Sentences Generator
And
Your saved sentences

No sentences have been saved yet

69 Sentences With "sedimented"

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

For all their flaws, these institutions possess what the political scientist Hugh Heclo called "sedimented deposits" of inherited knowledge.
Black corals like this one (Bathypathes) were not seen in the sedimented area where the dive began, but became more common as Deep Discoverer explored the region's rocky ridge and crest.
The open-air area known as Bosquet de la Colonnade has had its grey floor replaced with a "carpet" of blue glacial rock flour, sedimented rock generated by glacial erosion, surrounding the central sculpture of the space.
The Okeanos Explorer is currently making the rounds near the Marianas Trench, and the marine biologists on board are finding all sorts of amazing things, from fields of small sedimented balls through to slimy deep-sea acorn worms.
The microquartz is derived from the sclerae of sponges and the tests of radiolarians. During the Mississippian black lydites were sedimented in the Rhenish Massif in Germany.Schwarz, A. (1928).
The Rybachy Peninsula in northern Murmansk Oblast hosts Jotnian sedimentary rocks dated to have sedimented 1126±50 million years ago. These rocks are thrusted over by younger Vendian and Upper Riphean rocks.
In The Creation of Anne Boleyn, Bordo seeks to break down the “sedimented mythology turned into ‘history’ by decades of repetition” and rewrite Boleyn's story as an ambitious woman seeking power without the cache of distorted imagery around her appearance.
The lagoon has a sedimented bottom and no appreciable salt gradient. Species found there include Gammarus zaddachi and Gammarus duebeni.Kustbiotoper i Norden: hotade och representativa biotoper, TemaNord 2001:536, Copenhagen: Nordic Council of Ministers, 2001, , p. 302 Eurasian oystercatchers frequent it.
The fossil bearing paper shales are intercalated with larger deposits of volcanic material.Harding, I. C., & Chant, L. S. (2000). Self-Sedimented Diatom Mats as Agents of Exceptional Fossil Preservation in the Oligocene Florissant Lake Beds, Colorado, United States. Geology (Boulder), 28(3), 195-198.
The Duero River to its step by Castronuño. Is located in an area of moorland and sedimented banks. Therefore, this is an area of nesting and migratory water birds. The Duero is surrounded by forests of Ribera and constitutes a very interesting swamp ecosystem.
Detection of viral hemagglutinin also has been recommended as a diagnostic technique. Tissues are triturated in diluent and then sedimented by centrifugation. The supernatant fluid is tested for agglutinating activity for guinea pig erythrocytes. This test requires a minimum of laboratory equipment and is effective in the absence of antibody.
The village was founded in a clearing island in the area of the sandstone Keuper. The landscape relief was modeled out in the Neogene and especially in the Pleistocene. The valley filling sedimented by the creeks Weisach and Egelsbach comes from the Holocene. The river system of that time was directed south.
Tetillidae is a family of marine sponges. Tetillids are more or less spherical sponges (sometimes referred to as golf ball sponges) which are found commonly in all marine habitats at all depths throughout the world. They are especially common in sedimented habitats. Over a hundred species have been described in ten genera.
The Dakota sedimented sandstone later came to be inundated by the waters of a shallow inland sea. From some 66 to 70 million years ago and episodically continuing for millions of years, uplift from the Laramide Orogeny exposed the old sandstone seabed, by tilting up to 90-degree angles the steep red megaliths which we now see in the Garden of the Gods (Huber, 1998, pp. 7 and 130.) Portions of the Dakota Formation again cycled into episodes of erosion, allowing a detritus of coarse-grained sedimentary sand to be displaced some three miles (5 km) eastwards, to land at the site which we now know as Austin Bluffs. The feldspar-rich sedimented particles of "arkose" sand consolidated into new sandstone, i.e.
In sewage treatment works, the foul water first is screened to remove floating debris. Then it is sedimented to remove insoluble particles. After this, it is sprayed over a filter bed of clinker. Aerobic microbes soon grow in hollows in the clinker, where they kill harmful anaerobic bacteria in the water and remove much of the offensive organic waste.
2D x-tal with thermal fluctuations of particle positions. Red lines symbolize lattice-axis and green arrows symbolize the deviations of equilibrium positions. The Image shows a (quasi-) two-dimensional crystal of colloidal particles. This are micrometer sized particles dispersed in water and sedimented on a flat interface thus they can perform Brownian motions only within a plane.
