Mountain-ranges sentence example

mountain-ranges
  • He was studying the mountain ranges intently.

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  • Beyond them mountain ranges faded into shades of blue in the humid air.

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  • The basins of the Parana and Paraguay are separated by low mountain ranges extending north from the sierras of Paraguay.

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  • Only low brush could grow in so small a space... no trees to prevent a vehicle from plunging into the forested mountain ranges below and beyond.

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  • They were everywhere, like the mountain ranges surrounding their hideout.

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  • There is no other instance in Europe of a basin of similar extent equally clearly characterized—the perfectly level character of the plain being as striking as the boldness with which the lower slopes of the mountain ranges begin to rise on each side of it.

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  • It is occupied by the branches and offshoots of the mountain ranges which separate it from the great plain to the north, and send down their lateral ridges close to the water's edge, leaving only in places a few square miles of level plains at the mouths of the rivers and openings of the valleys.

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  • Nor do the highest summits form a continuous ridge of great altitude for any considerable distance; they are rather a series of groups separated by tracts of very inferior elevation forming natural passes across the range, and broken in some places (as is the case in almost all limestone countries) by the waters from the upland valleys turning suddenly at right angles, and breaking through the mountain ranges which bound them.

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  • This mountainous tract, which has an average breadth of from 50 to 60 m., is bounded west by the plain of Campania, now called the Terra di Lavoro, and east by the much broader and more extensive tract of Apulia or Puglia, composed partly of level plains, but for the most part of undulating downs, contrasting strongly with the mountain ranges of the Apennines, which rise abruptly above them.

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  • Elie de Beaumont, in his speculations on the relation between the direction of mountain ranges and their geological age and character, was feeling towards a comprehensive theory of the forms of crustal relief; but his ideas were too geometrical, and his theory that the earth is a spheroid built up on a rhombic dodecahedron, the pentagonal faces of which determined the direction of mountain ranges, could not be proved.'

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  • Differences in land forms do not exert great influence on the distribution of living creatures directly, but indirectly such land forms as mountain ranges and internal drainage basins are very potent through their action on soil and climate.

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  • Next in importance comes a mountain range, but here there is often difficulty as to the definition of the actual crest-line, and mountain ranges being broad regions, it may happen that a small independent state, like Switzerland or Andorra, occupies the mountain valleys between two or more great countries.

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  • Its principal mountain ranges were Cebenna or Gebenna (Cevennes) in the south, and Jura, with its continuation Vosegus or Vogesus (Vosges), in the east.

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  • The northern section is more broken and rugged; barren ridges and low rocky mountain-ranges, interspersed with fertile valleys, being its characteristic features.

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  • This plateau, however, is not a plain, but contains many buttes and mesas and isolated mountain ranges rising from 1000 to 8000 ft.

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  • The surface of Minas Geraes is broken by mountain ranges and deeply eroded rivercourses, the latter forming fertile valleys shut in by partly barren uplands, or campos.

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  • Hence the study of the mountain ranges of a continent is, for a proper apprehension of its physical conditions and characteristics, as essential as the examination of its extent and position in relation to the equator and poles, and the configuration of its coasts.

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  • North of this lies a broad belt in which the Mesozoic deposits and even the lower divisions of the Tertiary system are thrown into folds which extend in a series of arcs from west to east and now form the principal mountain ranges of central Asia.

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  • The Kuen-lun, Nan-shan and the mountain ranges of southern China are, perhaps, of earlier date, but nevertheless they lie in the same belt.

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  • There are, it is true, mountain ranges which are formed of folded beds; but in many cases the direction of the chains is different from that of the folds, so that the ranges must owe their elevation to other causes; and the folds, moreover, are of ancient date, for the most part Archaean or Palaeozoic. The configuration of the region is largely due to faulting, trough-like or tray-like depressions being formed, and the intervening strips, which have not been depressed, standing up as mountain ridges.

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  • Structurally, the folds of this region are of ancient date; but the area is crossed by a series of depressions formed by faults, and the intervening strips, which have not been depressed to the same extent, now stand up as mountain ranges.

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  • But within this region there is a very great variation between the vegetation of the more humid and the more arid regions, while the characteristics of the flora on the higher mountain ranges differ wholly from those of the plains.

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  • Climate.-Owing in part to the great differences in altitude in different regions of Caucasia and in part to the directions in which the mountain ranges run, and consequently the quarters towards which their slopes face, the climate varies very greatly according to locality.

