Plateaus sentence example

plateaus
  • The climate is severe on the plateaus, hot towards the Caspian, and dry everywhere.
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  • The elevated plateaus between these ranges are semiarid and inhospitable, and are covered with extensive saline basins, which become lagoons in the wet season and morasses or dry saltpans in the dry season.
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  • The flora of Argentina should be studied according to natural zones corresponding to the physical divisions of the country - the rich tropical and sub-tropical regions of the north, the treeless pampas of the centre, the desert steppes of the south, and the arid plateaus of the north-west.
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  • In the high plateaus are the Shat-el-Gharbi or Western Shat, the Shat-el-Shergui or Eastern Shat, the ZarhezGharbi and the Zarhez-Shergui, the Shat-el-Hodna and a number of others.
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  • On the plateaus the temperature passes from one extreme to the other, and rain seldom falls.
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  • It consists of a series of plateaus formed of sedimentary rocks which mainly belong to three formations of widely separated ages, and which rest on a platform of granitic and metamorphic rocks.
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  • The range has not so many offshoots as occur on the west side of Lebanon; under its precipitous slopes stretch table-lands and broad plateaus, which, especially on the east side looking towards the steppe, steadily increase in width.
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  • Tanganyika has been formed by the subsidence of a long narrow tract of country relatively to the surrounding plateaus, which fall to the lake in abrupt cliffs, some thousands of feet high in places.
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  • On the plateaus large numbers of cattle, goats and sheep are reared.
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  • At the least there should be some consideration of four separate systems of discovery - the Eastern, in which Chinese and Japanese explorers acquired knowledge of the geography of Asia, and felt their way towards Europe and America; the Western, in which the dominant races of the Mexican and South American plateaus extended their knowledge of the American continent before Columbus; the Polynesian, in which the conquering races of the Pacific Islands found their way from group to group; and the Mediterranean.
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  • The Lap- surface of the North American arch is sagged down- worth's wards in the middle into a central depression which fold= lies between two long marginal plateaus, and these theory.
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  • Taking their rise on the plateau formation, or in its outskirts, they flow first along lofty longitudinal valleys formerly filled with great lakes, next they cleave their way through the rocky barriers, and finally they enter the lowlands, where they become navigable, and, describing wide curves to avoid here and there the minor plateaus and hilly tracts, they bring into watercommunication with one another places thousands of miles apart.
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  • The largest of all, Great Salt Lake, is maintained by the waters of the Wasatch and associated plateaus.
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  • Abich (Sur la structure et la geologic du Daghestan, 1862), the successive folds of Jurassic limestones and slates, all nearly parallel to the Caucasus, which form lofty, narrow plateaus.
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  • Spurs from the Drakensberg, at right angles to the main range, cross the plateaus.
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  • Secondary ranges with heights of 5000 and more feet are numerous, whilst lofty isolated mountains rise from the plateaus.
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  • The earliest record of glass-making in the Low Countries consists in an account of payments made in 1453-1454 on behalf of Philip the Good of Burgundy to " Gossiun de Vieuglise, Maitre Vorrier de Lille " for a glass fountain and four glass plateaus.
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  • The rearing of these animals requires much patience and skill, in which no one has been able to match the Indian breeders of the Andean plateaus.
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  • Mr Gardiner regarded these banks as plateaus rising to different elevations beneath the surface of the sea from a main plateau rising steeply from the great depths of the Indian Ocean.
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  • The geological formations thus exposed show that the plateaus are composed of a base of eruptive material, overlaid by enormous deposits of reddish sandstones, conglomerates and quartzites, exposed in parts to a depth of 2000 feet.
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  • The general elevation of the country is about 500 ft., but the hills and plateaus which form the prominent feature in the scenery of Luxemburg range from 1200 to 1500 ft.
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  • The peculiar plants of the Rocky Mountain plateaus penetrate into the Trans-Pecos region, which the north Mexican flora, including the Agave lecheguilla, a valuable commercial fibre, is found along the Rio Grande.
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  • In formation it resembles the limestone Alps of Tirol and there are on its elevated plateaus a number of doline or funnel-shaped depressions into which the melted snow and the rain sink.
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  • The geography of the Western province includes many interesting features, the in many ways peculiar Albert Nyanza (q.v.), the great snowy range of Ruwenzori (q.v.), the dense Semliki, Budonga, Mpanga and Bunyaraguru forests, the salt lakes and salt springs of Unyoro and western Toro, the innumerable and singularly beautiful crater lakes of Toro and Ankole, the volcanic region of Mfumbiro (where active and extinct volcanoes rise in great cones to altitudes of from 11,000 to nearly 15,000 ft.), and the healthy plateaus of Ankole, which are in a lesser degree analogous in climate and position, and the Nandi plateau on the east of Victoria Nyanza.
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  • Still farther east, the plateaus of the Finisterre ranges are highly cultivated and artificially irrigated by a comparatively fair people.
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  • Its surface is diversified by several plateaus, those of Haanhof and of the Livonian Aa having an average elevation of 400 to 700 ft., while several summits reach Boo to loon ft.
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  • The edges of the plateaus are gapped by deep valleys; the hilly tract between the Dvina and its tributary the Livonian Aa has received, from its picturesque narrow valleys, thick forests and numerous lakes, the name of "Livonian Switzerland."
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  • Thus there is here a gap, easily traversed, across the Appalachian mountains and plateaus to the more level and fertile plains beyond.
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  • The dominating features of south New Zealand are not ferny plateaus or volcanic cones, but stern chains of mountains.
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  • The surface of this plain, however, ranges from level river valleys in the east to irregular plateaus broken by buttes and scored by canons in the west.
