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"landform" Definitions
  1. a natural feature of the earth’s surface

757 Sentences With "landform"

How to use landform in a sentence? Find typical usage patterns (collocations)/phrases/context for "landform" and check conjugation/comparative form for "landform". Mastering all the usages of "landform" from sentence examples published by news publications.

Prompting a government agency to rename a geologic landform, however, may be a first.
The cliffs are the third most southern landform and are a chillingly beautiful sight to behold.
Nature's most regal landform is the theme of MTN, the newest group exhibition at Black Ball Projects.
Many stations by Mount Fuji naturally highlight the famed landform in their stamp; others exhibit nearby beaches or ski slopes.
I would definitely still recommend visitors to China make plans to visit the landform if interested in the country's natural beauty.
But the researchers can't say for sure until they run computer models to see if such a landform is even possible on Pluto.
The Danxia landform is a spectacular sight, but I'm including it on this list because its beauty is exaggerated in many of the photos you see online.
This remarkable landform, unlike any other seen in our solar system, is perched on a much broader set of rounded ridges that are separated by flat valley floors.
One of the most interesting ones I saw on Reddit prior to my visit to China was the Danxia landform of Zhangye, also known as the "rainbow mountains."
Moist air arriving on ocean breezes would be trapped by the human-sculpted landform, forcing it up into the atmosphere where it would cool, condense into clouds, and eventually—hopefully!
The tasks of the Chang'e-4 include astronomical observation, surveying the moon's terrain, landform and mineral makeup, and measuring the neutron radiation and neutral atoms to study the environment of its far side.
A new short film from environmental organization Conservation International personifies the massive (and massively important) landform, voiced by Golden Globe Award nominee Lee Pace of Guardians of the Galaxy and Halt and Catch Fire fame.
Reported first by Honolulu Civil Beat and confirmed by HuffPost on Tuesday, East Island is the latest small landform in the Eastern and South Pacific to disappear due to extreme weather and sea-level-rise.
The tasks of the Chang'e-4 include astronomical observation, surveying the moon's terrain, landform and mineral composition, and measuring the neutron radiation and neutral atoms to study the environment on the far side of the moon.
Image: CNSA"The image clearly shows the landform of the [moonscape] around the lander and the rover, and the five-star red flag on the two devices is particularly eye-catching," noted the CNSA in a release.
Two hours on — the last half of it on a rutted, severely wash-boarded dirt road — I spied Fajada Butte, the towering landform at the head of a long, shallow sandstone canyon called Chaco, now the Chaco Culture National Historical Park.
In the midst of a xenophobic wave deeming immigrants as other, reifying the soundness of borders as if they were a natural landform, and the financing of overseas wars based on dominant historical narratives, the contemporary use of soil in installations, collections, and jewelry pieces has provided a site of gathering and discussion, and has aided in building empathy.
The Arabic alchemy sense entered Latin in the 12th century. Elixir is in all European languages today. ;erg (landform), hamada (landform), sabkha (landform), wadi (landform) : عرق ʿerq, sandy desert landscape. حمادة hamāda, craggy desert landscape with very little sand.
Danxia landforms cover several provinces in southeast China. Taining County, Fujian Province, has very good examples of "young" danxia landforms wherein deep, narrow valleys have been formed. As the landform gets older, valleys widen and one gets isolated towers and ridges.The danxia landform is named after Mount Danxia, one of the most famous examples of the danxia landform.
Venera Terra is a landform on the dwarf planet Pluto, discovered by the New Horizons spacecraft.
Limestone dissolves under the action of rainwater and groundwater charged with H2CO3 (carbonic acid) and naturally occurring organic acids. The dissolution process produces a distinctive landform known as karst, characterized by sinkholes and underground drainage. Solutional caves in this landform—topography are often called karst caves.
The landform was shaped by a massive glacier, carving its way from the land to the Atlantic Ocean.
Ordnance Survey Ireland . Use zoom and pan options for landform names. Retrieved: 20 September 2010.Placenames Database of Ireland.
Retrieved 12 October 2007. This word is still in use for the particular landform in the Northern Isles of Scotland.
This is an uncommon landform in central and southern England. It is private land and there is no public access.
Ruby Ridge is a mountain ridge in the Kaniksu National Forest (administered as part of the Idaho Panhandle National Forests) in northeastern Boundary County, Idaho, United States. The landform is most notable for being confused with another Ruby Ridge in the same county, but about south-southwest. The other Ruby Ridge has an elevation , is also located within the Kaniksu National Forest, and, interestingly, is the only other landform so named within the United States. (There is a third landform of the same name, located in Alberta, Canada, about to the east-northeast).
If a plug is preserved, erosion may remove the surrounding rock while the erosion-resistant plug remains, producing a distinctive landform.
Shi Niu Zhai is a national park that is made up of mainly Danxia landform- red bed characterised by steep cliffs.
It was preliminarily considered that Jangdo wetland was a concave landform formed by the weathering of granite intruding Precambrian silicified metasedimentary rocks. Various granite-weathered topography was observed. The formation scenario of Jangdo wetland is as follows. By flood or slope mass movement of regolith, rock fragments were moved to form a low- relief slope landform.
This new description and the new coordinates encompass the locations of the three summits—effectively combining the three into a single landform.
Lucerne Valley is a census-designated place and valley landform located in the southern Mojave Desert, within western San Bernardino County, California.
Pinnacle Mountain is situated between the Big Maumelle River to the north and the Little Maumelle River to the south. Its proximity to the Arkansas River and steep south slopes make it a prominent landform. The U.S. Board on Geographic Names once held that any landform greater than 1,000 feet of local relief classified as a mountain, while any landform less than 1,000 feet of local relief classified as a hill. Though Pinnacle Mountain is 1,013 feet above mean sea level, it is only 763 feet of local relief, which would have made it a hill.
Current ANSI identification is based on ecoregions and ecodistricts, and finer resolution is used to determine particular features and areas, such as a landform.
In the 2010 UNESCO list of world heritage sites, Mount Danxia was recorded as a natural World Heritage Site as part of China's Danxia landform.
In Swedish the word ås commonly refer to eskers, a glacial landform, but in the case of Söderåsen it corresponds to a tectonic landform called horst. The last glacial ice sheet, the Weichsel ice, left the area of Söderåsen 14,000 to 13,500 years BP. Following this there was a period up to 12,700 years BP of cold non-glacial conditions with permafrost and strong winds.
This landform is characterised by rugged strike ridges separated by alluvial flats. Nourlangie Rock Kakadu's coast and the creeks and river systems under tidal influence (extending about 100 kilometres inland) make up this landform. The shape of the estuaries and tidal flats varies considerably from the dry season to the wet season. During the dry season tidal action deposits silt along the river beds and banks.
Tomaree Head is a prominent landform at the entrance to Port Stephens and one that has been important to Aboriginal people and is included in their stories. The geological formation of the unusual combination of landform aeolian sands and volcanic derived clays is of some interest and research potential. Tomaree Head has been associated with many aspects of Australia's history from initial discovery by Captain Cook, early explorers, seafarers, settlers and industry including fishing, timber and farming. One of the outstanding qualities of Tomaree Head is its aesthetic appeal as a prominent landform with steep cliffs to the ocean and natural landscape in the attractive setting of Port Stephens.
Erosion of the piedmont plateau created iron-oxide rich clay soils. Three general landforms exist. Flat ridges, Hillsides and, Floodplains. Each landform has its own Ecology.
The Colorado River Aqueduct crosses the midpoint of the valley at Vidal Junction, California. The Vidal Valley also lies due east of the Danby Dry Lake landform.
Reed College, a private liberal arts college that was founded in 1908, is located within the confines of Southeast Portland as is Mount Tabor, a volcanic landform.
The scientific study of landforms is known as geomorphology. In onomastic terminology, toponyms (geographical proper names) of individual landform objects (mountains, hills, valleys, etc.) are called oronyms.
Walther Penck thought landform development depended on uplift rate. He saw three main types of landform and landscape development all of which begun with rumpfläches or primärrumpfs and ended with endrumpfs. The differences between them depended on their rate of uplift: peneplains developed in places with a low rate of uplift, intermediate forms developed in places of moderate uplift, and Alpine forms developed on places of rapid uplift.Chorley et al.
Karst towers landforms along Lijiang River, Guilin, China Oceans and continents exemplify the highest-order landforms. Landform elements are parts of a high-order landforms that can be further identified and systematically given a cohesive definition such as hill-tops, shoulders, saddles, foreslopes and backslopes. Some generic landform elements including: pits, peaks, channels, ridges, passes, pools and plains. Terrain (or relief) is the third or vertical dimension of land surface.
Comparison of these landform maps with mapping of variables related to crop or plant growth show a strong correlation (see below for examples and references for precision agriculture).
The ecology of this landform is considered an isolated outlier of the Ethiopian montane forest ecological zone, an important island of forest in a sea of semi-desert.
Such landforms are called crag and tail. If a plug is preserved, erosion may remove the surrounding rock while the erosion-resistant plug remains, producing a distinctive upstanding landform.
A smaller igneous landform is also present on Papuk, near Voćin. The two mountains are possible remnants of a volcanic arc related to Alpine orogeny--uplifting of the Dinaric Alps.
Most of the municipality was farmland - its dominant landform was the rich agricultural land of Sumas Prairie, which was created through the draining of Sumas Lake early in the 20th Century.
Cactus Plain is a landform within the Lower Colorado River Valley. It is adjacent to Bouse Wash, which is on the south. The wash drains northwest-west into the Colorado River.
Dr. Percy Edgar Brown (October 9, 1885–July 8, 1937) was a soil scientist at Iowa State University, Ames, Iowa. Brown is perhaps best known for the book, Soils of Iowa, which was published in 1936. The classic map, "Landform Regions of Iowa," was originally published in this text. Landform Regions of Iowa Dr. Brown was born on a farm at Woodbridge Township, New Jersey, on October 9, 1885. He graduated from Woodbridge High School in 1902.
Curlethney Hill is a landform in Aberdeenshire, Scotland within the Mounth Range of the Grampian Mountains. (Grid Reference NO 918 839)United Kingdom Ordnance Survey Map Landranger 45, Stonehaven and Banchory, 1:50,000 scale, 2004 The peak elevation of this mountain is 246 metres above mean sea level. This landform lies slightly southwest of the village of Netherley. The northwest boundary of the moorland atop Curlethney Hill is formed by the southwestern flanks of Craggie Cat, a nearby peak.
It is also often coated in winter or spring snowstorms as a white landform, with its loss of white being determined by season and duration of storm temperatures. Castle Dome's height is .
The landform known as Elephants Back is a rounded mass of solidified lava. Mineralization produced gold-bearing quartz veins, and relics of past gold mining activities are still present in the area.
Panzhou is a karst landform, with plateau mountain as the main body. The whole terrain is high in the northwest, low in the southeast, and uplifted in the central and southern parts.
Hill upon which the village of Saint-Paul-de-Vence is built, in Southern France A hill is a landform that extends above the surrounding terrain. It often has a distinct summit.
Because hummocks can both form and disintegrate rapidly (well within a human lifetime) they are an ideal landform to monitor for medium range environmental change. There are several explanations of earth hummock formation.
The region is pocketed by small human landform, i.e., strip-mines among a hummocky or ridge-swale topography. Streams drain and erode the area, moving soils and depositing them downstream. Elevation ranges from .
Pingos near Tuktoyaktuk View from top of a pingo towards another, within a partly drained lake, the Arctic Ocean in the background (near Tuktoyaktuk). July 20, 1975 Pingos are intrapermafrost ice-cored hills, ranging in height from and in diameter. They are typically conical in shape and grow and persist only in permafrost environments, such as the Arctic and subarctic. A pingo is a periglacial landform, which is defined as a non-glacial landform or process linked to colder climates.
The Adriatic Sea itself is a concordant landform, consisting of a body of water between parallel ranges. These Dalmatian types normally occur in high energy environments from where there is eustatic or isostatic change creating a submerging coastline. The second landform is the Haff type as in the Haffs, or lagoons, of the southern shore of the Baltic Sea, which are enclosed by long spits of sand parallel to the low coast. The converse of concordant coastline is a discordant coastline.
Irishtown Bend is the name given to both a former Irish American neighborhood and a landform located on the Flats of the west bank of the Cuyahoga River in the city of Cleveland in the U.S. state of Ohio in the United States. The landform consists of a tight meander in the Cuyahoga River, and the steep hillside above this meander. The neighborhood of Irish immigrants and Irish Americans emerged about 1830. Portions of the area became industrial in the late 1800s.
LandForm video map overlay marking runways, road, and buildings during 1999 helicopter flight test The NASA X-38 was flown using a hybrid synthetic vision system that overlaid map data on video to provide enhanced navigation for the spacecraft during flight tests from 1998 to 2002. It used the LandForm software which was useful for times of limited visibility, including an instance when the video camera window frosted over leaving astronauts to rely on the map overlays.Delgado, F., Abernathy, M., White J., and Lowrey, B. Real-Time 3-D Flight Guidance with Terrain for the X-38, SPIE Enhanced and Synthetic Vision 1999, Orlando Florida, April 1999, Proceedings of the SPIE Vol. 3691, pages 149–156 The LandForm software was also test flown at the Army Yuma Proving Ground in 1999.
The trail was opened in 1986 and follows the old Chicago and North Western Railway (C&NW;) Madison–Milwaukee mainline. The name refers to a drumlin, a glacial landform very common in the area.
Kumtag Desert The Kumtag Desert (, "kum-tag" meaning "sand-mountain" in a number of Turkic languages), is an arid landform in Northwestern China, which was proclaimed as a national park in the year 2002.
Wheeler Ridge is an unincorporated community in the southwestern San Joaquin Valley, within Kern County, California. It is at the junction of the valley floor and the Wheeler Ridge landform of the Tehachapi Mountains.
A post office called Bench was established in 1902, and remained in operation until 1923. The community was named for a prominent landform near the original town site, commonly referred to as a "bench".
If the ponor cannot contain the high runoff during a flood event an intermittent flow may continue through the valley beyond the sink. Such a landform is called a semi-blind or half-blind valley.
Palms in one of the many canyons. Base of Range The Bungle Bungle Range is the landform that is the major component of the Purnululu National Park situated in the Kimberley region of Western Australia.
Etymologically probably related and conceptually similar is the valley landform known as asiepen, which is mainly found in the south Westphalian area and generally also describes wet valley bottoms, mostly stream-bearing V-shaped valleys.
Two cirques with semi-permanent snowpatches near Abisko National Park, Sweden Upper Thornton Lake Cirque in North Cascades National Park, U.S. A cirque (; from the Latin word circus) is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic , meaning a pot or cauldron) and cwm (; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep.
Mount Magazine gets its name from French explorers who, while traveling through the area, witnessed a landslide on the mountain. The noise from the landslide was so great that one explorer described it as the sound of an ammunition magazine exploding, hence the name "Magazine". The U.S. Geological Survey's Geographic Names Information System (GNIS) indicates that the official name of this landform is "Magazine Mountain", not "Mount Magazine". Generally "Mount [Name]" is used for peaks and "[Name] Mountain" is used for ridges, which better describes this landform.
Meikle Carewe Hill. Author: C. Michael HoganMeikle Carewe Hill is a landform in Aberdeenshire, Scotland within the Mounth Range of the Grampian Mountains. (Grid Reference NO 921 828)United Kingdom Ordnance Survey Map Landranger 45, Stonehaven and Banchory, 1:50,000 scale, 2004 The peak elevation of this mountain is 266 metres above mean sea level. Meikle Carewe is a prominent landform visible from a number of coastal hills such as Kempstone Hill and Megray Hill; it also forms a major backdrop to the community of Netherley.
This conical hill in Salar de Arizaro, Salta, Argentina called Cono de Arita constitutes a landform. A landform is a natural or artificial feature of the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Typical landforms include hills, mountains, plateaus, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins.
The Ogo Mountains, also known as the Galgodon Highlands, are a mountain range in Somalia. They cross the Sanaag and Togdheer regions. With a mean peak height of , the ecology of this landform is semi-desert.
The East Styrian Hills south of Herberstein An interfluve is a narrow, elongated and plateau-like or ridge-like landform between two valleys.Ernst Neef (ed.): Riedel. In: Ders.: Das Gesicht der Erde (Taschenbuch der physischen Geographie).
Corsedardar Hill is a mountain landform in the Grampian Mountains of Aberdeenshire, Scotland.United Kingdom Ordnance Survey Map, Landranger, 1:50,000 (2004) This hill is located in the Lower Deeside region within the historic district of Kincardineshire.
According to the United States Census Bureau, the CDP covers an area of 1.2 square miles (3.2 km2), all of it land. The valley also includes Edna Fault, a prominent landform just south of the main community.
1st edition, 1996. p. 74. Descriptions of the landform vary. The United States Geological Survey classifies it as a "pillar", which it defines as a "[v]ertical, standing, often spire-shaped, natural rock formation"."Feature class definitions".
Pagosa Springs, CO. This is a general way in which the morphology of a stream can be described. Many of the Level I criteria can be determined through topographic and landform maps, aerial imagery, and geospatial data.
Queensland government. Retrieved 24 January 2018. A beach is a landform alongside a body of water which consists of loose particles. The particles composing a beach are typically made from rock, such as sand, gravel, shingle, pebbles.
Located within a 200 km-long karst landform belt in the southwest part of the province near Hanzhong City, the cluster is one of the largest on Earth. It includes forty-nine sinkholes and more than fifty funnels ranging from 50–100 metres in diameter. The area is in the Qinling-Bashan Mountains, spread over Hanzhong city's counties of Ningqiang, Nanzheng, Xixiang and Zhenba. It is the northernmost example of the humid tropical and subtropical karst landform area, lying roughly between the latitudes of 32 and 33 degrees.
Since that time, the ability to map and classify landform shapes and features has increased greatly. The advent of GPS has made it possible to map almost any variable one might wish to measure. Thus, a very increased awareness of the spatial variability of the environment that plants grow in has arisen. The development of technology like airborne LiDAR has enabled the detailed measurement of landform features to better than sub-meter, and when combined with RTK-GPS (accuracies to 1mm) enables the creation of very accurate maps of where these features are.
Section of Raisz' 1941 map of the Northwestern United States, showing his style of landform illustration. In 1921, A.K. Lobeck published A Physiographic Diagram of the United States, using an advanced version of the hill profile technique to illustrate the distribution of landforms on a small-scale map.Lobeck, A.K. (1921) A Physiographic Diagram of the United States, A.J. Nystrom & Co., digital scan at David Rumsey Map Collection, List No.7129.000. Erwin Raisz further developed, standardized, and taught this technique, which uses generalized texture to imitate landform shapes over a large area.
Edith Ronne, wife of the expedition leader, was a correspondent for the syndicate, posting dispatches from Antarctica for the duration of the expedition. She named a landform there, Cape Wheeler, in honor of her editor, John Neville Wheeler.
The Waterman Mountains are a low mountainous landform in Pima County, United States.Neal Erskine McClymonds. 1957 Notable among the tree species is the elephant tree (Bursera microphylla) which species exhibits a contorted multi- furcate architecture;C. Michael Hogan.
Curavacas Curavacas is a peak which is part of the Cantabrian Mountains system of mountain ranges. This landform is located in Triollo municipality, in Province of Palencia and in Castile and León autonomous community. Its height is 2,524 metres.
The park also includes active artesian mound springs which are considered to be the rarest landform in Australia.NSW National Parks and Wildlife Service. 2002. Salt Pipewort (Eriocaulon carsonii) Recovery Plan. NSW National Parks and Wildlife Service, Hurstville, New South Wales.
A typical workflow for tackling geological problem, starting from defining the problem down to data selection and interpretation, inspired by Gupta (1991)An example of a mineral quartz spectral reflectance curveRemote sensing can aid surficial geological mapping and landform characterization.
The Grizzly Valley is a landform of the upper Middle Fork Feather watershed that receives 29-37 inches of annual precipitation. The valley is the location of Lake Davis, an impoundment of Big Grizzly Creek by the 1967 Grizzly Valley Dam.
Western slopes of Torr Mor Torr Mor is a hill peak landform on the coastal east side of the Kintyre Peninsula in Scotland. The peak offers views over the Kilbrannan Sound. The Forestry Commission maintain a footpath over the hill.
The tallest among such landforms are Ivanšćica and Medvednica north of Zagreb and in Hrvatsko Zagorje as well as Psunj and Papuk which are the tallest among the Slavonian mountains surrounding Požega. Psunj, Papuk and adjacent Krndija consist mostly of Paleozoic rocks which are 350 - 300 million years old. Požeška gora, adjacent to Psunj, consists of much more recent Neogene rocks, but there are also Upper Cretaceous sediments and igneous rocks forming the main, ridge of the hill and representing the largest igneous landform in Croatia. A smaller igneous landform is also present on Papuk, near Voćin.
They provoke the visitor to interpret landscape on the largest and smallest scale. Stone rows on the 'North-South Line' at the Crawick Multiverse Jencks became a leading figure in British landscape architecture. His landscape work was inspired by black holes, fractals, genetics, chaos theory, waves and solitons. In Edinburgh, Scotland, he designed the landform at the Scottish National Gallery of Modern Art in collaboration with Terry Farrell and Duncan Whatmore of Terry Farrell and Partners. Jencks other works include the Garden of Cosmic Speculation at Portrack House near Dumfries; Designs for Black Hole Landscape, IUCAA, Pune, India, 2002; Portello Park, Milan 2002–2007 (Time Garden 2004–2007); Two Cells – Inverness Maggie's Centre, 2003–2005; Northumberlandia Landform, 2004; Cells of Life, Jupiter Artland, Bonnington House 2003–2010; Crawick Multiverse, 2006– ; Memories of the Future landform and reclamation project, Altdobern, Germany; Wu Chi, Black Hole Oval Terrace, Beijing Olympic Park, 2008; and The Scottish World, St. Ninians, Kelty, 2003, 2010+.
The Eastern region is the location of the Akosombo dam and the economy of the Eastern region is dominated by its high-capacity electricity generation. Eastern region covers an area of 19,323 square kilometres, which is about 8.1% of Ghana's total landform.
The city is situated in the Sonoma Valley, with the Mayacamas Mountains to the east and the Sonoma Mountains to the west, with the prominent landform Sears Point to the southwest. The city has an area of , none of it covered by water.
Mount Yushi () is a mountain in Dongyang township, Guangfeng District of Shangrao, Jiangxi, China. It is the highest mountain in the northeastern Guangfeng District. It belongs to Danxia landform. On the top of the mountain, there is a Buddhist temple named "Yushi Temple" ().
If all known seamounts were collected into one area, they would make a landform the size of Europe. Their overall abundance makes them one of the most common, and least understood, marine structures and biomes on Earth, a sort of exploratory frontier.
Punta Gorda is a landform in Colonia Department, Uruguay. According to the Treaty between Uruguay and Argentina concerning the Rio de la Plata and the Corresponding Maritime Boundary, it marks the mouths of the Uruguay River on the Río de la Plata.
Pedra de São Domingos is a rock formation located between the municipalities of Córrego do Bom Jesus and Gonçalves, Minas Gerais, Brazil. The gneiss landform is one of the highest points in the Mantiqueira Mountains. At its highest point, the elevation is .
Harrison's Rocks are a notable example of a periglacial tor landform, developed in rocks of the Tunbridge Wells Sand Formation of the Wealden Supergroup of early Cretaceous age. Harrison's Rocks is composed of a soft sandstone, which is prone to being worn away.
In places dolerite columns have collapsed into scree slopes.Lloyd, p.5 The face of the tiers has been eroded and retreated approximately since their formation, leaving the mountain Quamby Bluff as a solitary outlier. The central plateau's landform has been changed by glaciation.
The St. Croix Moraine runs through the park. This rolling and uneven landform is a result of the Wisconsin glaciation and two previous glaciations. Irregular hills and ridges (kames) surround kettles, depressions left by melting blocks of ice during the glaciers' retreat.
A gully in Kharkov oblast, Ukraine. Gullied landscape in Somalia. A gully is a landform created by running water, eroding sharply into soil, typically on a hillside. Gullies resemble large ditches or small valleys, but are metres to tens of metres in depth and width.
Bioregions are areas of Australia classified into large distinct bioregions based on common climate, geology, landform, native vegetation and species information, and are the reporting unit for assessing the status of Australia's native ecosystems and the level of protection in the National Reserve System.
The physical component is defined by the spatial and temporal configuration of the landscape elements (landform, landcover and land use types), and the behavioural component is defined by the behavioural responses, of organisms and/or processes, to the physical arrangement of the landscape elements, ,.
A similar legend about the killing of a giant beaver by a helper-spirit and the subsequent transformation of the corpse into a landform occurs among the native Mi'kmaq people of Nova Scotia (see Glooscap).Lonely Planet Guide: Canada. 8th ed. Lonely Planet, Oakland, 2002.
Mint Canyon is a fluvial landform in the Sierra Pelona range. It consists of terrestrial deposits from streams and lakes consisting mostly of sandstone and conglomerate with some claystone."Geologic Map of the Mint Canyon Quadrangle" (DF-57) by Thomas W. Dibblee, Jr., 1996.
For example, serpentinite is a kind of rock formed in a process called serpentinization, in which a host mineral produces a pseudomorph, and the original mineral is eventually replaced and/or destroyed, but is still present until the process is complete. Within geomorphology a relict landform is a landform that took form from geomorphic processes that are not active at present. In a Scandinavian context, this is often meant to imply that relict landforms were formed before the last glaciation and survived it under cold- based parts of the ice sheet. Climatic geomorphologist Julius Büdel estimated that 95% of mid-latitude landforms are relict.
A very peculiar feature of danxia landscape is the development of numerous caves of various sizes and shapes. The caves tend to be shallow and isolated, unlike true karst terrain where caves tend to form deep, interconnecting networks. In 2010, several danxia landscapes in southern China, with a general name of "China Danxia", were inscribed as a World Heritage Site.China danxia landform proclaimed world heritage The six inscribed danxia landform areas are: Mount Langshan and Mount Wanfo (Hunan Province), Mount Danxia (Guangdong Province), Taining and Mount Guanzhi (Fujian Province), Mount Longhu and Guifeng (Jiangxi Province), Fangyan, Mount Jianglang (Zhejiang Province), and Mount Chishui (Guizhou Province).
Olmsted used the term 'landscape architecture' describing the whole professional task of designing a composition of planting, landform, water, paving and other structures, using the word for the first time when designing the Central Park. This led to its adoption by Frederick Law Olmsted and Calvert Vaux. Olmsted and a man named George Oskar gave a different slant to the meaning of 'landscape architecture', using the term to describe the whole professional task of designing a composition of planting, landform, water, paving and other structures. Their first use of the term was in the winning entry for the design of Central Park in New York City.
El Malpaís National Monument is an example of this landform in New Mexico. Other examples are the Carrizozo Malpaís and Jornada del Muerto Volcano lava plain, in the Tularosa Basin's Jornada del Muerto Desert. The Malpaís de Güímar is an example in the Spanish Canary Islands.
This territory is located in the southeast and has an area of 2,071.8 km2. The municipalities of Lorca, Águilas and Puerto Lumbreras belong to this comarca. There is a remarkable water landform in the area: Guadalentín River. Another river that is present is the Luchena River.
The town is the capital of Saint Peter Basseterre Parish. The landform feature 'Monkey Hill' overlooks the town and is its namesake. The estimated population of the Monkey Hill area, which includes Upper and Lower Monkey Hill, St. Peter's, Parry's, Ogee's, Stapleton and Bayford's, is approximately 2,654.
Smith, D.W., and W.L. Verrill (1998) Vernal Pool-Soil-Landform Relationships in the Central Valley, California. in: C.W. Witham, E.T. Bauder, D. Belk, W.R. Ferren Jr., and R. Ornduff, eds., pp. 15-23, Ecology, Conservation, and Management of Vernal Pool Ecosystems – Proceedings from a 1996 Conference.
As the surrounding rock weathered, the harder shonkinite remained behind. The rock is roughly oblong, occupying about . The landform is high, and consists of clear outcrops at the north and south ends connected by a broken saddle ridge. The southern outcrop is higher than the northern outcrop.
The understory features abundant ferns and boulder laden mosses. A prominent landform in this upper reach created by Sonoma Creek is Adobe Canyon. Locally part of this upper reach flow is sometimes called Adobe Creek. Tributaries near the headwaters include Mount Hood Creek and Graywood Creek.
This angle is the maximum altitude at which Mercury is visible in a completely dark sky. False-color image of Carnegie Rupes, a tectonic landform—high terrain (red); low (blue). At middle latitudes, Mercury is more often and easily visible from the Southern Hemisphere than from the Northern.
Looking northeast across Strathlethan Bay to Dowie Point Downie Point is a prominent headland located at the southern edge of Stonehaven Bay in Aberdeenshire, Scotland. (United Kingdom, 2004) From the Stonehaven Harbour, there is a panoramic view of this cliff landform, especially from the tip of Bellman's Head.
The landform was presumably named after Admiral Andrew Ellicot Kennedy Benham (1832–1905) by American surveyors who were the probable discoverers of the geological feature. He was a United States Navy officer, who served with both the South Atlantic and West Gulf Blockading Squadrons during the American Civil War.
Another landform named in his honor is Amdrup Fjord . The Shipbuilding & Engineering Company's ship G.C. Amdrup is also named for him.Higgins, p. 26 Also named on his behalf is Leptognathia amdrupii, which was considered for transfer to the genus Chauliopleona by 2000 and transferred to Chauliopleona amdrupii by 2005.
HaMakhtesh HaKatan (, lit. The Small Crater) is a makhtesh, a geological erosional landform of Israel's Negev desert. One of five makhteshim in Israel, and seven in the world, it is the third largest in Israel at 5 km by 7 km. It was charted in 1942 by Jewish explorers.
The Sabine Valley is a landform in northern South Island, New Zealand.Peter Wardle. 1991 Much of the Sabine Valley is forested with beech canopy. Example understory vegetation is the presence of Archeria traversii within certain mountain beech forests in the upper Sabine Valley of northern South Island, New Zealand.
The Puna de Atacama or Atacama PlateauAtacama Plateau article at the Encyclopædia Britannica website is an arid high plateau, in the Andes of northern Chile (15%) and Argentina (85%). Historia de la relacciones exteriores de la Argentina Geomorphologist Walther Penck based his Grossfalt landform association on Puna de Atacama.
Physiotope is the total abiotic matrix of habitat present within any certain ecotope. The physiotope is the landform, the rocks and the soils, the climate and the hydrology, and the geologic processes which marshalled all these resources together in a certain way and in this time and place.
Situated 10 km north of Udharbond bus stand, is Madhura, a picnic destination and a marvelous place with the upper course of the blue Madhura River running rapidly between the hilly terrain. The typical landform attracts a lot of tourists. There is also a hanging bridge across Madhura River.
A 'saddle point' in mathematics derives its name from the fact that the prototypical example in two dimensions is a surface that curves up in one direction, and curves down in a different direction, resembling a riding saddle or a mountain pass between two peaks forming a landform saddle.
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984).
Moose Creek is a creek in western Yukon, Canada. The landscape surrounding Moose Creek lies in the Northern Cordilleran Volcanic Province. During the Cenozoic era, volcanic activity engulfed the Moose Creek area.Catalogue of Canadian volcanoes: Moose Creek However, the type of volcanic landform these volcanics represent is unknown.
Landscape designers draw upon design elements such as axis, line, landform, horizontal and vertical planes, texture, and scale to create aesthetic variation within the landscape. They may additionally make use of aesthetic elements such as pools or fountains of water, plants, seasonal variance, stonework, fragrance, exterior lighting, statues, and lawns.
The Ganges river delta in India and Bangladesh is one of the most fertile regions in the world. The volcano Mount St. Helens in Washington, United States. Natural landform - terrain or body of water. Landforms are topographical elements, and are defined by their surface form and location in the landscape.
Charles G. "Chip" Groat (born March 25, 1940 in Westfield, New York) is an American geologist. He is a professional in the earth science community with involvement in geological studies, energy and minerals resource assessment, ground-water occurrence and protection, geomorphic processes and landform evolution in desert areas, and coastal studies.
The east side of the mountain was resurveyed in 1948 by the Falkland Islands Dependencies Survey (FIDS) who named the feature for Alfred Stephenson, surveyor and leader of the BGLE party to George VI Sound in 1936. Another landform on Alexander Island happens to be named for Alfred Stephenson, Stephenson Nunatak.
The park contains several glacial landforms such as drumlins and moraine. The most prominent glacial landform in Jacques-Cartier National Park is the Jacques-Cartier Valley (French:Vallée de la Jacques-Cartier). The U-shaped valley is deep and was formed during the last glacial period.Le parc de la Jacques-Cartier - CGQ .
The major landform consists of craggy rocks and compact salt lake bottoms, intermedial areas and fixed dunes. Despite a fragile ecosystem, there is an abundance of birdlife. The region is a haven for migratory and resident birds of the desert. Many eagles, harriers, falcons, buzzards, kestrel and vultures are spotted here.
Biriwal Bulga is a 5813-hectare national park is situated on the northern edge of the Bulga plateau. It ranges in elevation from 130m to 670m. The national park's landform is predominantly dissected foothills which attributes to its elevation. The most common rocks found in this national park are mudstone, shale.
The columns typically have three to eight sides, six being most common. The columns are also divided horizontally by cross joints.Mitchell, Colin and Mitchell, Patrick (2005) Landform and Terrain: The Physical Geography of Landscape Brailsford Press. 3.pdf These columnar jointed sections represent the tops and bottoms of individual lava flows.
"Landform degradation on Mercury, the Moon, and Mars: Evidence from crater depth/diameter relationships." Journal of Geophysical Research 82(2): 376–388.Schaber, G.G., Boyce, J.M., & Trask, N.J. (1977). "Moon-Mercury: Large impact structures, isostasy and average crustal viscosity." Physics of the Earth and Planetary Interiors 15(2–3): 189–201.
Railroad and highway development in the late 1800s and 1900s skirted Tower Rock, but the landform itself remained pristine. The encompassing Tower Rock was added to the National Register of Historic Places on March 18, 2002. The Tower Rock State Park was created around the National Historic Site in 2004.
The location and size of the berm is subject to seasonal changes. For example, a winter berm that has been thrown up by storm surges in winter is usually much more prominent and higher up the beach than berms formed by summer high tides. A similar landform is a beach ridge.
This mesa landform, with an elevation between ,Neff, D., J., and N. G. Woolsey. 1979. Effect of predation by coyotes on survival of antelope fawns on Anderson Mesa. Special Report 8, Arizona Game and Fish Department, Phoenix, Arizona. has been the site of Lowell Observatory's Anderson Mesa Station since 1959.
View southwest across the Carrizo Badlands from the Wind Caves, in Anza- Borrego Desert State Park. The Carrizo Badlands are a landform of badlands that lie within Anza-Borrego Desert State Park in eastern San Diego County, and in the Carrizo Impact Area in western Imperial County, in southern California.
Eastern bank of the Zlatni Rat The beaches on either side of the spit extend for some altogether,Naklada Naprijed, The Croatian Adriatic Tourist Guide, p. 267, Zagreb (1999), . but the exact shape and length of the landform varies with regard to changes in tide, current, and wind. The spit points directly south.
He describes it as "A landform that pulls in the distant landscape of the Criffel mountain, the Nith River, Dumfries and the cosmic setting." The project received the following awards: 2011 Health Facilities Scotland Awards (design commendation), 2012 NHS Scotland HFS Environment and Design Award (winner) and the BREEM awards 2015 (shortlisted).
At 3,797 m, Großglockner is the highest mountain in Austria. As a general rule, the farther east the Northern and Central Alps run, the lower they become. The altitude of the mountains also drops north and south of the central ranges. As a geographic feature, the Alps literally overshadow other landform regions.
These unusual freshwater deposits in the Hangman Grits were mainly formed in desert conditions. As this area of Britain was not subject to glaciation, the plateau remains as a remarkably old landform. The bedrock and more recent superficial deposits are covered in part by moorland which is supported by wet, acid soil.
Cells of Life, a landform at Jupiter Artland The Metaphysical Landscape, was an exhibition of sculpture at Jupiter Artland, 2011. Jencks later exhibited at the Merz Gallery, Sanquhar 2016. The Garden of Cosmic Speculation, designed in part by Jencks and begun in 1988, was dedicated to Jencks' late wife Maggie Keswick Jencks.
Hommage à André Cailleux (1907-1986). Beginning in 1962 he and Callieux published a band of five works on the subject of geomorphology and climate, publishing the last one in 1974. The bulk of his works were published in French. Tricart considered that he had, 'a broad systems approach to landform genesis.'.
In the 1920s, Walther Penck developed an alternative model to Davis's. Penck thought that landform evolution was better described as an alternation between ongoing processes of uplift and denudation, as opposed to Davis's model of a single uplift followed by decay.Ritter, Dale F., R. Craig Kochel, and Jerry R. Miller. Process geomorphology.
Where human geography is concerned, the regions and subregions are described by the discipline of ethnography. A region has its own nature that could not be moved. The first nature is its natural environment (landform, climate, etc.). The second nature is its physical elements complex that were built by people in the past.
Rocky shoreline at Ardnave Point. In the background is the coast of north Islay east of Loch Gruinart.Ardnave Point (Scottish Gaelic, Àird an Naoimh) is a coastal promontory on the northwest of Islay, a Scottish island. This landform has a rocky northern shore and extensive dunes on the upland areas of the point.
Aerial view of Sears Point and the Napa Sonoma Marsh. View is to the northeast. Sears Point is a prominent landform that juts into the San Pablo Bay in Sonoma County, California, United States. This hill is the southernmost peak of the Sonoma Mountains and forms the southwestern ridge above Tolay Lake.
The mosque is located near the southern cemetery of the Muqattam Hills, a low range of hills to the east of Cairo. It has an average height of with the highest peak at above sea level. It is divided into three sections. The highest segment is a low mountain landform called Moqattam Mountain.
Separated from the center of the Cargo Muchacho Mountains by 7 mi, the volcanic landform is at the base of alluvial fans. Pilot Knob has a height of , and the entire mountain block is about 2 x 2 mi. The mountain has a rock quarry on its north side, visible from Interstate 8.
Pilot Knob is accessed from Interstate 8, the landform being east of the Algodones Dunes and east of El Centro, California in southeastern Imperial County. The All American Canal is cut from the south border of Pilot Knob, and can be seen in aerial views traversing the Algodones Dunes to the west.
The island is a basalt mesa landform with a shoreline of cliffs made of basalt columns. These geological formations make it "The Yellowstone Park of the Penghu". The columns can be seen in a path around the island. The southwest side of the island has a stepped basin known as "Lotus Terrace" ().
Pieniny, Poland Inside a ravine in Upper Missouri River Breaks National Monument, Montana, United States. A ravine is a landform that is narrower than a canyon and is often the product of streambank erosion.Definition of "ravine" at Merriam-Webster Ravines are typically classified as larger in scale than gullies, although smaller than valleys.
