviatile, lacuatine, pludal and beach deposits such as coral, stools, and beach rock. These are predominantly found along the coastal areas of Vigan. An important non-metallic mineral resource found in Vigan is the kind of clay that is used in making earthen jars locally called burnay. Earthenware of different uses and sizes are made of this kind of clay.

East of the San Joaquin Fault in the vicinity of Hospital Creek there is a flow pattern of alluvium that has been reported as a mud flow.C.Michael Hogan, Marc Papineau, Ballard George, et al., Environmental Assessment for the Proposed Residential and Commercial Development at the Westley Interchange, Earth Metrics Inc., Report 10529C, California State Environmental Clearinghouse, Sacramento, Ca., July, 1990 This flow pattern was deposited in the early Holocene or the late Pleistocene.

The rocks are covered by alluvium and lacustrine sediments to a maximum thickness of approximately . The bed of the lake is clay with the formation of some salt and gypsum pans. The Lake Gregory System consists of several interconnected waterbodies and is fed primarily by Sturt Creek. The creek has a catchment area of approximately and flows north to south as a single channel until a short distance south of Halls Creek.

The Coongan River is an ephemeral river in the Pilbara region of Western Australia. The headwaters of the river rise below the Chichester Range. The river flows in a northerly direction past Marble Bar then through the Gorge Range before discharging into the De Grey River, of which it is a tributary, at Mulyie Pool near Mount Woodhouse. The town of Marble Bar also draws approximately 180ML scheme water from the river's alluvium per year.

Changes in the concentration of nitrogen in the will affect the growth performance of K. serotina; however, limited information is known about the species' soil nutrient requirements. The plant can tolerate dry soil conditions, twhichhat enables it to perform better than native forest. According to Olsen, it is found in areas where the soil is free-drained, with different soil types, from sand and loam to alluvium, sedimentary and ultra- mafic rock.

Throughout the Navarro watershed, recent alluvium, stream channel, and terrace deposits provide groundwater recharge to surface streams and supply wells and springs. Only minor amounts of groundwater are contributed by the Franciscan Formation. Flows dry up in tributaries during summer months, with the only surface water present derived from springs. Only the mainstem Navarro River, North Fork Navarro River, and lower reaches of Anderson, Rancheria, and Indian Creeks contain year-round surface water.

This can be further classified as a strath terrace—a bedrock terrace that may have a thin mantle of alluvium—if the river is incising through bedrock. These terraces may be dated with methods such as cosmogenic radionuclide dating, OSL dating, and paleomagnetic dating (using reversals in the Earth's magnetic field to constrain the timing of events) to find when a river was at a particular level and how quickly it is downcutting.

Large basaltic rock formations exists throughout Vidarbha, part of the 66-million- year-old volcanic Deccan Traps. Bhandara and Gondia district are entirely occupied by metamorphic rock and alluvium, making their geology unique in Maharashtra. Buldhana has the Lonar crater created by impact of an asteroid. The eastern districts of Gondia, Bhandara, Gadchiroli and Nagpur are in earthquake zone 1, which has the least seismic activity in India, while other districts are in zone 2.

The economy of Katwa is based on agriculture and agro-related trades. The fertile soil of the surrounding areas is enriched by the alluvium from the Hooghly, Ajay and Damodar rivers. The major crops that are farmed in the countryside surrounding Katwa include rice, jute, mustard, sugarcane and various tropical vegetables. Katwa is an important center for marketing the region's agricultural products and for providing retail and consumer services to the surrounding population.

Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.

The Turlock Lake Formation is an Early Pleistocene geologic formation in the Sierra Nevada foothills in Sacramento County, California. Cities in/over the formation's area include Citrus Heights, Carmichael, and Roseville.California Geological Survey: Geologic Map of the Sacramento Quadrangle The Turlock Lake Formation is a fan deposit of dominantly granitic alluvium covering the westward extension of the North Merced Pediment and Gravels formation, and directly overlying the Mehrten Formation. California Division of Mines and Geology.

Located in central Ibaraki Prefecture, approximately north of Tokyo, Tōkai is bordered to the east by the Pacific Ocean. The village is about 15 kilometers northeast of the prefectural capital of Mito. with the Kuji River to the north. The area is located at the northern end of the Hitachi Plateau, and consists of lowlands which are alluvium and covered with rice paddy fields, and the plateau is diluvial, with upland fields and flatland forests.

Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.

Most of the valley floor is a deep fill of alluvium that is up to thick in the deepest portions. From the valley floor, steep hills rise abruptly to the canyon rim in less than . These hills are dissected by many steep and short side canyons. The major branch of Aliso Canyon is Wood Canyon, a -long, -deep gorge that runs generally southward to join Aliso Canyon about upstream of the ocean.

The Kankakee Outwash Plain (southern Lake, Porter, and LaPorte counties) is a flat outwash plain formed by the melting glacier, which was stopped at the Valparaiso Moraine. (Mickelson and others, 1984). Deposits are predominantly sand and gravel, but also include alluvium and fill materials. Deposits average less than 200 ft thick; in the lowlands they can be less than 50 ft thick, while in the upland they can be more than 200 ft thick.

Soils washed from slopes were deposited in valley bottoms as a rich, swampy alluvium. These new environments were then exploited to develop intensive, irrigated fields. The change from shifting cultivation to intensive irrigated fields occurred in association with a rapid growth in population and the development of elaborate and highly stratified chiefdoms (Kirch 1984). In the larger, temperate latitude, islands of New Zealand the presumed course of events took a different path.

A mountain known as Wilkes-Barre Mountain is also in the upper reaches of the watershed. The surficial geology in the vicinity of Warrior Creek mainly consists of strip mining land, urban land, a glacial or resedimented till known as Wisconsinan Till, and bedrock consisting of sandstone, shale, coal, and conglomerate. The bedrock mainly occurs near the creek's middle and upper reaches. There are also a few patches of alluvium and fill.

The elevation near the mouth of Tinker Creek is above sea level. The elevation near the creek's source is above sea level. The surficial geology along Tinker Creek in its lower reaches mainly includes a till known as Wisconsnain Till. Further upstream, the surficial geology along the creek consists mostly of alluvium, though there are various patches of Wisconsinnan Till, Wisconsinan Ice-Contact Stratified Drift, wetlands, lakes, and bedrock consisting of sandstone and shale.

Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.

As with the surrounding area, soil and rock formations on Webb Hill are red in appearance due to the presence of iron oxide.' Although portions of the older section of the city of St. George (particularly the southern part near the Virgin River) lie on floodplain alluvium, much of the city is built directly upon Jurassic, Triassic, and Permian period sedimentary bedrock. This includes Webb Hill. At its highest point, the hill reaches in elevation.

The elevation near the mouth of Butler Creek is above sea level. The elevation near the creek's source is above sea level. The surficial geology along Butler Creek near its mouth mainly consists of alluvium, although there is one patch of alluvial fan nearby. The sides of the valley are lined with a till known as Wisconsinan Till and there are some patches of bedrock consisting of sandstone and shale on nearby hills.

The surficial geology near the lower reaches of the stream mainly consists of alluvium (which contains stratified sand, silt, and gravel, as well as some boulders) and coal dumps. Further upstream, the surficial geology mostly features land that has been surface mined for coal, with some coal dumps to the east. Near the headwaters of the stream, there is surface mining land as well as a glacial or resedimented till known as Wisconsinan Till.

The soils are wet, alluvium and peat overlying Hercynian granite bedrock. Since grazing was withdrawn some of the marsh is overgrown with abundant common reed (Phragmites australis), rushes (Juncus sp) and grey willow (Salix cinerea). The drainage ditches, flow southward to Old Town Bay and divide the marsh into wet meadows with abundant soft rush (Juncus effusus), yellow iris and some ragged robin (Lychnis flos- cuculi) and greater bird’s-foot trefoil (Lotus pedunculatus).

Perched water tables in the basalt aquifers have contributed to increased well irrigation, which accounts for approximately 55% of the irrigable water. The granitic-gneissic terrain in the eastern hilly area of Vidarbha accounts for all tank irrigation. Tube- wells in the Tapi-Purna alluvium and shallow wells in the coastal sands are the other main sources of water. Special wells are being made by the Government for the villages lacking water.

338 The Alsatian Plain is flat and offers an attacker practically no cover other than occasional woods. The plain is also a drainage basin for the RhineDe Lattre, pp. 337-338 and is consequently cut by many streams and drainage canals with alluvium-coated bottoms, making them treacherous for vehicles to ford. Dotting the plain are small villages made up of sturdy masonry houses whose multi-storey construction offered defending troops a commanding view of the surrounding fields.

Large areas of strip mining land occur to the north of its valley. In its lower reaches, the surficial geology of the creek mostly features Wisconsinan Bouldery Till and Wisconsinan Ice-Contact Stratified Drift, which contains stratified sand and gravel along with some boulders. Wisconsinan Outwash, alluvium, alluvial terrace, fill, and coal dumps (large piles of coal waste) also occur near the creek's mouth. The valley of Turtle Creek is a deep and narrow strike valley.

Most part of this basin comprises rolling and undulating country except the western border which is formed by an unbroken line of ranges of the Western Ghats. The important soil types found in the basin are black soils, red soils, laterite and lateritic soils, alluvium, mixed soils, red and black soils and saline and alkaline soils. An average annual surface water potential of 78.1 km³ has been assessed in this basin. Out of this, 58.0 km³ is utilisable water.

Camp Pico Blanco is at elevation on the North Fork. Upstream tributaries include Jackson Creek, Pine Creek, Puerto Suelo Creek, and Comings Creek. A small creek enters the Little Sur River via a waterfall at the location of the seasonal reservoir in the camp proper. The immediate camp environment consists of seven distinct biotic habitats: coast redwood/mixed evergreen forest, white alder riparian woodland, herbaceous vegetation, aquatic habitat, bare alluvium, bare ground, and Sur Complex bedrock.

Swarupnagar is located at . Swarupnagar CD Block is bounded by Gaighata CD Block in the north, Kalaroa Upazila in Satkhira District of Bangladesh in the east, Baduria CD Block in the south and west, and Habra I CD Block in the west. Swarupnagar CD Block is part of the Ichhamati-Raimangal Plain, one of the three physiographic regions in the district located in the lower Ganges Delta. It contains soil of mature black or brownish loam to recent alluvium.

Rocks originating in the Carboniferous period are largely restricted to that part of the county to the east of the Red Rock Fault. They comprise mudstones, siltstones and sandstones of the Lower Coal Measures and of the Millstone Grit Group. A very small outcrop of Carboniferous Limestone formerly occurred near Astbury though this has largely been removed by quarrying. Coal Measures strata also occurs in the Neston area though it is obscured by glacial till and estuarine alluvium.

The Burstwick Drain extends for just over and drains an area of . Due to the agricultural nature of the land that it drains, the surface run-off from fields has contributed to the river's poor ecological status. The underlying geology of the region that the watercourse drains is glacial gravels, marshes and estuarine alluvium. The extreme western end of the haven has been the subject of many studies and is part of a local development order.

Virtually all groundwater in much of Cameroon is sourced from a combination of thin layers of unconsolidated alluvium, laterite soils and underlying fractured Precambrian crystalline basement rock, between eight and 20 meters thick. Small springs, including some thermal springs are found in the fractured bedrock around volcanoes. Cenozoic sediments from the Pliocene and the Quaternary form a key aquifer in the Douala Basin. During the dry season, the water table sometimes falls resulting in seawater intrusion.

Fimbristylis cymosa, commonly known as tropical fimbry, or St. John's sedge, is a sedge of the family Cyperaceae that is native to Australia. The rhizomatous perennial grass-like or herb sedge typically grows to a height of . It blooms between February and September and produces brown flowers. In Western Australia it is found near the coast, on dunes and behind mangroves in the Kimberley region where it grows in sandy-clay alluvium around basalt or sandstone rocks.

The area consists of bajadas (extensive flat aprons of alluvium) and the massive, fault-lifted Old Woman Mountains that extend some north-south and up to in an east-west direction. The elevations within the wilderness range from in the drainage bottoms to over at the top of Old Woman Peak. The mountains take their name from a granite monolith resembling the figure of an old woman, known as the Old Woman Statue (5,000 feet high).

One stated that fresh water carries salt from clay particles which is found abundantly in shale and mudstones. The soils at Bario are derived from accreting and non-accretin alluvium, consists of poorly drained clays, podzolic sands, and organic soils. Water-logged soils are suitable for rice cultivation, while better drained non-accreting alluvial soils are suitable for vegetables and citrus fruit cultivation. Bario valley has frequent flash floods because of steep mountain ranges and high surface runoffs.

The surficial geology consists of coal dumps, surface mining land, alluvium, Wisconsinan Outwash, Wisconsinan Till, urban land, and bedrock. The watershed of Nanticoke Creek is mainly forested, but urban land and mining land are also present. The city of Nanticoke is partially in the watershed and many unincorporated communities are there as well. The creek is named after the Nanticoke tribe, but was historically known as Muddy Run before appearing on maps with its present name by 1776.

Within the dam's fill, there were layers of organic residual soil that in one area contained a tree stump. The residual soil was used as foundation and in layers as well – above alluvium. This suggests that the foundation for the dam was not prepared properly, according to the study. In addition, the reservoir's auxiliary dam suffered a severe slope failure on its upstream face while areas around the rim of the reservoir had mild slope failures or distress.

Most LS is generated on highlands by erosional processes related to mass-wasting, sheet flow, rills and gullies. The deposited colluvium has a low travel distance and accumulates in midslope drapes near the site of erosion, in aprons or sediment wedges at the base of the slope or in fans at the mouth of gullies, debris flows and tributaries. Floodplains store alluvium through lateral and vertical accretion, i.e. bedload deposits are being incorporated into the floodplain.

Furthermore, early emphasis on genetic soil profiles was so great as to suggest that material lacking a genetic profile, such as recent alluvium, was not soil. A sharp distinction was drawn between rock weathering and soil formation. Although a distinction between these sets of processes is useful for some purposes, rock and mineral weathering and soil formation are commonly indistinguishable. The concept of soil was gradually broadened and extended during the years following 1930, essentially through consolidation and balance.

According to Thirumoorthy, the shrine is "the biggest brick temple complex dating to the pre-Pallava period". The temple is built on a cushion of alluvium on which a layer of man-made bricks were laid. On top of this were another four layers of man-made bricks separated by four layers of laterite. There were two types of bricks used: large-sized laterite bricks of the Sangam period and thin, tabular bricks of a later age.

About the Mountain: Topography and Climate , San Bruno Mountain Watch (nd). The foothills and eastern flanks of the range are composed largely of poorly consolidated Pliocene-Quaternary freshwater and shallow marine sediments that include the Colma and Merced Formations, recent slope wash, ravine fill, colluvium, and alluvium. These surficial deposits unconformably overlay the much older Jurassic to Cretaceous-aged Franciscan Assemblage. An old landfill about 135 deep existed at the site developed by the mixed-use Metro Center.

The soils of the Cotati area are characterized by recent alluvial materials, explicitly those areas bordering the Laguna de Santa Rosa and its tributary Washoe Creek. These materials are largely stream and valley alluvium, with artificial fill in some areas. Active faults near Cotati include the Rodgers Creek Fault ( east) and the Tolay Fault. To the west of Cotati are wetland habitat for Sebastopol meadowfoam, Pitkin Marsh lily, Showy Indian clover and several other endangered species.

This was a sheet of chalk covered by brickearth covered with topsoil. Over the last two millennia, much of this was stripped away, or mined, so the contours have constantly changed. Through the centre of this ran a shallow valley carrying a stream draining the Hoo Peninsula behind, through Islingham to Whitewall creek where it entered the Medway. This water flow formed a river meander upstream and a build up of alluvium pushing 1,000 yds into the river.

The bedrock of the area is rock from the Sherwood sandstone group. There are a few outcrops of sandstone but elsewhere the bedrock is covered by drift. Most of this consists of till except near the bank of the Mersey where it is recent alluvium. When borings were made in the 1870s prior to the building of chemical works a deep gorge measuring around 100 feet (30 m) was found in the bedrock which was filled with glacial deposits.

The Bell Canyon Creek watershed has three distinct areas with different levels of groundwater percolation. On mountainous slopes, which comprise about 65% of the watershed, the percolation rate is relatively low and produces a moderate amount of runoff during storms. On the deep alluvium of the valley floors, however, water soaks into the ground and flows subsurface into San Juan Creek. This area is the site of a thick riparian zone and produces little storm runoff.

The citation for the SSSI says: > Trodds Copse Site of Special Scientific Interest comprises ancient semi- > natural woodland, unimproved meadows and flushes overlying Bracklesham Beds, > Bagshot Sand, peat and alluvium. The habitats are drained by tributaries of > the Monks Brook, a branch of the River Itchen. The diverse geology and > varied drainage conditions give rise to a wide range of habitats. At least > ten woodland types can be identified, of which four are considered > nationally rare.

The Victoria County History in Nottinghamshire describes West Leake's geography as follows: > The portion of West Leake along the Kingston brook is alluvium with sand and > gravel. To the north east and west of the village are areas of gypsum, with > clay and limestone in the eastern part. The village lies about 150 feet > above sea level. The land rises to over 300 ft to the north-east and 200 ft > to the west at Moulter Hill.

The geology of the area is dominated by Pilliga sandstone, a coarse red to yellow Jurassic sandstone containing about 75% quartz, 15% plagioclase and 10% iron oxide, although local variations in soil type do occur. Sandstone outcrops with basalt-capped ridges are common in the south, while the Pilliga outwash areas in the north and west are dominated by alluvium from flooding creeks. Gilgais occur in some areas. In the west "sand monkeys" (abandoned creek beds) are common.

Two distinct volcanic phases are recorded at Negra Muerta, the first 9 million years ago and the second 7.6-7.3 million years ago. Each phase was associated with a pulse in caldera formation. Non-volcanic processes later in the caldera history include the deposition of alluvium and glacial till. The Acay ignimbrite was erupted 9 million years ago and covers a surface area of outside of the caldera, but some material is also found within the caldera.

However, a till known as Wisconsinan Till is found nearby in larger areas, and some bedrock consisting of sandstone and shale is also present. Additionally, there is one wetland patch nearby. The surficial geology in the creek's headwaters is fairly similar, but there is no alluvium above Lake Chrisann, only Wisconsinan Till. Soils in the vicinity of Hop Bottom Creek include Wyalusing silt loam, Holly silt loam, Wellsboro channery silt, and Lordstown and Oquaga stony silt loams.