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  • The Appalachian belt includes, with the ranges enumerated above, the plateaus sloping southward to the Atlantic Ocean in New England, and south-eastward to the border of the coastal plain through the central and southern Atlantic states; and on the north-west, the Allegheny and Cumberland plateaus declining toward the Great Lakes and the interior plains.
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  • The Paleozoic sediments, ranging in age from Cambrian to Permian, occupy the Great Valley, the Valley Ridges and the plateaus still farther west.
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  • Igneous intrusions consist only of unimportant dikes of trap. The most striking and uniformly characteristic geologic feature of the mountains is their internal structure, consisting of innumerable parallel, long and narrow folds, always closely appressed in the eastern part of any crosssection (Piedmont Plateau to Great Valley), less so along a central zone (Great Valley and Valley Ridges), and increasingly open on the west (Allegheny and Cumberland Plateaus).
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  • For a century the Appalachians were a barrier to the westward expansion of the English colonies; the continuity of the system, the bewildering multiplicity of its succeeding ridges, the tortuous courses and roughness of its transverse passes, a heavy forest and dense undergrowth all conspired to hold the settlers on the seaward-sloping plateaus and coastal plains.
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  • By 1755 the obstacle to westward expansion had been thus reduced by half; outposts of the English colonists had penetrated the Allegheny and Cumberland plateaus, threatening French monopoly in the transmontane region, and a conflict became inevitable.
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  • The accumulations of lava gave rise to the plateaus which form almost the whole interior of the county.
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  • Faulting, probably in Pliocene times, lowered the basaltic plateaus to form the basin of Lough Neagh, leaving the eastern scarp at heights ranging up to 1800 ft.
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  • The Allegheny ridges have only a thin stony soil; but good limestone, sandstone, shale and alluvial soils, occur in the valleys and in some of the plateaus of the extreme west.
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  • On the mountains and the high plateaus the winter is often very severe; snow lies for six months on the higher peaks of the Kabyle mountains.
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  • The chief wealth of the Arab tribes of the plateaus consists in their immense flocks of sheep. The horses and mules of Algeria are noted; and the native cattle are an excellent stock on which to graft the better European varieties.
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  • The flora of the high plateaus consists chiefly of grasses, notably various kinds of alfa or esparto, and aromatic herbs.
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  • Its market is attended by Kabyles, Arabs of the plateaus and people from the Sahara.
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  • From Arzeu a line goes south across the plateaus and crossing the Ksur range at a height of 4211 ft.
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  • The middle portion of the state is occupied by high plateaus, about 4000 ft.
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  • From mountain heights along its eastern border the surface of Kentucky is a north-western slope across two much dissected plateaus to a gracefully undulating lowland in the north central part and a longer western slope across the same plateaus to a lower and more level lowland at the western extremity.
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  • The denuded mountain slopes and plateaus of southern Mexico are due to the prehistoric inhabitants who cleared away the tropical forest for their Indian corn fields, and then left them to the erosive action of the tropical rains and subsequent occupation by coarse grasses.
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  • Guatemala is naturally divided into five regions - the lowlands of the Pacific coast, the volcanic mountains of the Sierra Madre, the so-called plateaus immediately north of these, the mountains of the Atlantic versant and the plain of Peten.
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  • The Cordilleran system on the western side of the continent is lofty, broad and complicated, with heavy forests near the north-west coast, but elsewhere with trees only on the higher ranges below the Alpine region, and with treeless or desert intermont valleys, plateaus and basins, very arid in the south-west.
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  • The Cordilleran Region.From the western border of the Great Plains to the Pacific coast, there is a vast elevated area, occupied by mountains, plateaus and intermont plains.
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  • The intermont plains are at all altitudes from sea-level to 4000 ft.; the plateaus from 5000 to 10,000 ft.; and the mountains from 8000 to 14,000 ft.
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  • There is also a province of plateaus between the central part of the Basin ranges and the southern part of the Rocky Mountains.
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  • A wonderful series of these forms occurs in southern Utah, where in passing northward from the Carboniferous platform one ascends in succession the Vermilion Cliffs (Triassic sandstones), the ViThite Cliffs (Jurassic sandstones, of remarkably cross-bedded structure, interpreted the dunes of an ancient desert), and finally the Pink Cliffs (Eocene strata of fluviatile and lacustrine origin) of the high, forested plateaus.
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  • Some of the high plateaus in the north are capped with remnants of heavy lava flows of early eruption.
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  • The Arid Transition life-zone comprises the western part of the Dakotas, north-eastern Montana, and irregular areas in Washington, Oregon, Idaho, Wyoming, California, Nevada, Utah, Colorado, Arizona, New Mexico and western Texas, covering for the most part the eastern base of the Cascade and Sierra Nevada Mountains and the higher parts of the Great Basin and the plateaus.
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  • The tierra caliente zone of the coast is tropical, humid, and unfavourable to Europeans, while the inland plateaus vary from subtropical to temperate and are generally drier and healthful.
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  • South of the Arctic circle they are, under ordinary circumstances, confined to the plateaus covered with dwarf birch and juniper above the conifer-region, though in Tromso amt and in Finmarken they occur in all suitable localities down to the level of the sea.
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  • The song and insectivorous birds - thrushes, flycatchers, vireos and woodpeckers - of this latitude, are well represented, and the high plateaus (particularly the Pocono plateau) have especial ornithological interest as the tarrying-places, during the migratory seasons, of many species of birds whose natural breeding ground is much farther north.