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  • The tree is very widely distributed, growing abundantly on most of the mountain ranges of northern and central Europe; while in Asia it occurs at least as far east as the Lena, and in latitude extends from the Altaic ranges to beyond the Arctic circle.

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  • It is abundant in most of the mountain ranges of southern and central Europe, but is not found in the northern parts of that continent.

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  • Physically the country is divided into two regions, the one a series of mountain ranges occupying the northern and eastern portions of the kingdom, and the other a plain which stretches southwards from Mukden, the capital, to the Gulf of Liao-tung.

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  • Physically Moravia may be described as a mountainous plateau sloping from north to south, just in the opposite direction of the adjoining Bohemia plateau, which descends from south to north, and bordered on three sides by mountain ranges.

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  • According to his view, all mountain ranges parallel to the same great circle of the earth are of strictly contemporaneous origin, and between the great circles a relation of symmetry exists in the form of a pentagonal reseau.

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  • The theory has not found general acceptance, but it proved of great value to geological science, owing to the extensive additions to the knowledge of the structure of mountain ranges which its author made in endeavouring to find facts to support it.

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  • Its semi-arid character is due to the mountain ranges on its northern frontier, which extract the moisture from the north-east trades and leave the Brazilian plateau behind them with a very limited rainfall, except near the Atlantic coast.

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  • The mountain ranges of the east of Brazil, from Cape St Roque to the mouth of the river Plate, are composed chiefly of crystalline and metamorphic rocks.

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  • The Cerro de Oro series is the most important group of these beds and takes a considerable share in the formation of the mountain ranges.

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  • Burma proper is encircled on three sides by a wall of mountain ranges.

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  • West of this line the rocks are chiefly Tertiary and Quaternary; east of it they are mostly Palaeozoic or gneissic. In the western mountain ranges the beds are thrown into a series of folds which form a gentle curve running from south to north with its convexity facing westward.

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  • It is still common in the dense forests which clothe the mountain ranges as high as 8000 feet.

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  • Roads with post-houses at intervals were made over the wildest mountain-ranges and the bleakest deserts for hundreds of miles.

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  • Its surface is roughly broken by mountain ranges extending southward from the Sierra de Ajusco, forming numerous valleys opening southward.

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  • The mountain ranges to the north of the province abound with coal, notably at Chai-tang, Tai-gan-shan, Miao-gan-ling, and Fu-tao in the Si-shan or Western Hills.

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  • From this region the country slopes towards the north-west, and is not distinguished by any considerable mountain ranges.

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  • Aragon consists of a central plain, edged by mountain ranges.

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  • But as each successive range, proceeding south, represents a higher step in the terraced ascent from the desert of Gobi to the plateau of Tibet, the ranges when viewed from the north frequently appear like veritable upstanding mountain ranges, and this appearance is accentuated by the general steepness of the ascent; whereas, when viewed on the other hand from the south, these several ranges, owing to their long and gentle slope in that direction, have the appearance of comparatively gentle swellings of the earth's service rather than of well-defined mountain ranges.

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  • But though the great morphological features of this latitudinal valley forcibly recall the latitudinal valleys of Tibet, the climatic differences give rise to differences between the basins corresponding to the differences between the mountain-ranges themselves.

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  • The mountain ranges in the south are largely inhabited by Miao-tsze, who are the original owners of the soil and have been constantly goaded into a state of rebellion by the oppression to which they have been subjected by the Chinese officials.

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  • In south Oran they determine the principal axes of the mountain ranges.

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  • It is characterized The Basla by numerous disconnected mountain ranges trending north and south, from 30 to 100 in.

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  • Strong mountain ranges follow the trend of the Pacific coast, 150 or 200 m.

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  • The climatic effects of relief are seen directly in the ascent of the higher mountain ranges to altitudes where low temperatures prevail, thus preserving snow patches through the summer on the high summits (over 12,000 ft.) in the south, and maintaining snowfields and moderate-sized glaciers on the ranges in the north.

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  • With this goes a general increase of precipitation with altitude, so that a good rainfall map would have its darker shades very generally along the mountain ranges.

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  • This vast area, shaped like a broad-limbed V or U, with Hudson Bay in the centre, is made up chiefly of monotonous and barren Laurentian gneiss and granite; but scattered through it are important stretches of Keewatin and Huronian rocks intricately folded as synclines in the gneiss, as suggested earlier, the bases of ancient mountain ranges.