The bog lies in the heart of the Forest of Dean, and is separated from the Woorgreens Lake and Marsh nature reserve by the B4226. The site has been a nature reserve since 1977, and represents the remains of an ancient acid bog which historically covered this area. This is one of the rarest habitats in the county. It is in the Coal Measures (in a depression), is on alluvium and fed by a stream from the north.

The Ware Formation overlies the Castilletes Formation and is overlain by Quaternary alluvium. The age has been estimated to be Late Miocene to Early Pleistocene (5.2 to 1.22 Ma), Uquian, Chapadmalalan and Montehermosan in the SALMA classification, with a narrow definition in the Pliocene (3.5 to 2.8 Ma). The marine invertebrate fauna of the Ware Formation shows a greater similarity with modern assemblages offshore of the Guajira Peninsula than with those of the underlying units.Moreno et al.

A small islet lies shortly upstream of the dam, where the James River previously split into two channels. The dam and reservoir rest on a wide plain of shale where the James River cut a canyon up to wide and deep. The shale (called Pierre Shale) has a dark gray, bedded appearance, and is mostly claystone or siltstone. The valley also contains many traces of alluvium, mainly deposited during the last ice age when the area was heavily glaciated.

The elevation near the mouth of Broad Hollow Run is above sea level. The elevation near the source of Broad Hollow Run is between above sea level. The surficial geology near the mouth of Broad Hollow Run consists of alluvium (which contains stratified sand, silt, gravel, and some boulders) and a till known as Wisconsinan Till. Further upstream, the surficial geology consists of Wisconsinan Till and alluvial fan, some of which is underlain by glacial lake clays.

Radstock lies on the Wellow Brook which then runs through Wellow to join the Cam Brook at Midford to form Midford Brook before joining the River Avon close to the Dundas Aqueduct and the remains of the Somerset Coal Canal. The base of the valley is of alluvium deposits. Above this on both sides of all of the valley is a band of shales and clays from the Penarth Group. These rocks are from the Triassic period.

India is a union of 28 states and 8 union territories. As of 2011, with an estimated population of 1.2 billion, India is the world's second most populous country after the People's Republic of China. India occupies 2.4% of the world's area and is home to 17.5% of the world's population. The Indo-Gangetic plains have one of the world's biggest stretches of fertile flat-deep alluvium and are among the most densely populated areas of the world.

The water volume of the lower course of the river diminishes as a result of extensive evaporation and water-diversion schemes. The Tarim's low-water period is from October through April. The spring and summer high waters begin in May and continue through September as the snows melt on the distant Karakoram, Tian Shan and Kunlun mountains. The Lower Tarim Basin is an arid plain composed of alluvium and lake sediments and is bordered by massive mountain ranges.

This has lowered the depth of the streambed to a few feet in locations where it was considerably deeper at times during the 20th century. Chief Gathering, LLC has an erosion and sediment control permit involving the stream. The surficial geology in the vast majority of areas near Trout Brook features a glacial or resedimented till known as Wisconsinan Till and bedrock consisting of sandstone and shale. However, there is also an area of alluvium near its mouth.

Vine-planted parcels are rather steep and climb up to 478 m height (near Osenbach). The lower part of the slopes consists of layers of limestone or marl covered by loess where the slope is rather smooth. The plain consists of a thick layer of alluvium deposited by the Rhine (silt and gravel). This zone is more fertile than the others, with an important aquifer close to the surface (less than 5 m deep): the Upper Rhine aquifer.

The Mississippi Alluvial Plain extends along the Mississippi River from the confluence of the Ohio River and Mississippi River southward to the Gulf of Mexico; temperatures and annual average precipitation increase toward the south. It is a broad, nearly level, agriculturally- dominated alluvial plain. It is veneered by Quaternary alluvium, loess, glacial outwash, and lacustrine deposits. River terraces, Swales, and levees provide limited relief, but overall, it is flatter than neighboring ecoregions in Arkansas, including the South Central Plains.

The larger part of Angola's income derives from oil production and by 2008 the country was Africa's second largest producer of crude petroleum. Angola is also the fourth largest producer of diamonds in Africa. Diamonds are obtained both from alluvial deposits and from the hundreds of kimberlite pipes which are scattered along a northeast – southwest line through Angola. The country is also a gold producer, the most important source being alluvium originating from Archaean greenstones dominantly around Cabinda.

Further upstream, the alluvium continues and is flanked by alluvial fan, Wisconsinan Ice-Contact Stratified Drift, Wisconsinan Till, and bedrock consisting of sandstone and shale. The surficial geology near the stream's headwaters features Wisconsinan Till and bedrock. In the Holocene Period, sediment from Roaring Run has forced Bowman Creek's channel to remain on the south side of its valley. This causes Bowman Creek to cut into bedrock, forming Evans Falls downstream of the mouth of Roaring Run.

These pectolite cavity fillings are a secondary occurrence within the volcanic flows, dikes, and plugs. When these rocks erode, the pectolite fillings are carried down the slope to end up in the alluvium and the beach gravels. The Bahoruco River carried the pectolite-bearing sediments to the sea. The tumbling action along the streambed provided the natural polishing to the blue larimar, which makes them stand out in contrast to the dark gravels of the streambed.

The beaches surrounding the trail terminus are composed of a variety of different rock types and formations. The rich mixture is a result of the combined erosive power of the ocean and relatively recent glacial activity. According to the Washington State Department of Natural Resources, the area's sediments are classified as Unconsolidated Deposition, translating to the geological equivalent of a grab bag. More finely, the deposits are listed as "Quaternary Sediments, Dominantly Glacial Drift, includes alluvium".

The Kurzeme Formation gray calcareous material is widespread, left from the most extensive period of glaciation. The last interglacial is marked by the Felicianova Formation alluvium, overlain by Baltic group sediments from the last glacial advance. Glacial retreat and oscillation took place from 25,000 to 12,000 years ago, leaving the 90 meter Latvia Formation, including the Jelgava Member lacustrine deposits. Major spillways drained the landscape, emptying the Baltic Ice Lake which flooded much of the region.

Formerly a deciduous forest dominated vegetation in the downstream part of the watershed of the Croche river, because the soil was rich in alluvium. In the late nineteenth and early twentieth centuries, the watershed of the river was cleared to make way for agriculture. Several farms were established. Despite its shallow depth, the river was used to float logs to feed sawmills and pulp mills located in the La Tuque and downstream on the Saint-Maurice River.

After the sandstone was deposited, the region experienced folding and faulting, and was submerged in a shallow sea. This allowed the creation of fossiliferous limestone roughly 390 million years ago, specifically the Rondout Formation and New Scotland Formation. The Rondout Formation's dolomite member, formed during the upper Silurian, was mined throughout the village because of its ability to form natural cement. The region experienced repeated glaciation, and large amounts of till and alluvium were deposited during the Wisconsonian glaciation.

'Wingham' has excelled in the UK where planted on fertile alluvium in river valleys, but has struggled on poorer chalk and clay soils, emulating the 'English' Elm U. minor 'Atinia'. At the Castellaccio trials site in Italy, specimens increased in height by up to 1.94 m per annum, with a commensurate increase in girth of 2.84 cm. The clone is not known elsewhere beyond Italy in continental Europe, and has not been introduced to North America or Australasia.

They all pass through forested country on Middle Jurassic geology. Shortly after, they pass into the department of Yonne. Near the border between the departments and just below Ravières, the river passes onto the Upper Jurassic where the valley bottom has accumulated Holocene alluvium. However, the Upper Jurassic rocks are available to supply the clay element of the materials for the cement works which lie between the river and the canal between Pacy-sur-Armançon and Lézinnes.

Balzac occupies the interior of a wide bend of the Charente. The bedrock of the large eastern half of the commune, which is the highest in altitude, consists of limestone dating from the Upper Jurassic (Kimmeridgian) period. The centre of the town, between Labbés, Genin, and Texier, is located on old alluvium from the Quaternary period. The western part of the commune, between La Chapelle and Chabots, contains other alluvial deposits which form a low terrace.

Alluvial fans are sedimentary areas formed by narrow valley streams that suddenly drop to lowlands and widen dramatically. Sedimentary in these types of deposits tend to be larger closer to the uplands and finer near the edges of the fan. Delta deposits, the third of type of alluvium, are finer sediments that are discharged from streams into lakes and eventually settle near the mouth of the river. Lake deposited parent material is called lacustrine parent material.

The west dam of Diamond Valley Lake Construction of the three dams was completed in 1999, requiring the excavation of of foundation material. The earth fill dam project required about of sand, clay and rock. Much of the materials needed were obtained from the project area. Core materials were obtained from the silty and clayey sandy alluvium in the floor of the reservoir and the rock fill came from the bedrock highlands of the reservoir's south rim.

Soil in Hanworth varies between gravel close to the surface and a clay-rich loam, with very narrow belts of alluvium closest to the streams. The land is relatively flat and drained by two watercourses heading southward and eastward respectively to meet the Thames in neighbouring historic parishes, the River Crane marking much of the northern border with Twickenham and the Port Lane stream matching approximately the western boundary. Elevations range from 11m to 16m OD.

The geology of the area consists of Alluvium, Oxford Clay and River Gravels. The land is generally fairly flat and low lying. It is surrounded by lakes created from disused gravel extraction sites, forming parts of the Cotswold Water Park and several have now been designated as Sites of Special Scientific Interest and nature reserves. The Edward Richardson & Phyllis Amey nature reserve consists of marsh and reedbeds which attract dragonflies and birds such as heron and great crested grebe.

The species is native to many tropical areas. In Australia it is native to Western Australia where it is found along streams and creeks in the Kimberley region growing in sandy-clay alluvium. It is also found across the top end of the Northern Territory and both Cape York Peninsula and north east Queensland. The species is also native in parts of Africa including the Democratic Republic of the Congo, Côte d'Ivoire, Kenya; Madagascar; Mali, Senegal and Tanzania.

When the Wisconsinian era ended, the glaciers melted and sea levels rose or so to their present level. Water backed up into Aliso Canyon and Wood Canyons, turning them into salt-water inlets. Over time, the creeks deposited enough sediment to fill the inlets with alluvium and create the present-day valley floor. This is the reason why the canyon resembles an aged U-shaped glacial valley instead of a relatively young V-shaped river valley.

A closer view of the cave Although it is referred to as a "cave", Mummy Cave is actually a broad, shallow alcove in a vertical cliff. It owes its depth to its overall size and the stability of the parent rock. The alcove's roof is about above the river, with the rock floor of the alcove at about above the river. By the time it was discovered, the alcove had been almost entirely filled with alluvium.

The headwater streams of these concave valleys are still in a youthful phase of active down-cutting. The places soils are derived from granite, basalt, or alluvium (stream overflow and slope wash deposits) and colluvium (scree processes). Differences in soil properties are a product of underlying parent material and landscape position. The main rainforests in the region occur astride three major geomorphic regions: the tablelands of the Great Dividing Range; the lower coastal belt; and the intermediate great escarpment.

Wadenhoe Marsh and Achurch Meadow is a 47.5 hectare biological Site of Special Scientific Interest south of Wadenhoe in Northamptonshire. This complex site on both sides of the River Nene has a variety of habitats and a diverse range of fauna and flora. The west of the river is alder woodland and marshy grassland. On the east there is the largest example in the county of unimproved grassland on alluvium and gravel, with over 100 flowering plant species.

The elevation near the mouth of Idlewild Creek is above sea level. The elevation near the creek's source is above sea level. The surficial geology along the lower reaches of Idlewild Creek consists mainly of alluvium, although a till known as Wisconsinan Till is more prevalent on the sides of the valley, and occurs along the creek itself at times. There are also a few wetland patches and one patch of Wisconsinan Ice- Contact Stratified Drift.

There is also a patch of alluvium further upstream, just below Little Butler Lake, and patches of bedrock consisting of sandstone and shale on nearby hills. A lake known as Little Butler Lake is situated on Little Butler Creek. It is a former kettle hole bog but was dammed several decades ago to create an open lake. It could return to being a bog within several hundred years, though this process would be expedited by removing the dam.

Wisconsinan Outwash, which consists of stratified sand and gravel, forms terraces along the flank of the valley of Beaver Run. Alluvium also occurs in the surficial geology in the vicinity of the stream, as does Wisconsinan Bouldery Till and a patch of Wisconsinan Ice-Contact Stratified Drift. Further upstream, there is Wisconsinan Till, alluvial fan, and a lake. Bedrock consisting of sandstone and shale occurs in the surficial geology near the stream's valley throughout much of its length.

This change in hydrology dried the historical floodplain, allowing this land to be developed and farmed. Invasive species, such as reed canary grass, once fed the grazing animals on the pastures, but now competes with native shrub and herbaceous plant species. The soil mixes present in North Creek’s floodplain consist of lake and marsh sediment, volcanic ash, floodplain alluvium, and organic deposits. The floodplain also contains stratified layers that suggest standing water and, “marsh to mixed marsh-forested wetland”.

Cut bank erosion and point bar deposition as seen on the Powder River in Montana. A point bar is a depositional feature made of alluvium that accumulates on the inside bend of streams and rivers below the slip-off slope. Point bars are found in abundance in mature or meandering streams. They are crescent-shaped and located on the inside of a stream bend, being very similar to, though often smaller than, towheads, or river islands.

Several of the islands have been joined to the mainland by alluvial deposits. Herodotus says that half of the islands had been already united to the mainland in his time (ii. 10); and Thucydides expected that this would be the case with all of them before long, since they lay so close together as to be easily connected by the alluvium brought down by the Achelous River (ii. 102.). This expectation, however, has not been fulfilled, which Pausanias attributed (viii. 24. § 11) to the Achelous bringing down less alluvium in consequence of the uncultivated condition of Aetolia; but there can be little doubt that it is owing to the increasing depth of the sea, which prevents any perceptible progress being made. The Echinades are mentioned by Homer, who, in the Iliad, says that Meges, son of Phyleus, led 40 ships to Troy from Dulichium and the sacred islands Echinae, which are situated beyond the sea, opposite Elis.Homer Iliad ii. 625. Phyleus was the son of Augeas, king of the Epeians in Elis, who emigrated to Dulichium because he had incurred his father's anger.

Older volcanic activity occurred in the field during the Oligocene and Miocene, generating calderas (usually large craters formed by the explosion or collapse of a volcano) such as the Central Nevada Caldera Complex and the Lunar Lake caldera which underlies much of the northern Lunar Crater volcanic field. The volcanism produced ignimbrites, andesitic lavas and tuffs such as the 24 million years old Buckwheat Rim Tuff that Lunar Crater is embedded in; some of these volcanic rocks form structural blocks such as the Citadel Mountain block and the Pancake Range and others are correlated to ignimbrite sheets elsewhere in Nevada. An early caldera-forming ignimbritic phase was followed by an andesitic lavic phase, and in the last 11 million years basaltic eruptions have taken place in the Basin and Range. These older volcanics also form the basement (underground rock surface) in the area, while parts of the region are covered by alluvium (sediment that was transported by water); sometimes the older volcanics are buried beneath this alluvium and playa deposits.

Three strong storms hit the north of Vietnam in 2005 (28 July one wind with level 7, 18 September with level 9 and on 28 September with level 12). There are two types of soil formed from the alluvium of the Red River. One is alluvial mud (which becomes loam) and one is sand. Transported by water the alluvial forms the coastal soil like light soil (sand and light loam and pure sand), medium soil and heavy soil (loam and clay).

It would be another two years before the Commonwealth Government became involved, with the establishment of a joint CSIR and Western Australia Department of Agriculture facility. As the Carlton Reach, Ord River experimental station site was river alluvium (red soil) and most of the surveyed agricultural land was "Cununurra Clay" (blacksoil - Volcanic soil eroded from the Antrim Plateau Volcanics), it was moved to a new site further down river and the new Kimberley Research Station (KRS) was established in 1946.

The elevation near the mouth of East Branch Roaring Brook is above sea level. The elevation near the source of the stream is between above sea level. The surficial geology in the vicinity of the lower reaches of East Branch Roaring Brook alluvium, Wisconsinan Ice-Contact Stratified Drift, bedrock consisting of conglomeratic sandstone and sandstone and shale, fill, and sand and gravel pits. Further upstream, the surficial geology mainly consists of a glacial or resedimented till known as Wisconsinan Till.

Olmos River (Río Olmos), is a river in the Lambayeque Region in northwestern Peru., United States National Geospatial-Intelligence Agency It flows off the west slopes of the Andes and its tributaries, such as Los Boliches, carry little additional water. As a result, it is a low flow stream, intermittent in its lower reaches only flowing during the rainy season (mid November to mid April). Before it can reach the Pacific Ocean it disappears into the alluvium of the Sechura Desert.

South of the Save River, unconsolidated sediments are an important source of groundwater, overlying the Mozambique Basin. A 30 kilometer wide belt of dune sands occupies the southern coast of the country, atop Cretaceous and Paleogene rocks and form a moderately productive unconfined aquifer. Thick alluvium in the Limpopo River and Incomati River valleys forms a major aquifer in high porosity sands north of Maputo. Marine and continental sandstones dominate deeper Cretaceous- Paleogene sedimentary aquifers and some also contain layers of limestone.

The surficial geology along most of Reyburn Creek features alluvium. However, Wisconsinan Outwash occurs along the creek in its lower and middle reaches and a glacial or resedimented till known as Wisconsinan Till occurs near the creek in its middle and upper reaches. Wisconsinan Ice-Contact Stratified Drift, which contains stratified sand and gravel and some boulders, also occurs in the watershed. Wisconsinan Bouldery Till and Wisconsinan Till Moraine also occurs in the vicinity of the creek, especially near its headwaters.

The parish of Stoke next Guildford lies across the River Wey just below Guildford. It was known as Stochae in the 11th century and as Stok in the 13th century. It is bounded on the west and north by Worplesdon, on the east by Merrow, on the south by St. Martha's, Shalford, and the Guildford parishes. The terrain includes the chalk ridge east of Guildford, the Thanet and Woolwich beds, the London Clay, and the sand and alluvium of the Wey Valley.