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  • Next comes a belt of fertile plateaus bounded on the east by the Little Khingan, or Dusse-alin, a picturesque well-wooded range, which stretches in a north-easterly direction from Kirin across Manchuria, is pierced by the Amur, and continues on its left bank, separating the Bureya from the Amgun.
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  • In the west coast lands European influence, fertile soil, comparatively good roads, agriculture, timber, and coalfields have created populous settlements on the coast at Padang (the capital of the west coast, with 35,158 inhabitants in 1897, of whom 1640 were Europeans), Priaman, Natal, Ayer Bangis, Siboga, Singkel, and also on the plateaus at Fort de Kock, Payokombo, &c. In the east coast lands it is only at the mouths of rivers - Palembang at the mouth of the Musi, with 53,000 inhabitants, and Medan in Deli, the residence of the highest civil and military officials of the east coast, in which a fine government house has been erected - that considerable centres of population are to be found.
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  • There is a railway connecting not only the coalfields of the Ombilin valley with Padang, but also the Ombilin river and the Lake of Singkara with the most productive and densely populated plateaus and valleys, north and south of the line of the volcanoes Singalang, Merapi and Sago.
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  • On the left bank are the elevated plateaus of the Hunsriick and the Eifel, separated from each other by the deep valley of the Mosel, while on the right bank are the spurs of the Westerwald and the Sauerland, the former reaching the river in the picturesque group known as the Seven Mountains (Siebengebirge).
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  • Little except oats and potatoes can be raised on the high-lying plateaus in the south of the province, but the river-valleys and the northern lowlands are extremely fertile.
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  • A low swelling separates it from the Baltic Sea; while in the south it rises gradually to a series of plateaus, which merge imperceptibly into the northern spurs of the Carpathians.
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  • These plateaus, with an average elevation of Boo to 1000 ft., are mostly covered with forests of oak, beech and lime, and are deeply cut by river valleys, some being narrow and craggy, and others broad, with gentle slopes and marshy bottoms. Narrow ravines intersect them in all directions, and they often assume, especially in the east, the character of wild, impassable, woody and marshy tracts.
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  • Paraguay proper, or the country between the Paraguay and the Parana, is traversed from north to south by a broad irregular belt of highlands, which are known as the Cordillera Ambaya, Cordillera Urucury, &c., but partake rather of the character of plateaus, and form a continuation and outwork of the great interior plateau of Brazil.
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  • The hills and plateaus appear to be composed chiefly of the same sandstone series which in the Brazilian province of Rio Grande do Sul contains seams of coal, with plant remains similar to those of the Karharbari series of India (Permian or Upper Carboniferous).
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  • It possesses large plateaus, such as that of Bavaria, which stretches away from the foot of the Alps, fertile low plains like that intersected by the Rhine, mountain chains and isolated groups of mountains, comparatively low in height, and so situated as not seriously to interfere with communication either by road or by railway.
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  • The valley of the Danube above Regensburg is flanked by plateaus sloping gently to the Danube, but precipitous towards the valley of the Neckar.
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  • Although there are very considerable differences in the range of temperature and the amount of rainfall throughout Germany, these are not so great as they would be were it not that the elevated plateaus and mountain chains are in the south, while the north is occupied by low-lying plains.
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  • In central Germany the high plateaus of the Erz and Fichtelgebirge are the coldest regions.
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  • In the vicinity of the rivers Benue, Faro and Kebbi, the people, who are good agriculturists, raise cereals and other crops, while on the plateaus stock-raising forms the chief pursuit of the inhabitants.
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  • This plateau, broken only by the valleys of the rivers, does not attain an elevation approaching that of the plateaus of the southern half of the continent, the culminating point (apart from particular mountain districts), situated in about 10 N., reaching a height of 3000 ft.
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  • Domestic animals include the horse and donkey in the plateaus, but baggage animals are rare in the coast-lands, where the tsetse fly is found.
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  • Other trees, found chiefly on the plateaus, are the baobab, the shea-butter tree, the locust tree, gambier, palms, including the date and dum palm (Hyphaene), the tamarind, and, in the arid regions, the acacia and mimosa.
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  • This continues as far as 29 N., after which the hills that close in the valley become lower, and the higher plateaus lie at a distance of 10 or 15 m.
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  • Formed mostly of horizontal strata of varying hardness, they present a series of terraces of minor plateaus, rising one above the other, and intersected by small ravines worn by the occasional rainstorms which burst in their neighborhood.
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  • The other desert regions of Egypt are elevated stony plateaus, which are diversified by extensively excavated valleys and oases, and in which sand frequently plays quite a subordinate part.
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  • The remainder and greater part of the county is occupied chiefly by the gently inclined Old Red Sandstone; in the dissected plateau of the Black Mountains north of Crickhowell the lower marls and cornstones are laid open, while south of Brecon the conglomeratic upper beds form the escarpment and plateaus of the Beacons.
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  • But the sameness is relieved along the western coast of the shires of Sutherland and Ross and Cromarty by groups of cones and stacks, and farther south by the terraced plateaus and abru p t conical hills of Skye, Rum and Mull.
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  • Seen from an eminence on their surface, the inference is irresistible that these plateaus are fragments of the original tableland, trenched into segments by the formation of the longitudinal and transverse valleys.
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  • That these high plateaus are planes of erosion is shown by their independence of geological structure, the upturned edges of the vertical and contorted schists having been abruptly shorn off and the granite having been wasted and levelled along its exposed surface.
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  • An instructive example of the similar destruction of a much younger platform is to be found in the terraced plateaus of Skye, Eigg, Canna, Muck, Mull and Morven, which are portions of what was probably originally a continuous plain of basalt.