Pecked curvilinear nucleated petroglyphs on a rock on Ring Mountain Ring Mountain is an elevated landform on the Tiburon Peninsula in Marin County, California. This mountain was named for George E. Ring, who served as a Marin County Supervisor from 1895 to 1903. A number of rare and endangered flora inhabit Ring Mountain.Earth Metrics Inc.
1121The identification of Mount Kamuriki as this location appears to be from legends in the Yamato Monogatari (951 AD), the Sarashina Nikki (1059 AD), and the Konjaku Monogatarishū, (c.1120 AD) among others. The mountain has a landform (the Bokodaki Iwa), which resembles a person carrying another person on his back up the mountain.
The resulting building form is monumental with enclosing, defining, and confronting space and adjacent buildings with a sense of elegance reflected in its green space. Designed by Michael Van Valkenburgh Associates, Inc., the landscape attempts to increase nature on the site through landform strips around the building's perimeter and construction of an arboreal bosque.
Sierra de Famatina in Argentina interpreted as part of a "grossfalt" by Penck. Penck thought earths surface could be divided into three types of regions each with an own landform association. First there were regions of grossfalt and general doming, then there were regions of pure doming, and at last there were regions of stability.
The Lahontan Valley is a basin in Churchill County, Nevada, United States. The valley is a landform of the central portion of the prehistoric Lake Lahontan's lakebed of 20,000-9,000 years ago. The valley and the adjacent Carson Sink represent a small portion of the lake bed. Humboldt Lake is to the valley's northeast.
The Matmor Formation near the northern rim of Makhtesh Gadol HaMakhtesh HaGadol (, lit. The Big Crater) is a makhtesh, a geological erosional landform of Israel's Negev desert. It measures 5 x 10 km.The Makhteshim Country and the connected Great Rift Valley Segment A makhtesh has steep walls of resistant rock surrounding a deep closed valley.
The Deadman Hills are a low mountain range in the central Mojave Desert, in San Bernardino County, southern California. The hills define the eastern side of Apple Valley, both the landform and community. California State Route 18 passes through the southern end of the range en route to the Lucerne Valley to the east.
This landform is a major part of the Nxai Pan National Park, and is a seasonal home to large herds of zebra and wildebeest. In the rainy season between December and April the pan becomes grassy and attracts these animals in their tens of thousands, along with smaller numbers of gemsbok, eland and red hartebeest.
There is generally little human influence on landform features visible within the city limits. However, in the northwestern part of the city there is a huge hollow, a remnant of a former sand mine. Although there were once plans to build a waterpark in this area, they were later abandoned and the site remains unused.
Driskill Mountain is a landform created by the erosion of unlithified Paleogene sediment. Its summit consists of nonmarine quartz sands of the Cockfield Formation. These sands overlie shallow marine and coastal clays, silts, and sands of the Cook Mountain Formation, which form the bulk of Driskill Mountain. Mountaintop flora include wild azalea and dogwood.
Fresnal Canyon is a major landform feature within the Baboquivari Mountains in the southwestern part of North America. This locale has been a notable place for archaeological recovery of pre-ceramic Native American habitation.Vorsila L. Bohrer. 2007 This canyon has a number of native flora and fauna, including presence of the elephant tree (Bursera fagaroides).
At Canyon de Chelly, the trail to White House Ruin,Lucchitta 2001 descends through the Shinarump Conglomerate, but also has a tributary slot canyon landform with large accumulations of the Shinarump erosional debris on the slot-canyon floor. The trail then descends through the cross–bedded cliffs (fossil sand dunes) of the De Chelly Sandstone.
A relief generation is a set of landforms within a larger landform assembly that can be distinguished by their shape, age, scale and process that created them. A relief generation is typically nested within a larger and older generation and host itself younger and smaller generations. The concept was coined by Julius Büdel in 1955.
Traditional morphotectonic methods directly associated landform structure with geologic origin, with little regard to actual geophysical data. In more recent decades, morphotectonists have developed a more analytic approach with the advancement of technologies including the advancement of dating methods, development of new geodetic tools, and the availability digital topographic data along with high-speed computing.
Sea level changes and the isostatic rise of land makes charting post-glacial coastlines a complex task, but it is evident that the island is ringed by post glacial raised beaches.McKirdy et al. (2007) p. 28. King's Cave on the south west coast is an example of an emergent landform on such a raised beach.
It is a substantial and relatively intact 19th- century lightstation of outstanding architectural quality. The headland is a dramatic landform of great natural beauty. The construction of the lightstation provides a counterpoint and human scale. While the vegetation has been modified over the 100 years it contributes to the evocative nature and character of the place.
Kastelli Hill (also Kasteli; or Καστέλι) is a landform at the city of Chania on the island of Crete in the present day country of Greece.J. Fisher, 2001 The Minoan city of ancient Cydonia was centered on Kastelli Hill,C. M. Hogan, 2008 which later was selected by the Romans as the site of an acropolis.
Hood Mountain with vineyards in foreground. According to the U.S. Census Bureau, the county has an area of , of which is land and (10.9%) is water. The county lies in the North Coast Ranges of northwestern California. Its ranges include the Mayacamas and the Sonoma Mountains, the southern peak of the latter being the prominent landform Sears Point.
Sagadahoc County within the State of Maine, location of a majority of Merrymeeting Bay. Merrymeeting Bay (also formerly known as Maremiten) is a large freshwater tidal bay in Sagadahoc, Lincoln, and Cumberland counties, in the U.S. state of Maine. Merrymeeting Bay's unusual geography defies common landform terms. It is not what is usually meant by the word bay.
The largest and most abundant solutional caves are located in limestone. Limestone dissolves under the action of rainwater and groundwater charged with H2CO3 (carbonic acid) and naturally occurring organic acids. The dissolution process produces a distinctive landform known as karst, characterized by sinkholes and underground drainage. Limestone caves are often adorned with calcium carbonate formations produced through slow precipitation.
Village is located on the foot of a hilly landform, exposing the village's terrain to massive soil erosion. Forest Conservation Botswana, through the village development committee has spearheaded efforts to reduce the soil erosion phenomenon affecting the village. Mosu village is situated at around 56km from Letlhakane village at -21.18749925°S 25.95166286°E latitude/longitude decimal degrees.
According to Leser, it is also called a sill (geology), and is a gently arched landform of various orders of size in topographic, sub-glacial or sub-hydric geology. It may be as small as a rock formation in a river or may assume continental scale.Leser, Hartmut (ed.). Wörterbuch Allgemeine Geographie, Munich: dtv, 2005, p. 822.
The Ötztal Alps, a mountain range in the central Alps of Europe, are part of the Central Eastern Alps, and can both be termed as ecoregions. A conifer forest in the Swiss Alps (National Park). An ecoregion is a "recurring pattern of ecosystems associated with characteristic combinations of soil and landform that characterise that region".Brunckhorst, D. (2000).
Tuba's topography is generally characterized by irregular rugged terrain and steep slopes with several mountain peaks rising from the table land itself. Mount Santo Tomas, the highest peak in the municipality soars to above sea level. Four major rivers/streams and 49 tributary/minor rivers and creeks intersect the landform and serve as the drains of the municipality.
The Cathedral in the Waitomo Glowworm Caves. Geological and volcanic activity has created around 300 known limestone caves in the Waitomo region over the last 30 million years. The limestone formation in the Waitomo Glowworm Caves occurred when the region was still under the ocean about 30 million years ago.Waitomo Caves: Landform Evolution, Waitomo, New Zealand.
Mangshi River Mangshi has an area of . There are two main plains in Mangshi named Mangshi Ba () and Zhefang Ba (). The city of Mangshi is situated at the east of Mangshi Ba. Mountain is the primary landform of Mangshi, making up approximately 84.48% of the territory. Mount Qingkou () is the city's highest point, with an altitude of 2,889.1 meters.
Amari () is a village and a municipality in Rethymno regional unit, Crete, Greece. The seat of the municipality is the village Agia Foteini.Kallikratis law Greece Ministry of Interior The municipal unit has an area of . One of the major geographic features of Amari is the Amari Valley, a landform of high elevation known for olive cultivation.
Climax Springs is located at (38.103626, -93.051339). According to the United States Census Bureau, the village has a total area of , all land. The town is located on a ridge-like landform in the northern Ozarks. It is approximately six miles south of the Lake of the Ozarks, and about 3.5 miles north of the Little Niangua River.
The Hangman Sandstone represents the Middle Devonian sequence of North Devon and Somerset. These unusual freshwater deposits in the Hangman Grits, were mainly formed in desert conditions. As this area of Britain was not subject to glaciation, the plateau remains as a remarkably old landform. Quartz and iron mineralisation can be detected in outcrops and subsoil.
Hanging canal (middleground) flowing from right to left along the west side of the long and narrow mesa landform near the mouth of Marijilda Canyon. At this point, the canal is about 50 meters above the western basin. The canal coursing upslope illusion is discernible. Prehistoric Bajada "hanging" canals of southeastern Arizona were constructed after c.
In simplest terms, a nabkha is a sand dune that forms around vegetation. It is an aeolian landform, a structure built and shaped by the action of wind. Nabkhas are common and occur in many regions. Well known nabkha fields occur in the Arabian Desert of Kuwait, the Hotan River Basin in Xinjiang, China,Wu, S., et al. (2008).
Savernake's landform is rolling downland, dissected by both dry and wet valleys. The valleys within the forest, of which there are four, are all dry, and the presence of Cretaceous deposits of Clay-with-Flints creates the damp, heavy soils suited to dense cover of oak and beech. There are patches of poor drainage and wet soil.
On the downside, higher frequencies are less susceptible to diffraction. This means that the signals will not bend around obstructions as readily as a VHF signal. This is a particular problem for receivers located in depressions and valleys. Normally the upper edge of the landform acts as a knife-edge and causes the signal to diffract downwards.
Jianglangshan or Mount Jianglang () is a mountain in Jiangshan, Zhejiang, China. Three peaks from north to south make its recognizable "river-shaped" arrangement, as follows: Lang Feng, Ya Feng and Ling Feng. Lang Feng has elevation of . The mountain exhibits Danxia landform, and was inscribed onto the World Heritage List in August 2010 as part of China Danxia.
Badrinath, Hemkund Sahib, Valley of Flowers and Auli. Chamoli also happened to be a birthplace of "Chipko movement". Chamoli proved itself "the most spectacular in its natural assets; be it scenery, valley aspects, water-edges, floristic varieties, dramatic landform or the climatic cardinalities". The district is also inhabited by Bhotiya ethnic group who adhere to Hinduism.
Raisz is best known for his physiographic maps, which describe landforms using his "orthoapsidal" or "armadillo" projection (essentially a small-scale variation on an isometric projection). Created for continents, nations and states, they form a solid corpus of work whose use continues today. Raisz Landform Maps, operated by his family, continues to publish much of his work.
Mikir Hills are a group of hills located to the south of the Kaziranga National Park, Assam. The easternmost Meghalaya comprising the detached Mikir Hills is partly isolated being surrounded by three sides. Karbi plateau or Mikir Hills is known oldest landform in Assam. It is pear-shaped and has an area of about 7000 sq. km.
The landscape there has been designated a UNESCO World Heritage Site. There are other more local names for similar landforms, such as a pavement barren, although this term is also used for similar landforms based on sandstone. In the United Kingdom the exposed landform is called a limestone pavement and thinly covered limestone is known as calcareous grassland.
In August 1992, Jiguan Cave was developed, completed on March 31, 1993, and it opened up in April 1993. Jiguan Cave belongs to the limestone cave, mainly consists of stalactites and stalagmites. It is geologically described as a karst landform. This cave reaches a length of meters, the vertical stratification is five, and it drops 138 meters.
Southern edge of Gruinart Flats. The Gruinart Flats is a low-lying landform on the western part of the isle of Islay in Scotland. The locale is an important conservation area, having been designated as an SSSI. Much of the Gruinart Flats is a marshy area operated by the Royal Society for the Protection of Birds.
By the early 20th century, the isthmus connecting the landform to Glasshouse Point had eroded, making it a proper island. Today, most of the island is a part of Colonial National Historical Park, including Historic Jamestowne. The rediscovery of the James Fort in 1996 by Jamestown Rediscovery has led to significant archaeological discoveries of the early colonial settler period.
Even though the Great Lakes–St. Lawrence Lowlands is the smallest landform region in Canada, Southern Ontario and Quebec have a dense population and are home to about 50 percent of the population of Canada. Historically, the lower Great Lakes-St. Lawrence River Valley region attracted European immigrants and United Empire Loyalists with its "diversified resource base".
Early explorers of the bay called the landform Ridge Point and Brannan Bluff, but by 1851 Table Bluff had stuck. Seth Kinman was an early resident. Because of its rich soil, Table Bluff has been the site of a small agricultural community since the 1850s. At present, hay fields and cattle ranches occupy most of the bluff.
The Nyangadzi river forms the border with Manicaland to the east. Much of the landform is rolling low hills divided by river valleys. About half the land is over altitude and the central watershed in the south and centre is at . Only a few isolated mountains and the spine of the Umvukwes Range in the west rise higher.
Nuvuk, once North America’s northernmost village, was located at the tip of Point Barrow, Alaska. The Iñupiaq name means "point" or "promontory of land" and refers both to the landform and the village. Archaeological evidence indicates that Point Barrow was occupied for over 1,500 years prior to the arrival of the first Europeans. Occupation continued into the 1940s.
In fluvial geography, a debouch is a place where a body of water pours forth from a narrow opening. Some examples are: where a river or stream emerges from a narrow constraining landform, such as a defile, into open country or a wider space; a creek joins a river; or a stream flows into a lake.
The landform and landcover within the basin is highly diverse. Ranging from lowland urban, agricultural, wetland and mangrove to natural riparian, plantations, upland agriculture and mountainous forest including primary forest. The area is classified by DENR as 77.5% forestlands and 22.5% alienable and disposable land. This is not a true land uses (or land cover) classification.
Sanming has four well preserved and protected National Parks. The city was labeled as the most "green" city of the most "green" province in China. Da Jin Hu, which is the most famous tourist spot in Sanming, is also well known as Taining Gorden Lake Geopark marked by UNESCO. The Geopark is famous for its unique Danxia Landform.
She had grounded during the night on a landform not on their charts. The crew took to the boats and waited near Mary for dawn. In the morning the crew discovered they she was on a sandbank, not a reef. Mary had lost her masts, she was half full of water, and her back was broken.
Mount Ararat, as seen from Armenia A mountain is a large landform that rises above the surrounding land in a limited area, usually in the form of a peak. A mountain is generally considered to be steeper than a hill. Mountains are formed through tectonic forces or volcanism. These forces can locally raise the surface of the earth.
During times of extremely high flow, the bars may become covered; only to resurface when the flow decreases. Most braid bars do not remain stable or in one location. However, vegetation succession on braid bars can increase the stability of the landform. They are commonly composed of sand or gravel and typically occur in braided rivers.
Drummers in Ijomu Oro village, Kwara State. Important tourist attractions in Kwara State include Esie Museum, Owu waterfalls, Imoleboja Rock Shelter, Ogunjokoro, Kainji Lake National Parks and Agbonna Hill Awon Mass Wedding in Shao. There is also Sobi Hill amongst others which is the largest landform in Ilorin, the state capital. A huge natural reserve also divides the state into East and West.
This site is designated due to its geological qualities: a spectacular landform created during the Ice Age. Cwm Dewi SSSI is one of the most important sites in Britain where Quaternary landforms and deposits can be studied. The valley which separates Dinas Island from the adjacent plateau was formed by the meltwater produced when an ice sheet which covered north Pembrokeshire thawed.
Craignish (Scottish Gaelic, Creiginis) is a peninsula in Argyll, on the west coast of Scotland. It lies around south of Oban, and north-west of Lochgilphead. The peninsula is around long, and is aligned along a north-east to south-west orientation, in common with much of the landform of coastal Argyll. To the south is Loch Craignish, which contains several small islands.
Convective precipitation occurs when air rises vertically through the (temporarily) self-sustaining mechanism of convection. Stratiform precipitation occurs when large air masses rise diagonally as larger-scale atmospheric dynamics force them to move over each other. Orographic precipitation is similar, except the upwards motion is forced when a moving air mass encounters the rising slope of a landform such as a mountain ridge.
Mount Rumpke is above sea level and the highest landform in Hamilton County, Ohio, clearly visible from U.S. Route 27. It is the largest landfill in the state of Ohio and the sixth largest in the United States. It is sometimes claimed that it is the highest point in Ohio, but in fact there are higher elevations in many Ohio counties.
Digital supervised or unsupervised landform classification employing crisp or fuzzy clustering logic have opened new possibility to the viable solutions. However, computation algorithms are subject to scale dependence matters and arbitrary definition of class boundaries. The presence of vegetation cover and rugged terrain may also reduce the applicability. Statistical and computational algorithms to identify correlations are developing vigorously for image analysis.
List of beaches of South Africa, A beach is a geological landform along the shoreline of a body of water. It usually consists of loose particles which are often composed of rock, such as sand, gravel, shingle, pebbles, or cobblestones. The particles of which the beach is composed can sometimes instead have biological origins, such as shell fragments or coralline algae fragments.
Hageman Peak () is a montane landform pinnacle rising to about at the northwest end of the Staccato Peaks in southern Alexander Island, Antarctica. The peak was photographed from the air by Lincoln Ellsworth in 1935, and was named by the Advisory Committee on Antarctic Names for Lieutenant Commander Roger H. Hageman, U.S. Navy, an LC-130 aircraft commander during Operation Deep Freeze, 1969.
Cerro Toro is a Cretaceous landform of the Magallanes Foreland in the Patagonian region of southeastern Chile.Ramos & Keppie, 1999Hubbard et al., 2008 The Cerro Toro is an element of the southern Andes and a product of the Andean orogeny, caused by the subduction of the Nazca Plate beneath the South American Plate. The formation of the Cerro Toro began in the Jurassic.
The city has been known by at least two Tagalog names, the first being Tangway, which was the name given to the area by Tagalog settlers. Tangway simply means "peninsula". The second is Kawit or "hook", referring to the hook-shaped landform along the coast of Bacoor Bay, and from which the Chinese Keit and Spanish Cavite are in turn derived.
The Bjorne Peninsula is located on the western coast of Ellesmere Island, a part of the Qikiqtaaluk Region of the Canadian territory of Nunavut. It protrudes northwest into Norwegian Bay from the island's mainland. Goose Point, a narrow isthmus, is the furthest northwest landform. Other areas of the peninsula include Schei Point (north), Little Bear Cape (west), and Great Bear Cape (southwest).
September 2011. Due to its situation on a geest, or slightly raised landform, the town was spared the great floods that inundated much of the region in the Middle Ages. Prior to the Reformation, Bunde belonged to the Roman Catholic Diocese of Münster. Bunde became predominantly Protestant in the early 16th century, largely following the Reformed (Calvinist) faith as in the adjacent Netherlands.
The range has a white soil and bedrock, resembling chalk, and was a 'white landform' Valley landmark before suburban development on it in the 1960s. The white rocks are marine shales. Geologists are unsure of its relationship with other rock formations in Southern California, although Thomas Dibblee has identified it as a member of the Sisquoc Formation.Dibblee, T.W., and Ehrenspeck, H.E., ed.
There are 66 snow-capped peaks in the territory, including 36 large ice peaks. The mountaintops have snow all the year round, and there are glaciers of different sizes around the peaks. The landform features severe drought and erosion, bare mountain and sparse vegetation. Due to the different rock types of the mountains, they are gray, black, yellow, red and white bare mountains.
Alki Point is a point jutting into Puget Sound, the westernmost landform in the West Seattle district of Seattle, Washington. Alki is the peninsular neighborhood on Alki Point. Alki was the original white settlement in what was to become the city of Seattle. It was part of the city of West Seattle from 1902 until that city's annexation by Seattle in 1907.
Point of Hellia.The Point of Hellia is a headland on the northwest coast of the Orkney Mainland,United Kingdom Ordnance Survey Map Landranger Map, Orkney Mainland, 1:50,000 scale, 2002 Scotland. This landform extends into the southern part of Eynhallow Sound, a seaway of the North Sea. Gurness, an Iron Age broch promontory fort, is situated on the Point of Hellia.
Map of river discharge in the Netherlands; the majority flows through the Grote rivieren The Rhine-Meuse delta and the rivers that flow into it form the Grote rivieren The Grote rivieren, literally translated Great (or Large) rivers, is a landform in the Netherlands. Also, the term is commonly used for a divide in Dutch culture linking to the broader Dutch-Flemish culture.
These subtropical rainforests are part of the Gondwana Rainforests of Australia and contain the rare Antarctic beech trees. Springbrook plateau has been described as "the Switzerland of Queensland" and a unique wonder. Springbrook was widely considered to be part of the McPherson Range. As the area's geology was understood it has now come to be typically described as a distinct plateau landform.
The summit is a total of above sea level. Historically, the western slope was generally free of vegetation, while the summit and eastern and southern slopes were lightly wooded. Directly to the south is Big Round Top, higher and densely wooded. The igneous landform was created 200 million years ago when the "outcrop of the Gettysburg sill" intruded through the Triassic "Gettysburg plain".
Danxia landform is formed from red-coloured sandstones and conglomerates of largely Cretaceous age. The landforms look very much like karst topography that forms in areas underlain by limestones, but since the rocks that form danxia are sandstones and conglomerates, they have been called "pseudo-karst" landforms. They were formed by endogenous forces (including uplift) and exogenous forces (including weathering and erosion).
Pitted surfaces abound and—in addition to the disrupted surfaces—are typically associated with the degradation of a glacial surface near the glacier's terminus. A lineated valley fill within a graben in the southern Phlegra Montes, descending down the massifs' western piedmont. HRSC digital terrain model. This particular landform was examined in detail by Colman Gallagher and Matthew Balme in a 2015 study.
Cebollera Vieja Peña Cebollera, Cebollera Vieja or pico de las Tres provincias is a mountain which is part of Sierra de Ayllón mountain range in Sistema Central system of mountain ranges. A tripoint related to the autonomous communities of Madrid, Castilla–La Mancha and Castile and León is located on this elevation. The height of this landform is 2,129 metres.
Ella is an unincorporated community in Morrow County, Oregon, United States. Ella lies along Immigrant Lane and the Oregon Trail east of Cecil and south of Boardman. Well Spring, mentioned in many immigrant journals, is east of Ella along the trail. About south of Ella is a landform known to immigrants as Well Spring Butte but later renamed Ella Butte.
The depression is flat and very shallow with fine textured sediment at its lowest portions. The lowest section of the Godzareh depression is 467 m above sea level. The depression only receives runoff water when the main tributaries are overflowing every 10 years on the average. In general, a geological depression is a landform that is sunken or lower than the surrounding area.
Depending on the type of geomorphologic classification employed and the author who suggested it, the karst landform can be defined either a doline or a "karst basin" (). It is traditionally called "karst basin", following the suggestion of Carmelo Colamonico, who first studied the doline and saw in its large size and shallow depth a good reason to distinguish it from a normal doline.
Crater Lake formed from a network of lakes and ponds, eventually reaching a depth of . Lake levels rose while the Wizard Island landform inside the crater was forming. Water interacted with lava flows to form pillow lava. Because of climate change patterns over time, Crater Lake's surface level has changed, dropping as much as for example at the beginning of the 20th century.
A Makhtesh is a geological landform considered unique to the Negev desert of Israel. A makhtesh has steep walls of resistant rock surrounding a deep closed valley which is usually drained by a single wadi. The valleys have limited vegetation and soil, containing a variety of different colored rocks and diverse fauna and flora. The best known and largest makhtesh is Makhtesh Ramon.
The Irishtown Bend landform is located on the west bank of the Cuyahoga River in Cleveland, Ohio. It runs from Columbus Road downstream to the Detroit-Superior Bridge, a distance of about . It extends from the shore of the Cuyahoga River up the hill to Franklin Avenue and W. 25th Street. The summit of the west side plateau is roughly above the river.
The Antarctic Circumpolar Current is the strongest current system in the world oceans and the only ocean current linking all major oceans: the Atlantic, Indian, and Pacific Oceans. Seawater density fronts after . The ACC connects the Atlantic, Pacific, and Indian Oceans, and serves as a principal pathway of exchange among them. The current is strongly constrained by landform and bathymetric features.
In 2010, it was categorized as an AAAA level tourist site by the China National Tourism Administration. In the 2010 UNESCO list of world heritage sites, Langshan was designated a natural World Heritage Site as part of China's Danxia landform. On August 3, 2016, it has been categorized as an AAAAA level tourist site by the China National Tourism Administration.
Geo of Ork from the sea.The Geo of Ork is a narrow and deep cleft in the cliff face of the northernmost point on the island of Shapinsay in the Orkney islands. The term geo or gya derives from Old Norse gjá. This landform was created by the wave driven erosion of cliffs along faults or bedding planes in the rock.
This word was created to avoid confusion with an English term for a vertical or steeply inclined karstic shaft in limestone. However, given widespread usage of this term for a type of fluvial sculpted bedrock landform, pothole is preferred in usage to swirlhole.Richardson, K. and Carling, P., 2005. A typology of sculpted forms in open bedrock channels. Special Paper 392.
The surface elevation is relatively consistent, varying in height from only to above the Ordnance Survey data. In the south there is an area of low-lying carr (landform) – Sun Beck, Birdforth Beck and Ings Beck, which are part of the tributary system of the River Swale, drain the land and separate Thormanby from Sessay, Birdforth and Carlton Husthwaite respectively.
223; Sansome, Minnesota Underfoot, pp. 110–11. The Minnesota River lies in the bed of the glacial River Warren, a much larger torrent that drained Lake Agassiz while outlets to the north were blocked by glaciers. The Coteau des Prairies divides the Minnesota and Missouri River valleys, and is a striking landform created by the bifurcation of different lobes of glacial advance.
Ruby Ridge is a mountain ridge in the Kaniksu National Forest (administered as part of the Idaho Panhandle National Forests) in southern Boundary County, Idaho, United States. The landform gained notoriety when an armed standoff named after the ridge occurred nearby in late August 1992, in which two civilians and one officer of the United States Marshals Service were killed.
Vivari Channel in Albania links Lake Butrint with the Straits of Corfu. In physical geography, a channel is a type of landform consisting of the outline of a path of relatively shallow and narrow body of fluid, most commonly the confine of a river, river delta or strait. The word is cognate to canal, and sometimes takes this form, e.g. the Hood Canal.
Kōnan is located in the northern part of the Nōbi Plain, on the southern bank of the Kiso River. The city extends 6.1 km from east to west and 8.8 km from north to south. The landform is generally a flat, fertile alluvial fan. Located approximately 20 kilometers from the Nagoya metropolis, it is also a traffic node bordering Gifu Prefecture.
Hooiberg is a high volcanic formation on the island of Aruba. It is located almost in the center of the island and can be seen from virtually anywhere on the island. The Dutch word hooiberg, literally translates into haystack in English, as the landform is said to resemble a stack of hay. Many have remarked about the panoramic views obtained atop Hooiberg.
Vallis or valles (plural valles )In Latin, the singular is valles (with a short 'e') or vallis, and the plural is valēs with a long 'e'. is the Latin word for valley. It is used in planetary geology to name landform features on other planets. Scientists used vallis for old river valleys they discovered when they sent the first probes to Mars.
Sheep grazing on southern slopes of Bogjurgan HillBogjurgan Hill is an elevated landform at the southern verge of the Fetteresso Forest in Aberdeenshire, Scotland.United Kingdom Ordnance Survey Map Landranger 45, Stonehaven and Banchory, 1:50,000 scale, 2004 Its top is at an elevation of above sea level. Historical features in this region of Kincardineshire include Fetteresso Castle, Drumtochty Castle and Muchalls Castle.
The name was changed to Verona (after Verona, Italy) upon its incorporation as a town on February 18, 1861. The town lengthened its name to Verona Island, matching the name of the landform on which it was located, in a March 27, 2004 referendum.March 27, 2004 name change referendum The island was once a shipbuilding village. In 1905 the last vessel was built.
In time, it became possible to construct radar maps from topographic maps. Preparation of the maps required the route to be flown by an aircraft. A radar on the aircraft was set to a fixed angle and made horizontal scans of the land in front. The timing of the return signal indicated the range to the landform and produced an amplitude modulated (AM) signal.
Alejandro de Humboldt National Park () is a national park in the Cuban provinces of Holguín and Guantánamo. It is named after the German scientist Alexander von Humboldt who visited the island in 1800 and 1801. The park was inscribed as a UNESCO World Heritage Site in 2001 for of its size, altitude range, complex lithology, landform diversity, and wealth of endemic flora and fauna.
The municipality contains much of the Waterberg Biosphere, a UNESCO designated Biosphere Reserve. The Waterberg Biosphere is a massif of approximately . Waterberg is the first region in the northern part of South Africa to be named as a Biosphere Reserve by UNESCO. The extensive rock formation was shaped by hundreds of millions of years of riverine erosion to yield diverse bluff and butte landform.
It is the most famous landform in Albay and in the whole Bicol Region. This active volcano falls under the jurisdiction of eight municipalities and cities of Albay: Camalig, Daraga, Guinobatan, Legazpi City, Ligao City, Malilipot, Santo Domingo, and Tabaco City. The western coast of the province is mountainous but not as prominent as the eastern range with the highest elevation at around ."Mount Pantao, Oas".
The Sturt Tillite formation was the first area in the world to provide definite evidence of Cryogenian glaciation (the Snowball Earth). It is hypothesised that the landform was created from glacial material that dropped from ice floating in the ocean which covered the area 800 million years ago. All kinds of fires are prohibited in the park. It is classified as an IUCN Category III protected area.
The plateau, a tectonic uplift on the much larger Colorado Plateau landform, is the highest in North America. It is over 900 square miles (2330 km²) of mostly forested highland, much of which is part of Dixie National Forest. It has over 50,000 acres (200 km²) of rolling hilly terrain above 11,000 feet (3350 m). The plateau includes Boulder Mountain which peaks at at Bluebell Knoll.
Captain (Sir) John Ross commanded the Victory during his second Arctic exploration (1829—1833), partly in order to regain credibility after charting a fictional landform, Croker Mountains, during his first Arctic expedition. He chose his nephew, Commander James Clark Ross, to be second in command. In 1830, while exploring within the Ross Strait, James Ross charted three islands. He named the group "Beaufort Islands" after Capt.
In the Mixedwood Plains ecozone of Southern Ontario, most land is privately owned and hence cannot be protected as a provincial park, nature reserve, or conservation area. Some of these ANSI lands are held by conservation groups, including Nature Conservancy of Canada and Ontario Nature. This also requires that multiple Life Science ANSIs to represent the features associated to a landform on a landscape fragmented by development.
October 1, 2017. At that time, experts cautioned that the island would likely not last a full year as a separate landform. As of September 18, 2017, Shelly Island was connected to land at low tide, with water continuing to separate the island from the mainland at high tide. Over the next few weeks, the channel between the island and the mainland began to deepen again.
The Lazareva Pećina, which translates Lazar's Cave, is the longest explored cave in Serbia. Located in Bor municipality, near Zlot, the cave is also sometimes referred to as Zlotska Cave. According to 2012's Recent Landform Evolution: The Carpatho-Balkan-Dinaric Region, the cave is long. The cave is situated near the entrance of the deep canyon carved into the mountains by the river Zlotska.
The resulting landform is an isthmus between the lake and the saltwater fjord, in Norwegian called "eid" as in placename Eidfjord or Nordfjordeid. The post-glacial rebound changed these deltas into terraces up to the level of the original sea level. In Eidfjord, Eio has dug through the original delta and left a terrace while lake is only above sea level.Geografi: landskap, ressursar, menneske, miljø.
The land is relatively flat on the saddle between Tai Sheung Tok (大上托), Mau Wu Shan (茅湖山) and Black Hill (五桂山). Ma Yau Tong is suitable for farming with rivers flowing towards the valleys east and west. The landform of the valley west of Ma Yau Tong was greatly changed by the construction of the Tseung Kwan O Tunnel.
The Danxia area is formed from a reddish sandstone which has been eroded over time into a series of outcrops surrounded by spectacular cliffs and many unusual rock formations known as Danxia landform. There are a number of temples located on the mountains and many scenic walks can be undertaken. There is also a river winding through the mountains on which boat trips can be taken.
These small areas above the beaches and dunes at Croyde and Braunton are characterised by their gently rolling landform sloping up from valley floor, small fields with medium to tall boundaries, a variety of building ages, styles and settlement size, much leisure-related development with strong influence of coastal or marine activities, much use of stone, winding narrow lanes, streams, and largely tranquil out of season.
Although geomorphometry started with ideas of Brisson (1808) and Gauss (1827), the field did not evolve much until the construction of the first DEM.Miller, C.L. and Laflamme, R.A. (1958): The Digital Terrain Model- Theory & Application. MIT Photogrammetry Laboratory Geomorphology has a long history as a concept and area of study, with geomorphometry being one of the oldest related disciplines.Schmidt, J. & Andrew, R. (2005) Multi-scale landform characterization.
Paha Ridge Landform Features of Iowa, Iowa Geological Survey, 2006. Accessed 2008-08-12. The word paha means hill in Dakota Sioux.Landforms of Iowa by Jean C. Prior, University of Iowa Press, Iowa City, 1991 Well known pahas include the hill on which the town of Mount Vernon, Iowa developed, Casey's Paha in Tama County, Iowa, and the Kirkwood Paha, home of Kirkwood Community College's campus.
In 1928, the Mineral scientist Jinglan Feng Noticed the widespread distribution of the red gluten layer. Jinglan Feng realized that this is a brand new landform and haven't been named. He decided to name it as DanXia, which come from the word in the ancient Chinese poem of CaoPi " Hibiscus Pool Poetry". The name "Dan Xia" refers to "丹(vermilion)霞(sunglow)" in Chinese.
At first Wilkie refused: he told the Financial Times, "When I realised that Jon was a property developer I didn't want to go anywhere near it". Wilkie was persuaded to join the project after visiting Heveningham with Hunt, studying the original Brown plans and taking inspiration from the landform. Work began in 1995, and parts of the estate were opened for private hire in 2013.
The subduction uplifted the region out of the sea and created a line of volcanoes. Later the crust started to pull apart, creating the current Basin and Range landform. Valleys filled with sediment and, during the wet times of glacial periods, with lakes, such as Lake Manly. In 2013, Death Valley National Park was designated as a dark sky park by the International Dark-Sky Association.
The bottom of the ice blocks became buried in sediment. As the blocks of ice melted, it left depressions in the ground called kettles. Some of these kettles filled up with water to become kettle lakes and kettle ponds. (see Kettle (landform)) ;Glacial Lake Carbon – Catastrophic Glacial Outburst Flood Glacial Lake Carbon was a lake created by the Puget Lobe damming the Carbon River.
Dudley Pond Dudley Pond is an 84 acre Great Pond in the Cochituate census- designated area of Wayland, Massachusetts. The Pond is a shallow glacial landform fed primarily by rain.Dudley Pond Overview Dudley Pond was used in the mid-1800s as a stand-by water source for Boston. At the time it was connected by pipe to the nearby and much larger Lake Cochituate.
Site planning in landscape architecture and architecture refers to the organizational stage of the landscape design process. It involves the organization of land use zoning, access, circulation, privacy, security, shelter, land drainage, and other factors. This is done by arranging the compositional elements of landform, planting, water, buildings and paving in site plans. Site planning is the design and process of planning for a new development project.
Mazarrón is located in the South of Region of Murcia. This municipality borders Cartagena and Fuente Álamo at its east, Alhama de Murcia and Totana and its North and Lorca at its West. In addition, it adjoins the Mediterranean Sea at its south. The main landform of the municipality is a mountain range named Sierra de Las Moreras, which is located in the west.
A concentric crater fill is a landform where the floor of a crater is mostly covered with many parallel ridges. It is common in the mid-latitudes of Mars,Dickson, J. et al. 2009. Kilometer-thick ice accumulation and glaciation in the northern mid-latitudes of Mars: Evidence for crater-filling events in the Late Amazonian at the Phlegra Montes. Earth and Planetary Science Letters.
Rugova is a suitable region for hiking, skiing, mountaineering, paragliding, and picnics. It was ranked as the fourth most important center for winter sports by the International Ski Federation (ISF). Furthermore, in April 2013, Peja won the "Tourism for Tomorrow" award for the project, "Peaks of the Balkans".www.wttc.org Rugova is rich with many landform elements such as caves, waterfalls, glacial lakes, high peaks, and tunnels.
The Sierra de Chinajá is a low karstic mountain range in Guatemala. It is situated in the north of the department of Alta Verapaz and covers an area of approximately . Its highest peak has an altitude of . The mountain range is isolated from other ranges and forms the last major topographic landform between the highlands of the Sierra de Chamá and the lowland plains of Petén.
The Analysis of Spatial and Temporal Trends in Yield Map Data over Six Years. Biosystems Engineering, 84(4), 455-466). It can be shown that an index map of yield (shows areas of consistent over-performance of yield and areas of consistent under-performance) correlates well with a landform classification map (personal communication, Aspinall (2011)Aspinall, D., 2011. Ontario Ministry of Agriculture and Food (OMAF).).
Lady Franklin Point is a landform in the Canadian Arctic territory of Nunavut. It is located on southwestern Victoria Island in the Coronation Gulf by Austin Bay at the eastern entrance of Dolphin and Union Strait. The Point is uninhabited but still had an active North Warning System. Originally part of the Distant Early Warning Line in the Northwest Territories, the site is known as PIN-3.
The city also has jurisdiction over the Baco Islands and the two Silonay Islets on Calapan Bay. The overall land characteristic is a wide plain with rivers, interspersed with wetlands at the seacoast periphery. The highest elevation is above sea level at Bulusan Hill, a long landform east of the city, which interrupts the mostly flat terrain north-east of the Halcon-Baco Mountain Range.
Aerial view of northeast Macanao Peninsula and the Laguna de la Restinga isthmus. The Macanao Peninsula is a geographic peninsula landform, that forms the western end of the Isla Margarita in the Caribbean Sea, in northern Venezuela. It is also a Venezuelan municipality, the Municipality of Macanao Peninsula (Municipio Península de Macanao), in the state of Nueva Esparta. The municipal seat is Boca de Río.
Soils range from clayey to fine clayey somewhat poorly to poorly drained deep soils. These soils are principally grown to paddy rice and can be used for fishpond during rainy season. This landscape is composed of two (2) minor landform units as follows: ::1. River terraces and levees – Narrow river terraces are topographic surfaces, which mark former valley floor levels and resulting from seasonal stream.
A chalk cliff face at the back of the cove slows further erosion. Erosion is just starting to the west, where the sea has again broken through the Portland limestone barrier at Stair Hole. The concordant coast may take one of two landform types. The Dalmatian type, named from Dalmatia on the Adriatic Sea, features long offshore islands and coastal inlets that are parallel to the coastline.