The Alb has a gorge there with small waterfalls, one of them manmade. A little higher up, a prominent end moraine embankment crosses the valley. The narrow water gap of the stream, the Menzenschwand splash dam reservoir (Menzenschwander Kluse), was previously used to store water for log rafting. The basin-shaped mouth area is a sedimented, former lake.
Deposition took place northeast of the Kaiserstuhl, as the winds blew from the southwest. The higher the place of sedimentation, the thinner the layer of the sedimented material is. At the Kaiserstuhl the thickness of the loess layer varies between 10 and 40 metres. There are, however, also areas in the southwest where no loess has been deposited.
The Erms is a river of the karstified Swabian Alb, Baden-Württemberg, Germany. It flows into the Neckar in Neckartenzlingen. On its way from the Karst spring to the next large municipality Bad Urach, a former Erms sedimented, especially during floods, no less than 8 valley cataracts, where chemically precipitated travertine repeatedly drops ca. 2–5 m.
Silurian lydite of Saxony, near Nossen (Nossen-Wilsdruff Slate Mountains) The oldest known radiolarites come from the Upper Cambrian of Kazakhstan.Tatiana J. Tolmacheva, Taniel Danelian & Leonid E. Popov. Evidence for 15 m.y. of continuous deep-sea biogenic siliceous sedimentation in early Paleozoic oceans Radiolarian ooze was sedimented here over a time span of 15 million years into the Lower Ordovician.
To what degree the lake was sedimented in ancient times remains unknown. Some of the earliest huts are down in the crater. Two streams flowing north to south flanked the lake on the west: the Fosso del'Osa, and the east: Fosso di San Giuliano. These originated in another body of water, believed to be Lacus Regillus, on the south side of the road.
Kieselkalk is also known as the Helvetic Siliceous Limestone. It has sedimented during the Lower Cretaceous epoch. It can contain up to 40% of very fine (1-10 μm), evenly distributed authigenic quartz crystals. Early diagenetic dissolution of opal sponge spicules led to silica enrichment of interstitial waters, which reprecipitated silica in the overlying horizons, forming tiny quartz crystals in pore spaces.
For example, oxygenic photosynthesis is catalyzed by RuBisCO, which prefers carbon-12 over carbon-13, resulting in carbon isotope fractionation in the rock record. "Giant" ooids of the Johnnie Formation in the Death Valley area, California, USA. Ooids are near-spheroidal calcium carbonate grains that accumulate around a central nucleus and can be sedimented to form oolite like this. Microbes can mediate the formation of ooids.
The name "white blood cell" derives from the physical appearance of a blood sample after centrifugation. White cells are found in the buffy coat, a thin, typically white layer of nucleated cells between the sedimented red blood cells and the blood plasma. The scientific term leukocyte directly reflects its description. It is derived from the Greek roots leuk- meaning "white" and cyt- meaning "cell".
Ashibetsu Lake is an artificial lake which rests quietly surrounded by a Virgin forest. In recent years, Ashibetsu Lake has become increasingly Sedimented. In dedicated electricity producing dams, the water intake amount is not affected by the sedimentation, however where there is a flood control mechanism, sedimentation becomes a problem. The sedimentation rate of the Ashibetsu Dam is approximately 79.8%, which is the highest for any multi-purpose dams.
The Nam Con Son Basin was developed during the Tertiary by complex rifting of a poorly known basement. The geological formation of Nam Con Son Basin can be separated into two major structural elements: A Pre-Cenozoic strata basement and a Cenozoic sedimented cover. The heterogeneous basement is composed of quartz diorite, granodiorite and Mesozoic metamorphic rocks. While the Pre-Tertiary basement shows an assemblage of volcanic, igneous and metasedimentary rocks.
On the eastern summit platform there are buried terraces beneath the sediment cover. Sediment layers cover almost the entire summit of Horizon Guyot, and consist mainly of sand, with clay and silt making up a minor part. Features on the sedimented seafloor are flat areas, hummocks, ripples and sediment waves. Seismic transects have revealed a relief of about in the underlying basement and the presence of a central peak.