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  • Though once consisting of great mountain ranges there are now no lofty elevations in the region except along the Atlantic border in Labrador, where summits of the Nachvak Mountains are said to reach 6000 ft.

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  • Similar wide tracts of less broken country occur, after a mountainous interruption, in northern British Columbia and to some extent in the Yukon Territory, where wide valleys and rolling hills alternate with short mountain ranges of no great altitude.

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  • Nearly all are natives of Europe, or the northern plains and mountain ranges of Asia and North America, though one (Larix Grifthii) occurs only on the Himalayas.

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  • There are no true mountain ranges in Maranhao, those indicated on the maps being only plateau escarpments marking either its northern margin or the outlines of river valleys.

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  • The centre and eastern are occupied by mountain ranges running N.E.

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  • Andalusia consists of a great plain, the valley of the Guadalquivir, shut in by mountain ranges on every side except the S.W., where it descends to the Atlantic. This lowland, which is known as Andalucia Baja, or Lower Andalusia, resembles the valley of the Ebro in its slight elevation above sea-level (300-400 ft.), and in the number of brackish lakes or fens, and waste lands (despoblados) impregnated with salt, which seem to indicate that the whole surface was covered by the sea at no distant geological date.

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  • The numerous affluents which enter it from the north water the beautiful eastern and southern slopes of the Merida, Caraboso and Caracas mountain ranges.

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  • The mountain ranges are spread out, rounded, disconnected, separated by flat valleys relatively of little depth.

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  • Save the last-named, all these peninsulas of Europe are essentially mountain ranges.

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  • Leaving, however, the larger question of the connexion between the great mountain ranges of Europe and Asia, we find that the Alps are formed of a series of wrinkles or folds, one behind another, frequently arranged en echelon.

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  • Three ' mountain ranges traverse the district - the Pegu Yomas, the Karen, and the Nat-taung or- "Great Watershed" - all of which have a north and south direction, and are covered for the most part with dense forest.

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  • Near its south-east corner the Caspian is entered by the Atrek, which drains the mountain ranges of the Turkoman (N.E.) frontier of Persia.

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  • These two mountain ranges unite at their northern extremities with the Vindhya chain of mountains, and thus is formed a vast triangle supporting at a considerable elevation the expanse of table-land which stretches from Cape Comorin to the valley of the Nerbudda.

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  • A row of low hills runs generally parallel to the mountain ranges already noticed, at a distance of 20 to 3om.

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  • Payer reported that from Cape Fligely land (Rudolf Land) stretched north-east to a cape (Cape Sherard Osborn), and mountain ranges were visible to the north, indicating lands beyond the 83rd parallel, to which the names King Oscar Land and Petermann Land were given.

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  • On two sides this area is bordered by belts of folded beds which form on the west the mountain ranges of the Adriatic and Ionian coasts, and on the north the chain of the Balkans.

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  • Though the mountain ranges of Lycia are all offshoots of Mt.

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  • In addition to the climatic changes due to altitude, there are others caused by local arid conditions, by volcanic influences and by the influence of mountain ranges on the temperature and rainfall of certain districts.

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  • In the first of these the mountain ranges are complex, appearing to radiate from a centre at which lies Merj el-Ghuruk, a small plain about 4 m.

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  • The valleys enclosed between the mountain ranges are numerous, fertile, and for the most part of exquisite beauty.

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  • The great peninsula of India, with its lofty mountain ranges behind and its extensive seaboard exposed to the first violence of the winds of two oceans, forms an exceptionally valuable and interesting field for the study of meteorological phenomena.

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  • Submarine mountain ranges connect not only the islands within the archipelago, but also the archipelago itself with Borneo and Celebes, so that only shallow channels connect the interior waters with the Pacific Ocean and the China Sea.

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  • The Philippines appear to be the remnants of a somewhat complex system of mountain arcs, which from their similarity of form and direction seem to be in some way connected with the mountain ranges of Annam.

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  • Crystalline schists occupy a large part of the country, forming all the higher mountain ranges.

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  • They are mentioned by Herodotus among the races conquered by Croesus, and they sent an important contingent to the army of Xerxes in 480 B.C. Xenophon speaks of them as being governed by a prince of their own, without any reference to the neighbouring satraps, a freedom due, perhaps, to the nature of the country, with its lofty mountain ranges and difficult passes.

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  • Conception are fertile coastal plains of considerable extent, separated from the interior deserts by various mountain ranges from 5000 to 7000 ft.