The Ebro River delta at the Mediterranean Sea Sacramento (California) Delta at flood stage, early March 2009 A river delta is a landform created by deposition of sediment that is carried by a river as the flow leaves its mouth and enters slower-moving or stagnant water.Miall, A. D. 1979. Deltas. in R. G. Walker (ed) Facies Models. Geological Association of Canada, Hamilton, Ontario.
Some also suggested this landform caused by the combined effect of shearing and extension or thrusting from crustal shortening. Starting from Permian, Junggar Basin was formed to initiate the foreland basin cycle. There presented extensional shearing and continuous deposition of non-marine foreland basin-fill till Triassic. Since the level of the trapped lake in the basin was rising, finer deposits covered widespread the basin with denudation.
Tourism in Liupanshui focuses on minority folk culture and karst landform tourism. This includes the underground lake in Qilin Cave Park (), Danxia Mountain (), about which Xu Xiake, the Chinese travel writer and geographer of the Ming Dynasty, had written. Yushe National Park () includes the Jiucai Ping Scenic Zone (). The flat-topped Jiucai Ping is the tallest mountain in Guizhou Province at about 2900 meters.
The Spenser Mountains is a topographic landform in the northern South Island of New Zealand. Located at the southern end of the Nelson Lakes National Park and north of the Lewis Pass they form a natural border between the Canterbury and Tasman regions. Several peaks are named after characters in Edmund Spenser’s allegorical poem, The Faerie Queene. Many of the early explorers were evidently literate men.
Elevation is the major factor in temperature levels, with the higher areas, on average, 10 °C (17 °F) cooler, day or night. The overnight lows are not like the "Garden of Eden" because heavy clothes or blankets are needed in the highlands, when the temperature drops to roughly 50–53 °F (10–12.2 °C) at night. The ecology of this landform is semi-desert.
Radar image of pancake domes in Venus's Eistla region. The two larger ones are approximately wide and rise less than above the surrounding plain. These wide and fairly low, flat-topped volcanoes are a type of landform that is unique to Venus. They were probably formed by extrusions of highly viscous lava that was too sticky to flow very far down-slope from their vents.
Longman Hill is a Bronze Age long barrow situated atop a prominent rounded landform in northern Aberdeenshire, Scotland near Banff Bay.United Kingdom Ordnance Survey Map 1:50,000 (2004) Due to the low-lying coastal plain characteristics, the elevation of Longman Hill affords a long-distance view as far as the Moray Firth.C.Michael Hogan (2008) Longman Hill, Modern Antiquarian Nearby is the village of Longmanhill.
The Tizguit Valley is a river-cut landform in the Middle Atlas mountain range, in the Fès-Meknès region of Morocco. Much of the valley is characterised by basaltic rock.J.J. Macaire and C. Cocirta. 1994 This valley is associated with forested areas that may provide habitat for the endangered Barbary macaque, Macaca sylvanus, a primate that prehistorically had a much wider range in northern Morocco.
In the Solinger Platt dialect the word siepenaat means "completely wet through". In East Westphalian Ravensberger Land and in Lipperland such landforms are known as Sieks. But after land amelioration for agriculture, they usually have a trough-shape today. It is possible that there is an etymological relationship between the Middle Low German term for a similar fluvial landform, sike , and the word Siepen.
In the 17th century the site was at the edge of Boston Harbor. During periods of development over the following 260 years, urban rubble and fill was deposited, creating made land between former wharfs. The sculpture is inspired by the dynamic historical landform alterations at the location, changing light and weather patterns found at the ocean's edge, and the industrial design of harbor navigational aids.
Searles Valley is a valley in the northern Mojave Desert of California, with the northern half in Inyo County and the southern half in San Bernardino County, California, United States. Searles Valley is located between the Argus Range to the west and the Slate Range to the east. Death Valley is to the northeast. The valley contains the landform features of Searles Lake and the Trona Pinnacles.
Froze- to-Death Mountain rises to an elevation of at its peak. It is the highest landform in the Froze-to-Death Plateau, a local name for an area within the Beartooth Mountains. Surrounding features include Froze-to-Death Lake and Froze-to-Death Creek. The mountain area is part of the Custer National Forest which is itself a part of the Absaroka-Beartooth Wilderness.
The agency is tasked with protection of coastal resources, including shoreline public access and recreation, lower cost visitor accommodations, terrestrial and marine habitat protection, visual resources, landform alteration, agricultural lands, commercial fisheries, industrial uses, water quality, offshore oil and gas development, transportation, development design, power plants, ports, and public works. The Commission's responsibilities are described in the California Coastal Act, especially the Chapter 3 policies.
Kitt Peak and surrounding peaks form a separate landform between the Quinlin Mountains and the Coyotes. The Quinlins are a linear range, northwest by southeast. From Kitt Peak and northeastwards, the mountains and hills separate into individual units. The Coyote Mountains Wilderness is the largest, and tallest unit in the northeast of the small Coyote Mountains range, which is only about 7 mi long.
There are three main types of mountains: volcanic, fold, and block. All three types are formed from plate tectonics: when portions of the Earth's crust move, crumple, and dive. Compressional forces, isostatic uplift and intrusion of igneous matter forces surface rock upward, creating a landform higher than the surrounding features. The height of the feature makes it either a hill or, if higher and steeper, a mountain.
Lake Pedder, south west Tasmania, prior to inundation as part of a hydro- electric development. Submergence of this unique landform assemblage and geoheritage feature beneath 15 m of water was one of many triggers to formulation of geoconservation philosophy. Geodiversity is the variety of earth materials, forms and processes that constitute and shape the Earth, either the whole or a specific part of it.Zwolinski, Zb. 2004.
London: Penguin, 1984, p. 95. . Their individual formation is that of a cirque. These steps are arranged one above and behind the other at different heights in the terrain and caused by the same geomorphodynamic processes, albeit resulting in different landform shapes depending on the type of rock and the depositional circumstances involved. The lower step often lacks the steep headwalls typical of cirques.
The average height of the troposphere is in the tropics, in the middle latitudes, and in the polar regions in winter. The total average height of the troposphere is . The lowest part of the troposphere, where friction with the Earth's surface influences airflow, is the planetary boundary layer. This layer is typically a few hundred meters to deep depending on the landform and time of day.
Stone run at Mount Kent, East Falkland A stone run (called also stone river, stone stream or stone seaVitosha Nature Park: Basic Information. Landscape. Vitosha Nature Park website.) is a rock landform resulting from the erosion of particular rock varieties caused by freezing-thawing cycles in periglacial conditions during the last Ice Age. The actual formation of stone runs involved five processes: weathering, solifluction, frost heaving, frost sorting, and washing.Stone, Phillip.
The major lakes were connected til Camrose reverse drained their headwaters, Miquelon. The landform lies partly within five different counties, Strathcona, Leduc, Beaver, Lamont and Camrose. The area is relatively undeveloped compared to the surrounding region, and is protected by in part by Elk Island National Park, the Cooking Lake–Blackfoot Provincial Recreation Area, the Ministik Bird Sanctuary, Miquelon Lake Provincial Park and a number of smaller provincial natural areas.
A designed landscape is an area of land which has been modified by people for primarily aesthetic effect. The term is used by historians to denote various types of site, such as gardens, parks, cemeteries, and estates. Such sites are often protected for their historic or artistic value. A designed landscape may comprise landform, water, built structures, trees and plants, all of which may be naturally occurring or introduced.
The Waterberg () is a mountainous massif of approximately in north Limpopo Province, South Africa. The average height of the mountain range is 600 m with a few peaks rising up to 2000 m above sea level. Vaalwater town is located just north of the mountain range. The extensive rock formation was shaped by hundreds of millions of years of riverine erosion to yield diverse bluff and butte landform.
Picture of the Wave Rock, a landmark flared slope in Western Australia. A flared slope is a landform consisting in a rock-wall with a smooth transition into a concavity at the foot zone. Flared slopes form due to weathering being more effective at the regolith or soil-covered base of rock walls. These landforms are common in granitic rocks but occur in other rock types as well, such as ignimbrite.
Charles Jencks Charles Alexander Jencks (21 June 1939 –13 October 2019) was an American cultural theorist, landscape designer, architectural historian, and co-founder of the Maggie’s Cancer Care Centres. He published over thirty books and became famous in the 1980s as theorist of Postmodernism. Jencks devoted time to landform architecture, especially in Scotland. These landscapes include the Garden of Cosmic Speculation and earthworks at Jupiter Artland outside Edinburgh.
A portion of the Shonkin Sag near Highwood, Montana, in 1920. The Shonkin Sag is a prehistoric fluvioglacial landform located along the northern edge of the Highwood Mountains in the state of Montana in the United States. The Sag is a river channel formed by the Missouri River and glacial meltwater pouring from Glacial Lake Great Falls. It is one of the most famous prehistoric meltwater channels in the world.
Tombolo near Karystos, Euboea, Greece Tombolo contrasted with other coastal landforms. A tombolo is a sandy isthmus. A tombolo, from the Italian tombolo, meaning 'pillow' or 'cushion', and sometimes translated as ayre, is a deposition landform in which an island is attached to the mainland by a narrow piece of land such as a spit or bar. Once attached, the island is then known as a tied island.
The Yokot'an inhabit 21 towns in a large area known as "la Chontalpa" that extends across five municipalities of Tabasco: Centla, El Centro, Jonuta, Macuspana, and Nacajuca. In Nacajuca, they form a majority of the population. The terrain is highly varied -- no single landform dominates -- and it has many bodies of water. The land is traversed by seasonally-flooding rivers, and there are numerous lakes, lagoons, and wetlands.
Roads within the cirque and around the central peak Roads in the area are very poorly maintained and are only wide enough for one vehicle. In order to pass the landform, a dangerous, but exhilarating, road which weaves down into the valley and clings to the sheer cliff face on the way back up must be braved. This journey is one of the draws for tourism in the area.
Coire an t-Sneachda (sometimes misspelled as Coire an t'Sneachda) is a glacial cirque or corrie landform in the Cairngorm or Am Monadh Ruadh mountain range in the Grampian Mountains of the Scottish Highlands. The summits of Cairn Lochan (1215m) and Stob Coire an t-Sneachda (1176m) lie above Coire an t-Sneachda's headwall. The Gaelic Coire an t-Sneachda roughly translates to the English language as "Corrie of the Snow".
Dalian Yinshitan Forest National Park or abbreviation () got its name from the giant rocks with vivid shapes. According to textual research from the Geologic Department of Beijing University, the mountains were formed by violent debris that happened 500 million years ago then followed by a landform of ancient debris flow. The mountains’ shapes supposedly reminded of different animals such as a lying horse, a turtle climbing a mountain.
The terrain of Wuqia County is low in the southeast, high in the northwest and southwest, surrounded by mountains. It is a typical mountainous terrain with an altitude of 1,760 - 6,146 meters and a horseshoe shape. The county is located in the wedge-shaped zone in the west of the Kashgar Delta (), which is a fold mountains of the Miocene. The landform appears in the mountains of erosion.
The Pouto Peninsula is a landform on the northern Kaipara Harbour in Northland, New Zealand. The Peninsula runs in the north west to south east direction and is approximately 55 km long. The width varies from about 5.4 km to about 14 km, with the widest part of the peninsula near its southern end. The Tasman Sea is to the west, and the Kaipara Harbour is to the south.
Ark Hill Ark Hill is a mountainous landform within the Sidlaw Hills in Angus, Scotland. This location has been proposed as a windfarm for generating renewable electrical power.Ark Hill Windfarm Proposal, Angus, Scotland Approximately two kilometres to the north is the village of Eassie noted for the presence of the Eassie Stone; this carved Pictish stone is dated prior to the Early Middle Ages.C.Michael Hogan, Eassie Stone, The Megalithic Portal, ed.
Four cities (Cajueiro da Praia, Ilha Grande Luís Correia and Parnaíba) make up the coast of the state. In Maranhão, some unique geographical features (like the Lençóis Maranhenses) are present. The area between Maranhão and Pará is dominated by the "Reentrâncias Maranhenses", a landform similar to a fjord but shorter, narrower and lower. Because of this particular geography, there are almost no beaches at this section of the Brazilian coastline.
The range defines the northern side of the Moreno Valley landform, and is north of the city of Moreno Valley. Their highest point is in elevation. The Box Springs Mountains parallel them along the southwest, and the La Loma Hills and community of Grand Terrace are to the northwest. ;Geology Geologically, the Kalmia Hills are on the northeastern edge of the Perris Block formation, along the San Jacinto Fault Zone.
A mud volcano or mud dome is a landform created by the eruption of mud or slurries, water and gases. Several geological processes may cause the formation of mud volcanoes. Mud volcanoes are not true igneous volcanoes as they do not produce lava and are not necessarily driven by magmatic activity. The Earth continuously exudes a mud-like substance, which may sometimes be referred to as a "mud volcano".
In February 1920, voters approved a $20 million bond issue as part of the Burnham Plan initiative for new lands to complete Grant Park, so as to create the South Shore Development. In 1920, the Field Museum was opened, with the exhibits moved from Jackson Park into the basement. By 1925, new landforms, including Northerly Island, the only offshore landform in the Burnham Plan actually built, were completed to 23rd Street.
In this book, "The Universe in a Single Atom," The Dalai Lama exhibits humble beginnings in science, including finding a brass telescope from the thirteenth Dalai Lama. With the telescope, he was able to find "the rabbit on the moon," a Tibetan saying for a landform on the moon. Utilizing other apparatuses such as cars and watches, the Dalai Lama took interest in the mechanical operations of the objects.
The range is northwest-southeast trending around the Three Lakes Valley where Dog Bone Lake is the large landform in the valley flatlands. The range sits mostly to the north and northeast of Three Lakes Valley. The southern terminus of the range lies in a mixture of hills associated with the north perimeter of the Desert Range to the south. The Desert Range is southwest trending around the Three Lakes Valley.
The Boura Mountains are a mountain range in Djibouti. With a mean peak height of is the ninth highest point in Djibouti, the ecology of this landform is semi-desert. The mountain is located approximately east of Ali Sabieh, 13 kilometres (8 mi) from Assamo by road. The altitude and size of the range affects its weather, with precipitation levels varying greatly and climatic conditions consisting of distinct zones.
The central and western domes are separated by a deep valley, which is now occupied by a reservoir. The central and eastern domes are linked by a low platform. A multistage process of landform development created these domes. The initial step in the development of Hyden Rock was the subsurface alteration by weathering of granite bedrock beneath a lateritised land surface during the Cretaceous Period between 100–130 million years ago.
It is used as a leisure ground for military staff and their friends and families, as well as for scientific research in the untouched Atlantic Rainforest found within the restinga. It has been used as a setting for several telenovelas, including Kubanacan and Da Cor Do Pecado Category:Landforms of Rio de Janeiro (state) Category:Coasts of Brazil Category:Spits (landform) Aerial view of Restinga da Marambaia. Rio de Janeiro - Brazil.
Manresa Island is a former island located in Norwalk, Connecticut, at the mouth of Norwalk Harbor in the Long Island Sound. The earliest name for the landform was Boutons Island, which dates to 1664. By the 19th century, the island had been purchased by John H. Keyser, who lived there and cultivated rare vegetation. He built a causeway in 1860, connecting the island to the mainland of South Norwalk.
As the salt receded, the overlying rock burden sank with it. Salt Valley, located to the immediate southwest, is an example of the resulting landform. At the edges of the valley, where Devils Garden is located, the cracked rock was slightly pulled apart. Rain and snow soaked into the vertical cracks, which dissolved the cementing minerals and loosened grains of sand to be carried away by running water.
The landform is that of eroded pediment plain with well-incised valleys forming a trellis pattern. The soils are developed over a deeply weathered layer of sedimentary rocks consisting of false bedded sandstones which underlies the area. The sediments are of lower cretaceous rocks or Abeokuta formation (Smyth and Montgomery, 1962) which spread monotonously in northwest and southwest directions. The soil is a gravelly Ultisol (Moormann et al.
A landform comprises a geomorphological unit and is largely defined by its surface form and location in the landscape, as part of the terrain, and as such is typically an element of topography. Landforms are categorized by features such as elevation, slope, orientation, stratification, rock exposure, and soil type. They include berms, mounds, hills, cliffs, valleys, rivers, and numerous other elements. Oceans and continents are the highest-order landforms.
The first step in completing an area-based assessment is to compile data in order to identify components of the landscape within a project area. Components of a landscape range from landform, geology, soil, vegetation cover, drainage patterns, built development, land uses, infrastructure, and heritage sites to cultural meaning. This step in the assessment of a landscape is not site specific, but instead, a general description of the landscape.
Illustration of a specimen of glacial fluting from the Great Lakes region A glacial flute is a landform created by the movement of a glacier around a boulder. They are long ridges on the ground parallel to the movement. Examples can be found in many places including Iceland, Alaska and Canada. As glaciers move along the surface of the earth, rocks are slowly mixed in with the ice.
The Interior Plains spread over much of the continent, with low relief. The Canadian Shield covers almost 5 million km2 of North America and is generally quite flat. Similarly, the north-east of South America is covered by the flat Amazon Basin. The Brazilian Highlands on the east coast are fairly smooth but show some variations in landform, while farther south the Gran Chaco and Pampas are broad lowlands.
The Ocoa Valley is a landform in central Chile located by the La Campana National Park. This valley is a locus where considerable archaeological recovery has taken place,Chile.com, 2008 yielding considerable finds of pre- European contact period. According to Dallman and Hogan, some of the greatest stands of the endangered Chilean Wine Palm, Jubaea chilensis are found on the slopes of La Campana that rise up from the Ocoa Valley.
In some geomorphological taxonomies, a mesoregion is a natural region of intermediate size. Mesoregions may be defined on the basis of morpholithogenic conditions and spatial connection.Recent Landform Evolution: The Carpatho- Balkan-Dinaric Region, edited by Dénes Lóczy, Miloš Stankoviansky, Adam Kotarba p. 325 A mesoregion is used in the regionalization of the area, it is a physical and geographic division unit, it is part of a macroregion, and consists of microregions.
Oosäär (also known as Oossaar, Oossäär, Kuradisäär) is a small islet in the Gulf of Riga, belonging to Estonia.Geographic Names Oosäär is approximately long and approximately at its widest, resembling a long, sinuous spit, but not connected to a larger landform. Vegetation is sparse and the island is made up largely of rocks and pebbles. Located a short distance off the coast of Varbla Parish, Oosäär is administered by Pärnu County.
Mount Tityros is a hill landform in western Crete in the vicinity of the modern-day city of Chania, Greece. In ancient times Mount Tityros was associated with the early Cretan city of Kydonia.Strabo (7 BC) GeographicaRobert Pashley (1837) Travels in Crete, J. Murray Residents of the ancient city of Kydonia dedicated a temple to the goddess Britomartis on Mount Tityros.C. Michael Hogan, Cydonia, The Modern Antiquarian, Jan.
On the west a driveway with entry on Antill Street separates Rusten House from other hospital facilities. East of the driveway there remains a tennis court currently used for car parking. The landform indicates that the natural levels were altered to extend the court surface level out towards Antill Street. The car parking area serves staff and visitors to the hospital facilities which are generally west of the Rusten House area.
The Arabic name Mokattam, which means cut off or broken off, refers to how the low range of hills is divided into three sections. The highest segment is a low mountain landform called Moqattam Mountain. In the past the low mountain range was an important ancient Egyptian quarry site for limestone, used in the construction of temples and pyramids. They represent the northwestern part of the limestone sampling area.
This makes it more susceptible to flooding, as it was threatened in the infamous Great Flood of 1993 and the New Year's Day Flood of 2016. Less than one mile south of Gorham is a large hill named Fountain Bluff. Though the bluff is not exceptionally well-known, its rock faces do attract occasional rock-climbers. Etched into cliffs on the north side of this landform are several Native American petroglyphs.
Takuyo-Daisan is a guyot that rises to a minimum depth of and is capped by an approximately square-shaped surface platform at about depth which has a surface area of about . Depressions up to deep cover the flat top. The top is surrounded by a wide and up to high ridge, especially on the northeastern and southern sides. It may be either a bioherm or a karst landform.
M-37 turns north along Garfield Avenue to Peninsula Drive, leaving US 31/M-72. The Mission Point Lighthouse at the northern end of M-37 on Old Mission Point M-37 follows Center Road up the middle of the Old Mission Peninsula. This landform divides Grand Traverse Bay into its east and west arms. The highway runs along a ridge at the center of the peninsula offering views of each arm of the bay.
View of Fraser Canyon near Fountain, British ColumbiaView of Fraser Canyon looking upstream from Fountain, British Columbia. Cisco Bridges - CPR bridge (black) in foreground, CNR bridge (orange arch) in background (with CPR train on it). Photo facing upriver. The Fraser Canyon is a major landform of the Fraser River where it descends rapidly through narrow rock gorges in the Coast Mountains en route from the Interior Plateau of British Columbia to the Fraser Valley.
Sarn Gynfelyn is a shingle spit on the coast of Cardigan Bay, in the county of Ceredigion, Mid-Wales, in the United Kingdom. It is located at Wallog, a few kilometres north of Llangorwen, close to Clarach Bay, south of Borth and north of the town of Aberystwyth. Similar landform examples are found at several points along the Cardigan Bay coast, known as sarnau. They are thought to be long subtidal banks of glacial moraines.
Hollows are a landform on the planet Mercury, discovered during the MESSENGER mission that orbited the planet from 2011 to 2015. Hollows are typically clusters of rimless depressions with flat floors and haloes of bright (high albedo) material surrounding them. Hollows are thought to form by loss of volatiles from the surface by sublimation, caused by the intense solar radiation on the airless planet. They are some of the youngest features on Mercury.
It is bounded by a steeper ascending slope on the landward side and a steeper descending slope on the seaward side (sometimes called "riser"). Due to its generally flat shape it is often used for anthropogenic structures such as settlements and infrastructure. A raised beach is an emergent coastal landform. Raised beaches and marine terraces are beaches or wave-cut platforms raised above the shoreline by a relative fall in the sea level.
The Coastal Barrier Resources Reauthorization Act of 2000 (Public Law 106-514) provided specifications for determining if an area was undeveloped at the time it was included within the CBRS, and ordered the development of a Digital Mapping Pilot Project for between 50 and 75 CBRS areas for the purpose of information precision and accessibility. If some portion of a barrier landform is developed, the remaining undeveloped portion may be included in the CBRS.
Much of the Palala River course is through the Waterberg Biosphere, a massif of approximately 15,000 square kilometers. Waterberg is the first region in the northern part of South Africa to be named as a Biosphere Reserve by UNESCO. The extensive rock formation was shaped by hundreds of millions of years of riverine erosion to yield diverse bluff and butte landform. The ecosystem can be characterised as a dry deciduous forest or Bushveld.
SH-127 begins in downtown Jay at the intersection of South Main Street (US-59/SH-10/SH-20) and South 5th Street. From this point, SH-127 eastbound proceeds north along South 5th Street to Cherokee Street, where it turns west. It turns back to the north along North 14th Street, which it follows out of Jay. Eastbound SH-127 then turns northwest, passing through a landform known as Muskrat Hollow.
The Goda Mountains lie northwest of the Gulf of Tadjoura, Tadjoura Region in Djibouti. They rise to 1,750 metres (5,740 ft) above sea level and are the nation's largest heavily vegetated area. The ecology of this landform is considered an isolated outlier of the Ethiopian montane forest ecological zone, an important island of forest in a sea of semi-desert. Lake Assal (literally translated to "honey lake") is a crater lake in central-eastern Djibouti.
There has been speculation in the scientific community about the nature of the landform. Following the major 16 July 1990 Luzon earthquake, scientists reconsidered their fault models and decided it likely that Benham Plateau has similarly displaced the Philippine Fault System to the west.Pinet and Stephan (1989) in Tectonics of Circum-Pacific Continental Margins p.179 After analysing older models such as that of Pinet and Stephan (1989), scientists reconsidered their fault models.
The volcanic rock landform of Xianju National Park was shaped 120 million years ago. With the Pacific Plate diving beneath the Eurasia Plate, volcanoes in the coastal area of southeastern China erupted on a large scale. Between two eruptions, there wasn't new lava reaching the crater. Thus, in the weathering process, the crater gradually collapsed into a bowl-shaped pit and then became a lake with more and more water retained in it.
Alford is a settlement in South Australia. Alford is in the Hundred of Tickera, northern Yorke Peninsula, about midway between the towns of Kadina and Port Broughton. The natural landform is undulating fertile plains, which often feature limestone and dunes. Founded on the agricultural industry, which surrounds the township, most of the original mallee scrub vegetation has been cleared for highly productive broad-acre wheat and barley farming, plus grazing and mixed farming.
During the age of New Imperialism in the late 19th century European explorers and scientists traveled across the globe bringing descriptions of landscapes and landforms. As geographical knowledge increased over time these observations were systematized in a search for regional patterns. Climate emerged thus as prime factor for explaining landform distribution at a grand scale. The rise of climatic geomorphology was foreshadowed by the work of Wladimir Köppen, Vasily Dokuchaev and Andreas Schimper.
Geomorphically, the Mishmi Hills are divided into 2 sections the flood plains of tributaries of Brahmaputra river and the Arunachal Himalayas consisting of snow-capped mountains, lower Himalayan ranges, and Shivalik ranges. The Hills reach heights above but have not been properly mapped. This hilly area is characterised by steeply sloping landform, sub-tropical evergreen forest and high rainfall. The central part of the Hills wrap around both sides of the Dibang Valley.
The Leshan Giant Buddha is located at the Lingyun Mountain’s Qifeng Peak. Qifeng Peak is located at the junction of the Minjiang River, Qingyi River, and Dadu River. Other than the Leshan Giant Buddha, the Danxia Landform also contains abundant history and cultural connotations, such as cliff tombs and cliff dwelling. The Mahao Cliff Tombs at the Leshan Giant Buddha scenic area were built in the Han Dynasty, indicating ancient local residents’ living habits.
Jubal Early's attack on East Cemetery Hill, July 2, 1863 (engraving from The Century Magazine). Cemetery Hill is a landform on the Gettysburg Battlefield that was the scene of fighting each day of the Battle of Gettysburg (July 1-3, 1863). The northernmost part of the Army of the Potomac defensive "fish-hook" line, the hill is gently sloped and provided a site for American Civil War artillery (cf. the heavily wooded, adjacent Culp's Hill).
The community lies in a district identified by Nova Scotia Museum of Natural History geomorphologists as an area of Sedimentary Lowland within the larger Atlantic Coast Region. The landform was carved through erosion of "weakly metamorphosed Carboniferous sandstones". These characteristics contributed to Cape Breton Island's richer freshwater habitats and areas of natural beauty. This has acted as a draw to European people purchasing homes around the county, particularly those sited near the shore.
Alcyone Cone () is an extinct volcanic cone near the center of The Pleiades, at the west side of the head of Mariner Glacier in Victoria Land, Antarctica. Named by a Victoria University of Wellington Antarctic Expedition field party to Evans Neve, 1971-72, after Alcyone, the brightest star in the Pleiades constellation. The geographical landform is situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
During the age of New Imperialism in the late 19th century European explorers and scientists traveled across the globe bringing descriptions of landscapes and landforms. As geographical knowledge increased over time these observations were systematized in a search for regional patterns. Climate emerged thus as prime factor for explaining landform distribution at a grand scale. The rise of climatic geomorphology was foreshadowed by the work of Wladimir Köppen, Vasily Dokuchaev and Andreas Schimper.
The area is an almost unspoilt example of coastal east Kalgan vegetation system. Composed of granite headlands separated by sandy beaches with lakes and interdunal wetlands, the area contains a number of specific ecosystems. Rocky granite areas exist, including Mount Taylor and Mount Martin, both of which are part of the Gardner Landform unit. The diverse landforms and soils support an array of different habitats and a large number of floral species.
There are no permanent streams in the ATW. The highest landform is Agua Tibia Mountain with an elevation of . Though the summer climate is hot, with limited shade and no water sources, there were no fires in the ATW for 110 years. In the last two decades, there have been four fires including the Palomar Mountain Fire (1987), the Vail Fire (1989), the Agua Tibia Fire (2000), and the Poomacha Fire (2007).
The Sugarloaf Mountain of Rio de Janeiro is a typical example of this landform and is the origin of the common bornhardt nickname "sugar loaf". Bornhardts are seen at their best in arid and semi-arid regions, but occur over a wide range of climates. Found in diverse topographic settings they mainly occur in multicyclic landscapes. Over geological time bornhardts may degrade to form other landforms such as nubbins (or knolls) and castle koppies.
Zamboanga PeninsulaRegion 9 Provinces (Region IX), formerly Western Mindanao, is located in the landform of the same name. It consists of Zamboanga City, Isabela City and the provinces of Zamboanga del Norte, Zamboanga del Sur, and Zamboanga Sibugay. Isabela City is the only territory not on Mindanao island itself and is a part of Basilan. The region's administrative center is Pagadian City and the whole region used to be a single province named Zamboanga.
The homestead sits on the eastern tip of the elevated ridge - almost a peninsula in landform. To its west are a number of farm outbuildings, some 19th century and some 20th century. A large ruin of a colonial brick structure, possibly an agricultural store building or barn, lies to the house's south-west. The garden is neglected for much of the late 20th century but is in essence a mid 19th century hill-top garden.
Exhumation through denudation could be considered as the process of exposing rock packages solely through the removal of their overlying unconsolidated sediments or solid rock layers. Denudation is here considered as a process that removes parts of the Earth's upper crust by physical processes that occur naturally (e.g. glaciers, wind, water, landslides). Through this form of exhumation, something previously buried in sediments, for example a landform, is uncovered and can be exposed.
Admiralty Inlet () is a body of water in Nunavut's Qikiqtaaluk Region. It extends southerly from Lancaster Sound along the western shore of Baffin Island's Borden Peninsula. The hamlet of Arctic Bay is located on Uluksan Peninsula, a landform that juts into Admiralty Inlet south of Sirmilik National Park. Several waterways extend from it, including Elwin Inlet, Baillarge Bay, Strathcona Sound, Victor Bay, Adams Sound, Levasseur Inlet, and Moffet Inlet, before it ends at Jungersen Bay.
13, No 3. P 209-215 Because of these persistent natural forces, sea walls need to be maintained (and eventually replaced) to maintain their effectiveness. The many types of sea wall in use today reflect both the varying physical forces they are designed to withstand, and location specific aspects, such as local climate, coastal position, wave regime, and value of landform. Sea walls are hard engineering shore-based structures which protect the coast from erosion.
The Big Smoky Valley is a landform of the Tonopah Basin between the Toiyabe and Toquima mountain ranges. It is about 100 miles (160 km) in length. Big Smoky Valley was so named on account of haze which frequently settles there. It is known by other names (some with different spellings): including Great Smoky Valley, Smokey Valley, Smoky Valley, Wen-A-No-Nu-Fee Valley, and Won-A- No-Nu-Fee Valley.
Many hypotheses explain the purpose of petroglyphs, depending on their location, age, and subject matter. Some may be astronomical markers, maps, and other forms of symbolic communication, including a form of proto-writing. Petroglyph maps may show trails, symbols communicating time and distances traveled, as well as the local terrain in the form of rivers, landforms, and other geographic features. A petroglyph that represents a landform or the surrounding terrain is known as a geocontourglyph.
James Venture Mulligan is buried in the Mount Molloy cemetery, Bakers Road, Mount Molloy, from Mount Molloy by road. A low cyclone fence, with three gated entrances, surrounds the cemetery. One entrance is for visitors on foot coming from the northern or road side, one for vehicles also from the north, and another for visitors on foot coming from the west. The landform is open woodland slightly sloping towards the south-east.
The northwest section, thus describes the entire landform as a central, and large valley with an attached feeder valley northwest, and in this case the northwest source, and actual course of the Las Vegas Wash. The valley is a fault-bounded structural and hydrologic basin made of alluvial-fan deposits. There are several aquifers contained within the valley including the Las Vegas Aquifer. These heavily depleted water sources exist at about in depth.
Takhti-Tepha Natural Monument () is a landform created by the eruption of mud, slurries, water and gases in proximity of Takhti-Tepha mountain range. This mud volcano is located on plane, south of Dali water reservoir, at 620 m above sea level in Dedoplistsqaro Municipality, Georgia and incorporated in Vashlovani Protected Areas.Takhti-Tefa in Georgia Protected Planet Mud craters, along with small open vents are constantly active, erupting mud, oil and gas.Takhti Tepha mud Volcano.
A caldera-like landform is located between the towns of Malasiqui and Villasis with a center at about 15° 55′ N and 120° 30′ E near the Cabaruan Hills. Several rivers traverse the province. The longest is the Agno River, which originates from the Cordillera Mountains of Benguet, eventually emptying its waters into the Lingayen Gulf. Other major rivers include the Bued River, Angalacan River, Sinocalan River, Patalan River and the Cayanga River.
Aerial view of the Tiburon Peninsula The Tiburon Peninsula is a landform of the San Francisco Bay Area's Marin County and is home to the incorporated municipalities of Tiburon, Belvedere, and a portion of Corte Madera, California.USGS, 0918-07 Much of the peninsula is unincorporated, including portions of the north side and the communities of Paradise Cay and Strawberry. Richardson Bay separates the peninsula from the Marin County mainland. Angel Island lies app.
The western shores of the bay are a lowland known as the Hudson Bay Lowlands which covers . The area is drained by a large number of rivers and has formed a characteristic vegetation known as muskeg. Much of the landform has been shaped by the actions of glaciers and the shrinkage of the bay over long periods of time. Signs of numerous former beachfronts can be seen far inland from the current shore.
Waubonsie State Park is a state park of Iowa, US, located in the Loess Hills region. It is named for Chief Wabaunsee of Potawatomi tribe. Waubonsie State Park is located in the unique Loess Hills, a landform found only along the Missouri River in Iowa and Missouri. As glaciers melted 14,000 to 28,000 years ago, the Missouri River became a major channel for huge volumes of water and sediment during the summer.
The Oak Ridges Moraine is a geological landform that runs east-west across south central Ontario, Canada. It developed about 12,000 years ago, during the Wisconsin glaciation in North America. A complex ridge of sedimentary material, the moraine is known to have partially developed under water. The Niagara Escarpment played a key role in forming the moraine in that it acted as a dam for glacial meltwater trapped between it and two ice lobes.
In 2005, Zhangye Danxia was voted by a panel of reporters from 34 major media outlets as one of the most beautiful Danxia landform areas in China. In 2009, Chinese National Geography magazine chose Zhangye Danxia as one of the "six most beautiful landforms" in China. The area has become a top tourist attraction for Zhangye. A series of boardwalks and access roads have been built to help visitors to explore the rock formations.
An ecoregion encompasses soil types and landform similarities. The Taiga Shield ecozone in the far north includes the Selwyn Lake upland and Tazin Lake Upland ecoregion. This would have vegetation generally corresponding to the Subarctic Woodland. The Boreal Shield ecozone is further divided into the Athabasca Plain and Churchill River Upland, and this area of Northern Saskatchewan has been described by the World Wildlife Fund as part of the Midwestern Canadian Shield forests ecoregion.
Killinaboy lies several metres above the present-day lake level, but Cahir Rock cannot have been overtopped by Inchiquin Lough because its upper surface is etched with rillenkarren, which are a sub-aerial solutional landform It has been pointed out that mushroom-shaped rocks close-to and far-from lakes in Ireland are similarly- shaped, thus the obvious question of whether all of Ireland's mushroom-shaped rocks have developed in a sub-soil environment remains.
Twelve Apostles stacks in Victoria, Australia The Duncansby Stacks at Duncansby Head, Scotland A stack or sea stack is a geological landform consisting of a steep and often vertical column or columns of rock in the sea near a coast, formed by wave erosion.Easterbrook, D.J. "Surface Processes and Landforms", p. 442, Prentice Hall, Upper Saddle River, New Jersey, 1999. Stacks are formed over time by wind and water, processes of coastal geomorphology.
"Processes of Coastal Bluff Erosion in Weakly Lithified Sands, Pacifica, California, USA." Geomorphology 97.3–4 (2008): 483–501. Print. Marginal-sea type coastline The southern banks of the United States border the Gulf of Mexico, intersecting numerous rivers, forming many inlets bays, and lagoons along its coast, consisting of vast areas of marsh and wetlands. This region of landform is prone to natural disasters yet highly and continuously developed, with man-made structures attaining to water flow and control.
The region is predominantly agricultural, with some wetlands, grassland, and forested areas. The Wisconsin DNR labels the majority of the landtype as the Watertown drumlins: "the landform pattern is undulating till plain with drumlins, lake plains, and muck areas common. Soils are predominantly moderately well drained silt and loam over calcareous sandy loam till or silty, loamy and clayey lacustrine." Small portions are associated with the Jefferson Lake Plains; the entire area is contained within the southeast glacial plains.
In the Grand Canyon, the Toroweap-Hurricane Fault causes a change of surface rock expression in the canyon's west, on the South Rim. The Esplanade Sandstone an erosion resistant member of the Supai Group creates a platform called The Esplanade. The landform is upstream on the Colorado River, South Rim, across from Toroweap Point, and the Toroweap Fault and Aubrey Cliffs are The Esplanade's west perimeter. The Aubrey Cliffs are the west edge of the Coconino Plateau.
The landform is composed of a raised plateau that has eroded to form granitic breakaways and the alluvial plains of the surrounding valleys. Acacia woodlands (dominated by Acacia aneura) and shrublands with spinifex grasslands (Triodia basedowii) dominate the vegetation. The area is located toward the inland extreme of two separate weather systems. The main influence on the climate is the east-west belt of high pressure systems which lies over the southern portions of Australia throughout the year.
The site is located on a natural levee of Bayou Grande Chenière and has twelve mounds, eleven arranged around a central plaza and one to the south, connected to the main group by a constructed landform. The site was connected by a manmade causeway to Bayou Grande Chenière. The elliptical plaza measures on its north-south axis by east-west. Mound 1, the largest, is a conical mound measuring and located on the eastern edge of the plaza.
The Izhora Plateau () is an elevated landform on Ordovician limestone bedrock in the southwestern part of Leningrad Oblast, between the Gulf of Finland in the north and the Luga River in the south. Its northern edge is formed by the erosional cliff known as the Baltic-Ladoga Klint. The highest part of the plateau is the Orekhovaya hill of Duderhof Heights at 176 m, situated in its extreme northeastern part. The plateau is mostly covered by agricultural lands.
Alpine gorge landform is common in the county area, due to intensive erosion by Niulan River and its tributary Shaba River. Only Zhaolu Basin in the east of the county, Longshu Basin in the north, and karst landscapes in the south are relatively flat. The terrain descends from west to the east, although Niulan River coastal region is an exception. The highest place is the top of Wulianfeng Mountain, in the altitude of more than 2,500 meters.