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  • Where lava has been piled up in successive nearly horizontal sheets, with occasional layers of tuff or other softer rock between them, it offers conditions peculiarly favourable for the formation of escarpments, as in the wide basalt plateaus of the Inner Hebrides.
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  • Rock-tarns are small lakes lying in rock-basins on the sides of mountains or the summits of ridges, and on rocky plateaus or plains.
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  • The two leading types of volcanic areas are the plateaus, in which sheets of porphyrites, basalts and even trachytes were emitted, sometimes with wide discharge of volcanic ashes, and the puys, or isolated vents, or scattered groups of vents, which discharged comparatively a small amount of lava and ashes.
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  • The Campsie, Kilpatrick and Dumbarton hills, the high ground from Greenock to Ardrossan, and the Carleton Hills in East Lothian are examples of the plateaus, while Arthur's Seat in Edinburgh and the Binn of Burntisland illustrate the puys.
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  • Above the highest Secondary rocks on the west coast come terraced plateaus of basalt, which spread out over wide areas in Skye, Eigg, 1VIull and Morven, and form most of the smaller islets of the chain of the Inner Hebrides.
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  • These plateaus are composed of nearly horizontal sheets of basalt - columnar, amorphous or amygdaloidal - which, in Ben More, in Mull, attain a thickness of more than 3000 ft.
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  • The volcanic episode to which these plateaus owe their origin was one of the most important in the geological history of Great Britain.
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  • That the volcanic period was a prolonged one is shown by the great denudation of the plateaus before the last eruptions took place.
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  • A remarkable feature in the volcanic phenomena was the disruption of the basaltic plateaus by large bosses of gabbro and of various granitoid rocks.
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  • Contrary to what might be anticipated from its size and from the habits of its African cousin, the Indian elephant is now, at any rate, an inhabitant, not of the plains, but of the hills; and even on the hills it is usually found among the higher ridges and plateaus, and not in the valleys.
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  • The rivers that drain the Atlantic slope of the Appalachians are comparatively short; those that drain the Pacific slope include only two, the Columbia and the Colorado, which rise far inland, near the easternmost members of the Cordilleran system, and flow through plateaus and intermont basins to the ocean.
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  • The Cogon, Fatallah and Konkure are all large rivers which descend from the plateaus through deep, narrow valleys in rapids and cataracts, and are only navigable for a few miles from their mouth.
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  • The greater portion is exceedingly hilly and in parts mountainous, and the interior consists almost entirely of highlands with here and there open valleys and plateaus of 50 to 60 sq.
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  • The principal plateaus are in the Tambunan and Kaningau valleys, in the basin of the Pagalan, and the Ranau plain to the eastward of the base of Kinabalu.
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  • Similar plateaus of minor importance are to be found dotted about the interior.
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  • On the east, the main cordillera abuts upon the region of plateaus and savannas, which occupies nearly half of the area of Nicaragua.
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  • The great rivers which flow eastward to the sea have fissured and moulded the surface into deep ravines alternating with high plateaus, ridges and isolated hills.
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  • Colorado embraces in its area a great variety of plains, mountains and plateaus.
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  • The last-named includes a number of lofty plateaus - the Roan or Book, Uncompahgre, &c., which form the eastern continuation of the high plateaus of Utah - and covers the western quarter of the state.
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  • In its lowest portions just behind the front ranges are the natural "parks" - great plateaus basined by superb enclosing ranges; and to the west of these, and between them, and covering the remainder of the state east of the plateau region, is an entanglement of mountains, tier above tier, running from north to south, buttressed laterally with splendid spurs, dominated by scores of magnificent peaks, cut by river valleys, and divided by mesas and plateaus.
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  • These "parks" are great plateaus, not all of them level, lying below the barriers of surrounding mountain chains.
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  • The stratified rocks of the Great Plains, the Parks, and the Plateaus contain enormous quantities of coal.
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  • Extensive plateaus (1500-1750 ft.), into which Lake Enare, or Inari, and the valleys of its tributaries are deeply sunk, and which take the character of a mountain region in the Saariselka (highest summit, 2360 ft.), occupy the remainder of Lapland.
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  • Along the eastern border the dreary plateaus of Olonets reach on Finnish territory altitudes of from 700 to moo ft.
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  • New Mexico is a region of mountains and high plateaus.
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  • Only the higher ranges and plateaus are timbered, and even there the forests are not dense.
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  • To the north is the main chain of the Himalayas, the lower ranges of which rise abruptly from the plain; to the south is the great elevated plateau or succession of plateaus known as the Assam range.
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  • The surface is made up of extensive plains covered with sand and deposits of alkaline salts, broken by ranges of barren hills having the appearance of spurs from the Andes, and by irregular lateral ranges in the vicinity of the main cordillera enclosing elevated saline plateaus.
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  • The whole of the north part of Tierra del Fuego is occupied by plateaus of horizontal Tertiary strata.
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  • The high altitudes of the Andean region also introduce vertical zones of temperature, modified to some extent by the rainless plateaus of the north, and by the excessive rainfall of the south.
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  • The cold antarctic, or Humboldt, current sweeps northward along the coast and greatly modifies the heat of the arid, tropical plateaus.
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  • Silver is found principally on the elevated slopes and plateaus of the Andes in the desert provinces of the north.
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  • The higher ranges intercept considerable moisture from the prevailing trade winds, and their flanks and valleys are covered with forest, but the plateaus are either thinly wooded or open campo.
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  • The name given to open plains and to the grass-covered plateaus of the interior.
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  • Karroo is a corruption of Karusa, a Hottentot word meaning dry, barren, and its use as a place-name indicates the character of the plateaus so designated.