There probably always were reversals of river current, which must have speeded traffic between Frisches Haff and the lake. The lake is surrounded by and includes marsh, swamp and alder thickets. On its surface are floating Nymphaea, submerged are Potamogeton and the marshes feature tracts of Phragmites. It should have sedimented over long ago but the high throughput of water from various sources brings fresh Oxygen into the lake, retarding its aging.
In the western Pyrenees, the marine sedimentation also carried on during the Eocene. In two subsiding basins on both sides of today's chain, limestones, marls, foraminiferous sandstones, and sandstones with a benthic fauna were sedimented. The Eocene sedimentary successions along the French northern edge of the Pyrenees (in the North Pyrenean Zone) are fairly thin and full of facies changes. There, short-lived transgressions and regressions can be followed into the Languedoc.
The George Klindt House is a two-story structure that follows a square plan with a corner wing on the back of the house. It features a Mansard roof and pedimented dormers, which are typical of the Second Empire style. The enclosed porch and sedimented pediment on the front indicates that this house is from a later date of the style. The house is located on a high hill above the street.
They were the theme of the 1998 exhibition at the Musée Rodin in Paris. In the cycle of works titled Terre ("Lands") created starting from 1988, the earth sedimented in layers, as in its natural state, is enclosed in a transparent glass parallelepiped through which can be seen the imprint left by a gesture of the artist, the upheaval in the soil which preserves the image of the hand that caused it.
In a recent study published in August 2019, researchers found that this nearshore species tends to dwell in the upper continental slope in highly sedimented areas, and also in association with rock out crops, authigenic carbonate crust, and mixed substrate areas in depths between 200-929 m. Longnoses inhabited areas with 3–6 °C temperatures. This research came from the first long-scale, long-term assessment of skates in deepwater of the eastern North Pacific.
The Lower Kimmeridgian sediments are sedimented close to the shore, they bear oysters, urchins, and ripple marks. The second sequence of the Malm starts in the Upper Kimmeridgian, only in places does it show regressive traits, nevertheless the sedimentary character changes. Laid down are breccias and the sediments also show synsedimentary reworkings; periodically interbedded limestones and marls carrying lignite horizons begin to form. The sediments can be dated by the ammonites Aulacostephanus and Aspidoceras orthocera.
Bowood is one of Capability Brown's finest parks. Laid out over 2,000 acres (8 km²) in the 1760s, it replaced an earlier, more formal garden of avenues and wildernesses. Brown's design encompasses a sinuous lake (almost 1 km long), with lawns sloping gently down from the house, and drifts of mature trees. Submerged in the lake are foundations of cottages forming the Mannings Hill hamlet, rediscovered by divers in 2007 in shallow but heavily sedimented water.
The view that radiolarites are mainly deposited under pelagic, deep water conditions cannot be asserted any longer. Layers enriched in radiolarians do even occur in shallow water limestones like the Solnhofen limestone and the Werkkalk Formation of Bavaria. What seems to be important for the preservation of radiolarian oozes is that they are deposited well below the storm wave base and below the jets of erosive surface currents. Radiolarites without any carbonates have most likely been sedimented below the calcite compensation depth (CCD).
1, pp. 1-14. Campaign speeches are an example of how rhetorical situations recur, producing sedimented genres. As a result of the institutions that execute the U.S. Constitution, every four years at the time of presidential elections, candidates deliver campaign speeches. Campaign speeches have become a distinct genre because they respond to highly similar situations that recur because of a structural or institutional basis. U.S. rhetoricians Karlyn Kohrs Campbell and Kathleen Hall Jamieson refer to genre as a “constellation of elements.
Gómez Piñeiro 1979: 35 It is also the core of the comarca of Greater Bilbao. It is surrounded by the municipalities of Derio, Etxebarri, Galdakao, Loiu, Sondika, and Zamudio to the north; Arrigorriaga and Basauri to the west; Alonsotegi to the south; and Barakaldo and Erandio to the east. Bilbao is located on the Basque threshold, the range between the larger Cantabrian Mountains and the Pyrenees.Gómez Piñeiro 1979: 38 The soil is predominantly composed of mesozoic materials (limestone, sandstone, and marl) sedimented over a primitive paleozoic base.
Individuals have the capacity to reflect on these realities, including their own social everyday reality. This type of reflection is often referred to as reflexivity. But, crucially, even reflexivity must draw on some "source material" or be rooted in intersubjectivity. It has, thus, been suggested that: "As agents exercise their reflexive capacities, they bring with them a past consisting of social experiences accumulated or sedimented into stocks of knowledge that provide the requisite guidance for going about their lives and interpreting their social reality".