However, responsibility for gorge formation is debated; "they may have formed while the ice sheet retreated north of the region and contributed a large quantity of meltwater, or more likely, they formed while the ice sheet covered the area and the subglacial water was under very high pressure". Whether a particular landform was created by local glacier or continental ice sheet is also still debated. Many pegmatite vein intrusions are visible around the water-eroded bedrock of the gorges.
Ringtail at Piestewa Peak As a landform, Piestewa Peak is relatively young, formed roughly 14 million years ago. However, it is composed of much older rock, primarily schist. Flora in this area is typical of the lower Sonoran Desert and includes almost all varieties of Arizona cactus such as saguaro, barrel, hedgehog, pincushion, jumping cholla and prickly pear. Trees and colorful shrubbery include palo verde, mesquite, ironwood trees, creosote (dominate), ocotillo, brittle bush, desert lavender and giant sage shrubs.
View from Põrguaugu mägi towards Pargimägi The Sinimäed hills are gently sloping mounds rather than mountains. Nevertheless, the hills are a dominant landform in the area - the height of the surrounding limestone plateau is on average 30 m above sea level, while the hills are up to 50 m higher. Pargimägi and Põrguaugu mägi are the two higher hills - 85 and 83 m, respectively, while Tornimägi is somewhat lower, 70 m. The ridge is about 3 km long.
Landsat image of the Fraser Lowland, which stretches from Chilliwack in the northeast to the Strait of Georgia in the southwest. Sediment deposited by the Fraser River is clearly visible. The Fraser Lowland is a landform and physiographic region of the Pacific Northwest, in the Canadian province of British Columbia and the U.S. state of Washington. It includes much of the Lower Mainland region of British Columbia and a portion of Whatcom County, south of the Canada–US border.
Sulphur Mountain is a mountain in Banff National Park in the Canadian Rocky Mountains overlooking the town of Banff, Alberta, Canada. The mountain was named in 1916 for the hot springs on its lower slopes. George Dawson had referred to this landform as Terrace Mountain on his 1886 map of the area. Sanson's Peak was named in 1948 for Norman Bethune Sanson who diligently attended the observatory recording equipment atop Sulphur Mountain for nearly 30 years.
In practice, mountains in Scotland are frequently referred to as "hills" no matter what their height, as reflected in names such as the Cuillin Hills and the Torridon Hills. In Wales, the distinction is more a term of land use and appearance and has nothing to do with height. For a while, the US defined a mountain as being 1,000 feet (304.8 m) or more tall. Any similar landform lower than this height was considered a hill.
The area was in the general vicinity of Nauo tribal land. The town takes its name from the explorer John Charles Darke, who was injured in a spear attack by Aborigines in the vicinity of the peak on 24 October 1844. He died the next day and was buried at the foot of the large peak. Governor Grey expressed a wish that some landform in the region of the grave should be named to honour him.
The Oak Ridges Moraine is an ecologically important geological landform in the Mixedwood Plains of south-central Ontario, Canada. The moraine covers a geographic area of between Caledon and Rice Lake, near Peterborough. One of the most significant landforms in southern Ontario, the moraine gets its name from the rolling hills and river valleys extending from the Niagara Escarpment east to Rice Lake. It was formed 12,000 years ago by advancing and retreating glaciers (see geological origins, below).
Taylor formally defined the landform as the Oak Ridges Moraine in 1913. He described its extent to be from King and Maple in the west to the Trent River in the east. He also proposed that its origin was overlapping, interlobate glaciation retreat, between the Lake Ontario Lobe and the older Lake Simcoe Lobe. This has become the accepted explanation for the moraine's development, though research in the 1970s suggested the moraine may not be interlobate.
Mount Taimu is a mountain and a scenic resort in Fuding. It offers a grand view of mountain and sea, and is famous for its natural scenery including granite caves, odd-shaped stones, steep cliffs, clear streams, cascading waterfalls, and cultural attractions such as ancient temples and cliff Inscriptions. The Danxia landform in Taining was listed by the UNESCO as one of the World Heritage Sites in 2010. It is a unique type of petrographic geomorphology found in China.
Cross Seamount, a landform arising from the ocean floor, is one of the more distant lesser seamounts surrounding the island of Hawaii. The NOAA has taken advantage of Cross Seamount’s position, and planted several weather buoys on the seamount. Very little is known about Cross Seamount's geology, as all of its studies as of March 2009 were of its ecology; however, it was mapped in 1996 by a four-year effort to map all of Hawaii's seafloor in detail.
The Upland South is defined by landform, history, and culture, and does not correspond well to state lines. This map shows the approximate region known as the Upland South. The terms Upland South and Upper South refer to the northern section of the Southern United States, in contrast to the Lower South or Deep South. It typically consists of North Carolina, Tennessee, Arkansas, and eastern Oklahoma, sometimes also Missouri, Virginia, West Virginia, Kentucky, and southern Illinois.
It preserves examples of mature plantings, garden layout, stone walls, bush houses, rotundas and other park structures which reflect changes in ideas and usage over time. The place is important because of its aesthetic significance. Queens Park has aesthetic significance as a major landmark in the city of Ipswich. Its natural landform of gentle slopes and elevated position contribute to the visual character of the town and important vistas can be obtained to and from the park.
Table Mountain is a mountainous landscape feature in Tuolumne County, California near the town of Jamestown. Table Mountain is an inverted valley, an elevated landform which follows the former contours of a river valley above level of the surrounding topography, rather than below it. It was created by lava flows which filled an ancient river bed. The resulting igneous rock resisted erosion better than the materials around it, leaving behind a sinuous rock formation elevated above the surrounding landscape.
Itai Sara, an amba in Degua Tembien An amba hillfort before its destruction in April 1868 after the Battle of Magdala An Amba ( āmbā, imbā) is a characteristic landform in Ethiopia. It is a steep-sided, flat-topped mountain, often the site of villages, wells, and their surrounding farmland. Such settlements were frequently located on these amba plateaus because they were very defensible and often virtually inaccessible from the ground. The original term in Amharic indicates a mountain fortress.
Set on the Kingston coastal plain and bounded by hills, it comprises a large group of buildings from the convict era, some of which have been modified during the Pitcairn period (from 1856 to the present), substantial ruins and standing structures, archaeological remains, landform and landscape elements. KAVHA's aesthetic qualities have been recognised since the earliest days of the first settlement. It is outstanding for its picturesque setting, historic associations, part ruinous configuration and subsequent lack of development.
Geographically and geologically the land around Feuchtwangen comprises the eastern part of the Swabian-Franconian Escarpment Land (Schichtstufenland), also sometimes called the gypsum-keuper landscape. Characteristic of this landform is the quick change from deep hollows to mostly wooded mountain ranges, which were formed as the result of keuper strata not being well able to withstand erosion. This also meant that streams in the region could carve broad valleys. The city of Feuchtwangen lies in the Sulzach valley.
Xanthic ferralsols of the Khorat and Udon series, characterized by a pale yellow to brown color, developed in midlands in processes still under investigation; as are those forming lowland soils resembling European brown soils.Lofjle, E.; Kubiniok, J. Landform development and bioturbation on the Khorat plateau, Northeast Thailand, Nat.Hist.Bull.Siam Soc. (56), 1996 In Australia vast areas formerly covered in rainforest have become so dry that oxisols have formed a hard ironstone cover upon which only skeletal soils can form.
A seamount is a large geologic landform that rises from the ocean floor but that does not reach to the water's surface (sea level), and thus is not an island, islet or cliff-rock. Seamounts are typically formed from extinct volcanoes that rise abruptly and are usually found rising from the seafloor to in height. They are defined by oceanographers as independent features that rise to at least above the seafloor, characteristically of conical form.IHO, 2008.
By the end of the 18th century the Wirral side of the Mersey had five ferry houses, at Seacombe, Woodside, the Rock, New Ferry and Eastham. Other communications were also improving. Turnpike roads linking Chester with Eastham, Woodside, and Neston were built after 1787. In 1793, work began on the Ellesmere Canal, connecting the Mersey with Chester and Shropshire through the fluvioglacial landform known as the Backford gap, and the town of Ellesmere Port began to develop.
It includes a cycle track which provides traffic-free cycling and has been described as "one of the finest stretches of the whole National Cycle Network". Another feature is a wave-shaped, grass-covered landform, created from pulverised fuel ash, a form of "land art". Another part of the project is the Burry Port Marina which provides berthing for 250 craft in three harbours. The Discovery Centre on the waterfront provides information on the park and its facilities.
Distribution of Na-Dene languages shown in red The vastness and variety of Canada's climates, ecology, vegetation, fauna, and landform separations have defined ancient peoples implicitly into cultural or linguistic divisions. Canada is surrounded north, east, and west with coastline and since the last ice age, Canada has consisted of distinct forest regions. Language contributes to the identity of a people by influencing social life ways and spiritual practices. Aboriginal religions developed from anthropomorphism and animism philosophies.
The grey mangroves are uniformly of the type Avicennia marina var. resinifera and cover most of the pre-settlement area, but the surrounding samphire salt flats have been greatly reduced in size by changes in the landform with Tecticornia flabelliformis now listed as threatened in the area. The inlet's deeper sections are dominated by strap or tape weed (Posidonia spp.). Eelgrass (Zostera muelleri) and garweed (Heterozostera tasmanica) dominate the shallows, often being exposed on mudflats at low tide.
Radar images captured by the Cassini spacecraft as it flew by Titan in October 2005 show sand dunes at Titan's equator much like those in deserts of Earth. One erg was observed to be more than long. Dunes are a dominant landform on Titan. Approximately 15-20% of the surface is covered by ergs with an estimated total area of 12–18 million km2 making it the largest dune field coverage in the solar system identified to date.
The Hill of Muchalls is a coastal mountainous landform situated approximately 1.4 kilometres west of the Bridge of Muchalls in Aberdeenshire, Scotland within the Mounth Range of the Grampian Mountains.United Kingdom Ordnance Survey Map Landranger 45, Stonehaven and Banchory, 1:50,000 scale The peak elevation of this mountain is 120 metres above mean sea level. From Megray Hill there are expansive views to the North Sea facing east. The summit affords scenic vies of the historic harbour of Stonehaven.
A syrt is a kind of an elevated landform in Russia and Central Asia. The word means "highland", "ridge" or "backbone" in Turkic languages (sırt) and is present in Turkic toponymy in the mentioned areas: in Tien Shan, Pamirs, South Urals, such as Obshchiy Syrt by Urals, Uzun-Syrt ("Long back") plateau by Koktebel in Crimea. It is a denudational upland or elevated flatland, a kind of dissected plateau. Syrts may be separated from each other by higher ridges.
The Lüneburg Heath seen from the Wilseder Berg in northern Germany. The Lüneburg Heath consists of pushed moraines made from Neogene sand deposits. These form nutrient-poor soils and are generally shrublands covered in heaths. A push moraine or pushed moraine is in geomorphology a moraine (a landform formed by glacial processes) that forms when the terminus advance of a lowland glacier pushes unstratified glacial sediment into a pile or linear ridge in front of it.
On September 24, 1631, Captain Luke Foxe named the landform "Cape Dorset" to honour his benefactor, Lord Chamberlain, Edward Sackville, 4th Earl of Dorset. Kingnait Hill, at high, is located on the island's north-west side. The shorter Eegatuak Hill is located north of the cape, on its eastern side, rising above sea level, and exhibiting a distinctive bowl-shape surmounted by a cairn. Mallik Island, directly to the north, is joined to Dorset Island by sand and boulders.
Wushao Mountain, Wushao Ling Mountain or Wushaoling () is a landform in Gansu Province, China, with significant desert elements on its northern slope. The mountain has been a barrier to transportation since ancient times, when the Northern Silk Road found a passage across its terrain.Silk Road, North China, C.Michael Hogan, the Megalithic Portal, ed. A. Burnham The western slope of Wushao Ling combined with adjoining slopes of Lanshan Mountain comprises over 30 percent of the desert area of China.
The prefecture level city of Sanming has a total area of and 82% of this extension is composed of mountainous areas, 8.3% of arable land and 9.7% of water or other type of terrain. Sanming is well known by its beautiful nature landscape with different landforms, including unique Danxia Landform and abundant Karst topography. The most famous spots include global geopark Taining Golden Lake in Taining County, Yuhua Cave in Jiangle County and Goose Cave in Ninghua County.
Cockatoo Island Industrial Conservation Area is about in Sydney Harbour, between Birchgrove Point and Woolwich Point, comprising the whole of the Island to low water. Cockatoo Island contains a wide variety of extant buildings and structures which contribute to the cultural landscape. The vistas to and from the island play an important role in the character of the setting. The island's present landform has been developed through quarrying and landfill with natural elements limited in extent and profile.
Hurley Butte is an elevated landform in the South Dakota Badlands that is the location of a Formerly Used Defense Site adjacent to the Pine Ridge Reservation and a few miles from Interior, South Dakota. The Strategic Air Command used Hurley Butte for the Interior Radar Bomb Scoring Site prior to establishing the Belle Fourche Strategic Training Range in the Devil's Tower/Black Hills area of Ellsworth Air Force Base. The base of the site remains visible at .
Makhtesh Ramon (; lit. Ramon Crater/Makhtesh ; ) is a geological feature of Israel's Negev desert. Located at the peak of Mount Negev, some 85 km south of the city of Beersheba, the landform is not an impact crater from a meteor nor a volcanic crater formed by a volcanic eruption, but rather is the world's largest "erosion cirque" (steephead valley or box canyons). The formation is 40 km long, 2–10 km wide and 500 meters deep, and is shaped like an elongated heart.
There are at least 2340 named lakes and reservoirs in Arkansas. The following list contains lists of lakes and reservoirs in Arkansas by county. A lake is a terrain feature (or physical feature), a body of liquid on the surface of a world that is localized to the bottom of basin (another type of landform or terrain feature; that is not global). Another definition is a body of fresh or salt water of considerable size that is surrounded by land.
In Siberia there are the Kinenin Maar and the maar of Lake Dal'ny among the volcanoes of the Kamchatka Peninsula. In Japan there are maars in the Kirishima-Yaku Volcanic Field in the Kirishima-Yaku National Park on Kyushu (Kagamiike Pond) as well as many on the volcanic island of Miyake-jima, Izu Islands (Furumio, Mi'ike, Mizutamari, Shinmio). Koranga maar and Numundo Maar are in Papua-New Guinea. Kawah Masemo maar is a landform on Mount Sempu volcano in Indonesia.
The BSG can trace its beginnings back to a meeting in Sheffield in 1958 where British geomorphologists gathered together to organise a Landform Survey of Britain. By 1959 this group appears to have been referring to itself as the British Universities Geomorphological Research Group. This short-lived group agreed, at its second annual meeting, to disband itself and voted unanimously (all 19 of them) to constitute the British Geomorphological Research Group (BGRG). The first BGRG AGM was held on 1 October 1960.
Slip-off slope (right) and left The depositional slip-off slope is on the left and a small river cliff on the right. River Ashes Hollow, UK. Schematic cross section of a meandering river channel showing slip-off slope formation A slip- off slope is a depositional landform that occurs on the inside convex bank of a meandering river. The term can refer to two different features: one in a freely meandering river with a floodplain and the other in an entrenched river.
Earth Science Handbook A mushroom rock, rock pedestal, or gour is a typical mushroom-shaped landform that is formed by the action of wind erosion. At an average height of from the base, the material-carrying capacity of the wind is at its maximum, so abrasion (erosion by wind in which transported materials hit an exposed rock surface and polish it or scratch it) is also maximized. In some cases, harder rocks are arranged horizontally over a softer rock, resulting in such erosion.
Early soil surveys were made to help farmers locate soils responsive to different management practices and to help them decide what crops and management practices were most suitable for the particular kinds of soil on their farms. Many of the early workers were geologists because only geologists were skilled in the necessary field methods and in scientific correlation appropriate to the study of soils. They conceived soils as mainly the weathering products of geologic formations, defined by landform and lithologic composition.
Quaternary Science Reviews 21 (2002), p. 1935 - 2017 After the first stage of aggradation and sediment transport, the Kobuk began a new phase of erosion and landform development. The river exhausted its supply of easily erodible sediment upstream, thus decreasing its sediment load and increasing its load carrying capacity downstream. With more capacity downstream, the river began to incise into the alluvial fan it previously created, moving sediment stored for a long time on its original floodplains to newer floodplains even further downstream.
Winton lies on the north bank of the Western River, a braided river that often runs dry, made of many small channels, a landform that gives this region, the Channel Country, its name. The Western is joined from the north by Jessamine Creek and Mill's Creek, both braided streams. Mistake Creek, likewise a braided stream, empties into the Western from the south. The Western itself flows westwards, eventually emptying into the Diamantina River at one of only three major confluences on that river.
Today, theory and application of landscape ecology continues to develop through a need for innovative applications in a changing landscape and environment. Landscape ecology relies on advanced technologies such as remote sensing, GIS, and models. There has been associated development of powerful quantitative methods to examine the interactions of patterns and processes. An example would be determining the amount of carbon present in the soil based on landform over a landscape, derived from GIS maps, vegetation types, and rainfall data for a region.
In the 16th-17th centuries, big estates, known locally as mas, were founded by rich landlords from Arles. At the end of the 18th century, they had the Rhône diked to protect the town and their properties from flooding. In 1858, the building of the digue à la mer (dyke to the sea) achieved temporary protection of the delta from erosion, but it is a changing landform, always affected by waters and weather. The north of the Camargue is agricultural land.
The largest craters with diameters over 60 km can have central domes, which are thought to result from central tectonic uplift after an impact; examples include Doh and Hár craters. A small number of very large—more than 100 km in diameter—and bright impact craters show anomalous dome geometry. These are unusually shallow and may be a transitional landform to the multi-ring structures, as with the Lofn impact feature. Callisto's craters are generally shallower than those on the Moon.
Cape San Pablo is a landform located in the Argentine Sea that belongs to the South Atlantic Ocean and is located in the east part of Tierra del Fuego island, the southernmost region of South America. It belongs to the Río Grande department, in the province of Tierra del Fuego, Antarctica and South Atlantic Islands, located in southern Patagonia. It is located at coordinates: 54 ° 16'57.98 "S 66 ° 41'30.99" W, about 50 km south-east of the city of Rio Grande.
Around 80 million years ago (Ma) cretaceous red sandstone and conglomerate was laid down by sedimentation from the lakes and streams. After another 15 million years, tectonic plate movements created many faults. About 23 Ma, movement of the Himalayan range disturbed the land around the Danxia landform in the Guangdong Province of China uplifting and completely changing the topography of the area. Over millions of years the steep cliffs that can be seen today, exposed by faults, were formed through weathering and erosion.
The Navajo Section is located in northeastern Arizona and northwestern New Mexico. It is named for the Navajo Nation, with about half of the area of the section on the Navajo Reservation. The section is characterized by broad rolling plains on easily eroded and carved rocks, with cuestas (ridges) and tablelands capped by gently dipping resistant sandstone beds. One of the most prominent landform features of the Navajo Section is Shiprock, a monadnock formation near the town of Shiprock, New Mexico.
For example, trees can reduce landslide potential where their roots penetrate to underlying rock, plants and their litter inhibit soil erosion, biochemicals produced by plants accelerate the chemical weathering of bedrock and regolith, and marine animals cause the bioerosion of coral. The study of the interactions between marine biota and coastal landform processes is called coastal biogeomorphology. Phytogeomorphology is an aspect of biogeomorphology that deals with the narrower subject of how terrain affects plant growth.Howard, J.A., Mitchell, C.W., 1985. Phytogeomorphology. Wiley.
The erosion of sea breeze, sunshine and rainwater for a long time cause weathering of rocks, which is called granite landform. A large number of Taiwan Acacia trees are planted here, yellow flowers blossom in spring, hence the name Yellow Flower Mountain. The park is rich in natural resources and cultural landscape, the forest coverage is over 90%. There are over 1440 tropical and subtropical plants in 102 families, including Podocarpus Nagi, which is called living fossil, fine-leaved grapes, and boxwood plants.
The Teifi and its tributaries are underlain by ancient Ordovician and Silurian mudstones which have been extensively glaciated during the ice ages. The resultant landform is one of gently rolling hills supporting a range of agriculture in which dairy and sheep farming dominate. Ceredigion had the reputation of supplying London with its milk in the 19th century. The landscapes of the Teifi valley are very attractive and the Teifi is considered by many to be one of the most beautiful rivers in Wales.
Mount Francis is a glaciated mountain summit located in the Chugach Mountains, in the U.S. state of Alaska. This landform is situated southeast of Valdez, southwest of Hogback Ridge, and northwest of Meteorite Mountain. This feature was named in 1898 by Captain William R. Abercrombie who led an 1898 expedition seeking a route from coastal Alaska to the Klondike. Precipitation runoff and meltwater from the mountain's glaciers drains into tributaries of the Lowe River, which in turn empties to Prince William Sound.
Map of Scotland showing the historic district of Clydesdale Clydesdale (pronounced ; in Scottish Gaelic, ) is an archaic name for Lanarkshire, a county in Scotland. From 1975 to 1996 it was also the name given to one of the nineteen districts of the Strathclyde region.Clydesdale, Undiscovered Scotland They take their names from strath, dale (place name element) (see dale as a landform) and the river Clyde. The district was formed by the Local Government (Scotland) Act 1973 and was roughly conterminous to Lanarkshire.
Oak Ridge is the landform of the Gettysburg Battlefield where the Eternal Light Peace Memorial was dedicated by President Franklin D. Roosevelt during the 1938 Gettysburg reunion. After the July 1, 1863 Battle of Oak Ridge, Whitworth rifled cannon fired from the Confederate position on Oak Hill onto Culp's Hill and Cemetery Hill. The ridge has numerous Battle of Gettysburg monuments and the 1895 Oak Ridge Observation Tower. In the 1920s, the Gettysburg Airport was established in the west slope of the ridge.
Hogback Ridge is a glaciated mountain ridge located in the Chugach Mountains, in the U.S. state of Alaska. This landform is situated east of Valdez, west of Thompson Pass, and the Richardson Highway traverses the southern base of the mountain. This feature takes its name from the Hogback Glacier on its northern slopes, and in turn the glacier was named in 1898 by Captain William R. Abercrombie. Abercrombie led an 1898 expedition seeking a route from coastal Alaska to the Klondike.
Some maps show West Cornwall as covering a smaller area, ending at a line between Hayle and Helston, making West Cornwall the distinct landform at the very South-Western tip of Cornwall. News outlets often use West Cornwall without any obvious correlation to either way of defining the area, but simply to refer to anywhere west of Truro. West Cornwall Hospital is located in Penzance, West Cornwall. Penzance, St Ives, Hayle, Helston and Land's End are notable places located in West Cornwall.
Hoste Peninsula Hardy (sometimes called "Pen Hardy") is a peninsula at one of the most southerly extremes of South America. It is the southern landform which extends into the Drake Passage to make the Bahia Nassau. It is part of a large island called Hoste, next to Isla Navarino and Isla Grande de Tierra del Fuego. It is located in the Commune of Cabo de Hornos, belonging to the Antártica Chilena Province of the Magallanes y Antártica Chilena Region, Chile.
The subject site was characterised by areas of high, moderate and low archaeological sensitivity. Areas of high archaeological sensitivity were identified in association with Woodhouse Creek and its tributaries. Areas of moderate archaeological sensitivity were identified across large portions of the western portion of the study area, including the two ridge crest landforms and the associated gently sloping landform associated with the Beulah homestead. The 2013 artefact report categoriesd the property into areas of low, moderate and high archaeological potential.
Between the Holyoke Range and the Pocumtuck Ridge, a stretch of , the Metacomet Ridge exists only as a series of mostly nondescript rises set among flat plains of sedimentary bedrock. Mount Warner, , in Hadley, Massachusetts, the only significant peak in the area, is a geologically unrelated metamorphic rock landform that extends west into the sedimentary strata.Zen, E-an, Goldsmith, Richard, Ratcliffe, N.M., Robinson, Peter, Stanley, R.S., Hatch, N.L., Shride, A.F., Weed, E.G.A., and Wones, D.R. (1983). Bedrock Geologic Map of Massachusetts.
A local developerTuart Properties is developing a parcel called Chittering Retreat into 45 rural residential lots. This development is mainly on cleared land although many mature trees exist on the gently undulating landform. Natural fresh water springs are not very common in the area however Chittering Retreat has a substantial fresh water spring. Developments such as Chittering Retreat help provide important infrastructure to the area such as the upgrading of Morley Road, Lower Chittering and undergrounding of some power services.
In low sun-angle photography additional scarps and splays can be observed. The erosion/sedimentation patterns and the path of drainages such as Canyon Creek may have been influenced by movement along the fault, and topographic ridges are offset. Finally ductile folding, vegetation and landform variations have also been recognized on the Meers fault. In some rock formations faulting has mainly led to warping, instead of brittle displacements and in several sites evidence of faulting appears to be concealed by floodplain sedimentation.
A rootless cone at Myvatn Lake, Iceland. A rootless cone, also formerly called a pseudocrater, is a volcanic landform which resembles a true volcanic crater, but differs in that it is not an actual vent from which lava has erupted. They are characterised by the absence of any magma conduit which connects below the surface of a planet. Rootless cones are formed by steam explosions as flowing hot lava crosses over a wet surface, such as a swamp, a lake, or a pond.
Finally bioconstruction refers to the physical construction of biological structures on ocean substrate. Marine biota interact with landform processes by building structures, accumulating carbonate sediments, accelerating erosion by boring or bioturbation, and marine plant life contribute to shoreline stability, especially in marsh and wetland environments.Bernal P., and P.M. Holligan (1992). Marine and Coastal Systems. In J.C.I. Dooge, Gordan Goodman, J.W.M. Riviere, Julia Marton- Lefevre, and Timothy O’Riordan (Eds.), An Agenda of Science for Environment and Development into the 21st Century (pp. 157-171).
Rootless Volcanic Cones in Iceland and on Mars, in The Geology of Mars: Evidence from Earth-Based Analogs, Chapman, M., Ed; Cambridge University Press: Cambridge UK, pp. 151–177. Also, phreatomagmatism produce tuff rings or tuff cones on Earth and existence of similar landforms on Mars is expected too. Their existence was suggested from Nepenthes/Amenthes region. Finally, when a volcano erupts under an ice sheet, it can form a distinct, mesa-like landform called a tuya or table mountain.
It is at edge of the area that defines the basin that Glasgow has developed within. The underlay is composed mainly of sedimentary rocks and freestone from the Strathclyde and Clackmannan groups of early to mid Carboniferous age (354 to 316 million years). The relatively soft and easily eroded rocks have resulted in the landform in the area being mostly flat with gentle undulations. The area of Giffnock is typically around to above sea level, with the highest point in the area reaching .
Looking northeast across Castle Haven to Bowdun Head Bowdun Head is a headland landform on the North Sea coast approximately one kilometre south of Stonehaven, Scotland.(Ordnance Survey, 2004) Slightly to the north is another headland, Downie Point. Somewhat to the south along the coast is Dunnottar Castle on the far side of the bay of Castle Haven. Other historic structures in the general vicinity include the Stonehaven Tolbooth, Fetteresso Castle, the Chapel of St. Mary and St. Nathalan and Muchalls Castle.
Location of the Kaiparowits Plateau within Utah The Kaiparowits Plateau is a large, elevated landform located in southern Utah, in the southwestern United States. Along with the Grand Staircase and the Canyons of the Escalante, it makes up a significant portion of the Grand Staircase-Escalante National Monument. Its extension to the southeast, Fiftymile Mountain, runs nearly to the Colorado River and Lake Powell, and is a prominent part of the northern skyline from the Glen Canyon National Recreation Area.
Megray Hill is a low-lying coastal mountainous landform in Aberdeenshire, Scotland within the Mounth Range of the Grampian Mountains.United Kingdom Ordnance Survey Map Landranger 45, Stonehaven and Banchory, 1:50,000 scale, 2004 The peak elevation of this mountain is 120 metres above mean sea level. This hill has been posited as a likely location for the noted Battle of Mons Graupius between the Romans and the indigenous Caledonians.Archibald Watt, Highways and Byways Round Stonehaven, Gourdas House Publishers, Aberdeen (1984)C.
Cultural heritage includes both Aboriginal and non-Aboriginal history and associated activities and works. It comprises important sites, structures and relics that may have aesthetic, historic, scientific and social significance to present and future generations. The geology, landform, climate and plant and animal communities of the area, plus location, have determined use by humans. Main forms of past disturbance include clearing (especially in southern portions of Ingalba and Big Bush Nature Reserves), sheep grazing, and logging for fences and firewood.
Bowland is dominated by a central upland landform of deeply incised gritstone fells covered with tracts of heather-covered peat moorland and blanket bog. The lower slopes of the fells are dotted with stone-built farms and small villages and are criss-crossed by drystone walls enclosing reclaimed moorland pasture. Steep-sided wooded valleys link the upland and lowland landscapes. In the northeast of the area are extensive coniferous plantations and the eastern limestone areas support high-quality species-rich meadows.
380px Horicon Marsh was created by the Green Bay lobe of the Wisconsin glaciation during the Pleistocene era. The glacier, during its advance created many drumlins (a glacial landform) in the region, many of which have become the islands of Horicon Marsh. The marsh and surrounding Dodge County have the highest concentration of drumlins in the world. During the glacier's retreat, a moraine was created, forming a natural dam holding back the waters from the melting glacier and forming Glacial Lake Horicon.
The Ombla rises at the foot of the Golubov Kamen massif, a landform that straddles the border between Croatia and Bosnia-Herzegovina. The river rises in an cave whose roof has an clearance above the surface of the water. The primary source is located at an elevation of below sea level, and the secondary sources are found at above sea level (a.s.l.). The spring is the largest karst spring in Croatia, and one of the largest ones in the Dinarides.
These landform differ only on the steepness of their backslopes and relative differences in the inclination of their backslopes and frontslopes. These differences depends upon whether the dip of the strata from which they have been eroded are either nearly vertical, moderately dipping, or gently dipping. In general, homoclinal ridges, or strike ridges, are associated with strata that dip between 10° and 30°. The symmetrical ridges that characterize hogbacks develop where the strata dip very steeply at 40° or more.
There are at least 3223 named lakes and reservoirs in Montana. The following list contains lists of lakes and reservoirs in Montana by county. A lake is a terrain feature (or physical feature), a body of liquid on the surface of a world that is localized to the bottom of basin (another type of landform or terrain feature; that is not global). Another definition is a body of fresh or salt water of considerable size that is surrounded by land.
Sandrivier range of the central Waterberg, 15 km south of Vaalwater It lies at the southern edge of the rugged Waterberg Massif, which is a biosphere that contains considerable biodiversity, including numerous large mammals (e.g. Giraffe, White Rhino, Blue Wildebeest). Waterberg is the first region in the northern part of South Africa to be named as a Biosphere Reserve by UNESCO. The extensive rock formation was shaped by hundreds of millions of years of riverine erosion to yield diverse bluff and butte landform.
According to the United States Census Bureau, Butte-Silver Bow has a total area of , of which is land and (0.08%) is water. The city is situated on the U.S. Continental Divide. Every highway exiting Butte (except westbound I-90) crosses the Divide (eastbound I-90 via Homestake Pass; eastbound MT 2 via Pipestone Pass; northbound I-15 via Elk Park Pass and southbound I-15 via Deer Lodge Pass). The city was named for a nearby landform, Big Butte, by the early miners.
To the north of the ridge lies the London Clay, and to the south the clays of the Wealden Group. The chalk is more resistant to weathering than the flanking clays, leading to the ridge's prominence over the surrounding terrain. The Hog's Back gives its name to the geomorphological landform known as a Hogback, which is a long narrow ridge or series of hills with a narrow crest and steep slopes of nearly equal inclination on both flanks.Huggett, JR (2011) Fundamentals of Geomorphology, 3rd ed.
Bridger Valley is a landform of Uinta County, Wyoming where Fort Bridger was established in 1843 to service emigrant traffic. For the next century, the region served as a crossroads for the "California/Oregon Trail, the Mormon Trail, the Pony Express Route, the Transcontinental Railroad, and the Lincoln Highway. Today, the valley is a historic byway, incorporating the small towns of Fort Bridger, Urie, Mountain View, and Lyman". Bridger Valley Historic Byway is an approximately 20 mile loop showcasing some of Wyoming's most treasured historical sites.
Sediments underlying fluvial terrace exposed in cutbanks along the Manú River, Peru In geology, a terrace is a step-like landform. A terrace consists of a flat or gently sloping geomorphic surface, called a tread, that is typically bounded on one side by a steeper ascending slope, which is called a "riser" or "scarp". The tread and the steeper descending slope (riser or scarp) together constitute the terrace. Terraces can also consist of a tread bounded on all sides by a descending riser or scarp.
Hydro-geomorphology is science that deals with occurrences of water with respect to landform. Hydrogeomorphology of a drainage basin is a function of rainfall kinematics, surface topography, drainage basin morphology and runoff etc. All these aspects are regarded as the potential to describe hydrogeomorphic properties of the drainage basin. Because of non-availability of hydrological data, discharge data and sediment load data over a sufficient period of time in ungauged catchments, various investigators have used the drainage basin parameters to study the hydrogeomorphology of the drainage basin.
Cerro do Jarau is a prominent, approximately wide, circular landform rising more than above the plains of the pampas in southern Brazil. The name (meaning Jarau hills) comes from the prominent crests of silicified sandstones, which form a semiring of elevated hills in the northern part of the structure. The origin of this structure has been debated for decades, and varied suggestions of its formation include either endogenous tectonic processes or large meteorite impact. However, no conclusive evidence to support either hypothesis has been presented to date.
Gardiner, S. (updated 2010) Wetland Management Profile – Arid and semi-arid lakes. Queensland Wetlands Program (Queensland Department of Environment and Resource Management). The characteristic landform of an almost flat, shallow, terminal lakebed in an arid and semi-arid zone is commonly called a playa. In dry times, playas consist of cracking clay flats that can be crusted and hardened to varying degrees depending on their substrate and position in the landscape, and sometimes might be covered in a thin layer of soluble salt deposits.
Herøy, northern Norway Strandflat () is a landform typical of the Norwegian coast consisting of a flattish erosion surface on the coast and near-coast seabed. In Norway, strandflats provide room for settlements and agriculture, constituting important cultural landscapes. The shallow and protected waters of strandflats are valued fishing grounds that provide sustenance to traditional fishing settlements. Outside Norway proper, strandflats can be found in other high-latitude areas, such as Antarctica, Alaska, the Canadian Arctic, the Russian Far North, Greenland, Svalbard, Sweden and Scotland.
Hong Kong Island is separated from Kowloon by Victoria Harbour, a natural landform harbour. The Kowloon Peninsula to the south of Boundary Street and the New Territories to the north of Hong Kong Island were added to Colonial Hong Kong in 1860 and 1898, respectively. Further from Victoria Harbour and the coast, the landscape of Hong Kong is fairly hilly to mountainous with steep slopes. The highest point in the territory is Tai Mo Shan, at a height of 958 metres in the New Territories.
The Cirque de Navacelles is large erosional landform, an incised meander, located towards the southern edge of the Massif Central mountain range in France. It is located near Saint-Maurice-Navacelles and Blandas between the Hérault department and the Gard department.Official website: Geography of the cirque The cirque is isolated, with only a few small villages in the surrounding area. However, with the completion of the Millau Viaduct in 2004 and the A75 motorway between Clermont-Ferrand and Pézenas, tourism in the region has increased.
The disposition of the Veiki moraines reflects the last glacier movements before an ice sheet retreats, and their final form is given by the melting of dead-ice and the development and sedimentation of glacial lagoons between dead-ice cored rims during interstadial periods. In the case of the Veiki moraines of Sweden, the interstadial during which the lagoons sedimented is believed to have occurred in the early Weichsel glaciation. Thus, the Veiki moraines of Sweden are a relict landform that has largely survived later glacier action.
Milešovka Hill in the Bohemian Central Uplands A conical hill (also cone or conical mountain) is a landform with a distinctly conical shape. It is usually isolated or rises above other surrounding foothills, and is often, but not always, of volcanic origin. Conical hills or mountains occur in different shapes and are not necessarily geometrically-shaped cones; some are more tower-shaped or have an asymmetric curve on one side. Typically, however, they have a circular base and smooth sides with a gradient of up to 30°.
The Weippe Prairie in 2010. After 11 days of very difficult travel over Lolo Pass, Mullan and his party emerged onto this easily traveled flat landform. With Native Americans either unwilling to talk, purposefully deceitful, or too unfamiliar with wagon travel to offer good advice, Mullan still needed to determine which of the remaining passes known to white explorers would be the best for a planned railroad or wagon road. On May 21, Mullan set out with a small party on horseback, following the Clark Fork.
The Glacial till plains are a till plain landform in Northern Ohio, located near the shore of Lake Erie and created by the retreat of the Wisconsin glaciation. Since glacial till is highly fertile soil, agriculture on the glacial till plains is very productive. The region has gently rolling moraine hills left over from the retreating glaciers, as well as small sandy ridges, which were formed as coastal dunes during periods in which Lake Erie was higher than it is today (14,000-12,000 years ago).Simonson, Bruce.
The Laojun Mountain () is a combination of the three national-level scenic spots in the Jade Dragon Snow Mountain, the Three Rivers Concurrent, and the Cangshan Erhai Lake. It is an important part of the Yulong Snow Mountain Scenic Area. This scenic spot is mainly composed of Laojunshan Jiujiu Longtan, Jinsi Factory Jinshan Yuhu, Dawn Meile Danxia Landform, New Main Natural Alpine Botanical Garden and other areas (attractions), with a total area of 715 square kilometers, which is under planning and development. Ecotourism resort.
The overall landform of the region around Cossack is a low, flat plain with occasional rocky hills and ranges. The vegetation is mainly grass, spinifex and low shrub, with occasional trees (mangroves) along watercourses and in gullies. The mangrove scrub becomes quite dense along the shoreline and at the mouth of the inlet. The main road from Roebourne to Cossack continues past the town of Wickham and the Cape Lambert iron ore port (operated by Pilbara Iron), and terminates at the fishing town of Point Samson.
This mechanism may be used in river engineering to design self-sustainable riffles, given a suitable sediment supply and flow regime. When an in-channel landform is shallow and narrow, instead of shallow and wide, it is called a nozzle. Riffles are biologically very important, because many aquatic species rely on them in one way or another. Many benthic macroinvertebrates are present in riffles, so fish often locate just downstream of a riffle to wait for these small creatures to drift down to them.
A granite outcrop in the Stirling Range National Park Granite outcrops of Western Australia are weathered landforms that occur throughout the state of Western Australia, composed primarily of the rock type granite. All recognised types of this landform can be observed, commonly as bornhardts, but also as inselbergs, castle koppies and Nubbins. Rising abruptly from the surrounding landscape they create a variety of microhabitats for plants, and provide seasonal resources and refuge for a range of animals. These areas thus have rich biodiversity and many endemic species.