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  • Forest growth in Wyoming is limited to the highest mountain ranges, the most important forests being in the Black Hills region in the N.E., on the lower slopes of the Bighorn Mountains, and in the Rocky Mountain ranges of the N.W.

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  • The low-lying country between the mountain ranges is covered for the most part by Tertiary and Quaternary deposits, but Cretaceous beds occur at several localities.

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  • The region is traversed by the broken mountain ranges which form the N.E.

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  • Between the two mountain ranges lies a broad plain, extending across the island from the bay of Famagusta to that of Morphou on the west, a distance of nearly 60 m., with a breadth varying from i o to 20 m.

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  • In the north and west there are extensive mountain ranges of calcareous formation, intersected by deep ravines; while farther south the land is more level, and there are many fertile valleys.

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  • The mountain ranges of Baluchistan consist chiefly of Cretaceous and Tertiary beds, which are thrown into a series of folds running approximately parallel to the mountain ridges.

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  • Beyond the Indus, to the north-west, the region of mountain ranges which stretches to a junction with the Hindu Kush south of the Pamirs, is usually known as Trans-Himalaya.

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  • The recent deposits, which cover so large a part of the depression between the Eastern and the Western Cordillera, appear to be partly of torrential origin, like the talus-fans at the foot of mountain ranges in other dry regions; but Lakes Titicaca and Pampa Aullaguas (Poopo) were undoubtedly at one time rather more extensive than they are to-day.

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  • This vertical arrangement of climatic zones is modified to some extent (less than in Argentina) by varying rainfall conditions, which are governed by the high mountain ranges crossing one corner of the republic, and also by the prevailing winds.

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  • The mountain-ranges of the interior of Bohemia are the Brdywald (2798 ft.) in the middle; the Tepler Gebirge (2657 ft.), the Karsbader Gebirge (3057 ft.) and the Kaiserwald (3238 ft.), in the north-west part; while the northern corner is occupied by the Mittelgebirge (2739 ft.), a volcanic massif, stretching on both sides of the Elbe.

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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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  • Above the plateau rise several irregular and generally ill-defined mountain ranges which attain altitudes of from 12,000 to over 15,000 ft.

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  • The remaining western portion of the state is lower, belongs in the Great Basin province, and is characterized by north-south mountain ranges separated by desert basins.

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  • Inasmuch as the streams entering the basin have no outlet to the ocean, their waters disappear by evaporation, either directly from alluvial slopes over which they pass, or from saline lakes occupying depressions between the mountain ranges.

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  • This alluvium gives gently sloping or level desert plains, from which isolated mountain ranges rise like islands from the sea.

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  • The mountain ranges of the Basin Region are most frequently formed by faulted and tilted blocks of the earth's crust, which have been carved by stream erosion into rugged shapes.

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  • The valley of the Cauca is much narrower than that of the Magdalena, and between Cartago and Caceres the mountain ranges on both sides press down upon the river and confine it to a narrow canyon.

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  • High temperatures prevail throughout the greater part of the Magdalena and Cauca valleys, because the mountain ranges which enclose them shut out the prevailing winds.

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  • This division is modified, however, by the location of mountain ranges and by elevation.

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  • In the Amazon region there is no great change during the year, and on the northern plains the so-called dry season is one of light rains except where mountain ranges break the sweep of the north-east trades.

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  • Beyond the coast plain, which here and there attains a height of 600 ft., are mountain ranges running parallel to the shore.

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  • The east and south-east winds, which contain most moisture, dissipate their strength against the Drakensberg and other mountain ranges which guard the interior.

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  • Very high mountain ranges usually consist of many ridges, among which rain-clouds are entangled in their ascent, and in such cases precipitation towards the windward side of the main range, though on the leeward sides of the minor ridges of which it is formed, may occur to so large an extent that before the summit is reached the clouds are exhausted or nearly so, and in this case the total precipitation is less on the leeward than on the windward side of the main range; but in the moderate heights of the United Kingdom it more commonly happens from the causes explained that precipitation is prevented or greatly retarded until the summit of the ridge is reached.

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  • Over the whole width of the country from coast to coast, or of the Welsh mountain ranges only, this is so; but it is nevertheless true that the leeward side of an individual valley or range of hills generally receives more rain than the windward side.

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  • The mountain ranges which shut off East Turkestan from the rest of the world rank among the loftiest and most difficult in Asia, and indeed in the world.