During pre-glacial times, Rogers Creek likely flowed through a saddle to the north of the gorge through which it currently flows. The saddle is now filled with glacial deposits and the road from Harveyville to Muhlenburg runs through its former location. The surficial geology along Rogers Creek mainly consists of alluvium and bedrock consisting of sandstone and shale. In most of the rest of the creek's watershed, the surficial geology features a glacial or resedimented till known as Wisconsinan Till.

Franklin lies in the northern part of Delaware County. It is bordered by Otsego County on the north, the towns of Davenport and Meredith on the east, the towns of Delhi, Hamden, and Walton on the south, and the town of Sidney on the west. Franklin has views of forested hills, streams, ponds, historic homes and commercial buildings, and numerous winding roads. Its surface is hilly upland made of shaly loam atop hardpan, while the valleys consist of gravelly loam and alluvium.

The elevation near the mouth of Kellum Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology along the valley floor of Kellum Creek in its lower reaches mainly consists of Boulder Colluvium (which contains numerous quartz, sandstone, or conglomerate boulders) and alluvium. Bedrock containing conglomeratic sandstone, sandstone, and shale occurs on the sides of the valley and a glacial or resedimented till known as Wisconsinan Till also occurs in the area.

The de-watering of the Walloon Coal Measures has been raised as a concern by landholders, as stock water bores drilled into the coal seams can be affected by reduced water flows or gas. Under Queensland law, gas companies are required to "make good" if there is an impairment on a landholder's bore. The Walloon Coal Measures are hydraulically connected to the aquifers of the Great Artesian Basin (within the Surat Basin) and in some locations immediately underlies the Condamine Alluvium.

The upper part of this river is sloping, therefore rain water from Annamite Range flows violently to the lower part in rainy seasons (in autumn), causing floods in it basin. Thanks to An Ma Dam, this situation has been stopped. Unlike other rivers in Vietnam which flow southeast, the Kiến Giang River flows northeast, and creates a narrow delta in Lệ Thủy District. Like all of the rivers in Central Vietnam, this river water is clear, which means that it carries little alluvium.

The Lishan Fault separates the Hsuehshan Range terrane Eocene to Oligocene sandstone and shale. The Chukou Fault (觸口斷層) provides the boundary for the Western Foothills terrane, which is shallow marine detritus from Miocene to Pleistocene. A deformation front forms the boundary with the undeformed coastal plains alluvium, which is still depositing. The Eastern Central Range terrane can be divided into the Tailuko belt on the west with greenschist metamorphism and the Yuli belt on the east with blueschist metamorphism.

Black cottonwood is a pioneer species that grows best in full sunlight and commonly establishes on recently disturbed alluvium. Seeds are numerous and widely dispersed because of their cottony tufts, enabling the species to colonize even burn sites, if conditions for establishment are met. Seral communities dominated or codominated by cottonwood are maintained by periodic flooding or other types of soil disturbance. Black cottonwood has low drought tolerance; it is flood-tolerant but cannot tolerate brackish water or stagnant pools.

Thái Bình river (Vietnamese: Sông Thái Bình) is the name of the Thái Bình river system's main river in Northern Vietnam. This river system joins with the Red River system and brings alluvium to create Red River Delta. Thái Bình river starts in the area of Đồng Phúc commune, Yên Dũng District, Bắc Giang Province - where the Thuong River and Cầu River join with each other. It then flows to Hải Dương Province and becomes the boundary between Bắc Giang and Hải Dương.

The plant grows in a variety of habitats but prefers to grow in more fertile soils, fully exposed to sun on lower mountain slopes. It has been found growing in fynbos, renosterveld, coastal vegetation and the vegetation found on the more fertile shale bands. It often grows in shale, but it is found in a variety of soil types as well: alluvium, sand and silcrete; as well as substrates derived from granite. It occurs at altitudes of 100 to 850 metres.

The larger part of Tyne and Wear is covered with a varying thickness of glacial till dating from the last ice age. Glacial sand and gravel is also widespread. Glacial lake deposits occur within the Team valley, a legacy of Glacial Lake Wear which resulted from the eastward flow of the region's rivers being blocked by North Sea ice at one time. The valleys of the Tyne and its tributaries the River Team and the River Derwent are floored by alluvium.

This fault extends throughout the city and is located in the alluvium just south of the Verdugo Mountains. The fault is mapped on surface in northeastern Glendale, and at various locations in Burbank. Other nearby faults include the Northridge Hills Fault ( northwest of Burbank), the Newport–Inglewood Fault (), Whittier Fault (), and lastly the San Andreas Fault () with its 8.25 magnitude potential on the Richter Scale. Burbank suffered $66.1 million in damage from the 1994 Northridge earthquake, according to the city's finance department.

Hasnabad is located at . Hasnabad CD Block is bounded by Basirhat I CD Block in the north, Debhata Upazila in Satkhira District of Bangladesh in the east, Hingalganj CD Block in the south and Sandeshkhali I and Minakhan CD Blocks in the west. Hasnabad CD Block is part of the Ichhamati-Raimangal Plain, one of the three physiographic regions in the district located in the lower Ganges Delta. It contains soil of mature black or brownish loam to recent alluvium.

These soils are well-drained, moderately coarse-textured soils derived from alluvium from granitic rock. The Hanford soils are important for the production of a wide variety of irrigated orchard, field, and truck crops. Vicinity watercourses include the Stanislaus River, the Tuolumne River and Dry Creek empties into the Tuolumne River. Area groundwater, which is the principal source of water supply in the city,Stanislaus County General Plan (1987) has been historically impaired in a fashion that is spatially variable.

This amount has been reduced due to extensive urbanization of the lower watershed which results in more water running off to the Pacific Ocean. However, water from irrigation run-off and other human activities is responsible for recharging an additional per year. The Christianitos and Mission Viejo fault zones split the watershed into distinct "Upper" and "Lower" groundwater basins. The groundwater mostly lies in alluvium, which ranges from a depth of in the lower elevations to almost none in the high elevations.

The Healdsburg Fault continues along the east side of the Cotati Valley north of Santa Rosa, and the Healdsburg Fault is actually a step-over from the Rogers Creek fault. The upper soil surface above the Santa Rosa Plain is composed of Plio-Pleistocene alluvial fan deposits. Further north, one encounters Quaternary alluvium from the Russian River and its tributaries. North and east of Healdsburg, the Healdsburg fault cuts through Lower Cretaceous marine rocks with stringers of Mesozoic ultrabasic intrusive volcanic rocks.

Lake Mweru, at an elevation of about , is a floodplain lake that has been formed by a process of erosion where the wind has carried off alluvium. The Luvua River leaves the north end of the lake at Pweto in the DRC. The river flows about northwest to Ankoro, where it meets the Lualaba. The middle course of the river is obstructed by a series of rapids, torrents and cataracts as it drops down from the plateau into the Congo Basin.

The remaining area is covered under sedimentary alluvium soil of Harka river of Ghaggar-Hakra River system (paleo Sarasvati River) to the north and east, and paleo channel of Yamuna through Bhiwani in the south and east. Among these hills, Khanak hill is the largest and tallest, and Tosham hill is the second largest smaller hill. The other neighbouring hills, in the order of decreasing size, such as Nigana Khurd, Riwasa, Dulehri, Dharan, Dadam etc. are composed of granite porphyries.

The elevation near the mouth of Baker Run is above sea level. The elevation near the source of Baker Run is between above sea level. The surficial geology in the vicinity of the lower reaches of Baker Run consists of alluvium, which contains stratified sand, silt, and gravel, and alluvial terrace. Further upstream, in the middle and upper reaches, there is a till known as Wisconsinan Till, which is underlain by glacial lake clays in the vicinity of the stream's middle reaches.

The site of Montans was occupied by a Gallic oppidum. Already, the Gauls were producing pottery on the site since the environment was favorable with the alluvium covering the terrace containing pockets of clay. Following the Roman occupation, the site became in the beginning of AD one of the most important centers of pottery production in the Gallo-Roman world. The pottery was exported, mostly by water down the Tarn and Garonne rivers all the way to places like Brittany and Great Britain.

The ecoregion covers an area of and is bisected by the Kali Gandaki River, which has gouged the world's deepest river valley through the Himalayan Range. It forms a critical link in the chain of interconnected Himalayan ecosystems, where altitudinal connectivity between the habitat types is important for ecosystem function. The soil is composed of alluvium deposited over the ages by the rivers that drain this young mountain range. At lower elevations, the ecoregion is flanked by the Terai-Duar savannas and grasslands.

Coll is formed largely from gneiss forming the Lewisian complex, a suite of metamorphic rocks of Archaean to early Proterozoic age. The eastern part of the island is traversed by numerous normal faults most of which run broadly northwest-southeast. Dolerite and camptonite dykes of Permo-Carboniferous or Tertiary age are also seen in the east of the island. Quaternary sediments include raised beach deposits which are frequent around Coll’s coastline whilst stretches of alluvium occupy some low inland areas.

Subsequently coastal and estuarine sands, silts and muds have been deposited widely throughout the Mersey and Dee estuaries whilst alluvium fills the floor of other river and stream valleys.British Geological Survey 1:625,000 scale geological map Quaternary Map of the United Kingdom South 1st Edn. 1977 Considerable areas of recent blown sand cover the coastal zone around Southport and southwards to Formby and peat has developed across lower ground as at Holland Moss and Sefton Meadows inland of Southport and Formby.

A post-glacial stream valley transects the gravel ridge along the north parish edge, revealing slight surface yellow sands (Thanets), over a generally gravely agricultural surface. Some large nodules of flint, and erratic Bunter pebbles surface on the valley bottom. The rich soils of the southward Thames alluvium have been reclaimed from a former natural (tidal) saltmarsh state, being gradually embanked from the medieval onward. An Inquisition of 1362 refers to one marsh on the manor as already within a 'wall'.

Giba River in Ethiopia A bedrock river is a river that has little to no alluvium mantling the bedrock over which it flows. However, most bedrock rivers are not pure forms; they are a combination of a bedrock channel and an alluvial channel. The way one can distinguish between bedrock rivers and alluvial rivers is through the extent of sediment cover.''' The extent of sediment coverage is based upon the sediment flux supplied to the channel and the channel transport capacity.

Bootherium is an extinct bovid genus from the middle to late Pleistocene of North America which contains a single species, Bootherium bombifrons.McKenna & Bell, 1997, p. 442. Vernacular names for Bootherium include Harlan's muskox, woodox, woodland muskox,The Academy of Natural Sciences helmeted muskox,Helmeted Muskox (Bootherium bombifrons) from Near Fort Saskatchewan, Alberta: Dating Evidence for Redeposition in Late Pleistocene Alluvium or bonnet-headed muskox. Bootherium was one of the most widely distributed muskox species in North America during the Pleistocene era.

The river runs through a wide band of granite and areas of recent alluvium, with a complex mix of sedimentary and igneous rocks, originating from the mountainous terrain of the Arthur Range which form the western boundary of the catchment area. and a region of clay-bound gravels to the eastern boundary. As well as the granites, the wide variety of rock types found along the course of the river include complex basement rock, ultramafic, old and young sedimentary rocks.

Old alluvium is found rather away from river courses, especially on uplands of the plain where silting is a rare phenomenon. A large number of small and usually seasonal rivers flow through the Terai, most of which originate in the Sivalik Hills. The soil in the Terai is alluvial and fine to medium textured. Forest cover in the Terai and hill areas has decreased at an annual rate of 1.3% between 1978 and 1979, and 2.3% between 1990 and 1991.

Study of the coins which had been crammed into a pot showed that the dateable sequence ended abruptly in 354AD. A first century AD pot was discovered in a house foundation trench at Trent Lane. In later Roman times climatic deterioration lead to flooding and some sites like Ferry Lane Farm were buried under alluvium while others were covered by sand-blown deposits – we still have episodes of sand-blow which can cause significant build-up at field edges and on the A1133.

Corymbia ptychocarpa is found from the Kimberley region of Western Australia and through the Top End of the Northern Territory to near Doomadgee in far north-western Queensland. It grows in sandy soils and alluvium along watercourses and near springs. In the Northern Territory it occurs on the Arnhem Plateau, Daly Basin, Ord Victoria Plain, Pine Creek and the Victoria Bonaparte biogeographic regions. Subspecies aptycha is restricted to the Top End between the Cobourg Peninsula, Yirrkala amd El Sharana in Arnhem Land.

Pohang () is a city in the province of North Gyeongsang, South Korea, and a main seaport in the Daegu-Gyeongbuk region. The built-up area of Pohang is located on the alluvium of the mouth of the Hyeongsan River. The city is divided into two wards (gu), Buk-gu or Northern Ward () and Nam-gu or Southern Ward (). This city has the largest population of North Gyeongsang Province and it has the third-largest land area of any city (si) in South Korea.

Peat evidence from near Bredon Hill and Birlingham in the Avon area shows that it was cleared by the earlier part of the period. A lack of cereal grain finds has been interpreted as indicating that the land was used for cattle farming. The clearance of forest land is also evidenced by alluvium deposits on the lower lands in the county, caused by river flooding. A move towards open settlements may be detected as the lands became more fully occupied.

Most of the commune is located on a rolling plateau formed of layers of limestone dating from the Cretaceous period. To the west the marsh consists of much more recent alluvium. Part of the commune consists of a succession of hills overlooking the Gironde estuary, which dominate a vast prairie wetland that extends west to Talmont-sur-Gironde and Meschers-sur-Gironde. The northwest of the commune retains some traces of the original forest that stretched to Chenac in Gallo-Roman times.

Maldon is a town of circa 15000 people on the tidal River Chelmer by the Blackwater Estuary in Essex. It is on the A414 east of Chelmsford, and north east of Charing Cross, London, using the A13. Essex is a county built on London Clay, overlain with pockets of gravel deposited by riparian action, the lowest land is made up of river alluvium and salt marsh. At Maldon the railway cutting (now a road cutting) provided a reference section for geologists.

The Glenrothes area's geology is predominantly made up of glacial deposits with the subsoil largely consisting of boulder clay with a band of sand and gravel in the area to the north of the River Leven. The river valley largely comprises alluvium deposits and there are also igneous intrusions of olivine dolerite throughout the area.Glenrothes Development Corporation, 1970, pp. 26–29. Productive coal measures were largely recorded in the southern parts of Glenrothes, approximately south of the line of the B921 Kinglassie road.

The District is developed from five different geological formations namely Granite, Birimian rocks, Voltaian shale, and Old Alluvium of mixed origin and Very Old River Terraces. Out of these, the dominant soil groups in the district are of granite origin. They form the predominant soils in the northern half of the district and more than half of the southern part. The second largest groups of soils are those derived from alluvia of mixed origin and those on very old river terraces.

Those investigators who include the alluvium in the unit tend to refer to the unit as the Servilleta Formation, while those who do not tend to refer to the unit as the Servilleta Basalt. The formation rests unconformably on the Picuris Formation, Santa Fe Group, or Hinsdale Formation. It is up to thick near Embudo but thins to thick adjacent to the Picuris Mountains. It is downfaulted against Santa Fe Group beds near Pilar and on the northeast side of the Picuris Mountains.

Coolmunda Dam, Leslie Dam, Cooby Dam, Perseverance Dam, Cressbrook Dam, Storm King Dam and the Glenlyon Dam are some of the major water storage facilities in the area. West of Toowoomba is the Toowoomba Wellcamp Airport. Bell, 2010 A wide street in the small town of Nobby The Darling Down is situated in the drainage basins of the Condamine River and Maranoa River and tributaries. The Condamine River flood plain is noted for its good soils formed by basaltic alluvium.

A caisson is constructed of reinforced concrete and installed into sand or gravel below the surface level of an adjacent river or lake. Screened conduits (also referred to as laterals or lateral well screens) are extended horizontally from ports in the caisson about 60 meters (200 feet) into surrounding water-bearing alluvium. The radial arrangement of screens forms a large infiltration gallery with a single central withdrawal point. A single collector may produce as much as 25 million gallons per day.

The village dates back some 7,000 years. It is situated at the northernmost point of the Madrie Plateau, at an altitude of 124 meters above sea level. The soil consists of alluvium, white chalk, clay, and sand. It overlooks the meandering of the Seine River and is built at the crossroads coming from Les Andelys to the north, Gaillon to the east, Louviers to the south, while the western border of the village is protected by the banks of the Seine.

It is a raised alluvium area along the Hooghly, which forms the western boundary of the district. The Bidyadhari forms the eastern boundary of Barasat II CD Block with Deganga CD Block, and as such it is partly in the North Bidyadhari Plain. Barasat II CD Block has an area of 114.04 km2. It has 1 panchayat samity, 7 gram panchayats, 109 gram sansads (village councils), 78 mouzas and 77 inhabited villages, as per the District Statistical Handbook: North 24 Parganas.

The fertile alluvium and extensive grasslands of the canyon floor were used primarily for grazing cattle. Several corrals still stand in the Wood Canyon area today. In 1871, pioneer Eugene Salter settled at the canyon mouth, but one year after, sold it to the Thurstons, who cultivated the present-day golf course area as an orchard. Eventually when the city of Laguna Beach was founded in 1926, the area at the mouth of Aliso Canyon, including Laguna Beach, became a popular camping area.

The lengthy excavation resulted in the revelation of rich Early Archeulian assemblage in fine-grained context in the gullies of Chirki area. Besides this, a great number of well-preserved fossil wood pieces, faunal specimens, and tree trunks were found in the alluvium. In 1981, Corvinus published her first classic monograph, “A Survey of the Pravara River System in Western Maharashtra, India”. Her second monograph, “A Survey of the Pravara River System in Western Maharashtra, India” was published in 1983.

West Bay is sited on deposits of river alluvium that indicate a former estuary. There are beaches and cliffs on either side of the harbour. The beaches were previously of a similar size—in terms of their seaward extent—but now East Beach is considerably larger, due to accumulation of finer sediment. East Beach is also designated a Site of Special Scientific Interest, and forms one end of Chesil Beach, a barrier beach which extends southeast for toward the Isle of Portland.

The last-named unit forms a part of the Lias Group of rocks of Toarcian age. Beneath all of these is the relatively thick Charmouth Mudstone Formation sequence rising from the edge of the valley floor alluvium. All faces of the hill are subject to large areas of landslip.British Geological Survey 2011 Bath, England and Wales sheet 265 Bedrock & Superficial Deposits, 1:50,000 (Keyworth, Nottingham: British Geological Survey) The high hill is just over to the north of the River Avon.