Rough map of the Portage Escarpment (black line) in New York, Pennsylvania, and Ohio. The Portage Escarpment is a major landform in the U.S. states of Ohio, Pennsylvania, and New York which marks the boundary between the Till Plains to the north and west and the Appalachian Plateau to the east and south. The escarpment is the defining geological feature of New York's Finger Lakes region. Its proximity to Lake Erie creates a narrow but easily traveled route between upstate New York and the Midwest.
View of the Genesee River and gorge The bedrock exposed in the gorge is Devonian in age, mostly shales, with some layers of limestone and sandstone. The rock was laid down in an ancient inland sea, and it holds many marine fossils. The landform of the section of the Genesee River valley represented by the park is geologically very young, caused by a diversion of the river from the old valley by the last continental glacier, which forced the river to cut a new section of valley.
East Cemetery Hill is a Gettysburg Battlefield landform used for the battle of East Cemetery Hill during the 1863 Battle of Gettysburg, Second Day. Located on the east of Gettysburg's Baltimore Street and the Baltimore Pike which meet on the hill, the hill is a northeast spur, and the east slope, of Cemetery Hill. The hill has numerous postbellum battlefield monuments, as well as artillery lunettes remaining from the Battle of Gettysburg. Slocum Avenue is on the south slope, while Wainwright Avenue is near the east base.
Paleocollapse is a rock structure resembling the karst landform, but is formed essentially by the dissolution of underlying sedimentary rock. It has also been called paleo-karst collapse.A CASE HISTORY OF A LARGE KARST INVESTIGATION: Lynn Yuhr, Richard C. Benson, Ronald D. Kaufmann, Daniel Casto and John JenningsPaleokarst in Iowa by Robert M. McKay This has the effect of collapsing the formerly intact rock above, forming extensive fractures, debris pipes, and open caverns. Normally, the process was started and completed in the geologic past.
Mt. Susitna is a roche moutonnée, a landform created when a glacier flows over a resistant, topographically high, bedrock body, creating a smooth-sided and teardrop shaped feature aligned with the direction of ice flow. The Anchorage bowl topography has been influenced by 5-7 glaciations. Over several thousand years, thick ice sheets from the Talkeetna, Chugach and Alaska Ranges flowed down Cook Inlet. The five well documented glaciations from oldest to most recent were the Mt Susitna, Caribou Hills, Eklutna, Knik and Naptowne.
These are identifiable by flat grassy areas which contradict the natural sloping landform immediately surrounding the site and are located within the approximate location of the buildings shown on an 1837 plan of the site. Part of the driveway traversing along the front of the site has evidence of a variety of small china, earthenware and glass shards, some likely to date from the early to mid nineteenth century. Occupants of the property have noted that these small pieces continue to rise to the surface over time.
Some researchers have interpreted these landforms as originating in the erosion of sulfate-bearing layers present within units of Ganges Mensa. Ganges Mensa is in the Coprates quadrangle of Mars, centered near the equator in the western hemisphere at 7.2° S and 48.8° W. The landform was named after a classical albedo feature that was published in a 1930 manuscript called La Planéte Mars authored by the French-Greek astronomer Eugène Michel Antoniadi. The International Astronomical Union officially approved Ganges Mensa's name in 2006.
Detail of the large limestone pavement in the Yorkshire Dales between Ingleborough and Pen-y-ghent. Limestone pavement above Malham Cove A limestone pavement is a natural karst landform consisting of a flat, incised surface of exposed limestone that resembles an artificial pavement.Introduction - Limestone Pavement Conservation Retrieved on 2008-06-29 The term is mainly used in the UK and Ireland, where many of these landforms have developed distinctive surface patterning resembling paving blocks. Similar landforms in other parts of the world are known as alvars.
The Las Vegas Valley is a major metropolitan area in the southern part of the U.S. state of Nevada. The state's largest urban agglomeration, the Las Vegas Metropolitan Statistical Area is coextensive since 2003 with Clark County, Nevada. The Valley is largely defined by the Las Vegas Valley landform, a basin area surrounded by mountains to the north, south, east and west of the metropolitan area. The Valley is home to the three largest incorporated cities in Nevada: Las Vegas, Henderson and North Las Vegas.
Cities and communities of the Las Vegas valley The valley is contained in the Las Vegas Valley landform. This includes the cities of Las Vegas, North Las Vegas, and Henderson, and the unincorporated towns of Summerlin South, Paradise, Spring Valley, Sunrise Manor, Enterprise, Winchester, and Whitney. The valley is located within the larger metropolitan area, as the metropolitan area covers all of Clark County including parts that do not fall within the valley. The government of Clark County has an "Urban Planning Area" of Las Vegas.
Currently there 26 World Geoparks in China. These include the Shilin Geopark in China's Yunnan Province, featuring a carbonate peak forest landform, which brings about the formation of various karst landscapes, such as stone teeth, corroded gullies and corroded funnels. The Huangshan Geopark in Anhui Province, famed for its grand and steep mountains, with 72 peaks of over 1,000 meters high. The geopark is picturesque with green and straight pines, jagged rocks of grotesque shapes, wide and imposing cloud sea, as well as many gushing warm springs.
A submergent landform: the drowned river valley (ria) of Georges River in the greater Sydney area, Australia Submergent coastlines are stretches along the coast that have been inundated by the sea by a relative rise in sea levels from either isostacy or eustacy. Submergent coastline are the opposite of emergent coastlines, which have experienced a relative fall in sea levels. Features of a submergent coastline are drowned river valleys or rias and drowned glaciated valleys or fjords. Estuaries are often the drowned mouths of rivers.
Kakadu's flora is among the richest in northern Australia with more than 1700 plant species recorded which is a result of the park's geological, landform and habitat diversity. Kakadu is also considered to be one of the most weed free national parks in the world. Grevillea The distinctly different geographical areas of Kakadu have their own specialised flora. The environment referred to as the "Stone Country" features "resurrection grasses" that are able to cope with extreme heat and long dry spells followed by periods of torrential rain.
The Sonoma Mountain AVA is an American Viticultural Area in Sonoma County, California, United States. It is centered on the Sonoma Mountain landform in the Sonoma Mountains. The appellation includes the town of Glen Ellen, California and is nearly surrounded by the Sonoma Valley AVA. The area is known for the diverse micro-climates that occur on exposed hillsides and shaded drainages, and as such is home to production for a wide range of varieties including Cabernet Sauvignon, Chardonnay, Pinot noir, Sauvignon blanc, Semillon, and Zinfandel.
A nymph (, ; Ancient: , Modern: ) in ancient Greek folklore is a minor female nature deity. Different from Greek goddesses, nymphs are generally regarded as personifications of nature, are typically tied to a specific place or landform, and are usually depicted as beautiful maidens. They were not necessarily immortal, but lived much longer than humans before they died. They are often divided into various broad subgroups, such as the Meliae (ash tree nymphs), the Naiads (freshwater nymphs), the Nereids (sea nymphs), and the Oreads (mountain nymphs).
In Scandinavian folklore, a rå (pl rår), is a spirit who is the keeper or warden of a particular location or landform. The rå is known both in Nordic culture and in the Sami culture, where it is called radie. It was important for humans to cultivate good relationships with them, since they had power over the natural forces and animals under their care, and could cause both good and bad luck for humans who interfered with the places and creatures under their watch.
Lyall Bay is predominantly a residential area, but also contains a part of Wellington's Southern Walkway, and the Southern Headlands Reserve, and Wellington's largest beach. The south-western border has Te Raekaihau Point as the dividing landform to Houghton Bay. The suburb has a bus service and is near to the Kilbirnie shopping centre and the Tirangi Road Airport Retail Park. There is a primary school (Lyall Bay School), a Playcentre, a lawn bowls club, two surf clubs, and a small range of shops.
The Westminster Road boundary of the property is bordered by a large rendered masonry fence which acts as a retaining wall, braced by a number of piers. The fence is capped with a row of face bricks. Centrally positioned in this fence is a wrought iron gate providing access to a series of concrete stair rendered with a red colouring. These stair reach a concrete landing level with the surrounding landform and from here a second series of concrete steps lead to the front door.
Ridge and swale, or in dunal areas dune and swale, is a landform consisting of regular, parallel ridges alternating with marshy depressions. Ridge-and-swale landscapes are most commonly formed by the gradual movement of a beach, for example as a result of gradually fluctuating water levels, or the shifting meanders of a river. In the river context, ridge-and-swale landscapes are commonly formed by scroll bars. They are also found along ocean coasts, for example on the Outer Banks of North Carolina.
Mount Zero-Taravale Sanctuary is a 600 km² nature reserve in north-east Queensland, Australia, 60 km north-west of Townsville. It is owned and managed by the Australian Wildlife Conservancy (AWC). It is located on the boundary of the Wet Tropics bioregion and Einasleigh Uplands bioregion, adjacent to the Wet Tropics World Heritage Area. The property varies in altitude from 350 m in the south-west to 1,050 m in the north-east, and in landform from rugged mountains to a broad alluvial valley.
Layers in the geopark The park is located in the northern foothills of the Qilian Mountains, in the counties of Linze and Sunan, which are under the administration of the prefecture-level city of Zhangye, Gansu province. The main areas of Danxia landform are in Kangle and Baiyin townships. The core area of the park, Linze Danxia Scenic Area, is located west of downtown Zhangye and south of the seat of Linze County. It is the most developed and most visited part of the park.
The highly serrated, jagged appearance of the Rockies and other tall mountain ranges may be attributed to their youth. By contrast the Kiamichi Mountains, which are much older—and now shorter—feature the highly eroded characteristics common among much older mountains. Geologists generally define a mountain as a natural landform topping at least 1,000 feet in elevation. Numerous of the mountains, particularly those along the Kiamichi River's lower reaches, measure between 700 and 900 feet in elevation. Although called “mountains” they are, more formally, hills.
Kempstone Hill is a landform in Aberdeenshire, Scotland within the Mounth Range of the Grampian Mountains.United Kingdom Ordnance Survey Map Landranger 45, Stonehaven and Banchory, 1:50,000 scale, 2004 The peak elevation of this mountain is 132 metres above mean sea level. This hill has been posited by Gabriel Jacques Surenne, Archibald Watt and C.Michael Hogan as the location for the noted Battle of Mons Graupius between the Romans and the indigenous Caledonians.Archibald Watt, Highways and Byways Round Stonehaven, Gourdas House Publishers, Aberdeen (1984)C.
Jamaica and the other islands of the Antilles evolved from an arc of ancient volcanoes that rose from the sea millions of years ago. During periods of submersion, thick layers of limestone were laid down over the old igneous and metamorphic rock. In many places, the limestone is thousands of feet thick. The country can be divided into three landform regions: the central mountain chain formed by igneous and metamorphic rocks; the karst limestone hills in the Cockpit area; the low- lying coastal plains and interior valleys.
Its name is derived from a soak known as Pine Hill Soak which is located near the conservation park's southern boundary. The conservation park was proclaimed on 17 September 1987. As of 2012, access to the conservation park for the purpose of petroleum exploration under the Petroleum and Geothermal Energy Act 2000 was not permitted. In 1992, the conservation park was described as follows. The land contains a field of “relict sand dunes and associated swale depressions.” The former landform supported a brown stringybark “open forest” with desert banksia being the “dominant shrub species” while the latter landform supported a “woodland of river red gum … and South Australian blue gum … with an open understorey of grasses, sedges and herbs.” The conservation park contains native pine which is “an occurrence close to the southern limit of this species' distribution” and which was considered as “suitable habitat” for the red-tailed black cockatoo - a species considered to be “threatened” at the time and which is “dependant on brown stringybark for food and nesting resources.” Further, visitation to the conservation park was described as “low.” The conservation park is classified as an IUCN Category III protected area.
The Trafalgar Moraine is a geological landform straddling Oakville and Milton in Ontario, Canada. A small portion of the moraine extends into Burlington at Milton's southern border. It is a subtler topological feature than the better- known Oak Ridges Moraine, primarily because it was formed as an end moraine at the terminus of a glacial ice sheet, instead of between two retreating ice lobes (known as interlobate). The ice sheet pushed material to form the ridge, which is composed of Halton Till sediment, rich in silt and clay.
Geomorphology is the scientific study of the origin and evolution of topographic and bathymetric features created by physical or chemical processes operating at or near Earth's surface. Geomorphologists seek to understand why landscapes look the way they do, to understand landform history and dynamics and to predict changes through a combination of field observations, physical experiments and numerical modeling. Geomorphology is practiced within physical geography, geology, geodesy, engineering geology, archaeology and geotechnical engineering. This broad base of interests contributes to many research styles and interests within the field.
Typical Canadian Shield landform Pinawa is located beside the Winnipeg River, which offers access to boating, kayaking, canoeing, and other water recreational activities. Other attractions include an 18-hole golf course, beach, outdoor pool, tennis courts, a curling rink, a hockey arena and many kilometres of cross-country ski trails. The Trans-Canada Trail runs through the town of Pinawa along the Riverside. Pinawa also hosts the Eastern Manitoba Concert Association or EMCA's concerts, held in the community centre's gymnasium in the secondary school building once a month between October and April.
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 width of this landform at its northern and southern ends is a little more than . However, its midsection is narrowed by the eastern corner of Moulin Huet Bay which is known as Petit Port; here, the promontory's width is only about . The point is approachable by the main road from Sausmarez Manor, leading to La Moye Lane which ends on the cliff tops. Mouilliere Rock, a dangerous rock for navigating ships is located offshore as are Les Grunes de Jerbourg, "very dangerous cluster of rocks a full half mile from the shore".
Around the residences are more formal grounds with banksia, acacia, Norfolk Island pines and New Zealand Christmas Bush. The present land formation coincides closely with the original site works plans. This landform is a low headland above extensive flat rock shelves near sea level and contrasts with the well built lighthouse and quarters to produce a scene of visual appeal. Norah Head consists of a small headland of low eucalypt woodland and banksia heath that is substantially contiguous with more extensive natural vegetation to the west on the edge of Tuggerah Lakes.
Cooke, H. J. (1980) "Landform evolution in the context of climatic change and neo-tectonism in the Middle Kalahari of north- central Botswana" Transactions, Institute of British Geographers 5: pp. 80-99, page 85 Kubu Island and Kukome Island are igneous rock "islands" in the salt flat of Sua pan.McIntyre, Chris (2007) Botswana: Okavango Delta, Chobe, Northern Kalahari: the Bradt Safari Guide (2nd edition) Bradt, Chalfont, St. Peter, England, page 381, Kubu Island lies in the southwestern quadrant of Sua Pan, contains a number of baobab trees, and is protected as a national monument.
The Louisiana Purchase Historic State Park commemorates the initial point from which the lands acquired through the Louisiana Purchase (1803) were subsequently surveyed. The protected area encompasses of forested wetlands, a landform which is regionally in decline due to agricultural development practices that include draining such areas. In the center of the park is a marker erected in 1926 on the survey point by the L'Anguille Chapter of the Daughters of the American Revolution. The site was listed on the National Register of Historic Places (1972) and designated as a National Historic Landmark (1993).
The bluffs support a very specialized ecosystem including vegetation adapted to the steep rocky vertical landform of the gorge sides.C. Michael Hogan and Amy Gregory, Ecology of Komati Gorge, Lumina Technologies, July 22, 2006 In addition there are favourable opportunities for bird habitat, providing more protection from certain predators; for example the threatened southern bald ibis inhabits these cliff habitats. Mammal species include big game animals as well as smaller fauna; for example zebra and giraffe can be found on the bushveld. Eland, Impala and other bovids are numerous.
Samuel Calvin 1882 Samuel Calvin (February 2, 1840 - April 17, 1911) was Iowa's first systematic geologist, helping to make the first bedrock and landform maps of Iowa, as well as leading geological research throughout the state. He was born in Scotland, attended Lenox College (now defunct) in Hopkinton, Iowa, where he later taught. One of his collaborators was Thomas Huston Macbride, the notable Iowa naturalist. Calvin became a University of Iowa professor in 1873 and the Iowa State Geologist in 1892, and led the Iowa Geological Survey from 1892 until his death.
According to its largest version, it includes five municipalities: Aledo, Lorca, Alhama de Murcia, Librilla and Mazarrón and has an area of 1,024.7 km2. If the a smaller version is adopted, the only municipality that doesn't belong to this territory is Mazarrón and has an extension of 706 km2. An important landform of the comarca is Guadalentín river – a stretch of it traverses the territory, hence its name. Part of Sierra Espuña, one of the most important mountain ranges in Region of Murcia, is located in the northwest of Bajo Guadalentín.
An objective of topography is to determine the position of any feature or more generally any point in terms of both a horizontal coordinate system such as latitude, longitude, and altitude. Identifying (naming) features, and recognizing typical landform patterns are also part of the field. A topographic study may be made for a variety of reasons: military planning and geological exploration have been primary motivators to start survey programs, but detailed information about terrain and surface features is essential for the planning and construction of any major civil engineering, public works, or reclamation projects.
Samuel Calvin (1840–1911) was Iowa's first systematic geologist, who helped to make the first bedrock and landform maps of Iowa, as well as lead geological research throughout the state.Calvin obituary, The Journal of Geology, July 1911, pp. 385-391. Calvin Hall at the University of Iowa is named for him. Clair Cameron Patterson (1922–1995) developed the lead-lead dating and calculated an age for the Earth of 4.55 billion years; a figure far more accurate than those that existed at the time and one that has remained unchanged for over 50 years.
Geological Society of America, 1988. Surface of the Earth, showing higher elevations in red. Geomorphology (from Ancient Greek: γῆ, gê, "earth"; μορφή, morphḗ, "form"; and λόγος, lógos, "study") is the scientific study of the origin and evolution of topographic and bathymetric features created by physical, chemical or biological processes operating at or near the Earth's surface. Geomorphologists seek to understand why landscapes look the way they do, to understand landform history and dynamics and to predict changes through a combination of field observations, physical experiments and numerical modeling.
The criticism by Stoddart proved "devastating" sparking a decline in the popularity of climatic geomorphology in the late 20th century. Stoddart criticized climatic geomorphology for applying supposedly "trivial" methodologies in establishing landform differences between morphoclimatic zones, being linked to Davisian geomorphology and by allegedly neglecting the fact that physical laws governing processes are the same across the globe. In addition some conceptions of climatic geomorphology, like that which holds that chemical weathering is more rapid in tropical climates than in cold climates proved to not be straightforwardly true.
The park centers on the Khvalanskyaya ridge, a raised plateau that stretches along the west bank of the Volga River (referred to as the 'Right Bank'). Because the bedrock is primarily chalk and marl, the landform reflects extensive erosion out from the center of the ridge, with undulating and hilly terrain and numerous interconnected ravines and gullies. The varied landforms create many micro- climates and habitats. The highest mountain (Belenkaya, almost entirely of chalk) is 369 meters in altitude, and there are five other mountains over 250 meters in height.
The Rock of Guatape (), or simply La Piedra or El Peñol, is a landmark inselberg also known as The Stone of El Peñol (),Sitio oficial de Guatapé in Colombia. It is located in the town and municipality of Guatapé, Antioquia. The town of El Peñol, which borders Guatapé, has also historically claimed the rock as their own and thus has led to different names for the site. The landform is a granitic rock remnant that has resisted weathering and erosion, likely as result of being less fractured than the surrounding bedrock.
Three kinds of streams are formed by headward erosion: insequent streams, subsequent streams, and obsequent and resequent streams (See Fluvial landforms of streams.) Insequent streams form by random headward erosion, usually from sheetflow of water over the landform surface. The water collects in channels where the velocity and erosional power increase, cutting into and extending the heads of gullies. Subsequent streams form by selective headward erosion by cutting away at less resistive rocks in the terrain. Obsequent and resequent streams form after time in an area of insequent or subsequent streams.
Sumas Prairie is a landform in British Columbia, Canada and the State of Washington, United States. Part of the Fraser Lowland, it was created by the draining of Sumas Lake early in the 20th Century, and extends from the Vedder Canal southwestwards into northern Whatcom County, Washington.BCGNIS entry "Sumas Prairie" All of its Canadian portion, except its northeasternmost area around Yarrow, which is part of today's City of Chilliwack, was formerly the District of Sumas, which was amalgamated into the City of Abbotsford in 1972.BCGNIS entry "Sumas (district municipality)" Lower Sumas Mountain, Abbotsford.
Over 400 million years ago, the Champlain thrust fault placed a 550 million- year-old slice of rust-red quartzite on top of gray shale in central Addison County. From this, hundreds of millions of years of erosion carved out the landform we now know as Snake Mountain. Around 13,000 years ago, the mountain stood as a small island in the deep waters of glacial Lake Vermont, the geological predecessor of Lake Champlain. Eventually the waters receded, exposing Snake Mountain and other hills along the thrust fault in the Champlain Valley.
Sands of Evie from above, with the island Rousay in the background The Sands of Evie is a sandy beach landform near the village of Evie on Mainland Orkney, Scotland, protected by the Point of Hellia headland.UK Ordnance Survey Map Landranger map, Orkney, 1:50,000 scale (2002) This beach forms the southern boundary of Aikerness Bay, an element of Eynhallow Sound. Immediately to the east is Gurness, a rather well preserved Iron Age broch. A Pictish slab was discovered on the Sands of Evie in 1967 and is now housed in Orkney Museum.
The shape of the landform and associated views, vegetation, iconography of engravings and associated series of stone arrangements on the northern ridgeline of the natural amphitheatre indicate that it is an area of women's ceremonial business. This is reinforced by traditional stories and beliefs. As such, the tangible and intangible values of the cultural landscape provide a unique and rich window into the traditional practise and instruction of sacred women's business. The full significance of the association with Aboriginal women is not able to be articulated in detail due to cultural and gender sensitivities.
The Monongahela National Forest is a national forest located in the Allegheny Mountains of eastern West Virginia, USA. It protects over of federally owned land within a proclamation boundary that includes much of the Potomac Highlands Region and portions of 10 counties. The Monongahela National Forest includes some major landform features such as the Allegheny Front and the western portion of the Ridge-and-valley Appalachians. Within the forest are most of the highest mountain peaks in the state, including the highest, Spruce Knob (4,863 ft), also the highest point in the Alleghenies.
Except in the period after a flood (when fresh material is deposited on a riffle), the sediment on the riverbed in a riffle is usually much coarser than on that in any other in-channel landform. Terrestrial valleys normally consist of channels – geometric depressions in the valley floor carved by flowing water – and overbank regions that include floodplains and terraces. Some channels have shapes and sizes that hardly change along the river; these do not have riffles. However, many channels exhibit readily apparent changes in width, bed elevation, and slope.
Rucker Canyon is a major canyon draining the western central-south of the Chiricahua Mountains, the central landform of the eastern third of Cochise County, Arizona's extreme southeast, bordering southwest New Mexico. It is famous for historic Camp Rucker. The canyon contains Rucker Creek, (Rucker Wash), and upstream closer to the headwaters, the small Rucker Lake. The wash drains into the southern region of the slightly north-west by due south Sulphur Springs Valley, east of north-south running U.S. Route 191 and the small communities of Elfrida, McNeal, and Sunizona.
Mitchell River silt jetties, looking from the south bank towards the north bank, with the Mitchell River in the foreground and Jones Bay in the distance. The rocks lining the banks have been placed to prevent erosion. The Mitchell River silt jetties are an unusually long, thin landform in the Gippsland Lakes region in Victoria, Australia. A type of digitate delta, they have been formed over thousands of years by sediment deposition from the Mitchell River during periods of low water flow and subsequent wash-through during periods of high water flow.
Even before this discovery, Phong Nha held several world cave records, including the longest river as well as the largest combined caverns and passageways. The park derives its name from Phong Nha Cave, containing many fascinating rock formations, and Kẻ Bàng forest. The plateau on which the park is situated is probably one of the finest and most distinctive examples of a complex karst landform in Southeast Asia. This national park was listed in UNESCO's World Heritage Sites in 2003 for its geological values as defined in its criteria viii.
Washington looking ~south across the Northport bridge over the Columbia River Flagstaff Mountain is a large mountain located southwest of Northport, Washington. The peak has an elevation of with over of vertical relief above the valley below. Flagstaff Mountain is composed of Paleozoic sedimentary and intrusive igneous rocks that have been complexly metamorphosed, faulted, and eroded to reveal the rugged landform observed today. The Hubbard and Flagstaff Mountain Barite mines near the summit represent some of the rich mining history in this region geologists refer to as the Kootenay Arc.
Chellanam is on a narrow landform about 10 km in length, starting from St. George Church at the southern end at the northern border of Pallithode village and Kattiparambu (near Thoppumpady). At the northern end it has a width of 250 metres, accommodating in between the villages of Chellanam, Maruvkad, Chalakadavu, Kandakadavu, Puthenthodu, Kannamaly, Cheriyakadavu and Kattiparambu. The landscape is filled with bungalows and courtyards. There was a canal (azhi) passing through this place to the sea which later closed naturally and formed in a place called Andhakaranazhi in Alappuzha district.
The Mitchell River delta is a classic form of digitate delta and ranks as one of the world’s finest examples of this type of landform. The river sweeps near the western shore of Lake King before hitting Eagle Point Bluff and heading east into the lake. Where the river meets the lake a river delta alluvial deposition of sediment has formed, known locally as silt jetties, which extend more than 8 kilometres east into the lake. Silt deposited by this process forms into long narrow banks which run many kilometres.
Aerial view from the northeast of Cape St. Elias and Pinnacle Rock (upper right) Cape Saint Elias is a cape in the U.S. state of Alaska. It is located at the southwest end of Kayak Island, 104 km (65 mi) southeast of Cordova, at . It is commonly believed that Mount Saint Elias, the second highest mountain in the United States and Canada, is named for this landform. The cape was named by Danish explorer Vitus Bering on July 20, 1741 for St. Elias, whose saint's day is July 20.
Thunder Butte (Lakota: Wakíŋyaŋ Pahá) is a prominent butte landmark located in the northwest corner of Ziebach County, South Dakota, in the United States.Rand McNally Atlas, 2006 Thunder Butte is a landform that can be seen for many miles in every direction, and serves now (as it has in the past) as an important orientation point for area residents, or a navigational aide for travelers crossing the surrounding plains. The prominent butte gives its name to a small community at its base, and to a small creek that runs into the Moreau River.
Birch Coulee Battlefield lies on what, in 1862, was open prairie stretching on to the north and west, with woods to the south. Defining the east edge is a steep wooded ravine, a landform known locally by the French term "coulee," also spelled "coulie" or "cooley." Birch Coulee, known to the Dakota as Tanpa Yukan (Place of the White Birch), is deep and runs for a total of down to the Minnesota River. A few hundred yards to the west of the coulee, the prairie rises slightly onto a gentle knoll.
Other landform depressions, not widely accepted as Carolina bays, are present within the northern Gulf of Mexico coastal plain in southern Mississippi and Alabama, where they are known as either Grady ponds or Citronelle ponds.Bernard, H.A., and Leblanc, R.J., 1965, Resume of the Quaternary geology of the northwestern Gulf of Mexico province, in: The Quaternary of the United States (H.E. Wright, Jr., and D.G. Frey, eds.), Princeton University Press, Princeton, New Jersey, p. 137-185. They are also known by a variety of names such as pocks, pock marks, , lacs ronds, and natural ponds.
Panama's topography The dominant feature of Panama's landform is the central spine of mountains and hills that forms the continental divide. The divide does not form part of the great mountain chains of North America, and only near the Colombian border are there highlands related to the Andean system of South America. The spine that forms the divide is the highly eroded arch of an uplift from the sea bottom, in which peaks were formed by volcanic intrusions. The mountain range of the divide is called the Cordillera de Talamanca near the Costa Rican border.
Layout of Sonoma Raceway, the track where the race was held. Sonoma Raceway, formerly Sears Point Raceway and Infineon Raceway is a road course and drag strip located on the landform known as Sears Point in the southern Sonoma Mountains in Sonoma, California, USA. The road course features 12 turns on a hilly course with of total elevation change. It is host to one of only two NASCAR Sprint Cup Series races each year that are run on road courses (the other being Watkins Glen International in Watkins Glen, New York).
The park ranges in altitude from above sea level immediately below Devil's Nose to just over asl in the south eastern corner of the park. 76% of the park lies above the contour. The landform of the park has been described as "a hilly upland with broad crests and dissected slopes" (Lauet al et, 1977). The northern section is a dissected plateau due to the South Para River, which has formed steep sloped valleys and narrow ridge tops; the central reserve area is an undissected plateau; and the southern area is dominated by Mack Creek.
One of Burhanuddin’s major undertakings was the establishment of the Saifee Burhani Upliftment Trust. This redevelopment project comprising 16.5 acres of landform has approximately 250 existing buildings, 1250 shops and 3200 families under its radar in South Mumbai. The idea is to incorporate the locality’s dilapidated structures into a more sustainable development project, with new buildings, modern infrastructure, wider roads, more open spaces and commercial establishments. Using the ‘best principles of urban planning’ the project aims to meet the present and future socio-economic needs of the people.
The landscape of the current hospital grounds shows an exposed quarried landform on the south side, approximately 20 metres high. The exposed rock has eroded somewhat due to environmental conditions; however this landscape remains a noticeable and strong feature of the site, the quarried section that formed a wall runs the full length of the southern boundary. A large expanse of the grounds was levelled to build the military barracks and parade ground. The topography was originally a gentle slope from the ocean cliffs towards what is known today as "The Hill".
The Boulder Bank is a very unusual naturally formed landform in Nelson, New Zealand. It is a 13 kilometre long stretch of rocky substrate which begins at the Mackay Bluff and ends at the Cut of the Nelson Harbour. Haulashore Island was once a part of the Boulder Bank, but the Cut made it an island, and it is no longer connected to the Boulder Bank. The Boulder Bank separates Tasman Bay and the Nelson Haven and is managed as a scenic reserve by the Department of Conservation.
The Cape Henry Lighthouse is a lighthouse at Cape Henry, the landform marking the southern entrance to Chesapeake Bay in the U.S. state of Virginia. The location has long been important for the large amount of ocean-going shipping traffic for the harbors, its rivers, and shipping headed to ports on the bay. The original lighthouse was the first authorized by the U.S. government, dating from 1792. It was also the first federal construction project under the Constitution, for an original contract amount of $15,200 (an additional $2,500 was required to finish the lighthouse).
The Forest Service argued that development at Hoodoo Butte and Hayrick Butte would require excavating and/or blasting of soil and rock on Hayrick Butte, which would potentially exacerbate erosion of local soil. The removal of this soil and rock would also substantially limit future revegetation, further reducing soil productivity in the area. The Forest Service statement also asserted that development of new trails would not lead to significant "scenic resource effects," and that any "landform modification" from a proposed snow play area would only have moderate and short-term effects.
The area around Loch Na Fooey is known as the site of the ancient "Finny volcano" (490 million years ago), formed as the Iapetus Ocean closed to bring the two halves of Ireland together. The volcano's landform is now gone but some of volcanic rocks are preserved in the area, including pillow lavas, and breccia. There is a small funnel-shaped island close to the south-eastern shore known as Red Island (An tOileán Rua). The waters hold a range of fish including wild brown trout and pike.
The initial master plan proved to be unsustainable due to the topography and geology of the area. Construction of the community began in 1971 and was branded as a rural enclave and alternative to the more dense subdivisions emerging in the Orange County basin with homes on large lots, hiking trails, a golf course, and low densities. Anaheim Hills is the first residential development to utilize "Landform Grading." The community grew quickly and by 1974 the Orange Unified School District had constructed a high school to serve the growing community.
Te Raekaihau Point is a rugged coastal landform in Wellington, New Zealand, adjacent to Princess Bay, between Houghton Bay to the west and Lyall Bay to the east on the south coast. One meaning of the name is "the headland that eats the wind". Te Raekaihau Point proceeds from the Southern Headlands Reserve and remains an undeveloped interface with the Cook Strait. The site was the centre of recent controversy as a non-profit developer had proposed building an educational and tourist aquarium building on the site, which remains undeveloped.
From the beginning of recordkeeping in the early 1800s to 1921, the average rainfall on the plain was about a year, with the rainiest months being June and July and the driest October. Prior to human settlement, the combination of landform and rainfall left the Erie Plain with typical prairie plants. Marshes and shallow lakes formerly dotted the landscape here, but human-caused drainage since 1800 has largely erased these and left highly fertile plains behind. Southeastern Michigan, however, still contains many of these distinctive hardwood forest swamps and marshy prairies.
The landform changes from grassy plains in the inner areas to salt marsh, shallow intertidal flats and rocky basalt platforms off the coast of Port Phillip Bay. Kororoit Creek flows through the Park into Port Phillip Bay. Regionally significant geomorphological areas can be found at the wetland terrain at the mouth of the Kororoit Creek as well as at the extensive sand bars off Kororoit Creek. The Park provides a protective buffer zone for the Wader Beach area of the Jawbone Flora and Fauna Reserve, which is located between Williamstown and Altona.
Layout of Sonoma Raceway, the track where the race was held. Sonoma Raceway, formerly Sears Point Raceway and Infineon Raceway is a road course and drag strip located on the landform known as Sears Point in the southern Sonoma Mountains in Sonoma, California, USA. The road course features 12 turns on a hilly course with of total elevation change. It is host to one of only two NASCAR Sprint Cup Series races each year that are run on road courses (the other being Watkins Glen International in Watkins Glen, New York).
Sanetti Plateau in Ethiopia. Ethiopian wolf with Helichrysum citrispinum - both are endemic species The Sanetti Plateau is a major plateau landform of the Ethiopian Highlands, located in the Oromia Region of Ethiopia It is part of the Bale Mountains, and primarily within Bale Mountains National Park. The Bale Mountains contain four distinct ecoregions: the northern plains, bush and woods; the central Sanetti Plateau with an average elevation of over 4000 meters; and the southern Harenna Forest. The Harenna Forest is one of the few remaining natural forests in the entire country of Ethiopia.
The new construction of University Park contains both landscape sculpture sequences and individual public artworks. University Park Common includes over 100 sculptural and graphic pieces as part of Traces, an artwork that marks moments in the 250 year history of the site. Commissioned by Forest City Boston, Traces tells stories of 18th and 19th century commerce and of technical innovations made in the local area. Bronze and stainless steel sculptures present moments in the activity of Simplex Wire and Cable, and a map sequence sculpture documents the changing landform of the site.
The 1st Geography Congress, held in Ankara City between 6–21 June 1941, divided Turkey into seven regions after long discussions and work. These geographical regions were separated according to their climate, location, flora and fauna, human habitat, agricultural diversities, transportation, topography, etc. At the end, 4 coastal regions and 3 inner regions were named according to their proximity to the four seas surrounding Turkey, and their positions in Anatolia. Distinct contrasts between the interior and the coastal areas of Turkey are manifested in landform regions, climate, soils, and vegetation.
Relationships are interpreted between landform development, current and past geologic processes, ground and surface water, and the strength characteristics of soil and rock. Processes evaluated include both surficial processes (for example, slope, fluvial, and coastal processes), and deep-seated processes (for example, volcanic activity and seismicity). Geotechnical zones or domains are designated based on soil and rocked geological strength characteristics, common landforms, related geologic processes, or other pertinent factors. Proposed developmental modifications are evaluated and, where appropriate, analyzed to predict potential or likely changes in types and rates of surficial geologic processes.
Pilot Knob (also, Avie Quah-la-Altwa, Ha-bee-co-la-la, and San Pablo) is a peak in Imperial County, California. Pilot Knob is located southeast of Ogilby, It rises to an elevation of . Pilot Knob is a rocky landform, geologically a Volcanic plug, west of Yuma, Arizona-Winterhaven, California; it is connected to the Cargo Muchacho Mountains, the central portion of the mountains being about north. Pilot Knob was named for its prominence as a landmark for riverboat traffic in the 19th-20th centuries on the Colorado River which borders Winterhaven-Yuma.
Fremantle Prison was built on a land grant of about from limestone quarried on-site, and timber cut from Mount Eliza. The site exhibits considerable changes in ground level, natural and man-made, as a result of its location and former use. The ground level is considerably higher in the south-western corner of the site with what remains of the natural landform, formerly known as Church Hill, now referred to as the South Knoll. The eastern portion of the site is also considerably higher than the ground level established around the main cell block.
Trad introduced the Mineral and Energy Resources (Financial Provisioning) Bill on 15 February 2018, and was passed in November the same year. The MERFP Act aims to ensure that land disturbed by mining activities is rehabilitated to a safe and stable landform that does not cause environmental harm, and can sustain an approved post-mining land use through requiring mining companies to develop Progressive Rehabilitation and Closure Plans. The Progressive Rehabilitation and Closure Plan requirements commenced on 1 November 2019 and have been integrated into the existing environmental authority processes for new mines.
Machias Bay is located in Down East Maine, and is fed primarily by the Machias River, which flows generally eastward from the town of Machias toward its confluence with the East Machias River, and then southward into the bay. The East Machias River flows generally southward from Hadley Lake, past the village center of East Machias. Shortly before it meets the Machias River, it bends sharply to the east before turning south again to empty into the other river. The landform between this bend and the point of confluence is locally known as "The Rim".
The Waterloo Moraine is a landform and sediment body that was created as a moraine in the Regional Municipality of Waterloo, in Ontario, Canada. It covers a large portion of the cities of Waterloo and Kitchener and the township of Wilmot, and some parts of the townships of Wellesley and North Dumfries. About 90% of the water supply of the Regional Municipality of Waterloo is derived from groundwater of the Waterloo Moraine aquifer system. During late 1989 and early 1990, groundwater contamination in Elmira forced the Region to shut down some well fields.
Lake Zürich and the island of Ufenau, the largest in Switzerland The canton of Zürich is situated in the eastern part of the Swiss plateau. It is entirely within the drainage basin of the High Rhine. It is characterized by Glacial landform and traversed by a series of rivers generally flowing south-east to north-west, listed west to east: Reuss, Reppisch, Sihl, Linth-Limmat (forming Lake Zürich), Glatt, Töss and Thur. The main lakes are the Lake Zürich (Linth- Limmat, 88 km2), Greifensee (Glatt, 8.4 km2) and Pfäffikersee (Glatt, 3.3 km2).
The results of those processes are large plains in eastern Slavonia, Baranya and Syrmia, as well as in river valleys. The plains are interspersed by horst and graben structures, which are believed to have broken the Pannonian Sea surface as islands. Psunj, Papuk and Krndija consist mostly of Paleozoic rocks that are 350 - 300 million years old. Požeška Gora and Dilj consist of much more recent Neogene rocks, but Požeška Gora also contains Upper Cretaceous sediments and igneous rocks forming the main ridge of the hill and representing the largest igneous landform in Croatia.