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  • It is made up of a number of parallel ranges enclosing great elevated plateaus broken by transverse ranges and deep ravines.
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  • Below this mountainous area the ranges open out and enclose extensive plateaus.
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  • On the west side of the Cordillera, which extracts the moisture from the prevailing easterly winds, the elevated plateaus have a limited rainfall in the north, which diminishes toward the south until the surface becomes absolutely barren.
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  • They are able to go without food and drink for long periods, and inhabit the arid and semiarid plateaus of the Andes and the steppes of Patagonia.
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  • On the higher and colder plateaus much attention is given to the breeding of llamas and alpacas.
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  • Another industry of a different character is that of breeding the fur-bearing chinchilla (C. laniger), which is a native of the higher plateaus.
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  • The soils in the southern part of Arizona are mainly sandy loams, varying from light loam to heavy, close adobe; on the plateaus is what is known as " mesa " soil; and along the rivers are limited overflow plains of fine sediment - especially along the Colorado and the river Verde.
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  • The fertile northern plateaus, the Camas and Nez Perce prairies and the Palouse country - a wonderful region for growing the durum or macaroni wheat - until 1898 had no market nearer than Lewiston, 50-70 m.
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  • Several secondary plateaus of lower altitude are also distinguished by geographers.
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  • Amongst the more important plateaus are the Assab or Kibyen country, having a general level of upwards of 4000 ft., and the Sura country, also reaching to elevations of from 3000 to 5000 ft.
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  • Both these extensive plateaus are situated in the south-west portion of the province.
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  • The Mounted pagans are confined to the healthy plateaus of the south-west corner of the province.
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  • Bauchi is a province of special importance from the European point of view because, with free communication from the Benue assured, it is probable that on the Kibyen and Sura plateaus, which are the healthiest known in the protectorate, a sanatorium and station for a large civil population might be established under conditions in which Europeans could live free from the evil effects of a West African climate.
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  • The peninsula of Cornwall and Devon may be looked upon as formed from a synclinal trough of Devonian rocks, which appear as plateaus on the north and south, while the centre is occupied by Lower Carboniferous strata at a lower level.
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  • The chalk and limestone plateaus are usually almost without inhabitants, and the villages of these districts occur grouped together in long strings, either in drift-floored valleys in the calcareous plateaus, or along the exposure of some favoured stratum at their base.
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  • It has mountains, plateaus and lowlands on a grand scale.
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  • The rest of the Daghestan region consists of a series of roughly parallel folds, of Jurassic or Cretaceous age, ranging in altitudes from 7500 up to 12,500 ft., separated from one another by deep gorge-like river glens which cut it up into a number of arid, treeless plateaus which have something of the appearance of independent ranges, or rather elongated tablelands of a mountainous character.
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  • Picturesque rolling plateaus, the three rivers and narrow valleys, from which rise high hills or precipitous bluffs, are the principal natural features of the district over which the city extends.
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  • Between the valley of the Upper Nile and the low lands which skirt the south-western shores of the Red Sea and the Gulf of Aden is a region of elevated plateaus from which rise various mountain ranges.
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  • On nearly every side the walls of the plateaus rise with considerable abruptness from the plains, constituting outer mountain chains.
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  • One result of the action of the water has been the formation of numerous isolated flat-topped hills or small plateaus, known as ambas, with nearly perpendicular sides.
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  • In the mountains and plateaus of Kaffa and Galla in the south-west of Abyssinia rise the Baro, Gelo, Akobo and other of the chief affluents of the Sobat tributary of the Nile.
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  • The atmosphere on the plateaus is exceedingly clear, so that objects are easily recognizable at great distances.
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  • In the valleys and lowlands the vegetation is dense, but the general appearance of the plateaus is of a comparatively bare country with trees and bushes thinly scattered over it.
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  • The giraffe is found in the western districts, the zebra and wild ass frequent the lower plateaus and the rocky hills of the north.
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  • Among the varieties are the greater and lesser kudu (both rather rare); the duiker, gemsbuck, hartebeest, gerenuk (the most common - it has long thin legs and a camel-like neck); klipspringer, found on the high plateaus as well as in the lower districts; and the dik-dik, the smallest of the antelopes, its weight rarely exceeding so lb, common in the low countries and the foothills.
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  • On the higher plateaus the hardier cereals only are cultivated.
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  • The soil of the Hawash valley proved particularly suitable for raising this crop. In the high plateaus the planting of seeds begins in May, in the lower plateaus and the plains in June, but in certain parts where the summer is long and rain abundant sowing and reaping are going on at the same time.
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  • The eastern portion of Utah consists of high plateaus, and constitutes a part of the Colorado Plateau province.
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  • The high plateaus consist of great blocks of the earth's crust which are separated from each other by fault-lines, and which have been uplifted to different heights.
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  • The people live along the streams in the valleys between the plateaus.
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  • In the southern part of the state the high plateaus are terminated by a series of giant terraces which descend to the general level of the Grand Canyon Platform in northern Arizona.
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  • The northernmost member of the high plateaus is a broad east-west trending arch known as the Uinta Mountains.
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  • In the south-eastern part of the state are lower desert plateaus, and several mountain groups which do not properly belong to the plateau system.
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  • The western members of the high plateaus drain into the Great Basin for the most part, and in this drainage system the Sevier river is perhaps most prominent.
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  • The lower basin portion of Utah is separated from the high plateaus by a series of great fault scarps, by which one descends abruptly to a level of but 5000 or 6000 ft.