The cliff is composed of Tertiary period volcanic ash mixed with larger rock fragments of volcanic origin. A similar alcove is being cut by the Shoshone at the mouth of Clocktower Creek. The cave fill has accumulated for at least 10,000 years and appears to have originated from nearby debris fans formed where weathered material has flowed down channels in neighboring cliffs. Apart from the depth and consistent nature of the alluvium, Mummy Cave is also characterized by extreme dryness.

Little Indian Run (also known as Indian Camp Run) is a tributary of Little Muncy Creek in Lycoming County and Sullivan County, in Pennsylvania, in the United States. It is approximately long and flows through Franklin Township and Jordan Township in Lycoming County and Davidson Township in Sullivan County. The watershed of the stream has an area of . The surficial geology in the stream's vicinity mainly consists of alluvium, bedrock, Wisconsinan Till, Wisconsinan Till Moraine, and Wisconsinan Ice-Contact Stratified Drift.

Dredging International was the chosen dredging contractor, and the value of the dredging contract is stated by them at €12.4 million. The scope of works consisted of dredging the main tunnel trench and subsequently backfilling the completed construction with sand and gravel. The contract provided also for restoration of the riverbed profile and the addition of a rock protection layer. Between May 1996 and March 1999, the company excavated 785,000 tonnes of silt and alluvium and 300,000 tonnes of sand and gravel.

Map with Hakra Ware sites in red Hakra Ware culture is a material culture which is contemporaneous with the early Harappan Ravi phase culture (3300–2800 BCE) of the Indus Valley. Hakra Ware culture is characterized by handmade vessels with mud and grit applied to the surface. The Hakra Wares culture also made structures in the form of subterranean dwelling pits, cut into the natural soil. The walls and floor of these pits were plastered with the yellowish alluvium of the Hakra valley.

They typically occur either lying on the surface of the ground or buried within sediments such as alluvium, colluvium, or glacial till. A weathering rind represents the alteration of the outer portion of a rock by exposure to air or near surface groundwater over a period of time. Typically, a weathering rind may be enriched with either iron or manganese (or both), and silica, and oxidized to a yellowish red to reddish color. Often a weathering rind exhibits multiple bands of differing colors.

Vine-planted parcels are rather steep and climb up to 478 m height (near Osenbach). The lower part of the slopes consists of layers of limestones or marls covered by loess where the slope is rather smooth. Finally, the plain consists of a thick layer of alluvium deposited by the Rhine (silt and gravels). This zone is very more fertile than the two previous with an important aquifer mainly close to the surface (less than 5 m deep): the Upper Rhine aquifer.

The elevation near the mouth of Lake Run is above sea level. The elevation of the stream's source is approximately above sea level. The surficial geology in the vicinity of the lower reaches of Lake Run consists of bedrock consisting of conglomeratic sandstone, sandstone, and shale; Wisconsinan Ice-Contact Stratified Drift; Wisconsinan Till, a glacial till; alluvium, fill; and sand and gravel pits. Further upstream, there is Boulder Colluvium, which contains numerous conglomerate, quartz, and sandstone boulders; Wisconsinan Till, bedrock, wetlands, peat bogs, and a lake.

The surficial geology in the vicinity of Rocky Run mostly consists of a glacial or resedimented till known as Wisconsinan Till. Wisconsinan Ice-Contact Stratified Drift, which contains stratified sand and gravel as well as some boulders, also occurs in the valley, as does alluvium. Boulder Colluvium and Wisconsinan Bouldery Till occur to the north of the stream and Wisconsinan Bouldery Till also occurs in the southeastern part of the watershed. Coal dumps, or large piles of coal waste, occur in some small areas in the watershed.

Con Lu, which is the smallest of the three islets is being widened by alluvium from the Red River and covered by sandy layer.Pham Dinh Viet Hong, Nguyen Duc Tu, Nguyen Viet Cach & Le Thanh Binh, Xuân Thủy National Park: Policy Brief, VEPA-MCD, Hanoi, Vietnam, 2007, p. 9. The Buffer Zone has a total area of 8.000 hectares. The Park is a delta and estuary islands (Ba Lat river-mouth) support coastal mangroves and the mud flat ecosystem in the Red River delta.

In 1928, the core of the area was designated a sanctuary and in 1978 it was declared a tiger reserve. Manas River and another tributary of Manas, the Hakua, flow through the sanctuary. A thick mantle of alluvium is the dominant soil of the terrain. Under subtropical climatic conditions (with of annual rainfall and temperature varying from a maximum of and a minimum of ), the forest consists of the semi- evergreen forest vegetation with mixed deciduous, littorals and swamps, and interspersed with bamboo and cane.

The vineyard was planted on a Kimmeridgian marly plateau, hanging over the Cher River. It is covered by a mixture of alluvium silica-clay soil. This mixture drains away the excess water and the in-depth marl cover preserves water, protecting it from a dry period. The soil has three layers: a soil made up of sand and gravel on an underlay of clay, a sandy soil covered by red sand and a sandy-silt soil on a clayey-sand or clay with slightly sandy soil.

Three types are predominant. Firstly, the Sienna- red Quaternary alluvium that is quite specific to the region and situated more on the heights: Merlot and Malbec are widely cultivated. Merlot and Cabernet are planted on clay and sandy gravel soils while Merlot is also grown on the widespread areas of clay and limestone. The Atlantic Ocean plays an important role in the temperate climate of le Bourgeais and this accentuates the expression of terroir, aided by the regulation of temperatures by the effects of the Gironde estuary.

The Montenegro Fault is part of the Romeral Fault System, running through the western slope of the Central Ranges. The fault is located to the west of the city of Armenia. The fault crosscuts and deforms the Pleistocene volcanic and volcano-sedimentary deposits of the Quindío Fan (), which covers about . The Montenegro Fault forms outstanding fault scarps as much as in height, beheaded streams, hanging valleys, ponded alluvium, aligned and offset drainages, as well as soil and rock slides on the face of the scarps.

The long Garzón-Pitalito Fault extends along the western slope of the Eastern Ranges southeast from the city of Neiva and crosses the upper part of the Magdalena Valley. In the northern half, the fault places Jurassic to Triassic sedimentary rocks on the eastern side in contact with Quaternary alluvium and colluvium on the western side. Along its southern half, the fault places Jurassic-Triassic rocks in contact with Cretaceous rocks. The Garzón- Pitalito Fault strikes toward and merges with the Algeciras Fault to the north.

Karamandere is a neighborhood in the northwest in Çatalca of Istanbul, founded in 1879 by communities immigrating from the Balkan Peninsula. There is the Black Sea in the northeast, Çilingoz Nature Park in the northwest, D 020 in the south, the state forest in the southeast, Danamandıra Nature Park in the southwest and Durugöl in the east. In the geography there are terraces, gravel, alluvium, stone chips, marble and gneiss, garden agriculture is done. Ferah Hill, Harman Hill and Bostantarla Hill are important peaks.

The elevation near the mouth of Dymond Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology in the vicinity of Dymond Creek consists mainly of a till known as Wisconsinan Till, alluvium, Wisconsinan Ice-Contact Stratified Drift, and bedrock containing sandstone, conglomeratic sandstone, shale, and coal. However, Wisconsinan Outwash containing stratified sand and gravel occurs near the creek's mouth and there are a few patches of alluvial fan near the lower and middle reaches.

The western part of the district has poor, ferruginous soil and hard beds of laterite with scrub jungles and sal (Shorea robusta) woods. Long broken ridges with irregular patches of more recent alluvium have marks of seasonal cultivation. During the long dry season large extents of red soil with hardly any trees lend the country a scorched and dreary appearance. In the eastern part the eye constantly rests on wide expanses of rice fields, green in the rains but parched and dry in summer.

Bhitargarh covers an area of , situated in the Amarkhana Union of Panchagarh Sadar Upazila within the Panchagarh District. The site is covered by sand and gravel which flowed down from the Himalayan foothills by glacial waters as well as monsoon rainfalls. Topographically, the land is part of the Old Himalayan Piedmont Plains while the gravel beds belong to the Upper Pleistocene stage, similar to the rest of Panchagarh District. The Upper Pleistocene layer is further overlain by Holocene deposits, evident in the alluvium sand, silt and clay.

The lagoon is constantly getting smaller and shallower under the effect of silting. On the contrary, the streams of northern Talesh and eastern Gilan, even the more abundant Polrud, do not bring alluvium enough to counterbalance the action of a coastal current going eastward, and thus could not build more than a narrow ribbon of lowlands, only a few kilometers wide between Astara and Safid-rud and to the east of Qasemabad, and some 10 km wide at the mouth of the Polrud around kelachay.

Bagdah is located at . Bagdah CD Block is bounded by Maheshpur Upazila in Jhenaidaha District, Chaugachha Upazila and Sharsha Upazila in Jessore District of Bangladesh in the north and east, Bangaon CD Block in the south and Hanskhali and Ranaghat II CD Blocks in Nadia district in the west. Bagdah CD Block is part of the Ichhamati-Raimangal Plain, one of the three physiographic regions in the district located in the lower Ganges Delta. It contains soil of mature black or brownish loam to recent alluvium.

At Tangshan and northward these sediments are thinner where the underlying strata crops out to form isolated hills. This underlying strata is a thick (typically 10 km) layer of mainly sedimentary strata such as limestone and sandstone, with large deposits of coal. Tangshan is located particularly over a northeast oriented syncline, a fold in the sedimentary strata that has brought massive deposits of coal close enough to the surface to be mined. In this area the overlying alluvium varies in thickness from several meters to around .

The low ridge between the Waikato and Waipa rivers is made of Walton Subgroup (eQa – pumiceous fine-grained sand and silt with interbedded peat, pumiceous gravelly sand, diatomaceous mud, and non-welded ignimbrite and tephra), covered in places by Piako Subgroup (1Qa – Late Pleistocene, mainly locally derived, stream and coastal alluvium, and minor fans, with up to of unconsolidated to very soft, thinly to thickly bedded, yellow-grey to orange- brown, pumiceous mud, silt, sandy mud and gravel, with muddy peat in some valleys).

The economy was agricultural, and included hunting and fishing. The surrounding peat fens was grazed intensively during the summer months, and Crowle common was managed by four grass-men, who controlled the grazing and charged those who brought stock to the common from other areas. During the winter, the stock was kept on higher ground or in yards, as much of the grassland was flooded between November and May. This had a beneficial effect, as water-borne alluvium improved the fertility of the soil.

The principal tributaries joining Krishna are the Ghataprabha River, Malaprabha River, Bhima River, Tungabhadra River and Musi River. Most of this basin comprises rolling and undulating country, except for the western border, which is formed by an unbroken line of the Western Ghats. The important soil types found in the basin are black soils, red soils, laterite and lateritic soils, alluvium, mixed soils, red and black soils and saline and alkaline soils. An average annual surface water potential of 78.1 km3 has been assessed in this basin.

A 100-year-old water main runs through the creek. The water main is made of cast iron and supplies water to a third of the Wyoming Valley. For a significant portion of its length, the surficial geology of the watershed of Coal Creek features a glacial or resedimented till known as Wisconsinan Till, as well as bedrock consisting of sandstone and shale. Near the creek's lower reaches, alluvium, coal dumps, Wisconsinan Ice- Contact Stratified Drift, and land where coal was once surface mined.

Water Logging in the Town, Saharsa Rajwanshi Nagar, Koshi CHowk, Saharsa (Koshi Division), Bihar The Koshi River and its tributaries flood annually, affecting about 21,000 km2 (8,100 sq mi) of fertile agricultural lands and affecting the rural economy. This is the most devastating river of Bihar, earning it the epithet "Sorrow of Bihar". The Bagmati River regularly breaches its embankments and frequently changes its meandering courses. The annual rate of deposition of alluvium is very high.. The Gandak River also flows through the southern part of Saharsa.

Geologically, the valley is an alluvium-filled synclinal basin, at an elevation of approximately 2,000 to 2,500 feet (600 to 800 meters). Most of the rocks are sedimentary, and the Miocene-age Monterey Formation outcrops to the south, in the foothills of the Sierra Madre. Pliocene and Pleistocene sedimentary formations occur in the foothills along the south side of the valley as well. The large Morales Thrust Fault separates the abruptly-rising block of the Caliente Range from the valley itself on the north.

Much of the alluvium in the river plains had not yet been deposited and the tidal river estuaries extended much further inland.Martin Welch: Early Anglo-Saxon Sussex: from Civitas to Shire, in Brandon (1978), p.14 It is estimated that the coastal plain may have been at least one mile broader than it is today. Before people reclaimed the tidal marshes in the 13th century the coastal plain contained extensive areas of sea water in the form of lagoons, salt marsh, wide inlets, islands and peninsulas.

As a result, a lowland plain with a width of up to 10 km was formed on the sea coast. In some places, remnant mountains up to 180 m high (Pigeon's Rock Mountain, etc.) rise in places by lakes and oxbows. vegetation and soil. The river beds are overloaded with alluvium, the amount of which increases in the lower reaches due to the general stretching and subsidence of the earth's crust along the edge of the continent, and due to the accumulation of catastrophic floods.

Ecoregion 73a is underlain by Holocene alluvium; it lacks the Pleistocene glacial outwash deposits of Ecoregion 73b. Soils on natural levees are relatively coarse-textured, well-drained, and higher than those on levee back slopes and point bars; they grade to very heavy, poorly-drained clays in abandoned channels and swales. Overall, soils are not as sandy as the Northern Pleistocene Valley Trains (73b) and are finer and have more organic matter than the Arkansas/Ouachita River Holocene Meander Belts (73h). Natural vegetation varies with site characteristics.

The landscape of Aldermaston is influenced by Paices Hill and Rag Hill, which are extremities of the chalk formation the North Wessex Downs as part of the Thames Basin Heaths. The topography of the land in the parish generally slopes northward to the River Kennet. The soil in the parish is high in clay. Due to the parish's location within the Kennet Valley there is a high concentration of alluvium, with the content largely determined by the London Clay Formation, the Bagshot Formation, and the Bracklesham Beds.

Gold miners excavate an eroded bluff with jets of water at a placer mine in Dutch Flat, California sometime between 1857 and 1870. Gold extraction refers to the processes required to extract gold from its ores. This may require a combination of comminution, mineral processing, hydrometallurgical, and pyrometallurgical processes to be performed on the ore. Gold mining from alluvium ores was once achieved by techniques associated with placer mining such as simple gold panning and sluicing, resulting in direct recovery of small gold nuggets and flakes.

The upper layers of soil are more recent alluvium. This recent layer is thickest near Soda Lake and thins out towards the mountains to the east and west. Throughout the valley the soil composition varies greatly and includes clay loams, silty clay loams, loams, sandy loams, and gravelly loams. The sandier soils tend to reside near the slopes of the valley and provide greater drainage while the soils with more clay are located on the valley floor near Soda Lake, and have much poorer drainage.

Sixteen caves are found within the area. The earth is mainly composed of stony rocks, sandy loam soils, and clay loam soils in the beds of wadis in the area. The soils in the hills have pockets of alluvium and sandy loam suitable for crop development, particularly on the hillsides and at the foot of the hills. Clay loam soils are found in the bowls and beds of wadis, which although suitable for farming are susceptible to gully and water erosion during the rainy season.

The commune sits on a limestone bedrock dating from the Upper Jurassic (Kimmeridgian). Alluvium dated from the Quaternary period cover the alluvial valleys of the Aume and Charente, the most recent being on the floodplain. There are also some areas of Sand on the slopes dating to the Quaternary glaciations.Land Information Visualiser, BRGM website BRGM Map on Géoportail Paper notice for Mansle, BRGM, 1984, Infoterre, consulted on 13 November 2011 The relief of the commune is that of a low plateau and a confluence of two valleys.

The village lies west of the A19 road and immediately north of the River Kyle. The village used to have a railway station on the East Coast Main Line that runs less than a mile to the east of the village. The soil contains some alluvium as well as sand and loam. The land to the east of the village is a good source of brick clay, and supports the York Handmade Brick Company who have supplied specialist bricks to The Shard and railway station.

Bulbostylis barbata is a flowering plant in the sedge family, Cyperaceae, that is native to Western Australia. The annual grass-like plant has a tufted habit and typically grows to a height of . It blooms between February to September producing brown flowers. It is rarely solitary and is found in rock crevices and along creek and rivers and on low-lying flats throughout a large area of the Kimberley, Pilbara, Mid West and Goldfields-Esperance regions where it grows in sandy-loamy alluvium over sandstone and granite.

Prairie Creek is the Redwood Creek tributary drainage basin including the inland portion of Prairie Creek Redwoods State Park. Prairie Creek drains southerly through a Plio-Pleistocene non-marine sedimentary and metasedimentary formation to a confluence with Redwood Creek approximately one mile upstream of Orick, California. The southern half of the channel exposes the Franciscan Assemblage and the lower reaches flow through Quaternary alluvium of the Redwood Creek estuarine floodplain. Prairie Creek was closely followed by U.S. Route 101 from Orick to the Klamath River drainage divide.

It is located approximately south east of Kowanyama and north east of Normanton in the Gulf Country of Queensland. The property is situated within the Nassau River catchment with both the Nassau and the Mitchell Rivers also flowing through the property. An additional 13 creeks and 8 lagoons are found on the property all useful for watering stock. The country is composed of flat open plains with the soil being grey clay loam derived from the Cainozoic age, sands of Quaternary age with other alluvium.

While the gold rush diminished less labour-intensive gold mining became more common. From the 1880s quartz mining (instead of alluvium) became possible, while massive dredges continued to work the old deposits. These dredges also inspired the first hydro electric power station at Bullendale near Queenstown in 1886. This gold boom peaked between 1890–1900 but put a lot of individual prospectors out of business. The 1893 Women's Suffrage Petition was the second of two mass petitions to the New Zealand Government in support of women's suffrage.

The Aravalli Craton (Marwar-Mewar Craton or Western Indian Craton) covers Rajasthan as well as western and southern Haryana. It includes the Mewar Craton in the east and Marwar Craton in the west. It is limited by the Great Boundary Fault in the east, the Thar desert in the west, Indo-gangetic alluvium in the north, and the Son River-Narmada River-Tapti River basins in the south. It mainly has quartzite, marble, pelite, greywacke and extinct volcanos exposed in the Aravalli-Delhi Orogen.