Khan became the captain of the BNS Umar Farooq and with this ship he travelled to the ports of Algeria, Yugoslavia, Egypt, Saudi Arabia and Sri Lanka. On 4 November 1979, Khan became the Chief of Naval Staff of the Bangladesh Navy and on 1 January 1980 he grew to the rank of rear admiral. Khan worked hard to modernise the Bangladesh Navy. In the aftermath of the Bhola cyclone in 1970, a small uninhabited offshore sandbar landform called the South Talpatti sandbar emerged in the Bay of Bengal.
The Gyeongju Basin is a landform in Gyeongju city, North Gyeongsang province, South Korea. It forms part of the watershed of the Hyeongsan River, which flows north through the basin where it is joined by the Bukcheon, Namcheon, Daecheon, and Sogyeon-cheon streams. The basin is surrounded by low mountains, most of which are also part of Gyeongju National Park. Specifically, it is bordered by Gowi Mountain (495 m above sea level) on the south, Seondo Mountain (380 m) and Ongnyeo Peak (215 m) on the west, and Gumi Mountain (594 m) on the north.
Retrieved 8 August 2007. Airborne lidar systems monitor glaciers and have the ability to detect subtle amounts of growth or decline. A satellite-based system, the NASA ICESat, includes a lidar sub-system for this purpose. The NASA Airborne Topographic Mapper'Airborne Topographic Mapper', NASA.gov. Retrieved 8 August 2007. is also used extensively to monitor glaciers and perform coastal change analysis. The combination is also used by soil scientists while creating a soil survey. The detailed terrain modeling allows soil scientists to see slope changes and landform breaks which indicate patterns in soil spatial relationships.
Chloroflexus is a thermophilic filamentous green bacterium found in hot waters at Yellowstone; filamentous structures within geyser cones at El Tatio may have been formed by this bacterium. In splash cones Synechococcus-like microbes are instead responsible for the structures, which resemble those of hot springs. The presence of microorganisms in sinter has been implicated in their tolerance to UV radiation, as sinter absorbs much of this incoming harmful radiation. Some microstructures found on the Home Plate landform on Mars are similar to these biogenic structures at El Tatio, but do not necessarily imply that the microstructures on Mars are biogenic.
Fitzroy Memorial Rotunda, erected in 1925 Edinburgh Gardens is a large park located in North Fitzroy. It is bounded by Brunswick Street and St Georges Road to the west, the curve of Alfred Crescent to the north and east, and Freeman Street to the south. It was created from a grant of land in March 1862 by Queen Victoria and laid out by Clement Hodgkinson, who designed many of Melbourne's parks and gardens.Source: Reserve File RS360, DSE, Melbourne, reproduced in Edinburgh Gardens Landscape Study, Landform Australia, Rew Swanson, 1987 At approximately in size, the park is large by inner urban standards.
A water gap is usually an indication of a river that is older than the current topography. The likely occurrence is that a river established its course when the landform was at a low elevation, or by a rift in a portion of the crust of the earth having a very low stream gradient and a thick layer of unconsolidated sediment. In a hypothetical example, a river would have established its channel without regard for the deeper layers of rock. A later period of uplift would cause increased erosion along the riverbed, exposing the underlying rock layers.
The Santa Rosa Mountains extend for approximately along the western side of the Coachella Valley within Riverside, San Diego, and Imperial Counties in Southern California. The range connects to the San Jacinto Mountains on its northern end, where the Pines to Palms Highway—California State Route 74, crosses them. The highest peak in the range is Toro Peak (elevation ), located approximately south of Palm Springs, just south of Route 74, and on the northeast side of Anza-Borrego's Upper Coyote Canyon. The Santa Rosa Mountains are also a Great Basin Divide landform for the Salton Sink Watershed on the east.
The Lower Curtis Glacier in North Cascades National Park is a well-developed cirque glacier; if the glacier continues to retreat and melt away, a lake may form in the basin Eventually, the hollow may become a large bowl shape in the side of the mountain, with the headwall being weathered by ice segregation, and as well as being eroded by plucking. The basin will become deeper as it continues to be eroded by ice segregation and abrasion. Should ice segregation, plucking and abrasion continue, the dimensions of the cirque will increase, but the proportion of the landform would remain roughly the same.
Evidence for longshore transport is readily apparent on the Canterbury Bight. These include the formation of the Kaitorete Barrier, a landform associated with longshore sediment transport. The Canterbury Bight is not eroding due to net longshore transport exceeding sediment inputs however as firstly, Banks Peninsula and the basalt cliffs at Dashing Rocks prevent significant longshore transport out of the Canterbury Bight system by obstructing further transport. Secondly, longshore transport appears to have abated as little sediment has accumulated at the down-drift end of the bight since the 1950s suggesting sediment is lost from beaches before reaching Banks Peninsula.
Landform feature in Chapelholms woods; this may indicate the boundary between the baronies of Fergushill and Eglinton. A number of properties in the surrounding area bear the name 'Fergushill,' including Knockentiber, North & South Fergushills near Eglinton and Fergushill in Auchentiber. In 1596, Fergushill and Middle Auchentiber were inherited by Robert Fergushill, whose wife Elizabeth was the daughter of John Craufurd of Craufurdland; when he died in 1625, it passed to his son, also named Robert. Sometime after 1660, it passed first to Robert's relative Alexander Craufurd, then to his eldest son John Crawfurd in the 1690s.
Lembert Dome is a granite dome rock formation in Yosemite National Park in the US state of California. The dome soars above Tuolumne Meadows and the Tuolumne River and can be hiked starting at the Tioga Road in the heart of Tuolumne Meadows, west of the Tioga Pass Entrance to Yosemite National Park. The landform is an example of a rôche moutonnée with clear lee and stoss slopes. Lembert Dome was named for Jean Baptiste Lembert, sometimes mistakenly referred to as John Lambert, who took up a homestead in a section of Tuolumne Meadows in 1865.
Morphological mapping schemes, emphasising slope, were the subject for discussion at early meetings of the BGRG. Time-consuming to undertake, such schemes produced information about form but not about the processes or the origin of land forms. These schemes evolved in the 1970s to produce geomorphological maps of the UK. Several articles published in the Geographical Magazine in 1975 and 1976 explained the landform maps produced for all parts of Britain. In 1985 the BGRG celebrated its first twenty five years by hosting the first International Geomorphology Conference in Manchester which led to the formation of the International Association of Geomorphology.
World Wind satellite photo of the Newfoundland Mountains (middle left) and surrounding entities -- Great Salt Lake Desert, Great Salt Lake, and landforms The Newfoundland Mountains are crescent-shaped, mostly only wide, and its closest neighboring landform across the salt flats, is northeast from the northeast range terminus, the Hogup Mountains. The northeast end of the range is a wider section, with the range's highest peak southerly (at the north section). The range is made of one ridgeline, and gets progressively lower in elevation, especially at the very south. The highpoint of the range is Desert Peak, .
Vidal Valley is a 20-mile (32 km) long valley in the far eastern Colorado Desert bordering the Colorado River. Most of the valley is in eastern San Bernardino County, California, but the outfall on the Colorado River is in northeast Riverside County. Vidal Valley forms the large border of the south side of the east-west block of the Whipple Mountains massif, the landform that forces the Colorado to flow southeast, then back southwest. The southeast exit of the valley into Parker Valley on the Colorado River skirts the north end of the Riverside Mountains (see photo).
Seven types of wattle were seen blooming at one time and many other indigenous plants. Six types of vegetation witnessed, consequent to the re-vegetation programme launched by the Park Administration with assistance from FOOPS, are in three landform zones reflecting the soils derived from the underlying geology. These landforms are the plains and the escarpment. The overall picture of floral abundance that has emerged after the area was declared a national park is identification of 124 indigenous plant species including more than 20 species which are in the category of rare or threatened or significant.
David Thompson, an English- Canadian fur trader, ignoring the Salish name already given, renamed the hill 'Brown Knowl' when he climbed in on February 26, 1812. Later, eastern settlers thought Mount Jumbo looked like a sleeping elephant. Locals saw the landform as a reclining elephant with its rump in the Clark Fork and its trunk pointing north toward the Rattlesnake Mountains; the round grassy mountain became known as 'Elephant Hill.' Miners christened a nearby copper mine 'Jumbo Lode' in honor of Barnum and Bailey's most famous attraction Jumbo, the largest elephant in the world, which Barnum acquired in 1882.
Sonoma Mountain is a prominent landform within the Sonoma Mountains of southern Sonoma County, California.Sonoma Mountain Study, a Specific Plan, Sonoma County Community and Environmental Services, February, 1978 At elevation of , Sonoma Mountain offers expansive views of the Pacific Ocean to the west and the Sonoma Valley to the east. In fact, the viticultural area extends in isolated patches up the eastern slopes of Sonoma Mountain to almost in elevation. The eastern and northern slopes are protected from afternoon heat and hence are more densely forested in oak woodlands, abetted by the well-drained, nutrient-rich soils.
Nathan Coley's sculpture at the Dean Gallery (Modern Two) in 2017. Modern One and Two are set in extensive parkland, where visitors can discover sculpture by such artists as Ian Hamilton Finlay, Barbara Hepworth, Henry Moore, George Rickey, Rachel Whiteread, Richard Long and Nathan Coley. The lawn to the front of Modern One was re-landscaped in 2002 to a design by Charles Jencks. This dramatic work, or Landform, comprises a stepped, serpentine mound reflected in three crescent-shaped pools of water. The façade of Modern One is home to Martin Creed’s Work No. 975, EVERYTHING IS GOING TO BE ALRIGHT.
This coast shows excellent examples of landforms, including the natural arch at Durdle Door, the cove and limestone folding at Lulworth Cove and a tied island, the Isle of Portland. Chesil Beach is a fine example of both a tombolo (a deposition landform in which an island is attached to the mainland by a narrow piece of land such as a spit or bar) and a storm beach (a beach affected by particularly fierce waves). The site has stretches of both concordant and discordant coastlines. Due to the quality of the varied geology, the site is the subject of international field studies.
Despite being together with fjords the most studied coastal landform in Norway, as of 2013 there is no consensus as to the origin of strandflats. An analysis of the literature shows that during the course of the 20th century, explanations for the strandflat shifted from involving one or two processes to including many more. Thus most modern explanations are of polygenetic type. Grand-scale observations on the distribution of strandflats tend to favour an origin in connection to the Quaternary glaciations, while in-detail studies have led scholars to argue that strandflats have been shaped by chemical weathering during the Mesozoic.
"História da Companhia de Jesus no Brasil", by Serafim Leite,Hallewell, 1985, p. 10 says that the library of Colégio Santo Inácio, in O Morro do Castelo, Rio de Janeiro. (This was a landform that existed in the city of Rio, the hill being one of the foundation points of the city in the sixteenth century and which housed landmarks of great importance, such as colonial forts and buildings of the Jesuits. Nevertheless, it was destroyed in an urban reform in 1922.) This centre is believed to have undertaken some printed jobs around 1724, the accuracy of the claim not be ascertained.
Aerial photo of part of Hurricane Mesa supersonic test track Hurricane Mesa () is a Utah landform near Hurricane, Utah, used for Cold War tests of rocket ejection seats for supersonic aircraft at the Hurricane Supersonic Research Site. The mesa is "flat bedrock of faultless Shinarump conglomerate" above the Virgin River valley, which allowed clearance for assessment of a longer flight trajectory up from the mesa and over the cliff for the test object (e.g., the anthropoid simulator--dummy--named "Hurricane Sam"). Currently the facility is still used to test military ejection seats for the US and Foreign Govt's.
The tallest among such landforms are Ivanšćica and Medvednica north of Zagreb—both are also at least partially in Hrvatsko Zagorje—as well as Psunj and Papuk that are the tallest among the Slavonian mountains surrounding Požega. Psunj, Papuk and adjacent Krndija consist mostly of Paleozoic rocks from 300–350 Mya. Požeška gora, adjacent to Psunj, consists of much more recent Neogene rocks, but there are also Upper Cretaceous sediments and igneous rocks forming the main, ridge of the hill; these represent the largest igneous landform in Croatia. A smaller piece of igneous terrain is also present on Papuk, near Voćin.
Concerned with denudation chronology (the reconstruction of long-term landform history), he became involved with study of the origin of tors in Scotland, on Dartmoor, the Pennines and South Africa. His view was that the British tors were a product of deep chemical weathering under a tropical climate in the Tertiary, exposed by erosion in the Pleistocene. This contrasted sharply with the views of others that tors are essentially arctic features produced by periglacial processes.French, H.M. (1976), The Periglacial environment, London: Longman, This was part of his wider view of the importance of pre-glacial events and forms.
Pratt Rock, also known as Pratt's Rock, is a rockface or other landform that includes a series of stone carvings in Prattsville, New York depicting the life of Zadock Pratt. Pratt was supposed to be buried in a tomb carved into the stone, but work was stopped after only a small recessed chamber was created because water leaked through the rock overhead, and excavating the stone was providing to be too difficult. The rock was originally a monument for Pratt's son, George W. Pratt, who was killed in the Civil War. It is considered the first memorial for the Civil War.
Recluse Nunatak () is an isolated rock exposure lying on the Handel Ice Piedmont, midway between Haydn Inlet and the Colbert Mountains in the west- central portion (facing towards the Wilkins Ice Shelf) of Alexander Island, Antarctica. The nunatak was first mapped from air photos taken by the Ronne Antarctic Research Expedition (RARE), 1947–48, by Searle of the Falkland Islands Dependencies Survey (FIDS) in 1960. The name given by the United Kingdom Antarctic Place-Names Committee (UK-APC) suggests the isolated position of the nunatak, considering this landform is situated far away from other landforms of Alexander Island.
Below Carter Bridge, the Clackamas River receives Hellion Creek from the left about from the mouth, passes Big Eddy Campground, receives Moore Creek from the right, and passes Lazy Bend Campground. Around from the mouth, the river receives the South Fork Clackamas River from the left opposite a landform known as Big Cliff. About later, the river enters North Fork Reservoir and soon receives the North Fork Clackamas River from the right. The Clackamas reaches the Faraday Dam, formerly known as the Cazadero Dam, about from the mouth and passes Faraday Lake, which is on the river's left about later.
There are supernaturally and socially derived consequences for those who disrespect cultural law. The womb-shaped amphitheatre is important for women's business. In particular, the shape of the landform and associated views, vegetation, iconography of engravings and associated series of stone arrangements on the northern ridgeline of the natural amphitheatre have been noted as indications that it is sacred area for women's business. Archaeological and anthropological research supports the combined cultural knowledge of local Aboriginal people which indicates that this area on the northern ridgeline is a place of teaching and ceremony related to sacred women's business.
Located within the southern of two parallel prominent ridges, the Gogebic range iron formation name is often used interchangeably with the range of hills that encompass it. The hills composing the Gogebic range vary from 100 to 600 feet above the surrounding terrain, and are a prominent landform visible for miles. The Gabbro, or Trap Range comprises a somewhat lower ridge of hills running parallel just to the north of the Gogebic Range. Since the two ranges of hills are made up of dissimilar rock types, the rock formation containing the iron ore deposits is located exclusively within the southern (Gogebic) Range.
Small village named Alongkong in middle belt of Wabane Hilly topography of Wabane Wabane have three distinct topographical regions and marks the end of the Manyu plain. The landform is undulating and characterised by elevated, prominent mountainous terrain, with altitude ranging from lowland Nkong (72 m), Bechati and Besali (570 m), through Alongkong (1470 m) to M’mouck Leteh (2200 m). At the Bamumbu Fondom, hill slopes are steep to very steep, narrow boulder strewn crests and deeply incised valleys. The area of Mmuock Leteh is equally undulating but with broad hilltops and gentle slopes suitable for intensive vegetable farming.
Ash Springs The Pahranagat Valley is a Tonopah Basin landform in Lincoln County, Nevada. The more fertile part of Pahranagat Valley is a narrow ribbon of green (no more than wide) like an oasis in the vast Nevada desert. It is approximately long running north and south and is watered by three large natural springs of water (Hiko Springs, Crystal Springs and Ash Springs) and many smaller ones as well. It has four lakes, two near the north end of the valley (Nesbitt Lake and Frenchie Lake) and two towards the south end (Upper Pahranagat Lake and Lower Pahranagat Lake).
Thus, these movements created the Blue Mountains and Hornsby Plateaux, with the lagging behind of the peneplain becoming the Cumberland Plain.Sydney Basin - landform Office of Environment and Heritage (New South Wales) The plateau was scoured by freshwater streams, which perforated a labyrinth of V-shaped valleys with intruding rocky ridges into the Hawkesbury Sandstone. The drainage activity is ascertained by the Hawkesbury Sandstone's impotence, which were employed by early watercourses. As the creeks carved deeper into the plateau, they began undercutting the sandstone walls of the valley, and as such, blocks of sandstone fell down, thus creating cliff lines.
Depending on the degree to which it was fractured by jointing, the granite bedrock underlying this surface was altered to varying depths beneath the land surface. This process formed underground "domes" of solid granite bedrock surrounded by deeply weathered, relatively loose, and disaggregated granite. Following separation of Australia and Antarctica and accompanying tilting of what became southwestern Australia, periodic erosion of the deeply weathered granite, which underlaid the surrounding land surface, exposed these buried solid bedrock domes over time as Hyden Rock.Twidale, C. R., J. A. Bourne, and J. R. Vidal Romani (2002) Multistage Landform Development in Various Settings and at Various Scales.
Retrieved on 2007-09-14 and its name has since become standard worldwide among volcanologists in referring to and writing about tuyas. The Tuya Mountains Provincial Park was recently established to protect this unusual landscape, which lies north of Tuya Lake and south of the Jennings River near the boundary with the Yukon Territory. Tuya Butte is regarded as among the best examples of this landform outside Iceland and Antarctica.Tuya Mountains Provincial Park Retrieved on 2007-11-08 Tuya Butte was named by Canadian volcanologist Bill Mathews in association with adjacent Tuya Lake and Butte Lake.
Canoelands is a small hamlet within Glenorie, consisting of some 80 houses and 247 people extending out towards the east from Old Northern Road. Canoelands is between the hamlets of Forest Glen and Maroota and is 10 km north of the village of Glenorie and 20 km south of the village of Wisemans Ferry. By road, Canoelands is 55 km north of the Sydney Harbour Bridge. The landform of the area is on Canoelands Ridge, a high, undulating, dissected plateau of Hawkesbury Sandstone with many steep gullies covered with dry sclerophyll forest, predominantly tall varieties of hardwood trees of the genus Eucalyptus.
The peak rises in Joshua Tree National Park, west of the Hexie Mountains, north of the San Bernardino Mountains and near Queen Valley. Malapai Hill is the product of the intrusion of magma into White Tank monzogranite, that cooled as basalt. The exact origin of the landform is not known: it might have been part of an older volcanic complex, or it might have never penetrated the surface but cooled underground and then became exposed as the somewhat softer granite around it was eroded over time. According to Argon dating techniques, the basalt of Malapai Hill is 15.93 ± 0.08 million years old.
Technically the landform extends south of the Baudó River down to Malaga Bay, but the area has been eroded into low hills and marshlands. From Cabo Corrientes north to Punta Ardita and on into Panama the Baudó Mountains meet the ocean in steep cliffs, rising up to as high as , with small indentations in the coast providing small pocket beaches, some sandy, but most are shingle or cobble. However, near river mouths the coast has been eroded and there are wide sandy beaches, tidal flats and even mangrove swamps. The highest point, Alto de Buey, is .
The Sand Ridge landform, which is the remnants of what was once the Tulare Lake archipelago, was the densest region of human habitation for hundreds of years because it provided stable land to build villages on, unlike the shores of Tulare Lake, which varied with the seasons. In times of low water, the Sand Ridge split Tulare Lake in two, the latter becoming the Tache and Ton Tache lakes. The islands were probably discovered by settlers in the 1850s. An 1853 map depicts the Sand Ridge region as a 'ridge of high ground' and not as islands.
Armour of basalt blocks In hydrology and geography, armor is the association of surface pebbles, rocks or boulders with stream beds or beaches. Most commonly hydrological armor occurs naturally; however, a man-made form is usually called riprap, when shorelines or stream banks are fortified for erosion protection with large boulders or sizable manufactured concrete objects. When armor is associated with beaches in the form of pebbles to medium-sized stones grading from two to 200 millimeters across, the resulting landform is often termed a shingle beach. Hydrological modeling indicates that stream armor typically persists in a flood stage environment.
The street layout is typical of the old quarters of many northern European cities. The castle is perched on top of a rocky crag (the remnant of an extinct volcano) and the Royal Mile runs down the crest of a ridge from it. Due to space restrictions imposed by the narrowness of this landform, the Old Town became home to some of the earliest "high rise" residential buildings. Multi-storey dwellings known as lands were the norm from the 16th century onwards with ten and eleven storeys being typical and one even reaching fourteen or fifteen storeys.
The Limpopo River Basin, the major landform of all of southern Africa, lies partly in Botswana, with the basins of its tributaries, the Notwane, Bonwapitse, Mahalapye, Lotsane, Motloutse and the Shashe, located in the eastern part of the country. The Notwane provides water to the capital through the Gaborone Dam. The Chobe River lies to the north, providing a boundary between Botswana and Namibia's Zambezi Region. The Chobe River meets with the Zambezi River at a place called Kazungula (meaning a small sausage tree, a point where Sebitwane and his Makololo tribe crossed the Zambezi into Zambia).
Bradford Kames is situated in the north-east of England in the county of Northumberland, some west of the coastal town of Seahouses. The esker is composed of a ridge and associated mounds, on a site of circa length orientated in a north-north-west - south-south-east direction, with the ground falling to the east. The SSSI citation for Bradford Kames describes it as providing "a striking example of the complex landform and sediment associations that developed during the wastage of the last ice sheet." At the north end of the site, Spindlestones Pond provides a habitat for great crested newts.
Blind thrust faults generally exist near tectonic plate margins, in the broad disturbance zone. They form when a section of the Earth's crust is under high compressive stresses, due to plate margin collision, or the general geometry of how the plates are sliding past each other. Diagram of blind-thrust faulting As shown in the diagram, a weak plate under compression generally forms thrusting sheets, or overlapping sliding sections. This can form a hill and valley landform, with the hills being the strong sections, and the valleys being the highly disturbed thrust faulted and folded sections.
The Gang Peak, located in the northeastern corner of the Mambilla Plateau, on the Mambilla-Gashaka- Cameroon tri-point boundary zone, is Nigeria's loftiest landform. Villages are found both on the hilltops and on valley bottoms, and are relatively isolated from one another particularly during the rainy seasons when river crossings can be difficult (and impossible for motorised transport). Agriculture is concentrated on the valley bottoms while the highlands have been extensively grazed since the 1940s, i.e. since the immigration of cattle graziers towards the end of British administration (it was part of British Cameroon until the referendum of 1959/61).
View of the Vermillion Cliffs (to the northeast) from the Kaibab Plateau, June 2008 The plateau, part of the larger Colorado Plateau, is bordered on the south by the Grand Canyon and reaches an elevation of . The plateau is divided between Kaibab National Forest and the "North Rim" portion of Grand Canyon National Park. Tributary canyons of the Colorado River form the plateau's eastern and western boundaries, and tiers of uplifted cliffs define the northern edges of the landform. Winter snowfall is often heavy (sometimes exceeding ), and this creates opportunities for backcountry Nordic skiing and snow camping.
There are six main landforms in Kakadu National Park: the Arnhem Land plateau and escarpment complex, known as the stone country; the outliers; the lowlands; the southern hills and basins; the floodplains; and the tidal flats. Each landform has its own range of habitats. Kakadu's varied landscapes and the habitats they contain are features that contributed to its listing as a World Heritage Area. The Mamukala wetlands Most of Kakadu was under a shallow sea approximately 140 million years ago, with the escarpment wall formed from sea cliffs and Arnhem Land from a flat plateau above the sea.
Danmark in Norway. It is a typical Nordic skerry. As suggested by its origin as islette, an Old French diminutive of "isle",Webster's New International Dictionary of the English Language, Second Edition, 1958 use of the term implies small size, but little attention is given to drawing an upper limit on its applicability. The World Landforms website says "An islet landform is generally considered to be a rock or small island that has little vegetation and cannot sustain human habitation", and further that size may vary from a few square feet to several square miles, with no specific rule pertaining to size.
The Snake River threads through the entire valley from its headwater in Yellowstone in the north to the mouth of the Snake River Canyon at the southern tip of the valley. Blacktail Butte is a prominent landform rising from the valley floor. The average elevation of the valley is over above sea level. High altitude and steep mountain slopes on all sides of the valley often cause calm winter nights to be very cold, as radiational cooling from snow-covered ground creates cold air near the surface, which then slides down into the valley due to the higher density of the air.
Many different kinds of wetlands exist, all characterized by unique compositions of plant life and water conditions. To list a few, marshes, swamps, bogs, fens, peatlands, muskegs, prairie pothole (landform), and pocosins are all examples of different kinds of wetlands. Because each type of wetland is unique, the same characteristics used to classify each wetland can also be used to characterize the amount of methane emitted from that particular wetland. Any waterlogged environment with moderate levels of decomposition creates the anaerobic conditions needed for methanogenesis, but the amount of water and decomposition will affect the magnitude of methane emissions in a specific environment.
Terracettes In geomorphology, a terracette is a type of landform, a ridge on a hillside formed when saturated soil particles expand, then contract as they dry, causing them to move slowly downhill. An example of this is the manger near the Uffington White Horse. It may also be described as a small, irregular step-like formation on steep hillslopes, especially on those used for pasture which are formed by soil creep or erosion of surface soils exacerbated by the trampling of livestock such as sheep or cattle. Synonyms are: catstep cattle terracing, sheep or cattle track.
The pueblo is located three miles south of Bernalillo off Highway 85 in southern Sandoval County and northern Bernalillo County, at . It is bounded by the city of Albuquerque to the south and by the foothills of the Sandia Mountains, a landform the people hold sacred and which was central to the traditional economy and remains important in the spiritual life of the community, to the east. A forested area known as the bosque surrounds the rest of the reservation, and serves as a source of firewood and wild game. A resident population of 4,414 was reported as of the 2000 census.
A major central wash follows the valley's southeast; the north has no major wash, and instead drainages are towards a central bajada landform region. The northern bajada extends north past Hachita, NM on the east and Old Hachita, NM on the west. The southeasterly excursion of the valley is caused by the bordering Big Hatchet Mountains on the southwest, which trend southeast; the valley narrows here, between the Apache Hills northeast, to between 5 and 7 miNew Mexico Atlas & Gazetteer, p. 52-53. wide. In the northwest where the valley widens, the Little Hatchet Mountains lie on the west perimeter.
The active cave system is one of the most heavily studied karst systems in Britain with reference to the conduit and diffuse flow characteristics of its hydrology. Charterhouse Caves include four major swallet caves that provide an indisputable record of Pleistocene landform development in the Mendips and surrounding area. Sun Hole Cave provides a varied fauna radiocarbon-dated to the end of the Late Devensian Cold Stage. Several types of limestone including Clifton Down Limestone, Cheddar Limestone and Cheddar Oolite are visible in the Gorge and surrounding areas with pale grey Burrington Oolite outcropping around Black Rock Gate.
Vents that issue volcanic material (including lava and ash) and gases (mainly steam and magmatic gases) can develop anywhere on the landform and may give rise to smaller cones such as Puu Ōō on a flank of Hawaii's Kīlauea. Other types of volcano include cryovolcanoes (or ice volcanoes), particularly on some moons of Jupiter, Saturn, and Neptune; and mud volcanoes, which are formations often not associated with known magmatic activity. Active mud volcanoes tend to involve temperatures much lower than those of igneous volcanoes except when the mud volcano is actually a vent of an igneous volcano.
The Oak Grove Fork Clackamas River arises at an elevation of above sea level and falls between source and mouth to an elevation of . The main stem begins in the Cascade Range near Abbot Pass, a mountain gap at , on the border between Clackamas County and Wasco County. Originating on the Warm Springs Indian Reservation, the river flows generally west about through the Mount Hood National Forest to the unincorporated community of Ripplebrook, where it joins the main stem of the Clackamas River. From its source, the river flows about through a landform known as Big Meadows before leaving the reservation.
Victoria Harbour is a natural landform harbour separating Hong Kong Island in the south from the Kowloon Peninsula to the north. The harbour's deep, sheltered waters and strategic location on the South China Sea were instrumental in Hong Kong's establishment as a British colony and its subsequent development as a trading centre. Throughout its history, the harbour has seen numerous reclamation projects undertaken on both shores, many of which have caused controversy in recent years. Environmental concerns have been expressed about the effects of these expansions, in terms of water quality and loss of natural habitat.
His music was so beautiful that Hades relented and allowed Eurydice to return to the world of the living. This striking landform seamlessly continues the garden's intellectual dialogue via an immense inverted pyramid and spiral rill, both set within a golden ratio. In 2015 The Grand Étang, or ‘large lake’ in French, a long-vanished lake of almost one- acre with a 75 ft tall water jet was recreated, to once again reflect the main frontage of Boughton. Located immediately to the north-west of the House, it is one of the earliest surviving features from the original gardens and designed landscape.
Originally, the Kinnickinnic River flowed almost directly into Lake Michigan, with water from the Milwaukee and Menomonee rivers flowing south from the center of the city before exiting to the lake. The landform that protected the harbor was a long marshy spit, called Jones Island, that extended southwards from the center of the city. To shorten the distance from the harbor entrance to the city, a "straight cut" was made across the base of the spit, at the northern end. The original harbor entrance was filled in, so that Jones Island was now a peninsula extending northwards, with its base to the south.
Kolbeinsey from the deck of RV Knorr, 2011 Kolbeinsey (also known as Kolbeinn's Isle, Seagull Rock, Mevenklint, Mevenklip, or Meeuw Steen) is a small islet off the northern coast of Iceland, north-northwest of the island of Grímsey. The island is the northernmost point of Iceland and lies north of the Arctic Circle. It is named after Kolbeinn Sigmundsson from Kolbeinsdalur in Skagafjörður who is said to have broken his ship there and died with his men, according to Svarfdæla saga. A basalt landform, devoid of vegetation, it is subject to rapid wave erosion and is expected to disappear in the near future.
At Cribarth, Variscan movement on this Caledonoid feature has given rise to a couple of folds in the limestone and overlying Twrch Sandstone from which the present landform has subsequently been carved, in part by glacial action. The southernmost lineament is the Neath Disturbance which runs ENE from Swansea Bay up the Vale of Neath and into the park at Pontneddfechan. The limestone is tightly folded here at Bwa Maen (Welsh: 'stone bow') and again at Moel Penderyn, through which it next passes. It passes beneath Pontsticill Reservoir, across the top of Dyffryn Crawnon and then down the shallow Onneu valley to Crickhowell.
Map of Cape Cod showing shores undergoing erosion (cliffed sections) in yellow, and shores characterized by marine deposition (barriers) in blue. Deposition is the geological process in which sediments, soil and rocks are added to a landform or land mass. Wind, ice, water, and gravity transport previously weathered surface material, which, at the loss of enough kinetic energy in the fluid, is deposited, building up layers of sediment. Deposition occurs when the forces responsible for sediment transportation are no longer sufficient to overcome the forces of gravity and friction, creating a resistance to motion; this is known as the null-point hypothesis.
In this area, human activity includes fruit and dairy agriculture, major urban areas, and some forestry and tourism attractions. The most prominent wildlife observed are white tailed deer, moose, and the grey squirrel, and vegetation includes a wide range of trees such as oak, hickory, maple, beech, and some pine and basswood species. The second sub-ecoregion is the Central USA Plains, an area of , that has a landform of smooth plains. The majority of this region’s surface material is moraine with some lacustrine, and the soil consists of calcium enriched prairie soils and forest soils on moraine.
Basalt dike in orange-red Hakatai Shale along Colorado River at Hance Rapid, river mile 76.5, Grand Canyon. Isis Temple and Cheops Pyramid on a fault-block (horst), sitting on "island" of Shinumo Quartzite, unit 3 of the Unkar Group. Bottom 3 units of Unkar above Granite Gorge, and Vishnu Basement Rocks. (3.5-mi by 2.0-mi block) At Apollo Temple landform, the Cambrian Tapeats Sandstone lies above the angular Great Unconformity with strata of the 3)-Chuar Group, the striped 2)-Nankoweap Formation, the dark 1-5)-Cardenas Basalt and red 1-4)-Dox Formation below.
Groundwater sapping is a geomorphic erosion process that results in the headward migration of channels in response to near constant fluid discharge at a fixed point. The consistent flow of water displaces fine sediments which physically and chemically weathers rocks. Valleys that appear to have been created by groundwater sapping occur throughout the world in areas such as England, Colorado, Hawai’i, New Zealand, and many other places. However, it is difficult to characterize a landform as being formed exclusively by groundwater sapping due to phenomena such as pluvial runoff, plunge-pool undercutting, changes in water table level, and inconsistent groundwater flow.
A protalus rampart (or pronival rampart) is a depositional landform of periglacial origin. It forms as rock debris falls onto a steep snow slope from a cliff above and slides down the snow surface to come to a rest at the foot of the slope. Over a long period of time, sufficient material can accumulate in this way to produce a distinct bank of stony material which, long after the snowbed has melted away, remains as a rampart (a bank or mound similar to a manmade rampart). The debris may also accumulate through avalanching or landslide.
A potrero is a long mesa that at one end slopes upward to higher terrain. This landform commonly occurs on the flanks of a mountain, as part of a dissected plateau. A loan word from the Spanish language, potrero is in current use in the southwestern United States, where it is sometimes translated as "tongue of land" and "enclosed piece of pasture land".John Peabody Harrington (1916) The Ethnogeography of the Tewa Indians, pages 29–618 in Twenty-ninth Annual Report of the Bureau of American Ethnology to the Secretary of the Smithsonian Institution, 1907–1908, Government Printing Office, Washington.
AMS, 1954) Due to its location south of the Qinling, Ankang is geographically considered to be part of southern China, yet, on administrative terms, as Shaanxi is officially part of Northwestern China, it is considered to be part of the Northwest. Ankang is located in the southeastern part of Shaanxi, north of the Daba Mountains and south of the Qinling. Measuring from east to west and from north to south, the prefecture-level city of covers an area of . The Han River (Hanshui) crosses it from west to east, forming a natural landform of "a plain between two mountains".
The range extends for approximately from the San Bernardino Mountains southeast to the Santa Rosa Mountains. The San Jacinto Mountains are the northernmost of the Peninsular Ranges, which run from Southern California to the southern tip of the Baja California Peninsula. The highest peak in the range is San Jacinto Peak (3,302 m; 10,834 ft), and the range is also a Great Basin Divide landform for the Salton Watershed to the east. San Jacinto mountains as viewed from the north, when approaching the gateway to Palm Springs, California on Highway 62 The Coachella Valley stretches along the eastern side of the range, including the cities of Palm Springs and Rancho Mirage.
Mount Finke is a monadnock in the Australian state of South Australia located in the gazetted locality of Yellabinna about north of Ceduna. In 1999, it was described as follows: > It is about 5km long with an elevation of 369 m AHD, it stands about 270m > above the surrounding landscape. Mt Finke is an isolated block of steeply > dipping quartzite believed to be part of a landform dating back some 250 Ma. It was named by John McDouall Stuart, the British explorer, on 7 August 1858 after William Finke who was a friend "associated with mining & pastoral activities." It has a locally diverse flora and fauna, including 266 plant species.
The landform has been re-shaped by the extraction of limestone and by the nearby mining of silica rock and its transport down-valley by various means. The former limestone quarry is now a car park; its walls are used by climbers and abseilers. The Dinas Rock Silica Mines just to the east of Dinas Rock itself used to provide large quantities of very pure crushed sandstone destined for the manufacture of refractory bricks for furnace linings and the like. A system of tramways, aerial cableways and inclines on the southern flanks of Dinas Rock conveyed the material from the mines to the valley below.
After completing the project in 1852, Gilliss sold the equipment and the buildings that housed it to the government of Chile, which formed OAN at that time. After two years of operating on Santa Lucia Hill, the director of the new observatory, Carlos Guillermo Moesta, noticed that daytime heating of the dark rock of the hill caused the entire landform to move slightly. As a result of this discovery Moesta decided it would be best to move the observatory elsewhere. A new facility was built in what is now Quinta Normal starting in 1857, and OAN officially moved to the new location in 1862.
Raak Plains and Pink Lakes, further west in Murray-Sunset National Park, are outstanding examples of the boinka landform complex of sandplains, gypsum flats, gypsite hills, salinas and source- bordering dunes. The country is extremely rugged, and contains a system of saline blue lakes formed by water that discharges from below ground. The discharge complex, which Phillip Macumber calls the "Raak boinka", is a broad depression with a distinctive outer boundary and markedly different appearance from the aeolian Mallee landscapes that surround it. It includes dunes and islands of sand and gypsum clay, plains of sand, clay and limestone, gypsum flats and halite salinas in the lowest parts.
During the last ice age, the area that would become the Fraser Valley was covered by a sheet of ice, walled in by the surrounding mountains. As the ice receded, land that had been covered by glaciers became covered by water instead, then slowly rose above the water, forming the basin that exists today. The valley is the largest landform of the Lower Mainland ecoregion, with its delta considered to begin in the area of Agassiz and Chilliwack, although stretches of floodplain flank the mountainsides between there and Hope. Several of the Fraser's lower tributaries have floodplains of their own, shared in common with the Fraser freshet.
St Mary's Church is bottom-right Consultant for Birmingham City Council, Dr Hilary Taylor, observed: > There is no doubt that Handsworth Park is a successful design, one where > everything from the basic landform to the elements of planting and ornament > were the outcome of careful consideration, both of the site and the > requirements of the local community. There are theatrical contrasts of > panoramic space and enclosure, apparently wild nature and intricate artistic > detail. All this is linked by an elegant circulation system which afforded > opportunities for healthy exercise and ensured that every landscape incident > was visited and enjoyed. Today, of course, it takes some time to perceive > all this.
The Darling Scarp originated as the local expression, in the Perth area, of the extensive Darling Fault, a major and ancient geological discontinuity separating the Archaean Yilgarn Craton in the east from the younger Pinjarra Orogen and overlying Phanerozoic Perth Basin to the west. The Darling Fault is exposed for over , from the area east of Shark Bay, to the southern coast of Western Australia east of Albany. The location of the scarp must once have coincided with the location of the fault, but the scarp has since eroded about eastwards. The original location of the scarp is indicated in places by an unusual landform known as the Ridge Hill Shelf.
Erosion of etchplains can result in the exposure of inselbergs such as bornhardt and tors. Generally the topography exposed at a stripped etchplain, that is an etch surface, after erosion of regolith is one with many irregularities as result of structurally defined areas of rock strength. A distinction can be made between etchplains and etch surfaces as the later may or may not be flat and can represent the landform arising from the stripping of an etchplain. As climate changes arid and semi-arid periods of pediplanation may alternate with more humid periods of etchplanation resulting in the formation of flattish surfaces (peneplains) of mixed origin (polygenetic).