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  • The floor of the Basin Region is formed of alluvium washed from the high plateaus and mountain ranges, a part of which has accumulated in alluvial fans, and part in the greatly expanded lakes which existed here in the glacial period.
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  • In the mountainous districts and high plateaus are the grizzly, formerly more common, the black bear, the four-striped chipmunk and the yellow-haired porcupine.
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  • The dusky grouse and grey ruffed grouse are confined to the mountains and plateaus.
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  • The lower plateaus and many of the basin ranges, as well as the basins themselves, are deserts.
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  • The higher plateaus, the Uinta and Wasatch mountains, bear forests of fir, spruce and pine, and the lower slopes are dotted with piiion, juniper, and scrub cedar.
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  • Extremely cold weather may occur on the lofty plateaus and mountain ranges, while the intervening valleys and basins have a milder climate.
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  • Both Salt Lake City and St George are near the boundary between the Basin Region and the high plateaus.
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  • Well out in the basin deserts the precipitation is still less; and the same holds true for the low desert plateaus in the south-eastern part of the state, where Hite has an annual precipitation of only 2.3 in., of which 0.4 in.
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  • On the other hand, the precipitation on the high plateaus probably exceeds 30 in.
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  • In the protected valleys between the high plateaus alluvial soils are cultivated; but the plateau summits are relatively inaccessible, and, being subject to summer frosts, are not cultivated.
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  • Comparatively poor, sandy soil is found on the lower desert plateaus in the south-east, where population is scanty.
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  • By this remarkable journey he proved that, for resolute and enduring men, travelling in the Central Asian plateaus was easier than had been supposed.
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  • The city is situated on two plateaus; the lower is occupied chiefly by factories, the upper by dwellings.
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  • There are several lofty plateaus in this region which form a huge central watershed for rivers flowing east to the Amazon, west to the Pacific, and north to the Caribbean Sea.
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  • The higher plateaus are called paramos, cold, windswept, mist-drenched deserts, lying between the elevations of 10,000 and 15,000 ft., which are often the only passes over the Cordilleras, and yet are almost impassable because of their morasses, heavy mists, and cold, piercing winds.
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  • The "sabana" of Bogota is a good illustration of the higher of these plateaus (8563 ft., according to Stieler's Hand-Atlas), with its mild temperature, inexhaustible fertility and numerous productions of the temperate zone.
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  • The lower valleys, plateaus and mountain slopes of this range are celebrated for their coffee, which, with better means of transportation, would be a greater source of prosperity for the republic than the gold-mines of Antioquia.
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  • It is worthy of note that the principal rivers of these three classes - the Patia, Cauca, Magdalena, Caqueta and Putumayo - all have their sources on the high plateaus of southern Colombia and within a comparatively limited area.
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  • The elevated plateaus and summits of the Andes are responsible, however, for many important and profound modifications in climate, not only in respect to the lower temperatures of the higher elevations, but also in respect to the higher temperatures of the sheltered lowland valleys and the varying climatic conditions of the neighbouring plains.
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  • The temperate and subtropical regions cover the greater part of the departments traversed by the Eastern Cordillera, the northern end of the Central Cordillera, the Santa Marta plateaus, and the Upper Cauca Valley.
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  • There are other open plains in northern Colombia, sometimes covered with a shrubby growth, and the "mesas" (flat-topped mountains) and plateaus of the Cordilleras are frequently bare of trees.
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  • Among the more common fruit-trees, some of which are exotics, may be mentioned cacao (Theobroma), orange, lemon, lime, pine-apple, banana, guava (Psidium), breadfruit (Artocarpus), cashew (A nacardium), alligator pear (Pers ea), with the apple, peach, pear, and other fruits of the temperate zone on the elevated plateaus.
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  • Maize, wheat and other cereals are cultivated on the elevated plateaus, with the fruits and vegetables of the temperate zone, and the European in Bogota is able to supply his table very much as he would do at home.
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  • The open plains, "mesas," and plateaus of the north support large herds of cattle, and several cattle ranches have been established on the Meta and its tributaries.
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  • The flat and round-topped hills (kopjes), which are very numerous on the various plateaus, scarcely afford relief to the eye, which searches the sun-scorched landscape, usually in vain, for running water.
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  • Besides these pans there are in the interior plateaus many shallow pools or vleis whose extent varies according to the dryness or moisture of the climate.
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  • These form the plains and plateaus of the interior.
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  • Among the south-eastern plateaus antelope are found at all seasons, and deer and big-horn (mountain sheep), and occasionally a few elk, in the winter.
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  • Sage-hens are occasionally seen on the dry plateaus and valleys, especially in Harney county.
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  • They are the margins of the great sandstone plateaus, from l000 to 2000 ft.
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  • The group is made up of an irregular series of terraced plateaus, rising here and there into rounded summits, and intersected in various directions by narrow, deep valleys.
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  • Agriculture is carried on chiefly on the plateaus of the Lower Harz; but there is excellent pasturage both in the north and in the south.
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  • The remainder consists of a region of heaths and plateaus to the northeast of the Gave de Pau, and of hills divided by numberless fertile valleys to the west of that river.
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  • The wild camel inhabits the lonely plateaus south of the Ala-shan.
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  • The Maymyo subdivision has very fine plateaus of 3000 to 3600 ft.
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  • They are really a chain of minor plateaus which rise 4500 to 6250 ft.
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  • Immediately west of the watershed are two small plateaus covered with basaltic debris, near el-Jish and Kades.
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  • Though rocky and difficult, Upper Galilee is not barren, the soil of the plateaus is rich, and the vine flourishes in the higher hills, especially in the neighbourhood of Kefr Bir'im.