The soil itself consists of granite, alluvium and organic deposits, with a high risk of erosion, where it is estimated 150 tons per hectare of soil will be lost annually. It is also an area where water catchment is important for water supply in Larut, Matang and Selama District since the water quality from the area is generally good. The water from Bukit Larut mainly flows to three major rivers in the district: Sungai Jana, Sungai Ranting, and Sungai Air Terjun.WWF Malaysia, December 2001. p.

Being accessible mainly by foot it remains relatively pristine, although there is some evidence of access by ATVs and there is some non-native European beach grass. Access to the estuary and beaches is not allowed to non-tribal members unless accompanied by a Tribal representative. The surficial geology of most of the Raft River's drainage basin is glacial outwash, with the estuary being more recent alluvium. The river's estuary and lower reach, up to the North Fork, is in a tsunami hazard zone.

Further away from the creek, there is a glacial or resedimented till known as Wisconsinan Till, as well as a few patches of Wisconsinan Ice-Contact Stratified Drift and bedrock consisting of sandstone and shale. There is Wisconsinan Outwash near the mouth of the creek and two patches of wetland near Broadway. The upper reaches of the watershed are mainly dominated by Wisconsinan Till, with bedrock occurring along the edges of the watershed. There are also a few patches of alluvium and three patches of wetland.

As of 2006, gold was mined from the Samti placer deposit in Takhar Province in the north by groups of artisanal miners. Badakhshan Province also had occurrences of placer gold deposits. The deposits were found on the western flanks of the mountains in alluvium or alluvial fan in several river valleys, particularly in the Anjir, the Hasar, the Nooraba, and the Panj Valleys. The Samti deposit is located in the Panj River Valley and was estimated to contain between 20 and 25 metric tons of gold.

The elevation near the mouth of Big Run is above sea level. The elevation of the stream's source is above sea level. The surficial geology along the valley floor in parts of the middle or upper reaches of Big Run mostly consists of alluvium, which contains stratified sand and gravel. However, there are patches of Wisconsinan Till, Wisconsinan and Illinoian Lag, Illinoian Till, and Illinoian Lag nearby, and the valley sides have surficial geology of bedrock consisting of sandstone and shale in some reaches.

This may occur due to an equilibrium reached in the fluvial system resulting from: slowed or paused uplift, climate change, or a change in the bedrock type. Once downcutting continues the flattened valley bottom composed of bedrock (overlain with a possible thin layer of alluvium) is left above either a stream or river channel. These bedrock terraces are the strath terraces and are erosional in nature.Burbank, D.W., and R.S. Anderson, Robert, 2001, Tectonic Geomorphology, Malden, MA: Blackwell Publishing Unpaired fluvial terraces on the South Fork of the Shoshone River, Park County, Wyoming, 1923.

The hills surrounding the lake area, towards the north east of Jaipur, have quartzite rock formations (with a thin layer of soil cover), which is part of Aravalli hills range. Rock exposures on the surface in some parts of the project area have also been utilised for constructing buildings. From the north east, the Kanak Vrindavan valley, where a temple complex is situated, the hills slope gently towards the lake edge. Within the lake area, the ground area is made up of a thick mantle of soil, blown sand and alluvium.

The island consists of alluvium that has been deposited by the Columbia River since the Pleistocene and overlies the Columbia River Basalt Group. Much of this is eroded remains of the Ringold Formation, which was placed by the Columbia River between 9 and 3 million years ago. The White Bluffs, which are a series of cliffs created by this erosion, are immediately east of the island. The White Bluffs became destabilized by water from the Columbia Basin Irrigation Project entering the groundwater system and flowing toward the Columbia River.

Bhabar is the gently-sloping coarse alluvial zone below the Sivalik Hills (outermost foothills of the Himalayas) where streams disappear into permeable sediments. The underground water level is deep in this region, then rises to the surface in the Terai below where coarse alluvium gives way to less permeable silt and clay. The Ganges River lies to the west and Sharda to the east. Being at the junction of Himalayas and the Indo-Gangetic Plain, Bhabar contains almost all the important trade and commerce hubs of Uttarakhand state.

The dam was constructed with the boulder clay and alluvium excavated from the reservoir bed. Later additions to the dam are formed with colliery waste from mining activity in the area. The overflow level of the dam was raised in the late 19th and early 20th centuries to increase the capacity of the reservoir. The dam was raised by approximately , a new bridge was built across the outflow basin above the old one, a new valve house was constructed on the raised crest and a wave wall was built along the crest.

Twyford lies on the chalk at the northern edge of the Hampshire Basin, dipping south from the southern limb of the Winchester anticline. Successively younger layers of chalk are exposed from north to south, from Turonian New Pit Chalk in the Plague Pits Valley south of St. Catherine's Hill, the Lewes Nodular Chalk at Twyford Down, the Seaford Chalk under the village, to the Santonian or Campanian Newhaven Chalk to the south. In the Itchen valley to the west the chalk is overlain by alluvium and tufa deposits.British Geological Survey (2002), Winchester.

El Salvador is a caldera in Chile. The mountains La Antena and Contreras form the southeastern margin of the caldera, while the high Cerro Indio Muerto massif lies inside the caldera. The terrain around the caldera is formed by a Paleozoic basement, Mesozoic sedimentary rocks and also Mesozoic volcanic rocks; the latter are separated from the first two units by branches of the Domeyko fault system; this fault system and its branches have controlled the emplacement of a large number of copper deposits. Later sequences include the Miocene Atacama gravels and Quaternary alluvium.

For example, some sedimentary layering promotes the formation of soil such as a silty cover on bedrock, or a sandy cover on a clayey alluvium layer. In both of these cases, a friable surface material has been established by nonpedogenic instances. Other instances of sedimentary surface cementation, or fine interbedded sequences of clay and sand, could be considered to be not conducive to the formation of a soil. Nonuniform parent materials may be difficult to find in soils and paleosols, although deviations from normally found minerals could lend clues to the original parent material.

The plains have a nearly straight shoreline. Paleogene and Neogene alluvium (from about 65 to 2.6 million years ago) with patches of ancient Archean gneiss and sandstone (from about 4 billion to 2.5 billion years ago), the plains are widest in the deltaic regions. Sand dunes of decomposed granites and zircon, created mainly by the action of wind at low tide, and lagoons are found along the Bay of Bengal. Chilka, the largest lake in the region (in the southwest), is salty; Samang and Sur (north and northeast of Puri, respectively) are freshwater lakes.

The Mayo Rey and Vina River cut north of this portion, leaving deposits of sedimentary stone except in the granite east. North of this lies a band of sedimentary alluvium, clay, limestone, and sandstone. Faults tentatively follow the Bénoué River north of this and form a barrier to split the remainder of the province, with metamorphic rocks such as gneiss, mica, and schists dominating to the south and sedimentary stone making up the north. Another large band of metamorphic rock makes up the territory northwest of the Bénoué basin.

Gullies can be formed or enlarged by a number of human activities. Artificial gullies are formed during hydraulic mining when jets or streams of water are projected onto soft alluvial deposits to extract gold or tin ore. The remains of such mining methods are very visible landform features in old goldfields such as in California and northern Spain. The badlands at Las Medulas for example, were created during the Roman period by hushing or hydraulic mining of the gold- rich alluvium with water supplied by numerous aqueducts tapping nearby rivers.

The two most substantial aquifers are the Pacific Coastal Plain alluvium and the karstic and fractured limestone that extend beneath the Sierra de los Cuchumatanes, Sierra de Chama, and Peten Lowlands. Other more limited aquifers are important for small-scale local demands. The mountains and hills of Guatemala contain many other types of aquifers, including volcanic pyroclastic and lava deposits, low permeability sediments, igneous, and metamorphic aquifers. Alluvial plains, valleys and lowlands make up about 50% of the countries territory and contain about 70% of the available ground water reserves.

In Australia it is found in Western Australia it is found in swamps, along creeks and rivers and other damp areas in the Kimberley region where it grows in sandy-clay alluvium often around basalt. It is also found across the top end of the Northern Territory and tropical parts of Queensland. The species has been introduced and is regarded as a weed throughout North and South America. It is thought to have been introduced into the West Indies as a contaminant late in the nineteenth century and was collected in 1886 in Puerto Rico.

The town of Franklin lies in the northern part of Delaware County, in an area of wooded hills, streams, ponds, historic homes, commercial buildings, and numerous winding roads. Its surface is hilly upland made of shaley loam atop hardpan, while the valleys consist of gravelly loam and alluvium. Ouleout Creek, which flows into the Susquehanna River, is the main surface water feature. The waterway was important to village development, not only for water supply but as transportation arteries for travel as well as shipment of lumber and goods to market.

Ukanc is a scattered settlement on a shady rolling plain at the west end of Lake Bohinj at the end of the valley, where mountain walls rise on three sides, closed in by Mount Vogel (), Little Peak (Mali vrh, ), Mount Peršivec (), and the Komarča Cliff (). It is connected by road to Bohinjska Bistrica. The soil largely consists of alluvium from the Ukanc Suha River (Ukanška Suha) and Žagar Gorge (Žagarjev graben), as well as the Savica River. In meteorological terms, Ukanc is one of the wettest places in Slovenia.

A surface layer that is 10 cm thick overlying bedrock can be by itself the solum. A soil that consists only of recently deposited alluvium or recently exposed soft sediment does not have a solum. In terms of soil horizon designations, a solum consists of A, E, and B horizons and their transitional horizons and some O horizons. Included are horizons with an accumulation of carbonates or more soluble salts if they are either within, or contiguous, to other genetic horizons and are at least partly produced in the same period of soil formation.

Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level. The district has a long coastline of 65.5 km along its southern and south eastern boundary.

Kaliachak III community development block is located at Kaliachak III CD Block is part of the Diara, one of the three physiographic sub-regions of the district. “The Diara is a relatively well drained flat land formed by the fluvial deposition of newer alluvium in the transitional zone between the Barind upland and the marshy Tal tract. The soil is light with sandy appearance and is very fertile. Mango gardens are common and mulberry is also grown in this natural division.” It covers 32.16% of the total area of the district.

Amdanga, the eponymous CD Block headquarters, is located at . Amdanga CD Block is bounded by Haringhata CD Block in Nadia district in the north, Habra II CD Block in the east, Barasat I CD Block in the south, and Barrackpore I and Barrackpore II CD Blocks in the west. Amdanga CD Block is part of the North Hooghly Flat, one of the three physiographic regions in the district located in the lower Ganges Delta. It is a raised alluvium area along the Hooghly, which forms the western boundary of the district.

Townend Farm The underlying composition here is of glacial clay with pockets of gravel, sand, peat and alluvium, and patches of dolomite and carboniferous limestone. This is a small hamlet incorporating Hall Farm, Garthorne Farm and Townend Farm on an approach road south of Newton Lane. It is the focus of the parish of Archdeacon Newton rural ward, and its councillor is Rosalind Tweddle. It is situated on flat land to the north-west of the Branksome suburb of Darlington, and to the north-west of the A1 road.

The Goleta Valley is a coastal plain between the Santa Ynez Mountains and the ocean, approximately three miles across. It consists of Holocene and Pleistocene alluvium, colluvium, estuarine deposits, as well as marine terraces created during interglacial high sea level episodes. The area has been subject to rapid geologic uplift, as evidenced by its coastal bluffs and narrow beaches. Between the flattest part of the Goleta Valley and the ocean is an area of uplift paralleling the shore which includes, from west to east, Isla Vista, Mescalitan Island, More Mesa, and the Hope Ranch Hills.

Maeander River's mouth Illustration of Miletus The ruins appear on satellite maps at 37°31.8'N 27°16.7'E, about 3 km north of Balat and 3 km east of Batıköy in Aydın Province, Turkey. In antiquity the city possessed a Harbor at the southern entry of a large bay, on which two more of the traditional twelve Ionian cities stood: Priene and Myus. The harbor of Miletus was additionally protected by the nearby small island of Lade. Over the centuries the gulf silted up with alluvium carried by the Meander River.

Also allowed within the AOC regulations are the varieties Cabernet Franc and Carménère. The INAO specifications demand the following production norms: a minimum of sugar, per litre of must, maximum base yield of 50 hecolitres per hectare, and a minimum alcohol by volume of 10%. A bottle from an estate within the Médoc AOC, in this case Château Laffitte Laujac. The regulations also exclude viticultural activity in the communes Carcans, Hourtin, Brach, Saumos, Lacanau, Le Temple, Le Porge, and on "land of recent alluvium and sand lying on impermeable subsoils".

A second feature are the wadis, which range from seasonal watercourses that flood only occasionally during the wet season to large wadis that flood for most of the rains and flow from western Darfur hundreds of kilometres west to Lake Chad. Many wadis have pans of alluvium with rich heavy soil that are also difficult to cultivate. Western Darfur is dominated by the third feature, basement rock, sometimes covered with a thin layer of sandy soil. Basement rock is too infertile to be farmed, but provides sporadic forest cover that can be grazed by animals.

The rocks underlying this area in the south of the Vale of York are Triassic Bunter sandstone but in this area they are largely overlain by later glacial drift deposits.British Geological Survey: Sheet 71 1973 The village is sited on the slightly raised Escrick moraine. This is one of the terminal moraines that was left in the Vale of York when the ice retreated at the end of the last ice age. The resultant soils vary from thick clay to sand and alluvium and their fertility is consequently very variable.

Alluvion, is a Roman law method of acquisition of heritable property (land). The typical cause is sediment (alluvium) deposited by a river. This sediment, legally termed the accessory, accreses (ie: merges with) a piece of land, the principal, (operating a subtype of the Roman mode of acquisition by accession) and thus accedes to the ownership of the principal land over time. It continues to have relevance in the modern age, as a result of the adoption of Roman property law by modern legal systems, primarily civil law jurisdictions.

The underlying bedrock of the valley is chalk which was laid down in the Cretaceous geological period. On the sides of the valley wind blown sand and loess overlay the chalk and in the valley bottom alluvium covers undifferentiated deposits of fragmented chalk which were eroded from the hillsides in the Devensian period of the Ice Age. In pre glacial times the Great Wold Valley was the seaward outlet of the River Ure from Wensleydale but the ice sheets in the Vale of York blocked and then permanently altered the course of the Ure.

The Eureka Dunes themselves are located in the southeasternmost tip of the valley and trend north–south, parallel to Last Chance Range. According to a USGS survey map, the surrounding mountain ranges contain rocks that date back to the Mississippian and Cambrian periods while the surficial deposits on the valley floor are made up mainly of alluvium dating to the Quaternary period.Workman, J.B., C.M. Menges, W.R. Page, E.M. Taylor, E.B. Ekren, P.D. Rowley, G.L. Dixon, R.A. Thompson, and L.A. Wright. 2002. Geologic Map of the Death Valley Ground-Water Model Area, Nevada and California.

This limestone plateau contains natural cavities which have been refurbished by man in the form of three or four floors of caves, some of which include antique grain silos. The valley of the Charente is made up of old and new alluvium which provides rich soil for farming and some sandpits. These alluvial deposits were deposited successively during the Quaternary period on the inside of two meanders of the river that are Basseau and Saint-Cybard. The oldest alluviums are on the plain of Basseau and reach a relative height of 25m.

The topmost layer of soft clay was removed from the alluvium in order to found the dam on the stable sandy deposits beneath, at an elevation of approximately . The remaining deposits consisted of the alluvial materials mentioned above. These deposits had many interconnecting layers of coarse sands and gravels, necessitating the installation of a steel sheet pile wall down to the firm shale, from the left to the right abutment. An aerial view of the main Fort Peck Dam structure looking westward with Milk Coulee Bay in the foreground.

In the beginning of 2012, a sapphire and ruby rush occurred 25 kilometers south-east of Didy. The rush was due to the exceptional color, clarity and size of the precious stones found there. Discovered in alluvium, in the core of a wild forest located in the Ankeniheny-Zahamena national park, sapphires and rubies required holes from 50 centimeters to 2 meters depth to be extracted. Following the arrival of 40,000 people on the occurrence, the government ordained to evacuate the area in June 2012 and the access was denied.

Glacial till deriving from the Anglian glaciation occurs widely across the county northwards of a rough line from Brentwood through Chelmsford to Colchester. The area remained unglaciated during the more recent late-Devensian glaciation (the 'last ice age'). Sheets of glacial sand and gravel occur widely to the south of Colchester and to the east of Chelmsford and are also evident in the valleys of the Brain, Ter, Pant, Stour and Blackwater. Along the coast are extensive areas of marine and estuarine alluvium, most widespread around the Foulness Island and Canvey Island areas.

The Zuni sequence formed in the Mesozoic, during a fifth major marine transgression lasting from the Middle Jurassic into the Cretaceous. The Cretaceous geochronology of the state is unclear and debated, between some who believe the state experienced dryland conditions and others who suspect it was flooded. The only Cretaceous deposits are unconsolidated marine and delta sands together with clay in the Southeast Lowlands, beneath Pleistocene alluvium. Previously, small circular deposits of Cretaceous clay in the Ozarks were suspected to be the remains of sinkholes in Ordovician dolomite.

View of the range in Mae Chaem District Landscape in Doi Suthep National Park The Thanon Thong Chai Range (, , formerly Thanon Range; Burmese Tanen Taunggyi)North of Thailand is a mountain range in northern Thailand. Its tallest peak is Doi Inthanon, the highest point in Thailand. Most of the range is in Chiang Mai Province, with parts in Mae Hong Son and Lamphun Provinces. Geologically in the Thanon Thong Chai Range, as in the other southern subranges of the Shan Hills, layers of alluvium are superimposed on hard rock.

Based on the found tools, the inhabitants probably mined stones from some quarries, but also used the materials from the greywacke deposits and the alluvium deposits. The raw materials were most likely exploited from the narrow, local area. Abundance of the "light white stone" artifacts doesn't match the materials used in other surrounding localities at the time: in Vinča itself they used magnesite, diatomite in Ilića Brdo, tuff in another locality of the same name Crkvine, near Mali Borak, etc. It appears that each settlement exploited the materials available in their immediate vicinity.

The rivulets that drain the plateau beneath Barbaggio and nearby Patrimonio gather into a single stream, the Ruisseau la Strutta or Rivière de la Strutta which, flowing between cliffs, crosses a short alluvial plain and empties into the Gulf of Saint Florent. Route D81 leaving Saint-Florent bears north-east along the alluvium and turns inland through the gorge. Just over the Barbaggio border at the base of a cliff is the prehistoric Abri de Strette meaning "Strette Shelter" where strette means "narrow place". It is one of the oldest continuously occupied sites in Corsica.