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  • Various mountain ranges mark the frontiers of Bosnia, on the west, Turkey on the south-west and south, and Bulgaria on the south and south-east.

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  • At the same time the relative altitudes, or the heights of the mountain ranges above the valleys which flank them, decrease from north to south.

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  • Though generally of slight elevation it contains mountain ranges with peaks rising to 8000 ft.

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  • The wide heated plains of the Sahara, and in a lesser degree the corresponding zone of the Kalahari in the south, have an exceedingly scanty rainfall, the winds which blow over them from the ocean losing part of their moisture as they pass over the outer highlands, and becoming constantly drier owing to the heating effects of the burning soil of the interior; while the scarcity of mountain ranges in the more central parts likewise tends to prevent condensation.

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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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  • On the opposite side of the river, in addition to the cultivated portions of the bank, there is a large tract extending from south of Kuhak, or the Seistan dam (band), to the gravelly soil below the mountain ranges which separate Seistan from Baluchistan and Narmashir.

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  • Here, as in the other great mountain ranges of central Europe, there are evidences of a much wider extension of the glaciers during the Ice age.

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  • The precise line of the western frontier is formed for a considerable length by portions of the chief rivers or by small tributaries, and on the north (between Portugal and Galicia) it is determined to a large extent by small mountain ranges.

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  • While, again, continuous mountain ranges and broad plains and table-lands give the prevailing character to the scenery, there are, on the one hand, lofty isolated peaks, such as Monseny, Montserrat and Mont Sant in Catalonia, the Pea Golosa in Valencia, Moncayo on the borders of Aragon and Old Castile, and, on the other hand, small secluded valleys, such as those of Vich and Olot among the Catalonian Pyrenees.

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  • The greater part of the interior of Spain is composed of a table-land bounded by the Cantabrian Mountains in the north and the Sierra Morena in the south, and divided into two by a series Central of mountain ranges stretching on the whole from east Table-land to west.

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  • Formerly the ibex was common on the mountain-ranges of Germany, Switzerland and Tirol, but is now confined to the Alps which separate Valais from Piedmont, and to the lofty peaks of Savoy, where its existence is mainly due to game-laws.

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  • Beyond this plain rise the mountain ranges already mentioned.

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  • On the western side one is reminded of scenes in the highlands of Ross-shire and Inverness-shire in Scotland, from the picturesque character of the blue, white, and pinkish crystalline peaks and the fantastic outlines of the mountain ranges which rise abruptly to a height of from z000 to nearly 3000 feet above the Button Grass.

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  • Fayetteville was where her family had decided she would go to college – close to them and safe, but she longed for those layered mountain ranges where wildlife abounded.

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  • How about the adventure of joining an expedition into the world's greatest mountain ranges.

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  • In the northeast and along the western corridor are low lightly wooded mountain ranges of mainly volcanic origin.

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  • The rock wren feeds chiefly in open slopes on mountain ranges.

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  • Laristan consists mainly of mountain ranges in the north and east, and of arid plains varied with rocky hills and sandy valleys stretching thence to the coast.

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  • Central America it is still common in the dense forests which clothe the mountain ranges as high as 8000 or goon ft.

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  • The mountain ranges which form part of the great Mexican Plateau consist of two marginal chains known as the Sierra Madre Occidental, on the west, the Sierra Madre Oriental, on the east, and a broken, weakly-defined chain of transverse ranges and ridges between the 18th and 10th parallels known as the Cordillera de Anahuac. All these chains are known locally under diverse names.

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  • Some things you can find on topographic maps free online are volcanoes and earthquake fault lines, mountain ranges and deserts.

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  • While not equipped with the massive mountain ranges of Colorado or California, New York has its own impressive mountain geography that supports numerous ski resorts.

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  • Ski vacations are available in European countries that contain part of the Alps, Carpathian or Pyrennes mountain ranges within their borders.

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  • French skiing is offered across several mountain ranges including the French Alps and the Jura mountains.

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  • While images of Italy usually include beautiful sea views and cities built hundreds of years ago, the Italian mountain ranges shouldn't be overlooked as an opportunity for skiing.

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  • Eastern Oregon is much drier than the west side of the state, because mountain ranges block weather systems from the coast and keep the area but warmer and drier.

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  • The North Coast benefits from a proximity to a maritime climate that is buffered by steep mountain ranges.

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  • It is the eighth largest lake in the world, and is situated between the high peaks of both the Carson and Sierra Nevada mountain ranges.

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