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  • The Triassic sandstones and marls, with marine Rhaetic beds above, are preserved mainly round the basaltic plateaus of the north-east, and extend for some distance into county Down.
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  • The Lower Lias appears at intervals under the scarp of the basaltic plateaus, and contributes, as in Dorsetshire and Devonshire, to the formation of landslips along the coast.
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  • This chalk appears to underlie nearly the whole basaltic plateaus, appearing as a fringe round them, and also in an inlier at Templepatrick.
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  • The more deep-seated type of these rocks is seen in the olivine-gabbro mass of Carlingford Mountain; but most of the igneous region became covered with sheets of basaltic lava, which filled up the hollows of the downs, baked the gravels into a layer of red flints, and built up, pile upon pile, the great plateaus of the north.
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  • The volcanic plateaus clearly at one time extended far west and south of their present limits, and the denudation of the lava-flows has allowed a large area of Mesozoic strata also to disappear.
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  • Probably before this period the movements of subsidence had set in which faulted the basalt plateaus, lowered them to form the basin of Lough Neagh, and broke up the continuity of the volcanic land of the North Atlantic area.
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  • But this lower region is broken up by masses of hills, with several elevated plateaus, especially in the south-west and south.
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  • Here the general contour of the country may be described as a succession of small plateaus decreasing in elevation to the extreme south.
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  • A succession of plateaus descends from the highest ridges on the north to the south, where a series of small ghats march with the nizam's territory.
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  • The small fertile valleys between the plateaus are watered by streams during the greater portion of the year, while wells of particularly good and pure water are numerous.
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  • Elsewhere the coast lowlands merely form the lowest steps of the system of terraces which constitutes the ascent to the inner plateaus.
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  • These four river-basins occupy the greater part of the lower plateaus of North and West Africa, the remainder consisting of arid regions watered only by intermittent streams which do not reach the sea.
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  • Of the rivers flowing to the Indian Ocean the only one draining any large part of the interior plateaus is the Zambezi, whose western branches rise in the west coast highlands.
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  • The more humid regions have a richer vegetation - dense forest where the rainfall is greatest and variations of temperature least, conditions found chiefly on the tropical coasts, and in the west African equatorial basin with its extension towards the upper Nile; and savanna interspersed with trees on the greater part of the plateaus, passing as the desert regions are appNoached into a scrub vegetation consisting of thorny acacias, &c. Forests also occur on the humid slopes of mountain ranges up to a certain elevation.
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  • Of the grasses of Africa alfa is very abundant in the plateaus of the Atlas range.
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  • The intervening plains and plateaus an now for the most part covered by Tertiary deposits, which am spread over much of the ancient massif.
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  • A different aspect is presented by the grass steppes of Murcia, La Mancha, the plateaus of Guadix and Huescar in the province of Granada, &c., all of which are covered chiefly with the valuable esparto grass (Macrochloa tenacissinla).
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  • Excluding this transitional zone, the Sudan may be described as a moderately elevated region, with extensive open or rolling plains, level plateaus, and abutting at its eastern and western ends on mountainous country.
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  • On the north it descends abruptly to the Black Sea; on the south it breaks down in rugged terraces to the lowlands of Mesopotamia; and on the east and west it sinks more gradually to the lower plateaus of Persia and Asia Minor.
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  • In the west of the northern peninsula the interior consists in part of plateaus of considerable extent enclosed by the coast ranges.
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  • The lakes of Argentina are exceptionally numerous, although comparatively few are large enough to merit a name on the ordinary general map. They vary from shallow, saline lagoons in the north-western plateaus, to great, picturesque, snow-fed lakes in the Andean foothills of Patagonia.
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  • The Vosges are buttressed on the west by the Faucilles, which curve southwards to meet the plateau of Langres, and by the plateaus of Haute- 20 E 4 F 6 G
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  • In the Shan States there are a few open plateaus, fertile and well populated, and Maymyo in the Mandalay district, the hill-station to which in the hot weather the government of Burma migrates, stands in the Pyin-u-lwin plateauYsome 3500 ft.
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  • Every kind of terrain is tenanted, from dense, moist and hot forests at the level of the sea to arid deserts, high plateaus and mountains.
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  • The weathering of this desert area is probably faimly rapid, and the agents at work are principally the rapid heating and cooling of the rocks by day and night, and the erOsive action of sand-laden wind on the softer lnyers; these, aided by the occasional rain, are ceaselessly at work, and produce the successive plateaus, dotted with small isolated hills and cut up by valleys (wadis) which occasionally become deep ravines, thus foiming the principal type of scenery of these deserts.
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  • The total area of the Karroo plateaus is stated to be over ioo,000 sq.
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  • Shallow sheets of water termed vleis, usually brackish, accumulate after heavy rain at many places in the plateaus; in the dry seasons these spots, where the soil is not excessively saline, are covered with rich grass and afford favourite grazing land for cattle.
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  • Of the mountains belonging to the table-land the most continuous are those of the Cantabrian chain, which stretches for the most part from east to west, parallel to the Bay of Biscay, btit Mountains, ultimately bends round towards the south between Leon and Galicia (see CANTABRIAN MOUNTAINS) - A peculiar feature of this chain, arid of the neighboring parts of the table-land, is the number of the parameras or isolated plateaus, surrounded by steep rocky mountains, or even by walls of sheer cliff.
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  • Minerals, fossils, mountains, plains and plateaus are all focused upon, and kids may also learn how to read maps as well as draw their own.
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  • You can find coniferous forests here, as well as tundra, and even "the Arctic" plateaus with unearthly landscapes, troubled only by freezing winds.