The relic shorelines at elevations of 3100 feet and 3018 feet can be seen mostly easily on Gidikwe Ridge, west of the Boteti River. The geologic processes behind the formation of the basin are not well understood. It is conjectured that there was a gentle down-warping of the crust, with accompanying mild tectonics and associated faulting; however, no significant plate boundary faults have been identified.Cooke, H. J. (1980) "Landform evolution in the context of climatic change and neo-tectonism in the Middle Kalahari of north-central Botswana" Transactions, Institute of British Geographers 5: pp. 80-99, pages 83-84 The main axis of the developing graben runs northeast-southwest.
The level of disturbance suffered by the swamp is too great to consider restoration as a feasible option for action, however management is focused on the values the swamp still retains. The swamp is now referred to by its post-collapse landform units: the intact, drying fissured channel and delta areas. The fissured areas have had a great deal of damage, while the delta - the mass of peat expelled into the reservoir - seems to be developing an ecological value in its own right. The delta area closest to the swamp is fairly stable, whereas the front rises and falls with the reservoir level but does not move laterally.
The peak of Isis Temple is only ~202 ft lower than Grand Canyon Village. Isis Temple is about 5 mi directly north of Grand Canyon Village on the South Rim, Grand Canyon; the Village is the west terminus of Arizona Route 64-(East Rim Drive), and north terminus of U.S. 180, from Valle, Arizona, and Williams, (about 58 mi south). Isis Temple is part of an uplifted, and sub-faulted block, (about 3.5 mi long x 2.0 mi wide),Arizona Road & Recreation Atlas, Benchmark Maps, p. 12-13. with a sub-peak landform, Cheops Pyramid, ,Arizona Road & Recreation Atlas, Benchmark Maps, p. 12-13.
Finally, they are also common as parasitic and monogenetic cones on complex shield and stratovolcanoes. Globally, cinder cones are the most typical volcanic landform found within continental intraplate volcanic fields and also occur in some subduction zone settings as well. Parícutin, the Mexican cinder cone which was born in a cornfield on February 20, 1943, and Sunset Crater in Northern Arizona in the US Southwest are classic examples of cinder cones, as are ancient volcanic cones found in New Mexico's Petroglyph National Monument. Cone-shaped hills observed in satellite imagery of the calderas and volcanic cones of Ulysses Patera, Ulysses Colles and Hydraotes Chaos are argued to be cinder cones.
Although the gap between South Bluff and Scotts Bluff is a natural landform in the northern Wildcat Hills, the area was not easily traversed. Originally, the main branch of the Great Platte River Road (customarily referred to as the Oregon Trail and also later the California Trail) passed to the south of the bluffs at Robidoux Pass. Beginning in 1851, after the construction of a road between the bluffs, Mitchell Pass became the preferred route of the Great Platte River Road. It was favored over Robidoux Pass because it was both shorter and emigrants remained closer to the North Platte River, an important water source.
In the Late Pliocene, andesitic lava and ash erupted from Magdalena-Lucia, Mount Andrassy, Mount Wullersdorf and Mount Pock, with these eruptions now forming the highest landform of the region. Rhyolite was later extruded from Mount Wullersdorf, Mount Andrassy and Glass Hill, and at the end of the Pliocene dacite was erupted from Mount Maria. The coastal platform was formed during the Quaternary period after series of eruptions of basaltic lavas. Basalt flows following eruptions from hills in the Table-Tiger area, Quoin Hill including in Mostyn caused much disruption of drainage and account for the upper alluvial valleys mentioned in the third region.
They are a very common landform in sandy deserts all over the world and are arc-shaped, markedly asymmetrical in cross section, with a gentle slope facing toward the wind sand ridge, comprising well-sorted sand. This type of dune possesses two "horns" that face downwind, with the steeper slope known as the slip face, facing away from the wind, downwind, at the angle of repose of the sand in question, approximately 30-35 degrees for medium-fine dry sand. The upwind side is packed by the wind, and stands at about 15 degrees. Barchans may be high and wide at the base measured perpendicular to the wind.
Related to the Braunton Great Field and Braunton Marsh, this landscape type is set back from the river Taw to the south and protected from westerly maritime influence by Saunton Sands and Braunton Burrows. Its key characteristics include; open flat landform, often with distinct vegetated floodplain edge, shallow watercourses screened by riparian vegetation, pastoral or arable land use with variable field sizes, rare survival of medieval open field strip system (Braunton Great Field), unenclosed or with stone walls and hedges as well as drainage ditches, unsettled, narrow winding lanes, open internally with views out screened by boundary vegetation, estuarine or river valley character and exceedingly tranquil.
The partnership company received planning permission that year to allow opencast coal extraction on what were termed the surface workings of the former colliery site, on the pre-condition that the site would be subject to land remediation and reclamation, followed by land restoration of the entire Tower Colliery site. The land reclamation works includes: removal of structures; removal of residual contamination; re-profiling of colliery spoil tips; removal of coal workings and mine entries; and provision of surface drainage. The project will create a sloping landform to reproduce semi-natural habitats on the site, and hence prepare the area ground for future mixed-use development.
Malpaís de Güímar on Tenerife, Canary Islands Malpaís is a term used in the Southwestern United States, Spain, Mexico, and other Spanish-speaking regions for a rough and barren landscape that consists of relict and largely uneroded lava fields exhibiting recognizable lava flows, volcanic cones, and other volcanic landforms. This type of volcanic landscape is extremely rough and difficult to traverse. It is characteristic of an arid environment because in more humid climates, lava fields are quickly destroyed by weathering and erosion. While the term describes many xeric places, it is strongly associated with Spanish-speaking countries and the Southwestern United States, where Spanish settlers named this landform.
The Baltic Klint in Ida-Viru County, Estonia The Baltic Klint (Clint, Glint; , , ) is an erosional limestone escarpment and cuesta on several islands of the Baltic Sea, in Estonia, in Leningrad Oblast of Russia and in the islands of Gotland and Öland of Sweden. It was featured on the reverse of the 50 krooni note of 1928 and on the 100 krooni note of 1992. The Baltic Klint is active landform showing some retreat in the present. However it is not known to which degree the Baltic Klint originated in postglacial time or if it evolved from cliff-like forms sculpted by the Fennoscandian Ice Sheet.
Signal Hill, viewed from the south, across Otago Harbour. Logan Point quarry is visible to the left, and the suburb of Ravensbourne to the right The view looking south across central Dunedin and the head of the Otago Harbour, from the New Zealand Centennial monument on Signal Hill Signal Hill (Maori: Te Pahuri o te Rangipohika) is a prominent landform in the city of Dunedin, New Zealand. It is located close to, and due north of, the head of the Otago Harbour and reaches an elevation of 393 m (1289 ft). The suburbs Ravensbourne, St. Leonards, and Opoho lie on its southern, eastern, and northwestern flanks, respectively.
In geological terms, it is a very young mountain as the granodiorite cooled and hardened only about 10 million years ago. The present landform is considered to be a mid-Pliocene peneplain, arched and deeply dissected, through which the Kinabalu granodiorite body has risen in isostatic adjustment. It is still pushing up at the rate of 5 mm per annum. During the Pleistocene Epoch of about 100,000 years ago, the massive mountain was covered by huge sheets of ice and glaciers which flowed down its slopes, scouring its surface in the process and creating the deep Low's Gully (named after Hugh Low) on its north side.
The Yunnu hill, iconic among the Wuyi Mountains. The region is part of the Cathaysian fold system and has experienced high volcanic activity and the formation of large fault structures, which were subsequently subject to erosion by water and weathering. The landscape is characterized by beautiful winding river valleys flanked by columnar or dome-shaped cliffs as well as cave systems. Peaks in the western portion of the Wuyi Mountains typically consist of volcanic or plutonic rocks, whereas peaks and hills in the eastern area are made up of red sandstone (particularly in the east) with very steep slopes but flat tops (Danxia landform).
The first major fire, set in 1800 to clear the lower slopes for pasture, swept through the stands of virgin red spruce on the summit and flanks of the mountain. Between 1810 and 1820, local farmers, who believed that wolves were denning in the blowdowns, set fire to the mountain again. The conflagration raged for weeks, destroying the topsoil and denuding the mountain above . The term "monadnock" is used by American geologists to describe any isolated mountain formed from the exposure of a harder rock as a result of the erosion of a softer one once surrounding it (a landform termed "inselberg" ["island-peak"] elsewhere in the world).
The CDP is named for Point Possession, a landform on the northwest side of the Kenai Peninsula that marks the southern side of the mouth of Turnagain Arm into Cook Inlet. The CDP extends from the point southwest along the shore of Cook Inlet to the mouth of the Swanson River, across which is the CDP of Nikiski. The Kenai Spur Highway enters the Point Possession CDP at the Swanson River and shortly dead-ends while still within the Captain Cook State Recreation Area; it leads southwest to the city of Kenai. The rest of the CDP is accessible only via four-wheel-drive roads.
Mining there stopped in 2004, and the pit was converted into the Pegswood Community Park, which includes "a dedicated nature reserve, a new woodland and ponds." The second phase of the park's construction would also "provide a fishing lake, an amphitheatre sculpted out of the landform and a footpath link from Pegswood to Morpeth." Extensive open- pit mining still takes place in the area, but such operations remain controversial even when former sites are restored. Like many other "former pit villages," Pegswood has benefited from increased interest among especially young families, who are attracted to such places for the countryside and the quality of education.
The following year climatic geomorphology was criticized in a 1969 review article by process geomorphologist D.R. Stoddart. The criticism by Stoddart proved "devastating" sparking a decline in the popularity of climatic geomorphology in the late 20th century. Stoddart criticized climatic geomorphology for applying supposedly "trivial" methodologies in establishing landform differences between morphoclimatic zones, being linked to Davisian geomorphology and by allegedly neglecting the fact that physical laws governing processes are the same across the globe. In addition some conceptions of climatic geomorphology, like that which holds that chemical weathering is more rapid in tropical climates than in cold climates proved to not be straightforwardly true.
The Gulf of Tehuantepec is located on the Pacific coast of southern Mexico Gulf of Tehuantepec () is a large body of water on the Pacific coast of the Isthmus of Tehuantepec, southeastern Mexico, at . Many (but not all) Pacific hurricanes form in or near this body of water. A strong, gale-force wind called the Tehuano periodically blows out over the waters of the Gulf of Tehuantepec, inducing strong upwelling of nutrient-rich waters which support abundant sea life. The gulf is in the path of the lowest landform between Mexico and Northern Central America, allowing unhindered wind passage from the Gulf of Mexico, and the Eastern Pacific Ocean.
Sierra de Manantlán. UNESCO - MAB Biosphere Reserves Directory Ecological characteristics The Reserva de la Biosfera Manantlan is located to the extreme north of the inter-tropical zone. The climate in the region is influenced by various factors in addition to its latitude, such as its proximity to the coast, the effect of its landform – orographic shade – and the breadth of the altitudinal range, which partly goes to explain the high regional biodiversity and the presence of numerous plant formations ranging from tropical forests to those of temperate-cold climates. The Reserva de la Biosfera Manantlan's varied and complex plant cover harbours a great wealth of flora.
The mountain rainforests of the ecoregion have a cooler climate than the Congolian lowland forests or the savanna of Uganda, Rwanda and Burundi, and therefore are home to a rich variety of Afromontane flora and especially fauna. The Albertine Rift montane forests are included on the Global 200 conservation list. The rare mountain gorilla (Gorilla beringei beringei) survives only in this ecoregion as do the L'Hoest's monkey, and a subspecies of the Hamlyn's monkey − as well as many endemic species of butterflies and birds including: Grauer's warblers, Chapin's flycatchers, and the Rwenzori turaco. The Lendu Plateau clawed frog is endemic to that landform in the ecoregion.
This long-meandering landform generally proved to be an inhospitable transportation barrier for thousands of years for past indigenous cultures. However, a natural break in this escarpment in the precise area that would become Ancaster village had for millennia created an opportunity for people to traverse up and down the escarpment providing a relatively easy navigable land transportation gateway from the head of the lake to the surrounding land on the escarpment and vice versa.Ancaster, A Glimpse into the Past, Ancaster Information Centre and Community Services. Andrew J.L. Barton, 1993 Ancaster Village circa 1927-32 Ancaster is the most westerly portion of the Golden Horseshoe conurbation of southern Ontario.
The outstanding feature of the mountain is the L-shaped glacial cwm which faces to the northeast. Its modern form is considered to be the result of a complex history of both glacial action and rock-slope failure, a portion of the west wall having collapsed after the main part of the last ice age. Some of the debris was re-worked during the Loch Lomond Stadial and parts stretch as far as the A470 road.Richard Shakesby, Classic Landforms of the Brecon Beacons, 2002, Geological Association Landform Guides series no 13 The rocks exposed in the main crag are Senni Beds of Devonian Old Red Sandstone, topped with Brownstones.
The Table, a tuya in British Columbia. Some researchers have attempted to analogize Ganges Mensa to the tuyas of British Columbia, which are thought to have formed as a result of subglacial volcanic activity. The Ganges Mensa province and other interior layered deposits in Valles Marineris have been strongly analogized to the Azas Plateau, a region in the Tuva Republic (a federal subject of Russia) near Lake Baikal and the Mongolian border. The Azas Plateau volcanic field is thought to have formed through subglacial volcanism; that mechanism is used accordingly to interpret the geomorphology of Ganges Mensa, which has been analogized to a terrestrial landform known as a tuya.
Layout of Sonoma Raceway, the track where the race was held. Sonoma Raceway, formerly Sears Point Raceway and Infineon Raceway is a road course and drag strip located on the landform known as Sears Point in the southern Sonoma Mountains in Sonoma, California, USA. The road course features 12 turns on a hilly course with of total elevation change. It is host to one of only three Monster Energy NASCAR Cup Series races each year that are run on road courses (the others being Watkins Glen International in Watkins Glen, New York and the road course layout for the Bank of America 500 at Charlotte Motor Speedway).
South Jersey is a peninsula, bordered by the Atlantic Ocean to the southeast, the Delaware Bay to the southwest, and the Delaware River to the northwest. All of South Jersey is part of the Atlantic Coastal Plain, a landform of broad plains and gently sloping hills that extends southward from the New York Bight to Florida. Much of the Atlantic Coastal Plain is covered by pine and oak-pine forests and salt marshes and is underlain by poorly consolidated sedimentary formations from the Cretaceous, Tertiary, and Quaternary age that dip seaward. The Atlantic Coastal Plain can be divided into three physiographic subprovinces: the Inner Lowlands, Outer Lowlands, and Central Uplands.
In the idealistic figure of Grey, Balch offers an outsider's perspective on the Northwest Pacific native culture, which the missionary views with mixed emotions. Early in the narrative Balch creates a scene that illustrates the romance's worldview, in which physical matter, unseen spirit, and human minds are subtly intertwined. While still in his New England village, Grey experiences a waking vision in which he sees throngs of Indians crossing a massive natural bridge arching over an unknown western river. The landform unveiled in this epiphany becomes the object of Grey's quest as he traverses the wilderness of North America.Balch, The Bridge of the Gods: A Romance of Indian Oregon, p. 36.
The Peace River as it winds past the town. Physiographically, the Town of Peace River lies within the Peace River Formation, a stratigraphical unit of middle Albian age in the Western Canadian Sedimentary Basin. The area developed on sediments of the former lake bottom of Glacial Lake Peace, which covered most of the areas in the region that were below 610 m in elevation.A. James Morgan, Roger C. Paulen, and Corey R. Froese The specific landform in which the town is situated is the Peace River Lowland which was incised by the Peace River and its tributaries right through the area's former glacial lake sediments and into the Cretaceous bedrock.
The Palos Verdes Peninsula (from Spanish Palos Verdes "Green sticks") is a landform and a geographic sub-region of the Los Angeles metropolitan area, within southwestern Los Angeles County in the U.S. state of California. Located in the South Bay region, the peninsula contains a group of affluent cities in the Palos Verdes Hills, including Palos Verdes Estates, Rancho Palos Verdes, Rolling Hills and Rolling Hills Estates. The South Bay city of Torrance borders the peninsula on the north, the Pacific Ocean is on the west and south, and the Port of Los Angeles is east. As of the 2010 Census, the population of the Palos Verdes Peninsula is 65,008.
Very good examples of this type of volcano can be seen in Iceland, however, there are also tuyas in British Columbia. The origin of the term comes from Tuya Butte, which is one of the several tuyas in the area of the Tuya River and Tuya Range in northern British Columbia. Tuya Butte was the first such landform analyzed and so its name has entered the geological literature for this kind of volcanic formation. The Tuya Mountains Provincial Park was recently established to protect this unusual landscape, which lies north of Tuya Lake and south of the Jennings River near the boundary with the Yukon Territory.
The construction of the form is aesthetically pleasing for its close relationship and integration with the natural island landform with the built form. The visible built work provides an indication of the massiveness of the concealed construction. It is a nationally representative example of the corpus of significant designers of fortifications – Jervoise and Scratchley, a regionally representative example that demonstrates fortification design in the late 19th century, and regionally representative as an example in the evolution of the design of coastal fortifications. The place has a strong or special association with a particular community or cultural group in New South Wales for social, cultural or spiritual reasons.
View of Arana Creek from Arana Gulch Bridge; the creek flows under the bridge and into the Santa Cruz Small Craft Harbor. View of Arana Creek and its floodplain from the Arana Loop hiking trail Arana Gulch is a creek and landform that forms part of the southeastern boundary of the city of Santa Cruz, California. The creek begins in the Santa Cruz Mountains and flows southwest into Monterey Bay into what was once called Woods Lagoon, now the Santa Cruz Small Craft Harbor. Hiking trail on Arana Gulch area Arana Gulch is named after José Arana, who came to Alta California in 1834 with the Hijar- Padres colonization group.
A lava bench is a volcanic landform with a horizontal surface raised above the level of the surrounding area. The Hawaiian islands are an example of land that was formed this way, and the Big Island is currently still expanding due to lava benches. The Kilauea Volcano releases lava that flows down the slope of the volcano and eventually encounters the ocean; this lava flow hardens when it comes into contact with the significantly cooler water of the ocean and forms an unstable lava bench. Eventually, when the material beneath the lava bench stabilizes, it becomes stable land that has been added to the island.
A hillock or knoll is a small hill,The Free Dictionary, "hillock" entry, retrieved December 18, 2007 usually separated from a larger group of hills such as a range. Hillocks are similar in their distribution and size to small mesas or buttes. The term is largely a British one. This particular formation occurs often in Great Britain and China. A similar type of landform in the Scandinavian countries goes by the name ”kulle” or ”bakke” (depending on the country) and is contrary to the above phenomena formed when glaciers polish down hard, crystalline bedrock of gneiss or granites, leaving a rounded rocky hillock with sparse vegetation.
Hill 40 is a militarily historic landform on the island of Guam. It is located about east of Bangi Point, south of Agat on the island's west coast, rising to a height of above the coastal plain, with a strategically significant view of the Agat Invasion Beach. This hill was the scene of some of the most intense fighting during the landing phase of the 1944 Battle of Guam as Allied forces sought to establish their beachhead against the defending Japanese forces. The American 4th Marine Regiment of the 1st Provisional Marine Brigade captured Hill 40 on June 21, 1944, the day of the landing.
The map has lost the Great Gulf and the peninsula continues to be too large, but it has merged with the Golden Chersonese as a single landform and bent more towards the east, apparently influenced by Arabic sources. Pietro Coppo's map (1520) is one of the last ones to show the Dragon's Tail. The Portuguese were aware of the peninsula's likely nonexistence by shortly after the fall of Malacca, when Albuquerque acquired a large Javanese map of Southeast Asia. The original was lost aboard the Froll de la Mar shortly afterwards but a tracing by Francisco Rodrigues was sent in its place as part of a letter to the king.
A joint initiative between the City of Toronto and the Toronto Region Conservation Authority (TRCA), the landform project involves the construction of new landforms south of the plant in Ashbridges Bay using the material removed from the DR&CW; tunnelling projects. The new landforms will provide improved sediment and erosion control in Ashbridges Bay, improving boat access and eliminating the need for regular dredging of the Coatsworth Cut area of the bay. Part of the reclaimed lands will also be the site of a new high-rate treatment facility, designed specifically to treat wastewater intercepted from combined sewers by the DR&CW; tunnels. Construction began in 2019 and is expected to conclude in 2025.
Across Bình Dương there are many different topographic regions, including low mountainous terrain with slight undulation, flat plains and alluvial valleys. There are some low mountains, including Châu Thới in Dĩ An and Cậu mountain (also called Lấp Vò) in Dầu Tiếng district and some low hills. Natural effects have created many different types of landform including worn areas, accumulative areas (due to the deposition of corrosive materials in the flow) and some areas that are worn, accumulative and depositional at the same time. This is due to rainfall and the flow affecting the ground, with the effects of wind, temperature, climate, the erosion and collapse due to gravity of the geology.
Homa Mountain, Kenya in 1994 An eruption of Pacaya, Guatemala in 1976 Mt. Banahaw, Luzon, Philippines in 1989 Kelimutu, Flores, Indonesia A complex volcano, also called a compound volcano, is mixed landform consisting of related volcanic centers and their associated lava flows and pyroclastic rock. They may form due to changes in eruptive habit or in the location of the principal vent area on a particular volcano. Stratovolcanoes can also form a large caldera that gets filled in by a lava dome, or else multiple small cinder cones, lava domes and craters may develop on the caldera's rim. Although a comparatively unusual type of volcano, they are widespread in the world and in geologic history.
Sentinel-2 satellite photo The Champlain Valley is the northernmost unit of a landform system known as the Great Appalachian Valley, which stretches between Quebec, Canada, to the north, and Alabama, US, to the south. The Champlain Valley is a physiographic section of the larger Saint Lawrence Valley, which in turn is part of the larger Appalachian physiographic division. Lake Champlain is one of numerous large lakes scattered in an arc through Labrador, in Canada, the northern United States, and the Northwest Territories of Canada. It is the thirteenth largest lake by area in the US. Approximately in area, the lake is long and across at its widest point, and has a maximum depth of approximately .
Howth has an extensive and varied coastline, and there are steep sea cliffs around parts, especially on the north coast. Key points on the coast, clockwise from Sutton, include Cush Point, Claremont Strand, the small headland at Howth village, Balscadden Bay, Kilrock, the Great and Little Baily, Lion's Head, Doldrum Bay, the Needles, Drumleck Point, Red Rock and Sutton Strand. Due to the shape of the landform, and its rocky nature, with thin soil covering, Howth features multiple streams, several fast-running streams, due to hard rock under a thin soil layer. These include the Bloody StreamCoulcour Brook, the Boggeen Stream, and the Offington Stream, and the Whitewater Brook, the Balsaggart Stream, and the Carrickbrack and Santa Sabina Streams.
The landform known as Bethel Island was created between 1859 and 1870 by several men, see the names and survey numbers below. (Source: California State Archives for Land Patent Certificate of Purchase for Swamp and Overflow Surveys Numbers 80, 81, 82, 83, 225, 226, 227 and 250). Alonzo Stone purchased much of the property formerly owned by Warren and Anne Bethell, and the area was briefly referred to as the "Stone Tract" in the 1930s. Prior to this, it was referred to as "Sandmound Ranch", "Sandmound Tract" or "Bethel Tract" and contained an estimated area of , and did not become an island until 1911, when Dutch Slough was dredged eastward to join with Sandmound Slough.
The ability to identify and interpret these journey and directional markers and their related songs, stories and ritual practises is traditionally passed down through generations of Aboriginal people.Hodgetts 2009 Transmission of knowledge is based on factors including age and gender, and was undertaken gradually over the course of a person's life. Ritualised movement through the Calga ACL involves this process of signal interpretation undertaken during travel along the natural pathways created by the terraced sandstone platforms and sloped contour of the land. In addition to providing necessary seclusion of vegetation and landform at key points, the landscape also offers key sightlines across and within the natural amphitheatre and into it from the Peats Road Ridgeline.
Riffle on the Onega River A riffle is a shallow landform in a flowing channel, and it has specific topographic, sedimentary, and hydraulic indicators. These are almost always assessed at a very low discharge compared to the flow that fills the channel (approximately 10–20%), and as a result the water moving over a riffle appears shallow and fast, with a wavy, disturbed water surface. The water's surface over a riffle at low flow also has a much steeper slope than that over other in-channel landforms. Channel sections with a mean water surface slope of roughly 0.1 to 0.5% exhibit riffles, though they can occur in steeper or gentler sloping channels with coarser or finer bed materials, respectively.
The Drakensberg mountains in South Africa are capped by a layer of Karoo basalts about thick, which overlay Clarens formation sandstones. They have long been considered a classic example of a landform created by scarp retreat following continental break-up, with the retreat controlled by an inland drainage divide. However, they have inland-facing scarps as well as seaward-facing scarps, so factors other than continental break-up have contributed to their formation. A 2006 paper argued that surface process models may be inadequate in explaining rates of scarp retreat, which can also be greatly affected by the types of rock encountered as the scarp retreats, and by other factors such as climate, tectonic processes and possibly plant cover.
The 1934 M6.3 Excelsior Mountains earthquake and the 1986 Chalfant Valley event were several smaller earthquakes that have occurred within the gap, and both generated limited surface faulting and some surface cracking in the Volcanic Tableland, which was created .7 million years ago from a major volcanic eruption that also formed the Long Valley Caldera northwest of Bishop. An estimated 500 cubic kilometers of material (tephra) produced in the event covers the northern Owens Valley as a rocky landform. The surface of the layered plateau is known as Bishop Tuff and features fumarole mounds and hundreds of north-south oriented fault scarps, many of which are visible on topographic maps, via aerial photography, and satellite imagery.
The family was originally from Ingatestone, Essex, England which is where their coat of arms originated as well, augmentation by Elizabeth I to John Boddie for service during the naval battle with the Spanish Armada. Their history is noted in Seventeenth Century Isle of Wight County, Virginia Folklore sometimes attributes the naming of the island to the dead "bodies" of drowned sailors that washed up from the ships that ran aground and sank off the Outer Banks in what is now known as the Graveyard of the Atlantic. Inlets frequently open and close along the Outer Banks, making landform naming inconsistent. Bodie Island, when it was an island, extended farther south than it does today.
LaBarge Rock in Chouteau County, Montana (occasionally referred to as La Barge Rock) is a dramatic landform in the shape of a large rock column or pillar, rising 150 feet from waters' edge of the Missouri River. It was named in honor of Captain Joseph LaBarge, a steamboat captain who cruised the Missouri River in the mid nineteenth century. Besides having a striking appearance, LaBarge Rock is located in a picturesque riverside setting which has attracted artists and photographers over two centuries. Access is difficult; the pillar is located at Missouri River BLM mile-mark 56Complete Paddler: A Guidebook for Paddling the Missouri River From The Headwaters to St. Louis, Missouri, David L. Miller, Farcountry Press, 2005, p.
The Sierra de Manantlán Biosphere Reserve is located to the extreme north of the Intertropical Convergence Zone. The climate in the region is influenced by various factors in addition to its latitudinal location, such as its proximity to the coast, the effect of its landform – orographic shade – and the breadth of the altitudinal range, which partly explains the high regional biodiversity and the presence of numerous plant formations ranging from tropical forests to those of temperate-cold climates. The Sierra de Manantlán’s varied and complex plant cover harbours a great wealth of flora. There are over 2900 species of vascular plants belonging to 981 genera (see Plants of the Reserva de la Biosfera Manantlan) for a growing list.
The impact of these ideas can be hinted in the models' employment of the concept of "evolution" rather than "change", implying a predictable direction of landscape and landform change. Davis wrote geography textbooks (such as Elementary Physical Geography (1902)) that described the “races of mankind”, noting that the European as the most advanced, and connects topography and climate to superiority/inferiority of human race which evolved on that continent. On North America, Davis wrote that “inhabitants of this great land were savages who did not know how to develop its riches”. This textbook chapter exemplifies how Davis promulgated theories of scientific racism, and was likely influenced by mentor and colleague Nathaniel Shaler, who published similar views on the subject.
There are many named subranges of all four subgroupings, particularly in the Selkirks and Monashees. The southward extension of the Selkirks, Purcells and Monashees into the United States are reckoned to be part of the Rocky Mountains and the designation Columbia Mountains is not used there (the Purcells, also, go by the name "Percell Mountains" in the United States). The Salish and Cabinet Mountains south of the Kootenai River are essentially part of the same landform, but are officially designated part of the Rocky Mountains in the United States. To the west of the Monashees and Cariboos, there are three intermediary upland areas which are transitional between the mountain ranges and the plateaus flanking the Fraser and Thompson Rivers.
The National Elephant Center is located on in Fellsmere, Florida. The Elephant Center featured on-site housing for staff and two barns for Asian and African elephants, each capable of supporting nine animals. The design called for barns to be connected by a central hub, surrounded by a habitat that can be subdivided depending on the needs of the elephants. The largest area of the Elephant Center was the Central Elephant Meander, a area that consists of multiple landscapes linked by a series of paths and trails. The area introduced landform and habitat elements from the savannahs and woodlands of the elephants’ home ranges, containing waterholes, sand dunes, plants and scattered browse.
Netherfield is a housing estate located opposite Milton Keynes General Hospital, it also has a large shopping district with various shops. The estate was largely designed by Dixon, Jones, Gold and CrossThe architects and architecture of London, p428 Kenneth Allinson around 1971, and is essentially modernist; it comprises several long parallel terraces, designed around the landform so that the roofline remains level: homes towards the top of the slopes are single storey; those at the bottom are three-storey. The choice of prefabricated construction materials was partly a consequence of a shortage of bricks in the UK at the time. Milton Keynes Council has gradually been renovating the estate, adding a pitched roof when funds permit.
This village is situated on a landform known since the mid-17th century as Oak Hill, and one of the seven principal elevations of Newton (the others being Nonantum Hill, Waban Hill, Chestnut Hill, Bald Pate Hill, Institution Hill, and Mount Ida). Oak Hill Park, a post-World War II subdivision of approximately 412 houses was built on a gravel quarry for the returning GIs. The Oak Hill Park development coincided with expansion in housing in various areas of Newton following the war, when underdeveloped land was utilized to create affordable housing for the returning veterans Many of these original post-World War II houses still exist while others have been replaced with newer, usually larger homes.
The Ridge Hill Shelf is a landform that forms part of the foothills of the Darling Scarp, a low escarpment that runs parallel with the west coast in southwest Western Australia. It was formed by coastal erosion of the scarp in the Pleistocene, when the sea level was higher, and the scarp located further west than at present. The action of coastal forces produced sand dunes that subsequently lithified into eolianite, and eroded the ironstone of the scarp, resulting in an iron-rich sandstone with a laterite cap. The iron gives the sandstone a dull purple-brown colour; depending on the extent of iron- enrichment, the sandstone may appear predominantly yellow, predominantly purple-brown, or a mottled combination of the two.
Muldraugh Hill is an escarpment in Bullitt, Hardin, Jefferson, and Nelson counties of central Kentucky separating the Bluegrass on the north and north- east from the Pennyrile on the south and south-west. This escarpment fades into the Pottsville Escarpment on the east, and terminates at the Ohio River in the west, although in truth it continues in Indiana as Floyds Knobs. In parts of its eastern stretches, Muldraugh Hill is little more than a slight hill, but in some of the western areas, it is represented by extensive areas of knobs. This landform consists mostly of siltstones and shales, with some minor limestones, lying between the limestones and dolomites of the older Bluegrass and the limestones of the newer Pennyrile.
The range lies in the northwest of the Arizona transition zone, and at the southwest of the Coconino Plateau, a subsection of the Colorado Plateau. The Aquarius Mountains are on the perimeter of the transition zone, and border the south-flowing Big Sandy River and Valley on its west; adjacent further west is the massif of the Hualapai Mountains, a block faulted Basin and Range landform bordered westwards by the north-south Sacramento Valley. Mohave County and northwest Arizona, is also a southeastwards extension of the Mojave Desert which extends down to Wickenburg, Arizona, on the southwest perimeter of the Arizona transition zone. Joshua trees can be found here, and the route north from Wickenburg, U.S. Route 93 in Arizona is called the Joshua Tree Highway.
Sonoma Raceway, the track where the race was held. Sonoma Raceway, formerly Sears Point Raceway and Infineon Raceway, is a road course and drag strip located on the landform known as Sears Point in the southern Sonoma Mountains in Sonoma, California, USA. The road course features 12 turns on a hilly course with of total elevation change. It is host to one of only two NASCAR Sprint Cup Series races each year that are run on road courses (the other being Watkins Glen International in Watkins Glen, New York), and one of six national series road course races (Xfinity Series racing at Watkins Glen, Mid-Ohio Sports Car Course and Road America; and the Camping World Truck Series at Canadian Tire Motorsport Park).
The flora of Danxia Mountain is mainly composed by the tropical and subtropical flora, but lacks the typical tropical genus, and the amount of the moss is relatively large. The landform of DanXia has significant effects on the growth of plants. Since the mount of DanXia has many deep valleys, grooves, the environment of Danxia is moisture, which in favor of the growth of moss.刘蔚秋 李植华 刘兰芳 丹霞山风景地貌的植物区系研究 1999 年 2 月 Also, The special landscape and the humid monsoon climate permit the growth of evergreen broadleaf forests, endemic plants, endangered and new species such as Danxia Viola, Danxia orchid, Danxia Firmiana and Danxia Chiritopsis.
Geologically, the Prenj range is part of the Dinaric Alps and formed largely of secondary and tertiary sedimentary rock, mostly limestone and dolomite with notable characteristics of a karst landform. Due to subterranean drainage, Prenj is relatively dry with few water sources, just a few tiny lakes and some smaller streams that source from these mountains: the Baščica and the Bijela, tributaries of the Neretva. Notable peaks are Zelena Glava (2115 m), Lupoglav (2102 m), Otiš (2097 m), Herač (2046 m), Osobac (2030 m) and Velika Kapa (2007 m). The Prenj mountains were part of the front line during the 1992–95 war in Bosnia and heavy combat took place in the mountains surrounding the eastern Bijela valley and the slopes above Konjic.
The main lake within the garden The reserve is located between Merrylands Road, Paton Street and the Cumberland Highway in Merrylands. The park's landform is made up of two main topographic regions — The northern half slopes gently from Merrylands Road towards the system of lakes in the centre of the park, whilst the section of park's south of the lakes is largely flat, with a small localised rise in elevation opposite of Paton St. Water is pumped from the main lake to an outlet near the Cumberland Highway. The quality of the lake is rather poor. Factors include silt laden runoff entering from adjacent areas, shallow waters, presence of marine animals and lack of reliable water supply to fill the lakes up during dry periods.
A montane meadow (polonyna) in the Ukrainian Carpathians A montane meadow (polonyna) in Bieszczady Mountains, Poland Polonyna (; ; , ; ; ) is a specific, regionally-focused geographic term, that is used as a designation for areas of montane meadows (a landform type) in the upper subalpine or alpine zones of the Carpathian Mountains. The term polonyna was introduced to English from Slavic languages, in order to designate various mountainous regions, mainly in the Eastern Carpathians, and also in the Western Carpathians. The polonyna type areas of montane meadows are very frequent in the Outer Eastern Carpathians, particularly in the Eastern Beskids. Throughout history, they were used for pasture, and in modern times they have become a popular destination for various forms of recreational tourism.
The Feather Canyon (or Feather River Canyon) is a landform in the Feather Headwaters between Pulga, California (west) and Keddie, California (east) along portions of the North Fork Feather River (west & downstream) and the East Branch North Fork Feather River (east & upstream). The canyon is the location of portions of California State Route 70 and the Feather River Route, including the Tobin Bridges. The Feather River Canyon, where the Camp Fire (2018) disaster began, is well-known for high winds. The so-called "Jarbo Gap winds" down the canyon from the northeast every fall are caused by high- pressure air over the Great Basin seeking a path through the Sierra Nevada to the low-pressure voids on the California coast.
Bintan, is the largest among the 3,200 islands of Riau Archipelago and is located east of the Batam Island. It has a coast line of and has rolling topography in its landform. The Riau Islands are a province of Indonesia, which encompassed the Riau Archipelago, Natuna Islands, Anambas, and Lingga Islands; in July 2004 the islands of Riau were divided from the existing Riau Province to form the new province with its capital at Tanjung Pinang. The archipelagos of Anambas and Natuna, located between mainland Malaysia and Borneo, are now part of this province Map of Bintan In the Tanjung Pinang city, the low tide reach or the mud flat part was built with stilts and were mosquito and rat infested.
An ingression coast, the Archipelago Sea off Naantali (Finland) An ingression coast or depressed coast is a generally level coastline that is shaped by the penetration of the sea as a result of crustal movements or a rise in the sea level. Such coasts are characterised by a subaerially formed relief that has previously experienced little deformation by littoral (tidal) processes, because the sea level, which had fallen by more than 100 metres during the last glacial period, did not reach its current level until about 6,000 years ago. Depending on the geomorphological shaping of the flooded landform – e. g. glacially or fluvially formed relief – various types of ingression coast emerge, such as rias, skerry and fjard coasts as well as förde and bodden coasts.
Kerala agro- ecological zones map Angadipuram is situated in the Malappuram district, which lies in northern Kerala, and is bounded on the north by Wayanad and Kozhikkode districts, on the northeast by Tamil Nadu, on the southeast and south by Palakkad District, on the southwest by Thrissur District, on the west by the Arabian Sea, and on the northwest by Kozhikode District (see Kerala eco zones map). The geographical distribution of laterite is not limited to Angadipuram in Malappuram district but it is also found in the midland regions and highlands of Kerala. Its occurrence extends to Aleppey, Quilon, Thiruvananthapuram, Kottayam, Trichur and Cannanore districts. Overall, in the landform of Kerala which has seven landscape ecological zones, laterites account for a major share of 50%.
The presence of ring-mold craters on the debris apron further supported the hypothesis that these geomorphological features are likely pure ice overlain by a very thin debris cover. A landform in the Phlegra Montes interpreted by some researchers to be eskers formed by the retreat of the glacial structure that produced its associated lineated valley fill. HiRISE. Image is across in the horizontal direction. In 2014, German researchers Stephan van Gasselt, Julia Schulz, and Csilla Orgel (Free University of Berlin) submitted abstracts to the European Geosciences Union General Assembly meeting in Vienna and the European Planetary Science Congress in Cascais, Portugal, tied to their work mapping the spatial distribution of and updating crater age dates on lobate debris aprons in the Phlegra Montes region.
Grovers Cliff is a shoreline escarpment at Broad Sound near the Port of Boston and by extension, the landform extending into the sea (headland) that is the "Highlands" section of Winthrop, Massachusetts. The headland is at the north end of Winthrop Beach and is noted for an 1847 survey station, WWI & II fortifications and a Cold War nuclear bunker used by the US Army, USCG, USN, USAF, and FAA as Fort Heath, the eponym of the landform's current apartment complex. A northern area of the headland is the municipal Small Park and the remainder is primarily the Fort Heath Apartments. Streets include Highland Avenue and Pond Street which had been constructed by the 1930s at the perimeter of Fort Heath.