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.
Rice grown in the delta areas rely heavily on the river water and sedimented minerals from the northern mountains, whilst the rice grown in the central regions require irrigation from the Irrawaddy River. The fields are tilled when the first rains arrive – traditionally measured at 40 days after Thingyan, the Burmese New Year – around the beginning of June. In modern times, tractors are used, but traditionally, buffalos were employed. The rice plants are planted in nurseries and then transplanted by hand into the prepared fields.
Sandstone palisades of hoodoo ribs erupt into stacked terraces, up to six-layers high, intermittently situated across the northern wall commanded by Eagle Rock and the neighboring Pulpit Rock. Its high white stone columns are easily visible from Highway I-25. In a wedding-cake array, Eagle Rock's three steep stone terraces step down the hillside. Each grey stone terrace maintains its hold against weathering erosion, where strengthened by a top stratum composed of a more resistant sedimented rock in a streak of golden-reddish tint.
Most likely the Canaveilles Group was deposited during the interval end- Neoproterozoic to lower Cambrian at the northern edge of Gondwana. The sediments are of marine origin and probably were left behind on the continental margin. Possible bioherms within the carbonaceous intercalations and the archeocyathid reefs in the Cadí Nappe point at shelf or shelf edge deposits with some incorporated reefal complexes. The rhyodacites probably were associated with an island arc, so it is possible that the Canaveilles Group was sedimented in a backarc position.
In the Lower Eocene (Ypresian), another transgressive period saw the sea advance north into the Médoc and south of Oléron; in the southeast it even reached the Montagne Noire. In the Aturian Gulf, Globorotalia-bearing marls were deposited, while farther east turritella-rich marls and limestones were formed. The newly inundated areas receive sands and limestones rich in alveolinids and nummulites. Meanwhile, iron-rich sands (in the Charente) and molasses (in the Libournais and in the Agenais) were sedimented in the continental north and northeast.
Acetobacterium carbinolicum is a homoacetogenic, strictly anaerobic bacterium that oxidises primary aliphatic alcohols. These Gram-positive, non-spore- forming and rod-shaped bacteria grow at optimal temperatures of about 30°C, but some subspecies are also psychrotolerant, being able to grow at a minimum temperature of 2°C, as the microorganisms belonging to the subspecies A. carbinolicum kysingense, which have been isolated from fine sand and mud sedimented in a brackish fjord in Jutland, Denmark, where concentrations of sodium chloride (NaCl) in water are up to 4.3%.
These two formations with their diverse fossils were historically thought to represent sequential time periods with different environments, but in 2009 the Canadian palaeontologist DavidA. Eberth and colleagues found that there was partial overlap across the transition between them. The two formations "interfinger" across a stratigraphic interval that is about 25 m (82 ft) thick, which suggests that the fluvial and aeolian environments coexisted when the area was sedimented. Photos of the interfingering contacts between the formations The environment of the Nemegt Formation has been compared to the Okavango Delta of present-day Botswana.
As is the case for most of the surrounding mountains, such as Old Rag Mountain, Humpback Rock is underlain by an enormous granite formation created during the Grenville Orogeny on the ocean floor about a billion years ago. About 400 million years later, during the Catoctin Formation, basaltic magma was deposited, forming a layer of greenstone over the granite. Over time, sand and rock sedimented on the ocean floor, forming quartzite and sandstone deposits. Finally, sedimentation of shells and skeletons of foraminifera resulted in deposition of a layer of limestone.
Contracts include surveying and mapping, engineering and construction, as well as tasks related to conservation and development of the Mississippi River and the river basin at Randolph. Maintenance related projects include dredging of the navigable channel of the Mississippi River at Randolph to remove sedimented sand and mud. Tasks related to conservation include dike construction to protect low- lying areas at Randolph from flooding and subsequent erosion. The Navigation Bulletin No. 2, issued by the USACE in 2006, describes a stone dike construction at Randolph with an approximate elevation of at river mile 770L.