The streambed of Keeler Creek, including many clam shells The elevation near the mouth of Keeler Creek is above sea level. The elevation of the creek's source is between above sea level. The surficial geology in the vicinity of the lower reaches of Keeler Creek mainly consist of alluvium (containing stratified sand, silt, and gravel), Wisconsinan Outwash, and sand and gravel pits with steep sides that can be dozens of feet deep. Further upstream, the surficial geology mainly consists of a glacial or resedimented till known as Wisconsinan Till.

Erigeron wilkenii is a rare North American species of flowering plant in the daisy family known by the common names Wilken's fleabane and Dieter's erigeron. It has been found only inside Dinosaur National Monument in the US state of Colorado.Tropicos, Erigeron wilkenii O'KaneBiota of North America Program 2014 county distribution map Erigeron wilkenii grows in the alluvium and rocky slopes inside a sandstone canyon. It is a perennial herb up to 20 centimeters (8 inches) tall, producing a thin taproot but not spreading to create clumps as is the case with many related species.

Ecological Subregions of the United States; Chapter 28; Prairie Parkland (Temperate), Section 251C--Central Dissected Till Plains; U.S. Forest Service; Rocky Mountain Region, Denver, Colorado; Obtained January 8, 2019 Loess (unconsolidated aeolian silt), as much as thick thins toward the east, covers most uplands. Pleistocene (pre-Illinoisan) till lies beneath the loess, covering the bedrock up to deep. Along the edges, it thins to less than . The Mississippi and Missouri floodplains have up to of unconsolidated Tertiary and Quaternary alluvium (gravel, sand, silt, and clay) over the bedrock, thinner in the river valleys.

Bridport is composed of several small suburban districts, some of which used to be separate villages. These include Allington, Skilling, Coneygar, Bothenhampton, Bradpole, Court Orchard and St Andrew's Well. One and a half miles from the town centre and within the town's boundary is West Bay, a small fishing harbour known as Bridport Harbour until the arrival of the railway. The geology of Bridport comprises rocks formed in the Pliensbachian, Toarcian, Aalenian, Bajocian, Bathonian and Callovian ages of the Jurassic Period, overlain by superficial Quaternary deposits of alluvium alongside the rivers.

Wormingford has a post office and a public house and restaurant called The Crown. Most of the parish lies on a relatively high plain which drains northwards to the River Stour and southwards to the River Colne. From the Stour the ground rises southwards to reach a height of more than 225 ft (70 m) in the south-west. A band of alluvium runs beside the Stour and there are river terrace deposits south of that, then, as the ground rises, bands of London clay, and sands and gravels.

Slurry pipelines are also being considered to desilt or remove silts from deposits behind dams in man-made lakes. After the Hurricane Katrina disaster there were proposals to remedy the environment by pumping silt to the shore. Proposals have also been made to de-silt Lake Nubia-Nasser in Egypt and Sudan by slurry pipelines, as Egypt is now deprived of 95% of its alluvium, which used to arrive every year. These projects to remedy the environment might alleviate one of the major problems associated with large dams and man-made lakes.

Residents of An Phú District are mainly farmers; most of the area is under rice cultivation with alluvium soil and freshwater which also allows much fishing. Every year, when all the communes are affected by water the fields become inundated. On the Cambodian border on the other side, opposite the town of Long Bình is a market area of Cambodia known as Chrey Thum (Koh Thum). As the road from An Phú to the capital Phnom Penh is Cambodia's most recent road from Vietnam, it has created good conditions for trade in the region.

The İğneada Floodplain Forests National Park (), established on November 13, 2007, is a national park located within Kırklareli Province in Marmara Region of Turkey. The national park covers an area of and is located at İğneada town on the Turkish-Bulgarian border at far from Demirköy district of Kırklareli Province. Streams running down from the Strandzha mountain range towards Black Sea formed alluvium on the shore, where floodplain () occurred due to seasonal floodings. The protected area is administered by the Directorate-General of Nature Protection and National Parks () of the Ministry of Environment and Forest.

The surficial geology of the surrounding valley in the lower reaches mainly includes bedrock and a till known as Wisconsinan Till. Further upstream, the surficial geology along the creek includes some alluvium, but mostly Wisconsinan Till. There are also a few patches of wetlands and lakes. The valley of Bell Creek in its upper reaches includes a "beaded valley" that was little affected by glacial erosion but considerably affected by glacial deposition, to the point that large amounts of glacial till partly or fully block off individual valleys.

The commune is made up of Campanian (Upper Cretaceous) chalk limestone, which covers a large part of the South Charente. The valleys are covered by alluvium from the recent Quaternary period.BRGM Map on the GéoportailInfoterrain Visualiser, BRGM website Printed Notice from Cognac, BRGM, consulted on 20 November 2011 The communal land has a quite hilly relief which rises gradually to reach, at its northern end near the hamlet of la Voûte, a height 95 m. The small Collinaud valley in the south of the commune is located where the town and the main road are.

The town sits on flat ground consisting mostly of clay with soil that is sand and alluvium, near the old Forest of Galtres. To the north is a small tributary of the River Foss called Golland Dike, and to the east is the River Foss which flows southward. The nearby village of Wigginton now merges with Haxby though the old Parish Boundary map still shows the dividing line. This runs east to west along the back of the houses on Wheatfield Drive on its southern edge as far as Barley Drive.

Situated on the banks of the river Jamuna, Gaighata is located at . Gaighata CD Block is bounded by Bangaon CD Block in the north, Sharsha Upazila in Jessore District of Bangladesh in the east, Swarupnagar and Habra I CD Blocks in the south and Haringhata CD Block in Nadia district in the west. Gaighata CD Block is part of the Ichhamati- Raimangal Plain, one of the three physiographic regions in the district located in the lower Ganges Delta. It contains soil of mature black or brownish loam to recent alluvium.

In a 2006 United States Geological Survey survey of the depth to water and water-level altitude in Arizona, the younger alluvium surficial deposits atop Santa Claus were viewed as ranging from unconsolidated to strongly consolidated alluvial deposits. Residing in the Sacramento Valley basin, the ground water in Santa Claus is contained in a basin-fill aquifer and other water-bearing sediments at a depth of approximately below the land surface. Additionally, the underground water level resides approximately at an altitude of above mean sea level and is moving directly South.

Kimberlites are peculiar igneous rocks because they contain a variety of mineral species with chemical compositions that indicate they formed under high pressure and temperature within the mantle. These minerals, such as chromium diopside (a pyroxene), chromium spinels, magnesian ilmenite, and pyrope garnets rich in chromium, are generally absent from most other igneous rocks, making them particularly useful as indicators for kimberlites. These indicator minerals are generally sought in stream sediments in modern alluvial material. Their presence may indicate the presence of a kimberlite within the erosional watershed that produced the alluvium.

The San Joaquin series became the official state soil on August 20, 1997, the result of efforts by students and teachers from Martin Luther King, Jr. Middle School in Madera, natural resource professionals, the Professional Soil Scientists Association of California, legislators, and various state universities. These soils are used for irrigated crops, such as wheat, rice, figs, almonds, oranges, and grapes, and for pasture and urban development. San Joaquin soils formed in old alluvium on hummocky topography. A cemented hardpan a few feet beneath the surface restricts roots and water percolation.

Most of the Dearne Valley area lies on the coal measures, comprising Carboniferous sandstone and slate with seams of coal. The valleys contain fertile alluvium deposited by their rivers, and the sandstone forms rolling ridges cut by the broad floodplains. The area has been settled continuously since prehistoric times, with villages developing on the drier sandstone ridges above the flood plain from at least the late Saxon period. Mining is recorded from at least the 13th century, and probably back to Roman Britain,Ling et al (2003) pp. 30–33.

The foundation excavations were extended below the original ground surface to remove liquefaction soils that would have made the dam unstable in an earthquake. To minimize foundation seepage through the alluvium, thick cut-off walls of plastic concrete were constructed across the three alluvial channels and excavated at least into bedrock. To reduce seepage through the rock foundation, the entire core width was consolidation grouted and a double-line grout curtain was installed to a depth of approximately . Grouting of the west dam took about two years to complete and required of grout holes.

To the east, the Monts du Matin extend as a long barrier of pleasant hills, dominated by the limestone prow of the Vercors. To the south, beyond the Drôme Valley, the plain ends at the foot of the massif carrying the vast forest of Marsanne, topped by wind turbines. To the north, beyond the Isère Valley, the Romanais continues, geologically, Valence plain. The lower Miocene molasse in the north of the plain was covered by outwash alluvium of the Isère, whose terraces today still mark the shape of the Valentinois.

Lime, kankar and free kankar are totally absent. These soils are poor in potash, nitrogen, humus and carbonate and differ greatly in consistency, color, depth and fertility. On the uplands they are thin and gravelly, sandy, porous and light coloured alluvium, generally transported from elsewhere, are found along river banks in alternate layers of sand and silt in East Ramanujganj, North Ambikapur, and Surajpur, along the river banks of the Rihand, Kanhar, and the Hasdeo rivers and their major tributaries. The colour of the soil is not uniform but varies from yellow to grey.

Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level. The district has a long coastline of 65.5 km along its southern and south eastern boundary.

Hawai Onsen is classified as a chloride and sulfate type hot spring. This is the same classification as Tōgō Onsen, which is across Tōgō Lake on a separate shore. In 1984, Hawai Onsen produced 1,500 liters of hot spring water every minute, with a source temperature of roughly 50 degrees Celsius. High-temperature water comes out through a gap in the granite bedrock at Hawai Onsen, which can be reached by digging through a layer of alluvium roughly 30 to 60 meters thick, as well as a 40 meter thick layer of diluvium.

Chawberia, a constituent panchayat of Bangaon block, is located at . Bangaon CD Block is bounded by Bagdah CD block in the north, Sharsha Upazila in Jessore District of Bangladesh in the east, Gaighata and Habra I CD blocks in the south, and Haringhata and Chakdaha CD blocks in Nadia district in the west. Bangaon is part of the Ichhamati-Raimangal Plain, one of the three physiographic regions in the district located in the lower Ganges Delta. It contains soil of mature black or brownish loam to recent alluvium.

Equisetum pratense occurs in alluvial woods, thickets, mossy glades, and calcareous meadows. It is a common pioneer species, commonly growing where instability or water erosion leaves an often open ground surface or where sandy alluvium accumulates beside streams. Where vegetation is more abundant, the fern occurs only as sparse and diminutive shoots, as the fern is succumbing to competition in a later seral community. The plant is widespread, occurring from Iceland and northern Britain and Northern Ireland through northern and central Europe as far south as the Alps.

The Tuscan Formation was created in a series of volcanic mudflows from extinct volcanoes, Mt. Maidu and Mt. Yana, between 10 and 2 million years ago during the Pleistocene. The formation dives beneath Chico and holds the city's immense aquifer from which it derives its water. The Tuscan Formation is visible in all of Upper Park, and forms the steep canyon walls of Chico Canyon, and makes up the famous Monkey Face rock formation. Lower Bidwell Park sits atop a deep soil complex of alluvium deposited by Big Chico Creek.

It is believed that the present course of the stream had been established prior to the formation of the mountains – as they rose, the creek's erosional force cut canyons and valleys into the bedrock, maintaining its course. The Hayfork Valley is an alluvial basin filled with sediments at least deep deposited by Hayfork, Carr, Barker, Big, Salt and other streams from the surrounding water. Approximately of the alluvium dates from the Holocene less than 12,000 years ago. The valley is underlain by the Hayfork Valley Groundwater Basin which ranges from below the surface.

Compton High school The major damage occurred in the densely-populated city of Long Beach on the south-facing coast of Los Angeles County. However, the damage was also found to have extended to the industrial area south of downtown Los Angeles. The magnitude of the earthquake is considered to be medium but a significant amount of damage was left due to unfavorable geological conditions (landfill, water-soaked alluvium) combined with poorly constructed buildings. In Long Beach, buildings collapsed, water tanks fell through roofs, and houses were tossed off their foundations.

The plant is found in subtropical regions extending into tropical areas in the northern end of its range. In Western Australia it is found along creeks and streams in the Kimberley, Pilbara, Gascoyne, Mid West and Goldfields-Esperance regions where it grows in sandy- clay alluvium often around limestone. The species is also found in north western and south eastern South Australia, Victoria, Queensland, the Northern Territory and New South Wales. It will grow well in full sun to part shade in well-drained soils but can need watering in summer when cultivated.

Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level. The district has a long coastline of 65.5 km along its southern and south eastern boundary.

Liguanea ( ) is an area of the island of Jamaica. Its name came from the language of the Yamaye people who currently inhabit some of the island's rural areas in Cornwall County. and named it after the iguana lizard that is endemic to the island, and an important source of food for the Yamaye. Geographically, the Liguanea Plains are the fertile flat lands of alluvium spreading south towards Kingston Harbour, but the area known as Liguanea is only a small part of the Kingston Corporate Area, a section of the parish of St Andrew.

It is native to an area in the Pilbara and Mid West regions of Western Australia where it is commonly found in river beds, hardpans and floodplains where it grows in loam, clay, alluvium and red sandy soils. It has a discontinuous distribution and is often found around the headwaters and upper catchment areas of the Fortescue, Gascyone and Murchison Rivers where it is found on alluvial plains growing in loamy soils as a part of low woodland or shrubland communities and are known to form pure stands.

Malda Sadar subdivision covers both the Barind Tract and the Diara, two of the three physiographic subregions of the district. The Barind “is made up of the ancient alluvial humps that are remnants of old riverine flood plains that remained unaffected subsequently by inundation and renewed silting.” It forms an upland slightly higher than the surrounding areas and extends beyond the borders of the district. “The Diara is a relatively well drained flat land formed by the fluvial deposition of newer alluvium in the transitional zone between the Barind upland and the marshy Tal tract.

Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level. The district has a long coastline of 65.5 km along its southern and south eastern boundary.

Corymbia polycarpa is found in Western Australia, the Northern Territory, Queensland and northwestern New South Wales. The species is quite common between Broome and Derby in Western Australia through the Kimberley region of Western Australia extending east over the Top End of the Northern Territory including nearby islands and across the Gulf of Carpentaria and southern Cape York Peninsula in Queensland. It is found near watercourses, in depressions or on floodplains growing in sandy or silty alluvium and less commonly in cracking clays and in skeletal sandstone or lateritic soils.

An abundant calcium supply is common to most white spruce locations in New York state (Nienstaedt and Zasada 1990). Chlorosis was observed in young white spruce in heavily limed nursery soils at about pH 8.3 (Stone, cited by Nienstaedt 1957). Wilde (1966) gave 4.7 to 6.5 as the approximate optimum range of pH for white spruce in Wisconsin, but optimum growth seems possible at pH levels up to 7.0 and perhaps higher (Sutton 1968). Alluvium on the floodplains of northern rivers shows pH levels from 5.0 to 8.2 (Zasada et al. 1977).

Rock sea wall near Coast Guard Station bordering Monterey Bay National Marine Sanctuary According to the United States Census Bureau, the city has a total area of , of which is land and (28.05%) is water. Sand deposits in the northern coastal area comprise the sole known mineral resources. Local soil is Quaternary Alluvium. Common soil series include the Baywood fine sand on the east side, Narlon loamy sand on the west side, Sheridan coarse sandy loam on hilly terrain, and the pale Tangair sand on hills supporting closed-cone pine habitat.

As the and the Dordogne, the Somme Valley made reference to prehistory and to the study of the Paleolithic. It was at Amiens that, for the first time, was defined one of the most ancient civilisations of humanity: The Acheulean. In 1853, haches taillées [carved axes], according to the term of the time, were collected in the old alluvium of the Somme at the level of the suburb of Saint-Acheul, east of the city. This discovery fascinated the greatest international experts of the time, Joseph Prestwich, Hugh Falconer, Charles Lyell and John Evans, who flocked to the site.

Dating was indicated by a number of coins discovered on the stones of the patio near the pool to the north, all from the days of the Great Revolt. The latest coin is dated with "4 years to the day of the Great Revolt", meaning the year 69. In the years following the destruction, winter rains washed alluvium from the hills down to the valley and down the slopes of Mount Zion to the west of the pool; the pool was filled with silt layers (up to 4 m in some places) until it was covered completely.

The Lower Platte Alluvial Plain is an extension of the broad Platte River Valley (27g) to the west; however, this region is within the Western Corn Belt Plains and contains a combination of vegetation, soils, and climate more similar to other areas in 47. Silty, loamy, and sandy soils are formed from alluvium, though not as sandy as the Platte River Valley (27g) to the west. Land use is mainly cropland with areas of irrigated agriculture. Tallgrass prairie, wet meadows, and scattered riparian forests are the potential natural vegetation of the area, with forests generally denser and older than in region 27g.

The embankment had a 6.1 m top width, with slopes 1 V : 3 H and 1 V : 2 H respectively for the upstream and downstream slopes and a clay core extending through alluvium to the rocks below. The upstream face had a 61 cm small gravel and a 61 cm hand packed rip- rap. It had a storage capacity of 1.1 × 108 m3. The dam had a height of 22.56 m above the river bed, a 164.5 m of crest length of overflow section, and a total of 3742 m of crest length for the earth dam.

Fairly rich soils made of alluvium and tidal deposits are found along the Petitcodiac and Memramcook rivers, and have often been exploited for agricultural purposes. A publication by the New Brunswick Department of Natural Resources notes that the soils in Salisbury, made from calcareous sandstone and mudstone, are fine-textured and, when properly drained, "are the most fertile glacial tills" in the watershed. In contrast, they note, soils deriving from local conglomerates are more coarse and sandy, and are less fertile. Albertite, a type of asphalt, was first found in Albert County in 1849 by the Canadian geologist Abraham Gesner, inventor of kerosene.

Striking examples underlie the lower and middle stretches of the Weaver valley and those of the Dee and Gowy near Chester. A considerable number of small glacial meltwater channels have been identified along the Mid Cheshire Ridge such as that known as Urchin's Kitchen near Kelsall whilst larger examples occur along the edges of the Peak District. There are notable examples at Lyme Park and southwards to Bollington and again in the Bosley area, south of Macclesfield. The floodplains of the majority of watercourses in the county are composed of alluvium which has accumulated in the post-glacial period.