It is still possible to appreciate the siting of the homestead in view of, and with frontage to, the Nepean River as part of the original land grant. The mid-19th century Southern Railway, though sited close to the homestead group, was constructed to maintain this visual relationship. The siting of the homestead group in a context of undulating landform, is an outstanding example of colonial landscape planning to form a picturesque composition with direct sightlines to the neighbouring Camden Park estate and the Great Dividing Range. The Glenlee homestead group is a rare and significant complex of buildings and plantings, approached by a formal drive and sited with commanding views over the countryside to the west and south-west.
The relatively resistant chalk rock has, through weathering, resulted in a classic cuesta landform, with a northward-facing chalk escarpment that rises dramatically above the low-lying vales of the Low Weald. The chalk escarpment reaches the English Channel west of Eastbourne, where it forms the dramatic white cliffs of Beachy Head, the Seven Sisters and Seaford Head. These cliffs were formed after the end of the last Ice Age, when sea levels rose and the English Channel was formed, resulting in under-cutting of the chalk by the sea. The South Downs run linearly west-north-westwards from the Eastbourne area through southern Sussex to the Hampshire downs, separating the south coastal plain from the clays and sandstones of the Weald.
For example, the function f(x,y) = x^2 + y^3 has a critical point at (0, 0) that is a saddle point since it is neither a relative maximum nor relative minimum, but it does not have a relative maximum or relative minimum in the y-direction. The name derives from the fact that the prototypical example in two dimensions is a surface that curves up in one direction, and curves down in a different direction, resembling a riding saddle or a mountain pass between two peaks forming a landform saddle. In terms of contour lines, a saddle point in two dimensions gives rise to a contour graph or trace in which the contour corresponding to the saddle point's value appears to intersect itself.
Guest musician Robin Hayes played cello on the third release landform(2008), the first time a guest musician had appeared on a computerchemist solo album. Uwe Cremer, otherwise known as Level Pi, was the guest musician on the fourth album, aqual measure(2009), and played guitar on the title track. A collaboration project started in July 2010 between Computerchemist and "Nemesis", ex-Hawkwind dancer and singer has produced several tracks, some of which were initially released for free under Creative Commons licensing which had been available on the computerchemist website for free download, with a full album promised at a later date entitled Chronicles of Future Present. The link as of August 2011 to this project is no longer active.
Cape Point in the left foreground, with the Cape of Good Hope almost right behind and some 2.3 km away Looking from behind the old lighthouse (at top left) to the new lighthouse (a sunlit speck of white very near the point). The lighthouses are 700 metres apart, and the new lighthouse 162 metres lower in altitude so as to remain visible during low cloud. Cape Point () is a promontory at the southeast corner of the Cape Peninsula, which is a mountainous and scenic landform that runs north-south for about thirty kilometres at the extreme southwestern tip of the African continent in the Republic of South Africa. Table Mountain and the city of Cape Town are close to the northern extremity of the same peninsula.
Both men are remembered upon a marble tablet installed at the Mechanics' Hall (The Bairnsdale Library). The Mitchell Delta is represented as a type-L under the Ramsar wetland type classification framework, which means that it is a permanent inland delta. The Mitchell Delta is a classic form of digitate delta (from Latin digitātus, having finger or toes) and is located near the western shoreline of Lake King at Eagle Point Bluff, extending into the lake as silt jetties formed by alluvial deposition of sediment. The Mitchell Delta represents one of the finest examples of this type of landform in the world and is a site deemed of international geomorphological significance and is one of the finest examples of a classic digitate delta in the world.
Its geographical components are the Bulkley Valley, the northern part of the Nechako Country, and the Omineca Country, including portions of the Hazelton Mountains and Omineca Mountains in the west and north of the regional district, respectively. The dominant landform is the Nechako Plateau. Neighbouring regional districts are the Kitimat-Stikine, Central Coast, Cariboo, Fraser-Fort George, and Peace River Regional Districts; on its north the boundary with the southern edge of the remote Stikine Region is separated from the Bulkley-Nechako Regional District by the 56th parallel north. The boundaries of the regional district near- entirely coincide with the territory of the Dakelh or Carrier peoples, and also some of that of the Dunneza (Beaver), but their reserves and governments lie outside the regional district system.
As the tides ebbed the land was gradually revealed and the peoples living in the area built ponds to block the tide and enclosed the sea area to set up land and improve the landscape. The regional landform of Beilun district is mainly characterized by hills and plains in the northwest and the middle, and hills in the southeast. It was separated by the Lingfeng mountain, thus, west of the mountain is the Changshan plain and east of the mountain is the Chaiqiao plain. The area is intertwined with water sources such as the Xiaolijiang, Yan, Tai, and Lujiang rivers, which originate from the southwest Shan 'ao, a piece of flat land in a mountain range, and flow through two plains.
However, owing to the containerization revolution of the 1960s, cargo traffic began to shift to East Coast ports, and shipping volumes in Toronto fell by almost half between 1969 and 1973. Thus, the need for an outer harbour never arose, and all cargo ships calling at Toronto still use the Inner Harbour, while the Outer Harbour sees only pleasure boat traffic. While the original need for the landform was eliminated, the site continued to receive excavation and construction waste from the building of Toronto's subways, office towers and other large projects. In the late 1970s, dredgeate from the nearby Keating Channel was also dumped on the emerging spit, which was seen as a better solution than dumping the polluted material into open water.
Goat Rock Beach Goat Rock Beach is a sand beach in northwestern Sonoma County, California, United States. This landform is a sub-unit of Sonoma Coast State Beach, owned and managed by the State of California. At the northern terminus of Goat Rock Beach is the mouth of the Russian River, and the southern end of this crescent shaped expanse is the massive Goat Rock, an iconic outcrop of the Sonoma Coast, which is barely attached to the mainland by a narrow isthmus. Goat Rock Beach is frequented by beachcombing visitors, but usually not in high numbers, except in mid-summer; there is some wading and surfing activity, although these uses are moderated by the rip current generated by a steep gradient into the water that leads to an underwater trench parallel to the waterline.
The hills are an outcrop of Precambrian bedrock, unique in the city of Ottawa, which otherwise is relatively flat. Its geology is complex, consisting of gneiss, granite, and marble substrates, and it supports a number of vegetation- landform ecologies, such as mature deciduous and mixed highland forest and mixed and coniferous lowland forest, which are rare in the area and southeastern Ontario. Typical to Canadian Shield, it has rolling terrain with highly irregular drainage and a thin soil cover with barren vegetation. A section of the hills, the Carp Barrens, spread along both sides of Thomas Dolan Parkway, is characterized by the "most extensive, best-expressed complex of granite bedrock barrens", not only on the Carp Ridge, but also in southern Ontario east of the Thousand Islands – Frontenac Arch.
Stephenson Nunatak () is a prominent, pyramid-shaped rock nunatak, rising to about 640 m, which rises 300 m above the surrounding ice at the northwest side of Kirwan Inlet in the southeast part of Alexander Island, Antarctica. Discovered and roughly surveyed in 1940-41 by Finn Ronne and Carl R. Eklund of the United States Antarctic Service. Resurveyed in 1949 by the Falkland Islands Dependencies Survey and named by the United Kingdom Antarctic Place- Names Committee for Alfred Stephenson, surveyor with the British Graham Land Expedition, who led a sledge party south into George VI Sound to about 72S in 1936. There happens to be another landform on Alexander Island which is named after Alfred Stephenson, that being Mount Stephenson, the highest point of Alexander Island rising to 2,987 m.
The Nanling (), also known as the Wuling (), is a major mountain range in Southern China that separates the Pearl River Basin from the Yangtze Valley and serves as the dividing line between south and central subtropical zones. The main range of Nanling Mountains stretch west to east about from Guilin and Hezhou of the eastern Guangxi to Ganzhou of the southern Jiangxi, north to south about from Yongzhou and Chenzhou of the southern Hunan to Qingyuan and Shaoguan of the northern Guangdong; With its branches, the whole mountains run west to east . There are trough basins in the Nanling, the most of the western basins in Nanling Mountains are composed of limestone, where karst regions are located. the most of the eastern basins are made up of red sandstone, where are danxia landform areas.
Eighty-one species of non-flying mammals were trapped at cross-river sites along the Juará River in another experiment. The river seemed to be a barrier for only a few taxa, with the majority either homogeneous throughout the research area or divided into monophyletic upriver and downriver clades. Patton argues that the geographic location of these clades suggest that landform evolution is an underappreciated factor in diversification in Amazonia. This project further suggests that riverine barriers are not the only mechanism for speciation.Patton, James L.; Da Silva, Maria Nazareth F.; Malcolm, Jay R. “Mammals of the Rio Juruá and the evolutionary and ecological diversification of Amazonia.” Bulletin of the American Museum of Natural History 244 (2000): 1-306 All these critics argue that other factors influence speciation in Amazonia.
The sky island concept originated in 1943 when Natt N. Dodge, in an article in Arizona Highways magazine, referred to the Chiricahua Mountains in southeastern Arizona as a "mountain island in a desert sea". In about the same era, the term was used to refer to high alpine, unglaciated, ancient topographic landform surfaces on the crest of the Sierra Nevada, California. The term was popularized by nature writer Weldon Heald, a resident of southeastern Arizona. In his 1967 book, Sky Island, he demonstrated the concept by describing a drive from the town of Rodeo, New Mexico, in the western Chihuahuan desert, to a peak in the Chiricahua Mountains, away and higher in elevation, ascending from the hot, arid desert, to grasslands, then to oak-pine woodland, pine forest, and finally to spruce-fir-aspen forest.
Some upland forests within the state lands are very mature in character, but these experienced timber harvesting in the 19th century and light management cutting by the state in the 1970s and 1980s. Zoar Valley's old growth is primarily deciduous, and varies in character and species composition depending upon location and landform characteristics. Northern hardwood stands, including eastern hemlock, sugar maple, American beech, yellow birch, northern red oak, and tulip tree, are widespread, especially on mesic north-facing slopes and on the lower reaches of south-facing slopes. Similar stands are found on the raised terraces within the canyon, where old- growth trees have been noted to achieve great size, both in terms of height and diameter (typically expressed as diameter at breast height [DBH], a standard measurement taken above the tree's base).
Researchers have identified two, three, four, or five stratigraphic units on the mesa that are most conspicuously defined by the presence, distribution, and length of long erosional flutes (interpreted by many researchers as yardangs and, historically, possibly as the result of groundwater sapping), and thematically consistent features of differing albedo. Yardangs are fleets of elongated linear features cut from bedrock by winds that blow in a sustained direction, surficially covering vast swaths of the mesa. These landforms are generally hundreds of meters long and tens of meters high, but they have been observed to become much larger on the northern face of Ganges Mensa. The mesa's southwestern face is steeper and contains the most well-incised examples of yardangs on the landform, suggesting that wind erosion was most severe on this part of the mesa.
A shingle beach in Batanes, Philippines Pebbles on a shingle beach in Somerset, England A shingle beach (also referred to as rocky beach or pebble beach) is a beach which is armoured with pebbles or small- to medium-sized cobbles (as opposed to fine sand). Typically, the stone composition may grade from characteristic sizes ranging from diameter. Torrisdale Bay, Argyll and Bute, Scotland While this beach landform is most commonly found in Europe, examples are found in Bahrain, North America and in a number of other world regions, such as the east coast of New Zealand's South Island, where they are associated with the shingle fans of braided rivers. Though created at shorelines, post-glacial rebound can raise shingle beaches as high as above sea level, at the High Coast in Sweden.
The origin of the term comes from Tuya Butte, one of many tuyas in the area of the Tuya River and Tuya Range in far northern British Columbia, Canada. While still in graduate school in 1947, Canadian geologist Bill Mathews published a paper titled, "Tuyas, Flat-Topped Volcanoes in Northern British Columbia", in which he coined the term "tuya" to refer to these distinctive volcanic formations. Tuya Butte is a near-ideal specimen of the type, the first such landform analyzed in the geological literature, and this name has since become standard worldwide among volcanologists in referring to and writing about these formations. Tuya Mountains Provincial Park was recently established to protect this unusual landscape, which lies north of Tuya Lake and south of the Jennings River near the boundary with Yukon.
A kame near Kirriemuir, Scotland A kame in Yellowstone National Park, Wyoming A kame among the glacial drift on the terminal moraine of the Okanagan Lobe of the Cordilleran Ice Sheet on the Waterville Plateau of the Columbia Plateau in Washington A kame is a glacial landform, an irregularly shaped hill or mound composed of sand, gravel and till that accumulates in a depression on a retreating glacier, and is then deposited on the land surface with further melting of the glacier. Kames are often associated with kettles, and this is referred to as kame and kettle topography. The word kame is a variant of comb (kame, or kaim is the Old Scottish word for comb), which has the meaning "crest" among others. The geological term was introduced by Thomas Jamieson in 1874.
Lake Mapourika, New Zealand A lake (from Latin word lacus) is a terrain feature (or physical feature), a body of liquid on the surface of a world that is localized to the bottom of basin (another type of landform or terrain feature; that is, it is not global) and moves slowly if it moves at all. On Earth, a body of water is considered a lake when it is inland, not part of the ocean, is larger and deeper than a pond, and is fed by a river. The only world other than Earth known to harbor lakes is Titan, Saturn's largest moon, which has lakes of ethane, most likely mixed with methane. It is not known if Titan's lakes are fed by rivers, though Titan's surface is carved by numerous river beds.
Analytical and numerical models that solve the diffusion equation for different initial and boundary conditions have been popular for studying a wide variety of changes to the Earth's surface. Diffusion has been used extensively in erosion studies of hillslope retreat, bluff erosion, fault scarp degradation, wave-cut terrace/shoreline retreat, alluvial channel incision, coastal shelf retreat, and delta progradation. Although the Earth's surface is not literally diffusing in many of these cases, the process of diffusion effectively mimics the holistic changes that occur over decades to millennia. Diffusion models may also be used to solve inverse boundary value problems in which some information about the depositional environment is known from paleoenvironmental reconstruction and the diffusion equation is used to figure out the sediment influx and time series of landform changes.
Murray and others (1975) proposed that Mercury's history could be divided into five periods: (1) accretion and differentiation, (2) “terminal heavy bombardment,” (3) formation of the Caloris basin (centered off map sheet at lat 30° N., long 195° ; U.S. Geological Survey, 1979), (4) filling of the large basins by “smooth plains,” and (5) a period of light impact cratering. Although these divisions have withstood well the assessments of subsequent investigators, they do not define a stratigraphy. Because the geologic map of the Bach region constitutes a synthesis of observation with interpretation, we shall explore several aspects of the region's geologic development. The history of the region begins prior to the formation of any presently visible surface, when Mercury's internal evolution played a key role in determining subsequent landform development.
Being the western boundary of the Sonoran Desert, the eastern mountainslopes are hotter and drier, while the western side is affected by the Pacific Ocean and receives more precipitation with cooler temperatures. There are several major vegetation areas ranging from sand dunes/sand fields, chaparral, and mesquite to riparian zones of willow and cottonwood, desert fan palm oasis woodland, and pinyon pine woodland, with the highest elevations supporting lodgepole pine timberline forest. Another factor influencing plant and animal species is the "island" aspect of the San Jacinto Mountains and the Peninsular Range, the unique isolation of the landform on three sides-the Pacific Ocean to the west, the Salton Trough/desert environment to the east, and the San Gorgonio Pass to the north. Biologists believe that this isolation has contributed to evolution of subspecies such as the San Diego mountain kingsnake.
Akto County is located in the three major geographic regions of the Pamirs, the northern slopes of the Kunlun Mountains and the oasis on the western edge of the Tarim Basin. The landform is dominated by mountains, with the mountainous area accounting for 96.39% of the total area of the county, and the mountainous areas generally at an altitude of 4,000-5,000 meters. The Kungay Mountain () in the northwest is the boundary mountain of the county with Wuqia County, with an elevation of 5,753.7 meters. The Sarikol Range () in the southwest is more than 4,500 meters above sea level; the highest peak of Kongur Tagh () in the central part is 7,719 meters above sea level, the peak of Kongur Tiube () is 7,530 meters high above sea level, and the peak of Muztagh Ata () is 7,541 meters high.
It is also possibly the only remnant of the natural landform of the original foreshores of Sydney Cove which has survived relatively unchanged over two centuries of European settlement, and can therefore symbolise the first place of meeting between Aboriginal people and British settlers at Sydney Cove in 1788. Macquarie Obelisk is the oldest surviving milestone built to mark the place from which all public roads in the Colony were to be measured, and is the second oldest known European monument in Australia. Macquarie Place is the oldest urban park in Australia, together with Hyde Park, and has been in continuous use as a public space for over 190 years. Both Macquarie Place and the Obelisk were constructed less than 30 years after the arrival of the First Fleet near the original shores of Sydney Cove and First Government House.
The Banks Group and Blagdon estate developed and sponsored the construction of Northumberlandia, or the Lady of the North, a huge land sculpture in the shape of a reclining female figure, which was part- commissioned and sponsored by Ridley. Now run by a charity group called the Land Trust, it is the largest landform in the world depicting the human form, and, through private funding, cost £3m to build. Attracting over 100,000 people per year, the Northumberland art project, tourism and cultural landmark has won a global landscape architecture award, and has been named 'Miss World'. The Royal Agricultural Society of England awarded the Bledisloe Gold Medal in 2015 to Ridley for the work done on his Blagdon estate, saying that it "wanted to highlight the extensive environmental improvement work that has been undertaken across the land".
The remnant cultural landscape has many features of individual significance such as the original cottage, early homestead, garden, entry drive from the old Cowpastures Road (Camden Valley Way), the 1957 garden studio and the remaining estate area. Historically the quintessential landscape character – based on the traditional juxtaposition of homestead area, with its dominant garden, and cleared pastureland beyond – represented one of the best examples of this intentional contrast as well as the siting of a homestead group on a landform summit in the Cumberland Plain / Camden area. The place currently retains some key historical visual relationships – vistas to Orielton, Studley Park, the spire of St. John's Church, Camden and the Razorback Range. Its historical relationship to other nearby early grants (Orielton & Oran Park) and its place in the development of the local area can still be appreciated.
Round Hill Head is a distinctive granite landform at above sea level, a landmark for mariners as the north west extreme of Hervey Bay and the bluff termination of hills, well covered with wood and grass, sloping down around Round Hill, which is high due south. The headland has naturally grassy areas running from the ocean on the east to the sheltered creek on the west and this swathe has been referred to as "Mrs Cook's Drive" since the turn of the century. Round Hill Creek on the western side of the headland has a very narrow channel, which has maintained its depth at soundings taken since 1770, but is encumbered with shifting sandbanks. The sandy beach is fringed by mangroves and backed by cotton woods, paperbark and palms in the wetter gullies, with ironbark on the drier slopes.
In addition to the obvious elongation of tails and the abstracted nature of many of the shapes, colored silts and sand were often used to decorate the mounds. The land was often scraped or raked to move earth from surface soils towards a new mound and in doing so, artful colored sand and silt patterning was sometimes employed as adornment. In terms of positioning, some mounds may have had celestial alignments although with certainty bird mounds were placed in such a way as to suggest that they were flying up or down a hillside, and animal mounds were often placed so as to suggest animals walking along natural landform as well such as a ridge or hillside. It is possible that predominant wind patterns may have been taken into consideration when choosing locations and orientations for bird mounds.
West Don Lands in 2009, prior to redevelopment Construction at the West Don Lands from Corktown Common in 2013 In 2001, the new Waterfront Toronto agency was commissioned by the federal, provincial and municipal governments to redevelop the Toronto waterfront. It was given the responsibility to take lands owned by either of the three levels of government in the waterfront area and make them available for development, sometimes building infrastructure such as parks or roads to make development possible. A flood protection landform was built to allow development to proceed. In 2006, the agency announced a new plan to create a residential community in the abandoned area. Under the overall plan of the Waterfront Toronto initiative, plans for the area include nearly 6,000 new residential spaces with twenty percent being allocated as 'affordable' or 'subsidized' housing.Bunce, Susannah. 2009.
Variations in their composition and structure have resulted in massive, well-jointed steel-grey cliff faces alternating with structural benches of vesicular amygdaloid lava and ash layers, all of which contribute to the pyramida-shaped hills and crest-level plateaux or mesas. Earth sculpturing under the tropical climate completed the panorama-sharply defining the landform features in the semi-arid conditions, and rounding the hilltops under water condition. Fluvial action by the Krishna, Bhima, Godavari, Tapi-Purna and Wardha-Wainganga river systems has further aided in the compartmentalisation of the Desh into broad, open river valleys, alternating with plateau interfluves, that form the ribs of the Sahyadrian backbone. In sharp contrast, the hill torrents of the Konkan, barely a 100 km long, tumble down as roaring streams which flow in deeply entrenched valleys to terminate in tidal estuaries.
City & Harbor According to the United States Census Bureau, the city has a total area of , of which is land and is water. The City of Mackinac Island exists on the island of the same name, and it also nominally includes the entirety of nearby Round Island, situated in the Straits of Mackinac immediately to the south, which is uninhabited, and is owned and overseen by the United States Forest Service in its entirety, and is managed as part of the Round Island Wilderness Area and the Hiawatha National Forest. While all of Mackinac Island, the landform, is located within the corporate limits of the City of Mackinac Island, today 82 percent of the island's landmass is owned by the State of Michigan and managed by the Mackinac Island State Park Commission (MISPC). The City has direct jurisdiction over only 18 percent of the island.
5)-(horizontal)-Shinarump Conglomerate, 4)-(horizontal)-Moenkopi Formation, 3)-vertical cliffs of De Chelly Sandstone, and 2)-skirts/erosion slopes of Organ Rock Formation-(horizontally bedded) The angular unconformity below is upon the 1)-low angle dipping Cedar Mesa Sandstone, commonly of southeast Utah In Monument Valley, of Arizona and south Utah, only larger landforms still contain the protective caprock of the Shinarump Conglomerate. The vertical cliffs of highly resistant De Chelly Sandstone protect the highly erodable Organ Rock Formation that forms 'erosion skirts' at the base of the vertical monuments in Monument Valley. For larger mesas, or larger connected land forms, where the more erodable overlying Moenkopi Formation, has not been lost, (with the caprock Shinarump also being undermined), larger sections of Shinarump are thus preserved. Perimeter mesas in the Monument Valley region have the caprock protecting the upper surface, plants, and alluvium from easy erosion of the landform surface.
In 2006, Ross A. Beyer (NASA's Ames Research Center) submitted an abstract to the 37th Lunar and Planetary Sciences Conference reporting on his work characterizing in detail the aeolian morphologies present across the surface of Ganges Mensa. Beyer also investigated a crater off the eastern edge of the mesa which appears to demonstrate evidence of burial and later exhumation. The unveiled portions of that crater superpose a toe of the mesa, adding significant evidence to the hypothesis that Ganges Mensa was once a much more extensive landform that has since been greatly weathered. Beyer also submitted an abstract to the American Geophysical Union meeting that year to report on the relationship of light- toned mound deposits in Ganges Chasma to the basal unit of Ganges Mensa, using OMEGA spectral data to note similarities in kieserite signatures between the sulfate-bearing mesa layers and those mounds.
Map of the Clay Belt The Clay Belt is a vast tract of fertile soil stretching between the Cochrane District in Ontario, and Abitibi County in Quebec, covering in total with of that in Ontario. It is generally subdivided into the Great Clay Belt to the north running eastward from Kapuskasing, past Lake Abitibi and on to Amos, and the V-shaped Lesser Clay Belt to its south, running from Englehart down to the Wabi River to the northern tip of Lake Timiskaming, and long the eastern side of Timiskaming and back up to Rouyn- Noranda. The Clay Belt is the result of the draining of the Glacial Lake Ojibway around 8,200 BP, whose lakebed sediment forms the modern landform. The Clay Belt is surrounded by the Canadian Shield, forming an island of "southern flatlands" in the midst of the hilly and rocky surroundings.
List of geological features on Mercury is an itemization of mountains, valleys, craters and other landform features of the planet Mercury. Different types of features are named after different things: Mercurian ridges are called dorsa, and are named after astronomers who made detailed studies of the planet; valleys are called valles, and are named after ancient abandoned cities, towns, and settlements; crater chains are called catenae and are named after radio telescope facilities; plains are called planitiae, and most are named after mythological names associated with Mercury; escarpments are called rupes and are named after the ships of famous explorers; long, narrow depressions are called fossae and are named after works of architecture; bright spots are called faculae and are named after the word snake in various languages. See also list of craters on Mercury, list of albedo features on Mercury, and list of quadrangles on Mercury Longitude is west longitude.
Los Alcazares has generally some of the best beaches in the Murcian region, many of them have been awarded "Blue Flag Status" from the Spanish Tourist board based on their cleanliness, safety and atmosphere, especially the promenade in Los Alcazares is worth visiting. However, all its beaches have lost the "Blue Flag Status" in the recent years due to the bad state of the coastal salty lagoon that faces Los Alcázares Beaces (Mar Menor) and the high level of pollution of the water landform. The Los Alcazares side of Mar Menor beaches stretches from Los Alcázares to San Javier and San Pedro del Pinatar. With a surface area of nearly 170 km², a coastal length of 70 km, and warm and clear water no more than 7 m in depth, it is "the largest swimming pool in the world", in the opinion of famous swimmer and Hollywood actress Esther Williams.
The regional district's dominant landform is the Rocky Mountain Trench, which is flanked by the Purcell Mountains and Rocky Mountains on the east and west, and includes the Columbia Valley region, the southern half of which is in the regional district (its northern half is in the Columbia-Shuswap Regional District). Another distinct area within the regional district is the Elk Valley in the southern Rockies, which is the entrance to the Crowsnest Pass and an important coal-mining region. Other than the Columbia and Kootenay Rivers, whose valleys form the bottomlands of the Rocky Mountain Trench, also included in the regional district are the northernmost parts of the basins of the Flathead, Moyie and Yahk Rivers (the Moyie and Yahk are tributaries of the Kootenay, entering it in the United States, and the Flathead is a tributary of the Clark Fork in Montana).
In 1608, Captain John Smith traveled 170 miles from Jamestown (established the previous year) exploring the shores, rivers, creeks, and streams to the upper Chesapeake Bay towards the Susquehanna River, leading the first European expedition to the Patapsco River, named after the native Algonquian peoples who fished shellfish and hunted. English royal and proprietary land grants from 1661 were combined in 1702 by James Carroll who named it Whetstone Point because of the landform shape resembling a sharpening stone. The area is now known as Locust Point a residential and industrial area. The port was founded on this site in 1706 by the colonial General Assembly of the Province of Maryland and designated one of the official Port of Entry for the tobacco trade with the Kingdom of England. In 1729–1730, the point was incorporated into newly established Baltimore Town to the northwest at "The Basin" of the Northwest Branch of the Patapsco.
The surface terrain is therefore divided into two overall types of landform: the plain, or flat surface of the fill, and the anticline at the edges, taking the form of hilly country in which the outcrops of the original rock are visible along with alluvial fans formed from the outwash of the more severe anticlinal terrain; that is, the Apennines and the Alps. The valley is broadly divided into an upper, drier part, often not particularly suited for agriculture, and a lower, very fertile, and well irrigated section, known in Lombardy and western Emilia as la Bassa, "the low (plain)". The upper areas of the Po valley take local names which reflect in their meanings their being modestly suited for farming. So we have the Piedmontese vaude and baragge, the Lombard brughiere and Groane, or, exiting from the Po valley proper, the Friulian magredi, areas remote from easily reachable water tables and covered with dense woods or dry soils.
The Hunter-Bowen Orogeny was a significant arc accretion event in the Permian and Triassic periods affecting approximately 2,500 km of the Australian continental margin. The Hunter-Bowen Orogeny occurred in two main phases, a Permian accretion of previously formed passive-marginal Devonian and Carboniferous sediments in the Hunter region and mid-west region of what is now New South Wales, separated by rifting, back-arc volcanism and a later Permian to Triassic event resulting in arc accretion and metamorphism during a subduction event. The Hunter-Bowen Orogeny has resulted in the New England Fold Belt, a tectonic accretion of metamorphic terranes and mid-crustal granitoid intrusions, flanked by Permian to Triassic sedimentary basins which were formed distally to the now-eroded orogenic mountain belt. While the Great Dividing Range north of Sydney is a prominent landform, this is more the result of Cenozoic volcanism and crustal uplift since the Jurassic than the result of the original orogenic belt which is essentially mimics.
The plain agricultural areas in the county are mainly divided into two parts, one is the front flood fan of the Pamir Mountains, and the other is the Gez-Kushan River Delta (). These two plains, in terms of large landform types, belong to the Kashgar Delta () and are an oasis on the southwest edge of the Tarim Basin. The Gez-Kushan River Delta, located in the southern part of the Kashgar Plain (), the northern part of the northern slope of the Pamir-West Kunlun Mountain Range, the triangle between the Gez and the Kushan rivers, covers an area of about 800 square kilometers, has a distribution population of more than 100,000, accounting for about 68% of the total population of the county. It is composed of the flood of the Gez river and the Kushan River - alluvial fan and Gez River - the dympastain plain saticity of the Yuepuhu River, mainly including Akto Town, Yumai, Barin, Pilal, Jamaterak and other agricultural areas.
Structure from Motion photogrammetry with multi-view stereo provides hyperscale landform models using images acquired from a range of digital cameras and optionally a network of ground control points. The technique is not limited in temporal frequency and can provide point cloud data comparable in density and accuracy to those generated by terrestrial and airborne laser scanning at a fraction of the cost.. Structure from motion is also useful in remote or rugged environments where terrestrial laser scanning is limited by equipment portability and airborne laser scanning is limited by terrain roughness causing loss of data and image foreshortening. The technique has been applied in many settings such as rivers, badlands, sandy coastlines, fault zones, landslides, and coral reef settings. SfM has been also successfully applied for the assessment of large wood accumulation volume and porosity in fluvial systems, as well as for the characterization of rock masses through the determination of some properties as the orientation, persistence, etc.
Seeking to promote his development, Sellers named the landform Nob Hill after a fashionable area of San Francisco. A well-known photograph from 1937 shows Sellers posing with a large "Nob Hill" sign in an empty expanse of desert near what is now Silver and Tulane SE. On the north side of Central, the Monte Vista Addition was platted in 1926 by William Leverett. Due to topography and drainage concerns, the streets were laid out in an irregular pattern around two intersecting diagonal boulevards, Campus and Monte Vista. Leverett also set aside a large plot for a public elementary school in order to make the development more attractive to potential residents. Opened in 1930 as only the second elementary school on the East Mesa, Monte Vista Elementary School is still operating and has been listed on the National Register of Historic Places. By 1930, over 100 houses had been built in the Monte Vista Addition.
The park's ribbon cutting ceremony was on September 9, 2009. The Park was designed by Landscape Architects Phillips Farevaag Smallenberg of Vancouver in collaboration with Landscape Architects, The Planning Partnership of Toronto, Public Art Consultant Karen Mills and Douglas Coupland. The park incorporates integrated artwork in the form of a landform (the bluff) and stand alone art pieces by Douglas Coupland: a canoe large enough for people to stand in and see over the Gardiner to Lake Ontario, a colourful display of large fishing bobbers, a sculptural beaver dam, programmed tree lighting (which will be more evident as the trees fill out), a pair of "iceberg benches" situated near the canoe, the "heart-shaped stone" bronze artwork which was cast from a stone retrieved by Terry's brother at the end of his journey and a one-mile run called the Terry Fox Miracle Mile. The developers of Concord CityPlace are Concord Adex Developments.
Ages obtained on the Mount Melbourne volcanic field include 2.96±0.2 million years, 740,000±100,000 years and 200,000±40,000 years for Baker Rocks, 2.7±0.2 million years and 450,000±50,000 years for Cape Washington, 74,000±110,000 years and 50,000±20,000 years for Edmonson Point, less than 400,000 years for Markham Island, 745,000±66,000 years for Harrows Peak, 1.368±0.09 million years for Pinkard Table, 1.55±0.05 million years, 431,000±82,000 and 110,000±70,000 years for Shield Nunatak, and 2.5±0.1 million years for Willows Nunatak. The northeastern parasitic cone formed after the bulk of the volcano and appears to be younger than the summit of Mount Melbourne. Radiometric dating has shown that the appearance of a landform at Mount Melbourne is not indicative of its age; some well preserved vents are older than heavily eroded ones. On the other hand, a lack of proper margins of error and lack of details on which samples were dated has been problematic for radiometric dating efforts.
The volcanism of Canada is represented by many types of landform including lava flows, volcanic plateaus, lava domes, cinder cones, stratovolcanoes, shield volcanoes, submarine volcanoes, calderas, diatremes, and maars, along with examples of more less common volcanic forms such as tuyas and subglacial mounds. It has a very complex volcanic history spanning from the Precambrian eon at least 3.11 billion years ago when this part of the North American continent began to form. Although the country's volcanic activity dates back to the Precambrian eon, volcanism continues to occur in Western and Northern Canada where it forms part of an encircling chain of volcanoes and frequent earthquakes around the Pacific Ocean called the Pacific Ring of Fire. But because volcanoes in Western and Northern Canada are in remote rugged areas and the level of volcanic activity is less frequent than with other volcanoes around the Pacific Ocean, Canada is commonly thought to occupy a gap in the Pacific Ring of Fire between the volcanoes of western United States to the south and the Aleutian volcanoes of Alaska to the north.
The primary geological processes that have modified the lunar surface are impact cratering and volcanism, and by using standard stratigraphic principles (such as the law of superposition) it is possible to order these geological events in time. At one time, it was thought that the mare basalts might represent a single stratigraphic unit with a unique age, but it is now recognized that mare volcanism was an ongoing process, beginning as early as 4.2 Ga (1 Ga = 1 billion years ago) and continuing to perhaps as late as 1.2 Ga. Impact events are by far the most useful for defining a lunar stratigraphy as they are numerous and form in a geological instant. The continued effects of impact cratering over long periods of time modify the morphology of lunar landforms in a quantitative way, and the state of erosion of a landform can also be used to assign a relative age. The lunar geological time scale has been divided into five periods (Pre-Nectarian, Nectarian, Imbrian, Eratosthenian, and Copernican) with one of these (the Imbrian) being subdivided into two epochs.
The historical pillar of Tojinbo (priest-tojinbo)'s house whose name has been given to the landform of Tojinbo from which he was reputedly thrown by followers of the temple for punishment for his misbehavior, in Heisen-ji, Katsuyama, Fukui, Japan Tōjinbō is also a well-known place in Japan to commit suicide. According to statistics, as many as 25 people commit suicide派遣切られ東尋坊へ 履歴書の裏「これ以上は無理。」 December 25, 2008 (in Japanese) Asahi Shimbun Retrieved February 26, 2018 by jumping off the 70-foot-high cliffs annually, a number which has risen and fallen with Japan's national economic hardships and unemployment rates. In the 2000s, Yukio Shige, a retired police officer, frustrated at having had to fish so many bodies out of the sea and the inaction of local authorities, began patrolling the cliffs for potential jumpers. Although 14 people committed suicide there in 2016, in the next year, there has been no suicide for months.
Rosetta Head as a headland was formed when the sea reached its present level 7,500 years ago after sea levels started to rise at the start of the Holocene. As a landform, it is a large domed inselberg which is considered to be "the most prominent feature along Encounter Bay coastline" and whose form is due to its origins via the geological processes of metamorphism and intrusion followed by two phases of erosion; firstly via the action of a northward-moving glacier during the Permian which created the distinctive dome shape and then by wave action from the south due to the sea level rise during the Holocene. When viewed from the adjoining coastline, it is considered to be a typical example of a glacial terrain known as a roche moutonnee. Geologically, Rosetta Head is the result of the intrusion of molten granite (known as Encounter Bay Granite) into a grey metamorphic rock (known as the Kanmantoo group) which was subsequently elevated as part of a mountain building event known as the Delamerian Orogeny between 475 and 500 million years ago.
The "head" of the Sleeping Giant, image taken from the north, looking to the south The Sleeping Giant landform was well-known to Native Americans in the United States."Learn More About the Sleeping Giant Tonight," Great Falls Tribune, June 12, 2008. Members of Native American tribes as far away as present-day Minnesota knew of the landmark, and told the leaders of the Lewis and Clark Expedition about it. The Lewis and Clark Expedition camped below the Sleeping Giant and explored the area around it during their initial passage through the region in 1805. The Sleeping Giant region was designated a wilderness study area in 1981. In late 1982, United States Secretary of the Interior James G. Watt removed the Sleeping Giant area from protection as a WSA, concluding that the area would never meet the definition of a wilderness area because it was too small and some mineral rights in the area were owned by private citizens or companies."Wilderness Society Attacks Watt Over Protected Land," Associated Press, August 10, 1983. The Sleeping Giant region was granted WSA status again in 1985, and the WSA enlarged in 1988.
It was erected in this location by Governor Macquarie to mark the place from where all public roads were to be measured and has continued to perform this function over most of the history of European settlement in Australia, for over 190 years. The park and monument were well recognised landmarks of colonial Sydney and appeared in many nineteenth century artist views, including paintings by Conrad Martens. Although the original importance of Macquarie Place as the main town square of Sydney, the geographic and symbolic centre of the Colony, the setting to First Government House and the landmark qualities of Obelisk are now less apparent than in Colonial times due to the level of surrounding changes, the park and its monuments remain one of the few tangible links to this first Colonial town centre and thereby part of the earliest history of European settlement in Australia. It is also possibly the only remnant of the natural landform of the original foreshores of Sydney Cove which has survived relatively unchanged over two centuries of European settlement, and can therefore symbolise the first place of meeting between Aboriginal people of the Eora Country and British settlers at Sydney Cove in 1788.
U.S. Highway 93 now features forty wildlife crossing structures. The project received the Transportation Planning Excellence Award from the Federal Highway Administration in 2008. Jones & Jones pioneered the habitat immersion approach to zoo design with the development of the gorilla and African savannah exhibits at Seattle’s Woodland Park Zoo (Hyson, 23; Hancocks, 118). In 1978, zoo director David Hancocks approached the firm for a master plan. Rather than the traditional arrangement of animal enclosures behind concrete walls and bars, Hancocks and his design team, led by Grant Jones, sought to recreate the animals’ natural habitat. The gorilla forest was developed in the first phase of the project: careful manipulation of landform, plants, and sight lines immersed not only the gorillas but also the visitors in the animals’ native habitat. The landscape immersion method has been described as “an astonishing departure from conventional zoo design because it reflected a pronounced shift in philosophy” from a homocentric to a biocentric view of the world (Hancocks, 118). The philosophy is now widespread (Hyson, 23), and since the late 1970s, Jones & Jones has developed master plans and specialized habitat designs for scores of zoos on four continents.

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