In addition to these two currents, a large submarine canyon acts as a primary conduit for the transfer of sediment from the continental slope to the deep- sea. Organisms living in the depths of Barkley Canyon have evolved to be able to persist in areas with high pressure, no light, and low nutrients/food availability. The Barkley Canyon instruments span a diversity of habitats, each of which is associated with its own specialized biological community. Most of the areas within Barkley Canon are characterised by a soft, finely sedimented seafloor.
The Eastern Andes Metamorphic Complex is a large coherent but varied group of metamorphic and sedimentary rocks –in other words a geologic complex– that crops out in the eastern Patagonian Andes in Chile and Argentina. The metamorphic grade of rocks varies but does not exceed greenschist facies, the only exception to this are rocks near plutons affected by contact metamorphism. The sedimentary protoliths sedimented in the Late Paleozoic. The pressures and temperatures of metamorphism of the Eastern Andes Metamorphic Complex are different those usually expected from accretionary complexes.
The centrifugation process itself has four variables that can be controlled to selectively remove desired components. The first is spin speed and bowl diameter, the second is "sit time" in centrifuge, the third is solutes added, and the fourth is not as easily controllable: plasma volume and cellular content of the donor. The end product in most cases is the classic sedimented blood sample with the RBC's at the bottom, the buffy coat of platelets and WBC's (lymphocytes/granulocytes, PMN's, basophils, eosinophils/monocytes) in the middle and the plasma on top.
It is part of the series of formations with the presence of Toarcian black shales, being among the most important of the Alpine-Mediterranean domain. Those Shales on the Northern Calcareous Alps was sedimented based on a strong dependency on the overall palaeobathymetric situation of the region, as recovered by the microfacies types as well as in the composition of the biota. The deeper part is domain of the Sachrang Shales, with a basin radiolaria-rich lithologies, and a parallel series of submarine topographic highs a dominance of echinoderm-and mollusc- biomicrites (Unken Shales) and a strong increase in resedimentation can be observed.
With falling sea levels in the Upper Barremian, black, pyrite-bearing claystones and lagoonal limestones rich in ostracods and characeans were sedimented. After the Barremian/Aptian boundary, marked by another high stand of the sea, there were four more sea-level oscillations during the Aptian and the Albian, bringing about a very significant sediment accumulation (in some places up to 3000 m). Due to sinking grabens in the Atlantic domain, the water masses of the Atlantic and the Tethys mixed for the first time. The Aptian/Albian sediments are characterised by the competitive interplay between fine-grained terrigenic and organic material.
Coccoliths are the main component of the Chalk, a Late Cretaceous rock formation which outcrops widely in southern England and forms the White Cliffs of Dover, and of other similar rocks in many other parts of the world. At the present day sedimented coccoliths are a major component of the calcareous oozes that cover up to 35% of the ocean floor and is kilometres thick in places. Because of their abundance and wide geographic ranges, the coccoliths which make up the layers of this ooze and the chalky sediment formed as it is compacted serve as valuable microfossils.
The origin of the outlaw label is debated. According to Jason Mellard, author of Progressive Country: How the 1970s Transformed the Texan in Popular Culture, the term "seems to have sedimented over time rather than exploding in the national consciousness all at once". The term is often attributed to "Ladies Love Outlaws", a song by Lee Clayton and sung by Waylon Jennings on the 1972 album of the same name. Another plausible explanation is the use of the term a year later by publicist Hazel Smith of Glaser Studios to describe the music of Jennings and Tompall Glaser.
He pointed out the paradoxical relationship between Giddens' "dialectic of control" and his acknowledgement that constraints may leave an agent with no choice. He demanded that Giddens better show how wants and desires relate to choice. Giddens replied that a structural principle is not equivalent with rules, and pointed to his definition from A Contemporary Critique of Historical Materialism: "Structural principles are principles of organisation implicated in those practices most "deeply" (in time) and "pervasively" (in space) sedimented in society",Giddens, A. (1981). A contemporary critique of historical materialism: vol 1: Power, property, and the state.
Socio-economic conditions of the feudal period and administrative-territorial units that made up the so-called "countries" gave rise to specific types of costumes with local specificity for the Romanian lands. But regional variations should be reported to the prototype that has formed the basis, which shows the unity and diversity of Romanian popular costumes. The climax of the artistic value of traditional costumes was reached in the mid-nineteenth century, when ennobled the Romanians bodies throughout the country. In the context of building the national conscience were sedimented the key-insignia of Romanian port, that distinguish it from surrounding ethnic groups.