The regional geology in the Eastern Ghats mobile belt, where the caves are located, is represented by the khondalite suite of rocks (garnetiferrous sillimanite gneisses, quartzo-feldsphatic garnet gneisses) of Archaen age. Quaternary deposits consist of red bed sediments, laterites, pediment fans, colluvium, alluvium and coastal sands. The caves in the reserved forest area basically host a variety of speleothems of various sizes and irregularly shaped stalactites and stalagmites. The carbonate rocks are pure white, and coarsely crystalline and the deformed and banded marbles cover a triangular area of ; surrounded by diopside–scapolite–feldspar calc-granulites.

The Keilor cranium was discovered by James White in October 1940 while excavating a sand deposit near the junction of the Maribyrnong River and Dry Creek, about north of Keilor, Victoria (Mahony 1943:3). Archaeologist Sandor (Alexander) Gallus, was among the first to recognise the importance of the river terraces in the 1960s and 1970sGary Presland, Keilor Archaeological Site, eMelbourne website. Accessed 21 November 2011 and excavated the site with teams from the Archaeological Society of Victoria, the Victoria Archaeological Survey and La Trobe University focusing on the lower stratigraphic layers known as the D-Clay and the underlying Older Dry Creek Alluvium.

The Alt then flows at a low gradient across an alluvium plain in a northwesterly direction before turning southwards and emptying into the River Mersey at Hightown between Crosby and Formby. The Alt's catchment boundary reaches as far as Banks and Crossens in the north and out to Burscough and Kirkby in the east. It drains a catchment area of and flows a distance of from source to the Mersey Estuary. The river flows through varying types of land: Sherwood Sandstone in the Huyton area, Coal Measures in the West Derby area and eventually Mercia Mudstone in the Maghull/North Sefton area.

Impermeable deposits of the lake such as the "blue clay" generate groundwater accumulations that are exploited for irrigation purposes. The Verdos Alluvium of the Denver Basin may correlate to certain deposits on the shores of Lake Alamosa. While it was formerly thought that the Great Sand Dunes were formed from sediments on the floor of Lake Alamosa but later research indicated that these sediments probably played an only minor role. The development of the dunes however certainly post-dated the disappearance of Lake Alamosa as the lake would have impeded the transport of sand across the San Luis Valley.

Underground Egyptian tombs built in the desert provide possibly the most protective environment for the preservation of papyrus documents. For example, there are many well-preserved Book of the Dead funerary papyri placed in tombs to act as afterlife guides for the souls of the deceased tomb occupants. However, it was only customary during the late Middle Kingdom and first half of the New Kingdom to place non-religious papyri in burial chambers. Thus, the majority of well-preserved literary papyri are dated to this period.. Most settlements in ancient Egypt were situated on the alluvium of the Nile floodplain.

The Armenia Fault is part of the Romeral Fault System on the western slope of the Central Ranges of the Colombian Andes. The fault crosses the city of Armenia and displaces Pliocene to Pleistocene volcanic and volcano-sedimentary deposits of the Quindío Fan (), which covers about . The geometric and neotectonic features of the Montenegro and Armenia Faults are very similar. The fault forms well developed fault scarp as much as high, characterised by beheaded streams, ponded alluvium, aligned and offset drainages, soil and rock slides on the face of the scarp, and localised tilting of terrain.

Geologically, Cairo lies on alluvium and sand dunes which date from the quaternary period.El-Shazly E.M. (1977) The Ocean Basins and Margins, The Geology of the Egyptian Region (Plenum press, New York-London) “The Eastern Mediterranean.” Retrieved 20 September 2020El-Sohby M.A., Mazen S.O (1985) Proceedings, Eleventh International Conference on soil Mechanics & Foundation Engineering (san Francisco), Geological Aspects in Cairo subsoil Development, 4, pp 2401–2415. Retrieved 20 September 2020 Until the mid-19th century, when the river was tamed by dams, levees, and other controls, the Nile in the vicinity of Cairo was highly susceptible to changes in course and surface level.

None of this geologic structure is visible on the ground surface since the Central Valley is wide and flat, but enough wells had been drilled in the general vicinity to give early prospectors the idea that a petroleum reservoir might be nearby. Underneath several hundred feet of Holocene-age alluvium, deposited by thousands of years of runoff from the mountains that ring the Central Valley, is the Pleistocene Tulare Formation, which forms an impermeable cap to the underlying San Joaquin Clay, the principal gas-bearing unit. This unit varies in thickness from 2,200 to , and has an average porosity of 28%.

The Sub-Himalaya tectonic plate is sometimes referred to as the Cis-Himalayan tectonic plate in the older literature. It forms the southern foothills of the Himalayan Range and is essentially composed of Miocene to Pleistocene molassic sediments derived from the erosion of the Himalaya. These molasse deposits, known as the "Murree and Sivaliks Formations", are internally folded and imbricated. The Sub-Himalayan Range is thrust along the Main Frontal Thrust over the Quaternary alluvium deposited by the rivers coming from the Himalaya (Ganges, Indus, Brahmaputra and others), which demonstrates that the Himalaya is still a very active orogen.

The Sierra de Luquillo consists of a series of summits linked by a horseshoe-shaped ridge. Running from west to east, the peaks include El Toro, El Cacique and El Yunque, joined by a ridge known as Cuchilla el Duque to Pico del Oeste and Pico del Este. The mountains were formed by tectonic activity some 37 to 28 million years ago, the island being on the junction between the North American Plate and the Caribbean Plate. The main rock types are pyroclastic rocks, quartzdiorite and contact metamorphic hornfels, with some outcrops of alluvium, basalt and mafic rocks.

Seasonal bushfires, flooding and erosion evoke an ever-changing mosaic of riverine forest and grasslands along the river banks. On recently deposited alluvium and in lowland areas groups of catechu (Acacia catechu) with rosewood (Dalbergia sissoo) predominate, followed by groups of kapok (Bombax ceiba) with rhino apple trees (Trewia nudiflora), the fruits of which rhinos savour so much. Understorey shrubs of velvety beautyberry (Callicarpa macrophylla), hill glory bower (Clerodendrum sp.) and gooseberry (Phyllanthus emblica) offer shelter and lair to a wide variety of species. Terai-Duar savanna and grasslands cover about 20% of the park's area.

Somewhat paradoxically, however, Eis (1967a)Eis, S. 1967a. Establishment and early development of white spruce in the interior of British Columbia. For. Chron. 43:174–177. observed that on both mineral and litter seedbeds, seedling mortality was greater in moist habitats (alluvium and Aralia–Dryopteris) than in dry habitats (Cornus–Moss). He commented that in dry habitats after the first growing season surviving seedlings appeared to have a much better chance of continued survival than those in moist or wet habitats, in which frost heave and competition from lesser vegetation became major factors in later years.

Due to significant glacial and stream erosion throughout the recent geologic past, many parts of Massachusetts have shallow depth to bedrock of only a few feet, although some areas have sediment over 500 feet thick. Much of the soil and sediment in the state was deposited during the Pleistocene glaciations and takes the form of glacial till, moraine deposits, and glacial stratified deposits commonly found in valleys and low-lying areas. Swamps and flood plain alluvium typically emplaced more recently in the Holocene. Bedrock tends to be unweathered, but thick saprolite deposits have formed in parts of the Housatonic River valley.

It is native to Pilbara and Kimberley regions of Western Australia with the range extending into western parts of the top end and central parts of the Northern Territory. It has a scattered distribution with the bulk of the population situated in the Tanami Desert straddling the border between Western Australian and the Northern Territory. Disjunct populations are found near Onslow from Yanrey Station to Minderoo Station and around Telfer. It is often found in cracking clay pans and in clay depressions along drainage lines but also in sandy alluvium type soils in minor watercourses and in clay or sandy loam soils.

The bridge (2003) The bridge consisted of four fixed spans, one swing span and a fifth swing span, and carried a double-track railway.The swing bridge runs east west, the swing section is closer to the east bank of the river. (Ordnance Survey, 1891, 1:2500) Pier foundations for the bridge spans were of base diameter cast iron cylinders, which tapered to diameter at the high water level, each column was around long. The piers were sunk into the river alluvium using a mass placed on them, and then by the pneumatic Caisson process until bedrock was reached.

Glacial material and sediment covers some lava flows, and deep wells have found buried lava flows at depths of . The basement in the region is formed by plutonic rocks of Mesozoic age, metasedimentary and metavolcanic rocks which crop out in the White Mountains and the Sierra Nevada; the valley floor is covered with alluvium. Tectonically, Owens Valley is a graben formed by the movement of the Sierra Nevada-Great Valley block with respect to the rest of North America. Farther south lies the Coso volcanic field, which is also geothermally active unlike Big Pine volcanic field.

Bay Area newspapers reported on aftershocks that were felt in a number of locations. These shocks were only reported at locations that were within the intensity VII or higher isoseismals. The Sonoma Index-Tribune reported that at Sonoma there were four strong aftershocks and more than twenty lighter shocks (that at most just rattled windows) later that night. The San Francisco Call stated that while the aftershocks were heaviest near Tubbs Island, they were more frequent near Lakeville at the Petaluma marshes, and this was interpreted as the alluvium under the island suppressing the lighter shocks.

Wave action in the lake washed sediments back and forth in the shallows on the southwestern shore, forming ooids and depositing them on steeper benches near the shore in 2- to 40-foot thicknesses. When the lake drained (2 to 4 million years ago), the oolite was left behind, along with siltstone, volcanic tuffs and alluvium from adjacent mountain slopes. The other sediments eroded away, while the more resistant oolite weathered into hummocks, small arches and other intriguing natural "sculptures." The Shoofly Oolite lies on public land west of Bruneau, Idaho managed by the Bureau of Land Management (BLM).

The river has a catchment area of of which an area of is composed of estuarine wetlands. The floodplain is composed of reddish grey sand loam produced from the underlying sand material of Cainozoic age. The underlying geology is predominantly alluvium of Quaternary age with areas of older rock made up of sandstone of Middle Jurassic age in the Bathurst Range and the granite of Late Silurian age in the Great Dividing Range of the upper catchment. Fringing vegetation is made up of Stringybark, Bloodwood, Moreton Bay Ash and Ironbark trees with a ground cover of coarse grasses such as speargrass.

Tōgō Onsen is classified as a chloride and sulfate type hot spring, with a spring source temperature of 85 to 94 degrees Celsius. Tōgō Onsen’s hot spring waters can be found near Matsuzaki station. Here, there is a 300-meter deep cavity in the layer of granite bedrock. This cavity is filled in with conglomerate sedimentary rock, called the Oshikagawa pyroclastic layer, along with diluvium and alluvium layers on top of it. Tōgō Onsen’s water originates from the granite, Oshikagawa, and diluvium layers, and its heat source is thought to be waste heat from the granite layer.

The Mounds Gravel remains as gravel alluvium from the Teays River, which once flowed north of current day St. Louis transporting sediments shed by the rising Rocky Mountains. Some geologists have suggested that the Mounds Gravel originated from erosion of the Central Highlands, when a large river flowed south through Kansas and Oklahoma to the Gulf of Mexico, until it was rechanneled to the present Mississippi River during the Illinoian glaciation. As Missouri experienced terrestrial erosion in the Pliocene, the Ozark Dome uplifted. Missouri did experience the Pleistocene glaciations, with the most recent glacial till from 600,000 years ago.

Then it narrows again as the river flows west out of the valley through a narrow canyon between the Sierra Madre and La Panza ranges, to the Santa Maria Valley and its river mouth on the Pacific Ocean. The agricultural fields are in the center of the valley, near the Cuyama Highway junction and the two primary towns, where the alluvium is rich and the valley is a wide floodplain.Lantis, Steiner, Karinen, p. 193-4 North of the major portion of the valley is the Caliente Range rises, over which is the Carrizo Plain, a much larger inland valley.

The relief of the delta's landscape is low but not flat.Profile of the Irrawaddy Delta from Henzhada to the river mouth, in feet The soils consist of fine silt, which is replenished continuously by fertile alluvium carried downstream by the river. As a result of heavy rainfall varying from a year in the delta,Map on the rainfall in Myanmar retrieved 17-12-2008. and the motion and sediment load of the river,A detailed documentation of sediment dynamics can be found in The Journal of Geology the delta surface extends into the Andaman Sea at a rate of about per year.

The Northern Pleistocene Valley Trains ecoregion is a flat to irregular alluvial plain composed of sandy to gravelly glacial outwash overlain by alluvium; sand sheets, widespread in the St. Francis Lowlands (73c), are absent. The Pleistocene outwash deposits of Ecoregion 73b are usually coarser and better drained than the alluvial deposits of Ecoregions 73a, 73d, and 73f. They were transported to Arkansas by the Mississippi River and its tributaries and have been subsequently eroded, reduced in size, and fragmented by laterally migrating channels or buried by thick sediments. Ecoregion 73b has little local relief or stream incision.

Formerly this area was part of the northern branch of Lake Como, which extended as far north as Samolaco, known in antiquity as (Latin for "Head of the Lake"). Subsequently, the frequent flooding of the Adda deposited alluvium and formed the Pian di Spagna, thus separating the two lakes. The lakeside settlements include Novate Mezzola to the north, Verceia, San Fedele and Bocca d'Adda (once the mouth of the Adda) on the eastern shore, and Dascio and Albonico, (both frazioni of the commune of Sorico) to the west. The 10th- century lakeside Tempietto di San Fedelino, is near the northern shore.

The creek flows southwest and then south through the dissected Allegheny Plateau, through rock from the Mississippian sub- period and Devonian period. Much of the Plunketts Creek valley is composed of various glacial deposits, chiefly alluvium. Although the Plunketts Creek watershed was clear-cut and home to a tannery, sawmills, and a coal mine in the nineteenth century, today it is heavily wooded and known for its high water quality, fishing, and other recreational opportunities. The watershed now includes parts of the Loyalsock State Forest, Pennsylvania State Game Lands, and a State Game Farm for raising pheasant.

However, Meginness (1892) refers to coal mines in Plunketts Creek Township, and there is an unnamed tributary of Plunketts Creek in "Coal Mine Hollow" on the right bank between Dry Run and King Run, so it seems a small coal mine operated there in the past. Much of the Plunketts Creek valley (and those of its tributaries) is composed of various glacial deposits. Closer to the mouth, there are large deposits of alluvium, as well as alluvial fan and alluvial terraces. Many of the glacial deposits are associated with the Wisconsin glaciation, with stratified drift and till, as well as outwash present.

Alluvium begins to be seen about midway down the Spruceton Valley, with outwash visible as the stream bends towards the north at the hamlet of West Kill. Closer to Lexington and the stream's mouth there are some kame areas along the banks. Most of the eroded bedrock that has reached the West Kill's streambed is, in its upper reaches, imbricated, worn into small plate-shaped rocks that nest with each other in a scale-like pattern. There are also areas where the bedrock forms lateral and vertical grade controls, Diamond Notch Falls being the most prominent example.

Schaber, Gerald G. "The U.S. Geological Survey, Branch of Astrogeology—A Chronology of Activities from Conception through the End of Project Apollo (1960–1973)", 2005, U.S. Geological Survey Open-File Report 2005-1190. (PDF) Since the crater's formation, the rim is thought to have lost of height at the rim crest as a result of natural erosion. Similarly, the basin of the crater is thought to have approximately of additional post-impact sedimentation from lake sediments and of alluvium. These erosion processes are the reason that very few remaining craters are visible on Earth, since many have been erased by these geological processes.

Ground displacement damaged sidewalks and roads, with cracks in the more rigid asphalt and concrete often exceeding the width of the shift in the underlying soil. Accentuated damage near alluvium had been documented during the investigation of the effects of the 1969 Santa Rosa earthquakes. A band of similarly intense damage further away near Ventura Boulevard at the southern end of the valley was also identified as having been related to soil type. Federal, county, and private hospitals suffered varying degrees of damage, with four major facilities in the San Fernando Valley suffering structural damage, and two of those collapsing.

Two to four earthquakes occurred during the Holocene in the last 6,000 years, one of which occurred 1,100–1,300 years ago and the other 2,000–2,900 years ago. The dates have been obtained through radiocarbon dating on soil in trenches dug in the fault scarp and of offset alluvium deposits. Additional faulting appears to have occurred over 12,000 years ago, but evidence thereof was partly eroded away during a time of a wetter climate and prior to the Holocene the fault might have been inactive for 100,000–130,000 years. The slip rate has been estimated to be , which is typical for intraplate faults.

The total population for the great spotted woodpecker is estimated at 73.7–110.3 million individuals, with 35% of the population in Europe. The breeding range is estimated as , and the population is considered overall to be large and apparently stable or slightly increasing, especially in Britain, where the population has recently overspilled into Ireland. For this reason the great spotted woodpecker is evaluated as a species of least concern by the IUCN. Breeding densities have been recorded as between 0.1–6.6 pairs/10 ha (0.04–2.7 pairs/10 acres), with the greatest densities in mature forest growing on alluvium.

The geology of the site consists mostly of the Triassic Hawkesbury Sandstone with some sections of the park having the more recent richer Wianamatta shale capping. Deep below the Hawkesbury sandstone belt lies Narrabeen Shales which is mixture of shale and sandstone under which and within which are untapped coal seams which run right through Sydney and are mined extensively where they come closer to the surface south of the National Park near Wollongong. Sections of recent alluvium fringes of estuarine watercourse where the endangered ecological communities; swamp oak woodlands and swamp mahogany woodlands grow still.

During the Quaternary Period, the most recent one million years, Pleistocene terraces were laid down along the major rivers in this area of the United States, with Holocene alluvium that are at least thick and contain sand, gravel, silt, clay and volcanic ash. The next layer was formed during the Permian Period, which occurred 230 to 270 million years ago. This consists of red sandstone and shale which is to thick, with gypsum on the outcroppings. The Permian "redbeds" are subdivided into the Cimarronian Series (2850 feet) at the base, overlain by the Custerian Series (400 feet, top eroded).

Most of the parish is a little over above sea level with the extensive nearby ings being even lower. The village is surrounded by arable farmland and patches of woodland. The soil consists of the alluvium of the Ouse flood-plain and patches of glacial sand and gravel east of the village and in the north-west is covered with outwash sand and clay. Streams draining into the Ouse include Wood Dike, which forms a short section of the southern parish boundary, and Howden Dike, which joins the river at the north end of the village.