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  • As evident in a line graph of the historical LIBOR rate USD, the numbers for all of these rates went through basically the same peaks, valleys and plateaus over the course of the 1990s and 200s.
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  • If you have been taking yoga for a while, a private yoga lesson can help you get past plateaus in your practice or help you explore and deepen your practice.
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  • Use it as a tool for reaching ever higher and higher plateaus in your waitressing career, and an inspiration always to aspire to more in life in general!
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  • Plateaus happen to just about anyone, especially those who are trying to lose a lot of weight.
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  • Now that we've got a better idea of what causes plateaus, let's find a way to get over them as quickly as possible.
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  • It is often used as a method of getting past aerobic exercise plateaus.
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  • In the north, however, the hot lowlands are malarial and unsuited to north European settlement, while the dry, elevated plateaus are celebrated for their healthiness, those of Catamarca having an excellent reputation as a sanatorium for sufferers from pulmonary and bronchial diseases.
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  • On the arid plateaus of the north-west, the guanaco and vicuna are still to be found, though less frequently, together with a smaller species of viscacha (Lagidium cuvieri).
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  • The same is true of the plateaus of Livonia, " Wendish Switzerland," and the government of Kovno, which do not exceed moo ft.
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  • Taking their origin from a series of lacustrine basins scattered over the plateaus and differing slightly in elevation, the Russian rivers describe immense curves before reaching the sea, and flow with a very gentle gradient, while numerous large tributaries collect their waters from over vast areas.
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  • Straggling forests, mainly of conifers, characterize the high plateaus of central Utah.
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  • Frost and snow are occasionally experienced among the mountains and on the inland plateaus, but never along the coast.
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  • To the south the province is shut in by the wide mountainous tract which stretches from the Bay of Bengal through Bastar to the Godavari, and west of that river is continued onward to the rocky ridges and plateaus of Khandesh by a succession of ranges that enclose the plain of Berar along its southern border.
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  • The provinces may be divided into two tracts of upland and three of plain, consisting of the Vindhya and Satpura plateaus, and the Berar, Nagpur and Chhattisgarh plains.
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  • The northern part can best be regarded as a low plateau (once marine sediments) sloping southward, traversed by the large diluvial valleys of the Mississippi, Red and Ouachita rivers, and recut by smaller tributaries into smaller plateaus and rather uniform flat-topped hills.
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  • The northern and western provinces of Cambodia which fall outside the densely populated zone of inundation are thinly peopled; they consist of plateaus, in many places thickly wooded and intersected by mountains, the highest of which does not exceed 5000 ft.
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  • Water is plentiful in the Elburz, and situated in well-watered valleys and gorges are innumerable flourishing villages, embosomed in gardens and orchards, with extensive cultivated fields and meadows, and at higher altitudes small plateaus, under snow until March or April, afford cool camping grounds to the nomads of the plains, and luxuriant grazing to their sheep and cattle during the summer.
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  • Vast numbers of small lakes stud the Vitim and upper Selenga plateaus; the lower valley of the latter river contains the Goose Lake(Gusinoye).
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  • Of the great inland region, which includes the arid campos of the north, the partially-wooded plateaus of Minas Geraes, Goyaz and Matto Grosso, the temperate highlands of the south, and the tropical lowlands of the Paraguay basin, no adequate description can be given without taking each section in detail, which can be done to better advantage in describing the individual states.
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  • The valleys and coast belt, though practically free from malarial fever, are hot and humid, and fires in dwelling houses are seldom required even in the coolest months; the lower plateaus are cool and the air dry; the uplands are bracing and often very cold, with snow on the ground in winter.
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  • The downs or plateaus occupy all the southern part of the country, sloping gradually westward from the Drakensberg.
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  • The banken veld district is also generally healthy though hotter than the plateaus, and malarial fever prevails in the lower valleys.
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  • Salt is obtainable from the many pans in the plateaus, notably in the Zout(salt)pansberg, and was formerly manufactured in considerable quantities.
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  • Fruit farming is a thriving industry, the slopes of the plateaus and the river valleys being specially adapted for this culture.
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  • The population is estimated at about 6,124,000 The country consists chiefly of a range of plateaus and wooded mountains, running north and south and declining on the coast to a narrow band of plain varying between 12 and 50 m.
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  • The ascent to the plateaus is generally by three tiers of hills rising one behind the other.
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  • Through these gorges dash magnificent cascades, others leaping the escarpments of the plateaus in waterfalls of great volume and depth.
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  • The rest of the country is occupied by ranges of hills and plateaus 2000 to 4000 ft.
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  • Over both sandstone and granite great sheets of lava have been poured, and these, protecting the softer beds beneath from further denudation, now stand up as the high plateaus and hills called harra.
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  • Within the limits indicated the country consists mainly of sandy desert and rugged and arid steppes and plateaus through which the Nile forces its way to Upper Egypt.
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  • In the north the desert plateaus are comparatively low, but from Cairo southwards they rise to 1000 and even 1500 ft.
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  • Most of these main streams flow through profound gorges in a tropical climate, while the upper slopes yield products of the temperate zone, and the plateaus above are cold and bleak, affording only pasture and the hardiest cereals.
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  • High plateaus like that of Pamir (the " Roof of the World ") and Armenia, and lofty mountain chains like the snow-clad Caucasus, the Alai, the Tian-shan, the Sayan Mountains, exist only on the outskirts of the empire.
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  • The southwest monsoon which brings rain in Cochin-China coincides with the dry season in Annam, the reason probably being that the mountains and lofty plateaus separating the two countries retain the precipitation.
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