It correlates magnetostratigraphically with the upper part of chron C 13r and biostratigraphically with the calcareous nannoplanktonzone NP21. The member therefore belongs to the upper Priabonian and has an absolute age of 34.0 to 33.75 million years BP. The Bembridge Marls Member was mainly sedimented in fresh or brackish water as indicated by cirripedia and gastropods like Terebia. The lower section of the member is of estuarine origin, whereas the upper section was laid down by rivers inhabited by prosobranchs like Viviparus. Relatively short-lived marine inraids are recognizable in horizons like the Bembridge Oyster Bed 1.5 metres above the base and a limestone band with bivalves like Corbicula and Nucula.
Southern California Quarterly "Cinco de Mayo's First Seventy-Five Years in Alta California: From Spontaneous Behavior to Sedimented Memory, 1862 to 1937" Spring 2007 (see American observation of Cinco de Mayo started in California) Retrieved October 30, 2007. "Far up in the gold country town of Columbia, California, Mexican miners were so overjoyed at the news that they spontaneously fired off rifle shots and fireworks, sang patriotic songs and made impromptu speeches." Columbia, in its heyday, was California's second-largest city although only about 2,000 people now live in this region. It was even considered briefly as a site for the state capitol of California.
The Husserlian elucidation of lifeworld provided a starting point for the phenomenological sociology of Alfred Schütz, who tried to synthesize Husserl's phenomenology of consciousness, meaning, and the life-world with Max Weber's sociology and its focus on subjectively meaningful action. Jürgen Habermas has further developed the concept of the lifeworld in his social theory. For Habermas, the lifeworld is more or less the "background" environment of competences, practices, and attitudes representable in terms of one's cognitive horizon. Compared to Husserl with his focus on consciousness, however, Habermas, whose social theory is grounded in communication, focuses on the lifeworld as consisting of socially and culturally sedimented linguistic meanings.
This force causes sedimentation of macromolecules, and can even cause non-uniform distributions of small molecules. Since different fragments of a cell have different sizes and densities, each fragment will settle into a pellet with different minimum centrifugal forces. Thus, separation of the sample into different layers can be done by first centrifuging the original lysate under weak forces, removing the pellet, then exposing the subsequent supernatants to sequentially greater centrifugal fields. Each time a portion of different density is sedimented to the bottom of the container and extracted, and repeated application produces a rank of layers which includes different parts of the original sample.
Old Rag Mountain is underlain by Old Rag Granite, named for its ubiquitous exposure on the mountain, formed during the Grenville Orogeny about a billion years ago. About 400 million years after the Grenville orogeny during the Catoctin Formation, deposition of basaltic magma occurred during the formation of the Iapetus Ocean, forming a layer of greenstone over the granite. This was followed by the Weverton Formation, Harpers Formation, and Antietam formation in which sand and rock sedimented on the ocean floor forming quartzite and sandstone deposits. Finally a period of sedimentation of shells and skeletons of foraminifera resulted in deposition of a layer of limestone.
The lake and the surrounding wetlands, together with local forests, are regarded as a valuable local natural resource worth to protect.Haninge Municipality, Kvarntorp However, while the lake system as a whole is regarded as sensitive to further loads of surface runoff, Dammträsk is one of the lakes in Haninge already to contaminated to be regarded as vulnerable.Haninge Municipality, Dagvattenstrategi It has been a conscious decision to redirect water from Rudasjön to Dammträsk, and, as much of the waste the lake receives is sedimented into the lake, Drevviken, the lake downstream is saved from contamination. The price to pay, has been the dense vegetation in the lake.
The Guaymas Fault, named for the city of Guaymas, Sonora, Mexico, is a major right lateral-moving transform fault which runs along the seabed of the Gulf of California. It is an integral part of the Gulf of California Rift Zone, the northern extremity of the East Pacific Rise. The Guaymas Fault runs from the San Pedro Martir Basin located at the southern end of the San Lorenzo Fault (the next transform to the north), and extends southward to the Guaymas Basin, a heavily sedimented rift which includes both continental and oceanic crust and contains numerous hydrothermal vents. The Guaymas Fault is often grouped together with the three transform faults to its north as the Guaymas Transform Fault System.