The main lies mostly within London Clay with sections within the overlying alluvium and underlying Lambeth Group and Thanet Sand. The predominance of the London Clay lengths is by design, as being easily excavated, largely impermeable and somewhat self-supporting for short periods it is a near-ideal tunnelling material. Where the hydraulics have required entry into the Lambeth Group and Thanet Sand, tunnelling was considerably more difficult. In particular, the Thanet Sand requires a high boring torque, is highly abrasive and, most challengingly, sufficiently permeable to contain a water table continuous with the underlying Chalk and measured at pressures up to .

Pamban Island in which Rameswaram is located Most of the area is covered by the unconsolidated sediments of the Quaternary age except in the northwestern part, where isolated patches of Archaean crystallines and Tertiary sandstone are exposed. The Archaeans are mainly represented by the Charnockite group of rocks comprising garnetiferous granulite and the Khondalite group of rocks made up of quartzite and gneisses. The Tertiary sandstone (Cuddalore Formation) comprises pinkish, yellowish, reddish (variegated colours) medium to coarse grained sandstone and clay stone. It is overlain by thin alluvium and exposed towards the north of the Vaigai River.

The Li River and tributaries drain the area from Guilin to Yangshuo, descending from 141 m at Guilin to 103 m at Yangshuo. Mean flow past Guilin is 215 cubic metre per second, and alluvium sediments consisting of well sorted gravels covered by silty sand, form floodplains and terraces along its route. Yet, it is the 2,600 m of Devonian and Carboniferous limestones and karst terrain within the Guilin Basin, that gives the area a dramatic landscape. Two distinctive types of karst are found, Fengcong, and Fenglin, which have evolved for the past 10-20 million years, within the Cenozoic.

The municipality of Yabucoa is located in the south-eastern coast of Puerto Rico. The valley of Yabucoa is surrounded by the hills of the San Lorenzo Batholith on three sides and by the Caribbean Sea on the fourth. The hills surrounding the Yabucoa valley as well as the bedrock underlying the alluvium in the valley are composed of the San Lorenzo Batholith, a large, igneous intrusive body emplaced during the Late Cretaceous (Rogers, 1977; Rogers and others, 1979). The San Lorenzo Batholith is a composite body that is composed of gabbro (Kd), diorite, tonalite, granodiorite, and quartz monzonite.

Outlet Creek is an Eel River tributary draining the Little Lake Valley northerly through a canyon of the California Coast Ranges.DeLorme California Atlas and Gazetteer (1st edition) (2008) map 47 The Northwestern Pacific Railroad bridges the creek twelve times, following it through the canyon. California State Route 162 bridges the creek once, following the canyon closely downstream of Longvale, California, and U.S. Route 101 bridges the creek twice, paralleling it less closely upstream of Longvale. After leaving Quaternary alluvium of the Little Lake Valley, the canyon exposes undivided Cretaceous marine sedimentary and metasedimentary rocks upstream of Longvale and Franciscan Assemblage downstream of Longvale.

Basingstoke is situated on a bed of cretaceous upper chalk with small areas of clayey and loamy soil, inset with combined clay and flint patches. Loam and alluvium recent and pleistocene sediments line the bed of the river Loddon. A narrow line of tertiary Reading beds run diagonally from the northwest to the southeast along a line from Sherborne St John through Popley, Daneshill and the north part of Basing. To the north of this line, encompassing the areas of Chineham and Pyotts Hill, is London clay, which has in the past allowed excavation for high quality brick and tile manufacture.

Rajarhat Bishnupur, a constituent panchayat in Rajarhat block, is located at . Rajarhat CD Block is bounded by Barasat II CD Block in the north, Bhangar II CD Block in South 24 Parganas district in the east and south, Rajarhat-Gopalpur Municipality and Bidhannagar municipality (both part of Bidhannagar Municipal Corporation since 2015) in the west. Rajarhat CD Block is part of the North Hooghly Flat, one of the three physiographic regions in the district located in the lower Ganges Delta. It is a raised alluvium area along the Hooghly, which forms the western boundary of the district.

Elsdon 1997, p. 7 The bedrock under the western half of the town belongs to the Great Oolite Group of Jurassic Sandstone, Limestone and Argillaceous rocks formed 168−165 million years ago; Kellaways and Oxford Clay formations, dated to 165–156 million years ago, underlie the eastern half. Alluvium deposits are found along the Slea's course, and Fen sand and gravel are found to the east and south. The town is on the edge of the Fens, a low- lying region of the East of England which, before drainage from the 17th to the 20th centuries, were marshy and liable to flooding.

Rochester lies within the area, known to geologists, as the London Basin. The low-lying Hoo peninsula to the north of the town consists of London Clay, and the alluvium brought down by the two rivers—the Thames and the Medway—whose confluence is in this area. The land rises from the river, and being on the dip slope of the North Downs, this consists of chalk surmounted by the Blackheath Beds of sand and gravel. As a human settlement, Rochester became established as the lowest river crossing of the River Medway, well before the arrival of the Romans.

Augury was founded in 2011 by Saar Yoskovitz, who currently serves as their CEO, and the company's Chief Technology Officer Gal Shaul. In 2015, the company received $7 million in investment from a Series A round of funding, in 2017, it received $17 million in venture funding,Industrial IoT Startup Augury Secures $17 Million In Series B Funding To Expand Partnership Strategy and in 2019, it received an investment of $25 million in a Series C venture capital round, bringing its investment total to $51 million. The company has offices in New York and Haifa, Israel. In January 2019, Augury acquired Alluvium.

Despite these historic impacts this block is of conservation significance as it is the largest remaining area of complex mesophyll vine forest on alluvium within the Wet Tropics biogeographic region. In addition small areas of Complex Mesophyll Vine Forest on rocky basalt slopes remain on hills adjacent to Jarra Creek. The Department of Defence has managed the TTA over past 20 years has and used the area for jungle training. The TTA is currently managed under an Environmental Management Plan (EMP), developed in 1997, that is consistent with the protection of Wet Tropics of Queensland World Heritage values.

Mekong River in Khong Chiam At Khong Chiam the Mun River, the biggest river of the Khorat Plateau, joins the Mekong, which forms the northeastern boundary of Thailand with Laos. It is called "Maenam Song Si" or the "Mun River alluvium" because the brown water from Mekong River mixes with the blue water of the Mun. It is about from Ubon Ratchathani city centre. The area in the Dângrêk Mountains where the borders of the three countries, Thailand, Laos, and Cambodia meet is promoted as the "Emerald Triangle", in contrast to the "Golden Triangle" in the north of Thailand.

The village and parish lies on a bedrock of Oxford clay and in regions there are superficial Glaciofluvial and River Terrace deposits of sand and gravel from the Quaternary period, together with alluvium (clay and silt) from the same period. The land in the north of the parish is characterised as Oadby Member Diamicton, again from the Quaternary period, with rocks formed during Ice Age conditions by glaciers scouring the land. The village, which is approximately above sea level, lies just to the north of Junction 16 of the A14 road that runs from the Port of Felixstowe to the Catthorpe Interchange, Leicestershire.

Cassiterite (tin ore) from Botallack Mine, St Just Wolframite from the Camborne-Redruth-St. Day District of Cornwall Lee Moor china clay pit showing hydraulic mining in progress Large mineral deposits are found in the vicinity of the batholith and these have been mined for thousands of years. The area has been famous for its tin since about 2000 BC. The minerals formed when fluids escaped along fractures in the hot granite as it cooled and are typically found in veins or washed into streams to form alluvium. The mineral deposits are associated with multiple lodes and fractures that dip steeply and cut across both the granites and the country rocks.

Nijhum Dwip (03) Nijhum Dwip (Char Osmani, Baluar Char, Golden Island )Abdul Aouwal, "Nijhum Dwip National Park Bangladesh", Ontaheen, 16 June 2016 2:50 pm is a small island under Hatiya upazila of Noakhali. A cluster of islands (mainly, Ballar Char, Kamlar Char, Char Osman and Char Muri) emerged in the early 1950s as alluvium in the shallow estuary of the Bay of Bengal on the south of Noakhali. These new sandbanks first drew the attention of a group of fishermen, who named it Baular Char. In 1974 the Forest Department began an aforestation program for twenty years on the north side of the island.

It can progress through the fluvial system through facies changes from hillslope colluvium, to floodplain and wetland alluvium, to fine-grained lacustrine and estuarine slackwater deposits. The temporal nature of LS is time-transgressive, meaning that initiation and peak rates of deposition can take place at different times within a fluvial system, as well as at different times between regions. The intermittent transport of LS can be thought of as a cascading system that reworks LS deposits from hillslopes, into channels and onto floodplains, such that anthropogenic sediment will be mixed with and non-anthropogenic sediment. River systems record past and present imprints of anthropogenically-forced changes to the environment.

The La Plata or Chusma Fault extends across the eastern slope of the Central Ranges of the Colombian Andes, southeast of the city of Neiva in southwestern Colombia. The fault displaces Triassic, Jurassic and Cretaceous sedimentary rocks, as well as Tertiary volcanic rocks. Coalescent Quaternary alluvial fan deposits are offset by the La Plata Fault. The trace is characterised by old retreated and declined scarps, en-echelon semiparallel associated faults that cut alluvial deposits of the Páez River and local lahar deposits, a well developed topographic fault-line expression, and a probable pull-apart basin filled with Quaternary alluvial fans and alluvium near the town of La Plata.

Mount Lebanon and eastern Anti-Lebanon mountain ranges Lebanon is divided into four distinct physiographic regions: the coastal plain, the Lebanon mountain range, the Beqaa valley and the Anti-Lebanon mountains. The narrow and discontinuous coastal plain stretches from the Syrian border in the north where it widens to form the Akkar plain to Ras al-Naqoura at the border with Israel in the south. The fertile coastal plain is formed of marine sediments and river deposited alluvium alternating with sandy bays and rocky beaches. The Lebanon mountains rise steeply parallel to the Mediterranean coast and form a ridge of limestone and sandstone that runs for most of the country's length.

The major part of the catchment consists of generally fine grained felspathic sandstone beds up to one metre thick interbedded with dark grey shale and siltstone of Middle to Upper Ordovician age. There is a small area of intrusive rock of Devonian age consisting of granite and granodiorite near Paddys Hill and a larger area of similar material of Silurian age at Mount Selwyn. Along the middle reaches of the Buckland River there are alluvial and colluvial deposits of Pleistocene age consisting of clay, silt, sand, gravel and conglomerate. Recent deposits of alluvium with a similar composition extend along the river channel for about 2.5 km upstream of the Buckland Bridge.

Geologic map of Hispaniola. Mzb are Mesozoic amphibolites and associated metasedimentary rocks, Ki are Cretaceous plutons, Kv are Cretaceous volcanic rocks, uK are Upper Cretaceous marine strata, Ku are Cretaceous sedimentary and volcanic rocks, K are Cretaceous marine strata, IT are Eocene and/or Paleocene marine strata, uT are Post- Eocene marine strata, T are Tertiary marine strata, V are volcanic rocks, and Q are Quaternary alluvium. The black triangles indicate the Late Eocene Hatillo Thrust fault. The island has the largest economy in the Greater Antilles, however most of the economic development is found in the Dominican Republic, the Dominican economy being nearly 800% larger than the Haitian economy.

Someșul Mic (formed by the confluence of Someșul Rece with Someșul Cald) originates in the Apuseni Mountains, and Someșul Mare springs from the Rodna Mountains. Someșul Mare has a length of 130 km and an area of 5,033 km2 and a slight asymmetry in favor of the left side of the basin. For the entire basin of Someș, the asymmetry on left becomes pronounced between Dej and Ardusat to change in the opposite direction after receiving the Lăpuș on the right side. The valley of Someșul Mare has much auriferous alluvium that, until the early 20th century, were brought to the surface using traditional tools.

The village and parish lies on a bedrock of Oxford clay and in regions there are superficial Glaciofluvial and River Terrace deposits of sand and gravel from the Quaternary period, together with alluvium (clay and silt) from the same period. The land in the north of the parish is characterised as Oadby Member Diamicton, again from the Quaternary period, with rocks formed during Ice Age conditions by glaciers scouring the land. The village, which is approximately above sea level, lies on the B660 just to the north of Junction 16 of the A14 road that runs from the Port of Felixstowe to the Catthorpe Interchange, Leicestershire.

This tunnel was dug using the method of wooden planks on top of a foundation made of chalk and shale. It contains a lining of iron positioned under a brick roof. The construction of the tunnel on the rive droite was more delicate because of its less solid alluvium, thus three additional beams were required which were assembled at Mirabeau. The presence of a railroad line running from Invalides to Versailles (line C of the RER) made work particularly difficult, and a final beam was buried under the tunnel. Work began in August 1907 but was not finished until 1913, also delayed by the 1910 Great Flood of Paris.

Syngenetic ice wedges, like the epigenetic variety, find their roots in the geological term syngenetic, which means forming at the same time as the surrounding material. This is because syngenetic ice wedges grow as the upper permafrost surface rises in response to the addition of material on the ground surface. This allows syngenetic ice wedges to grow very deep, as the surface around them rises with the accumulation of alluvium (in floodplains), peat (in tundra), and gelifluction deposits (at the bottom of a slope), among other materials. Syngenetic ice wedges may only form if the thermal contraction and subsequent ice-veinlet growth can keep pace with the addition of new material.

The craters of Qal'eh Hasan Ali are constructed within a basement of Eocene volcanic rocks and granodiorite, with the exception of the two outlying craters which are found in desert alluvium. Qal'eh Hasan Ali lies on the Lut block, over continental crust with a thickness exceeding . Qal'eh Hasan Ali and several volcanic centres and more farther north may be part of an alkaline volcanic province associated with the Nayband strike-slip fault, the projection of which crosses the Qal'eh Hasan Ali field. Volcanism along this fault has been K-Ar dated at 15.6–14.3 mya in the north and 2.6–2.2 mya farther south.

Barind Tract (alternately called the Varendra Tract in English and Borendro Bhumi in Bengali) is the largest Pleistocene era pysiographic unit in the Bengal Basin. It covers most of Dinajpur, Rangpur, Pabna, Rajshahi, Bogra, and Joypurhat districts of Rajshahi Division and Rangpur Division in Bangladesh as well as entirety of Uttar Dinajpur, Dakshin Dinajpur and most of Maldah districts in West Bengal, India. It is made up of several separate sections in the northwestern part of Bangladesh, and, northern part of West Bengal, India covering a total area of approximately of mostly old alluvium. On the eastern edge of the tract is a lower fault escarpment.

View of Semeru and Bromo eruption with Mount Batok in East Java The Indonesian island of Java is almost entirely of volcanic origin, and contains numerous volcanoes, 45 of which are considered active volcanoes. As is the case for many other Indonesian islands, volcanoes have played a vital role in the geological and human history of Java. Indeed, land is created on Java as a result of lava flows, ash deposits, and mud flows (lahars). Volcanoes are a major contributor to the immense fertility of Java, as natural erosion transports volcanic material as alluvium to the island's plains, forming thick layers of fertile sediment.

The timing of the test put it within the Operation Storax fiscal year, but Sedan was functionally part of Operation Plowshare, and the test protocol was sponsored and conducted by Lawrence Livermore National Laboratory with minimal involvement by the United States Department of Defense. The explosive device was lowered into a shaft drilled into the desert alluvium deep. The fusion-fission blast had a yield equivalent to 104 kilotons of TNT (435 terajoules) and lifted a dome of earth above the desert floor before it vented at three seconds after detonation, exploding upward and outward displacing more than of soil. The resulting crater is deep with a diameter of about .

Over millions of years the upper seams in this area were washed away and the lower seams outcrop around Ipstones, Foxt and Alton. The coalfield's eastern boundary is the Millstone Grit and Limestone of the Pennines around Ipstones Edge. Despite the coalfield being detached from its much larger neighbour, the North Staffordshire Coalfield, and developing from the latter in relative isolation, geological analysis by the National Coal Board in the mid 20th century correlated the coal seams of the two coalfields. Around the coalfield the measures are covered with alluvium and marl with sizeable amounts of industrial sand, gravel and limestone predominating in certain areas.

The valleys of most watercourses are open to the southern and southeastern moist sea winds, which leaves a peculiar imprint on climate, vegetation and soil. The river beds are overloaded with alluvium, the amount of which increases in the lower reaches due to the general stretching and subsidence of the earth's crust along the edge of the continent, and due to the accumulation of catastrophic floods. As a result, a low-lying plain with a width of up to 10 km was formed on the coast. Over its flat marshy surface with many lakes and oxbows, remnant mountains up to 180 m high rise in places (Pigeon's Rock Mountain, etc.).

8, part 2 The underlying Devonian Old Red Sandstone outcrops over 2 km southeast, just north of the M4 motorway. The superficial geology in the area of the Taff's Well spring comprises an unknown thickness of river alluvium and river terrace deposits. The Taffs Well sub-unit is bound to the south west by the Tongwynlais or Taff's Well Fault, which runs north- south, crossing the River Taff, and passing very close to the Taff's Well Thermal Spring. The Taffs Well Fault is a continuation of the Daren-ddu fault which is a major NW-SE trending fault in the Coal Measure rocks of the South Wales Coalfield.

The valleys of the Indre and its tributaries, which have cut the base of the limestone plateau during alternating glacial and interglacial periods of the Pleistocene, are covered with recent alluvium, giving the soil a hydromorphous tendency, often with a shallow water table. The slopes between the plateau and the valleys are eroded washed silt or gravel deposits and clay from the Turonian and Senonian strata; this type of soil is called "perruche" (parakeet) in the Loire Valley. The land area of Chambourg-sur-Indre is 2,839 hectares (on 1 January 2014), the average area of a French commune being 1,510.2 hectare. The altitude of this area varies between and .

The Meers fault has been in existence for most of the Phanerozoic. It may have begun as a rift margin fault in the Proterozoic-Cambrian associated with the Southern Oklahoma Aulacogen but its maximum activity took place during the Mississippian and Permian when the Wichita Mountains and the Slick Hills were offset along it by about and the Meers Valley formed along the fault. More fault movements occurred in the Permian and the Pleistocene although there are no post-Permian rock formations in the area that could allow an estimation of post-Paleozoic movements. However, Pleistocene sediments and Holocene alluvium have been offset, indicating fault movement during this time.