Even the site of the colony of the mother-city of Magnesia in Thessaly was not established until W. M. Leake got the site correctly identified in 1824 (Journal of a Tour in Asia Minor pp 242ff). In the winter of 1842-3, a French team struggled with swampy ground and a high water table at the heavily sedimented site, and succeeded in removing 40 meters of the temple's frieze, comprising 41 blocks, and some other architectural elements. These were taken to the Louvre Museum, but the excavations were never published. In 1887 Osman Hamdi Bey, director of the Archaeological Museums of Constantinople, carried off to Constantinople a further 20 meters of frieze blocks from the Artemision.
Steppes in New Barag Right Banner Topography of Inner Mongolia in China Officially Inner Mongolia is classified as one of the provincial-level divisions of North China, but its great stretch means that parts of it belong to Northeast China and Northwest China as well. It borders eight provincial-level divisions in all three of the aforementioned regions (Heilongjiang, Jilin, Liaoning, Hebei, Shanxi, Shaanxi, Ningxia, and Gansu), tying with Shaanxi for the greatest number of bordering provincial-level divisions. Most of its international border is with Mongolia, which, in Chinese, is sometimes called "Outer Mongolia", while a small portion is with Russia's Zabaykalsky Krai. Inner Mongolia largely consists of the northern side of the North China Craton, a tilted and sedimented Precambrian block.
Their location in not excessively deep and eutrophic waters favour an increase in biomass and the number of species thanks to the support and the protection offered by the solid substrates together with their vertical gradient given by their sticking up from the bottom and the enormous food availability in the form of already sedimented suspended organic material.Molin E., Fiorin R., Riccato F., Artico G., Campaci P., Comunità macrobentonica di tre substrati rocciosi del Golfo di Venezia (Nord Adriatico), Biologia Marina Mediterranea 16 (1), 2009: 278-279 Oases with extreme biologic richness with an increase in the number of species and also a considerable biomass per surface unit are thus formed. These areas are also extremely favourable for egg deposition, ogive-shaped capsules, larvae or reproductive forms which need a solid anchorage.
"But the sheer coverage here is leading us all to come to the conclusion that it has to be sedimented oil from the spill, because it's all over the place." By January 2011, USF researchers found layers of oil near the wellhead that were "up to 5 times thicker" than recorded by the team in August 2010. USF's David Hollander remarked, "Oil's presence on the ocean floor didn't diminish with time; it grew" and he pointed out, "the layer is distributed very widely," radiating far from the wellhead. In 2013, some scientists at the Gulf of Mexico Oil Spill and Ecosystem Science Conference said that as much as one-third of the oil may have been mixed with deep ocean sediments and dragged to the bottom of the ocean floor where it remains, risking damage to ecosystems and commercial fisheries.
In seismic profile, the main body of the seamount rises steeply over in predominantly unsedimented volcanic slope to the thinly sedimented ( to ), from an Emperor point of view, gently domed summit region between to high peak profile, which covers about 3400 square kilometers of area. From analysis of seismic reflection survey data and core material recovered by drillings at Site 432, the shipboard party of Deep Sea Drilling Project (DSDP) Leg 55 proposed that Nintoku Seamount was in an intermediate atoll stage (no lagoon but fringing reefs and banks and extensive carbonate bank interiors) before subsidence removed the island below the wave base. It was further thought that a few small remnant volcanic peaks and domes still pierce the sedimentary deposits. Nintoku Seamount apparently remained at or above sea level long enough to be almost completely devastated by subaerial erosion and wave action.
It is a denial of human reality, an effort to evade freedom, a flight from responsibility, a choice against choice, an assertion of being the only point of view on the world, an assertion of being the world, an effort to deny having a point of view, a flight from displeasing truths to pleasing falsehoods, a form of misanthropy, an act of believing what one does not believe, a form of spirit of seriousness, sincerity, an effort to disarm evidence (a Gordon innovation), a form of sedimented or institutional version of all of these, and (another Gordon innovation) a flight from and war against social reality. Gordon rejects notions of disembodied consciousness (which he argues are forms of bad faith) and articulates a theory of the body-in-bad-faith. Gordon also rejects authenticity discourses. He sees them as trapped in expectations of sincerity, which also is a form of bad faith.

No results under this filter, show 69 sentences.

Copyright © 2024 RandomSentenceGen.com All rights reserved.