Watershed Sentence Examples

watershed
  • The line of the highest summits and of the watershed ranges is about 30 to 40 m.

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  • The lake in Peru which is third in size is that of Parinacochas on the coast watershed, near the foot of the snowy peak of Sarasara.

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  • The present caravan road keeps the high ground to the west near the watershed, and avoids the Pass of Michmash altogether.

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  • It is known that the Kafirs occupy the crest of the Hindu Kush eastwards of the Khawak, but how far they extend north of the main watershed is not ascertainable.

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  • It surmounts the watershed by means of Sapperton tunnel, 2 m.

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  • Between the Jur and the Nile, and following a course generally parallel with these rivers, several streams run north from the Congo-Nile watershed and join the Bahr-el-Ghazal.

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  • Its mountains, which belong to the Adriatic watershed, and form a continuation of the Montenegrin highlands, are less rounded and more dolomitic in character.

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  • However, the campaign against the Newbury bypass marks a watershed in transport policy.

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  • The frontier was to follow the watershed of the Julian Alps from Tarvis as far east as the Snjeznik (Schneeberg) and to reach the sea just east of Volosca, Fiume being expressly reserved to Croatia.

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  • On the east side of the watershed the ground slopes rapidly from its height of 2500 ft.

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  • But, a little farther, at the Dreiherrenspitze (11,500 ft.) we have to choose between following the watershed southwards, or keeping due east along the highest crest of the Greater Tauern Alps.

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  • Finally our watershed turns south and ends near the great limestone plateau of the Birnbaumerwald, between Laibach and Gorz.

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  • In the Eastern Alps the longest glacier is the Pasterze (rather over 64 m.), which is not near the true main watershed, though it clings to the slope of the Greater Tauern range, east of the Dreiherrenspitze.

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  • But the next two longest glaciers in the Eastern Alps (the Hintereis, 64 m., and the Gepatsch, 6 m.) are both in the Oetzthal Alps, and so close to the true main watershed.

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  • These are usually divided into three groups, the Central (the watershed between the two passes named), the Western or French, and the Eastern or Italian; in the following lists the initials " C," " W," and " E " show to which group each peak and pass belongs.

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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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  • Mecklenburg lies wholly within the great North-European plain, and its flat surface is interrupted only by one raiIge of low hills, intersecting the country from south-east to north-west, and forming the watershed between the Baltic Sea and the Elba.

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  • To the north-west these hills form the watershed between the valleys of the Arghandab and the Tarnak, until they are lost in the mountain masses of the Hazarajat - a wild region inhabited by tribes of Tatar origin, which effectually shuts off Kandahar from communication with the north.

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  • To the north-west, and parallel to the long ridges of the Tarnak watershed, stretches the great road to Kabul, traversed by Nott in 1842, and by Stewart and subsequently by Roberts in 1880.

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  • This is the most direct route to northern India, but it involves the passage of some rough country, across the great watershed between the basins of the Helmund and the Indus.

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  • Near Eupen, south of Aix-la-Chapelle, it turns southward, and near Anon south-east as far as the crest of the Vosges mountains, which it follows upto Belfort, traversing there the watershed of the Rhine and the Doubs.

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  • To adopt a figure, it is probable that the sources from which the two streams of life - animal and vegetable - spring may not be separable by a well-defined watershed at all, but consist of a great level upland, in which the waterways anastomose.

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  • Recognizing this, the corporation of Birmingham, under an act of 1892, acquired the watershed of the Elan and Claerwen, and constructed on the Elan three impounding reservoirs whence the water is conducted through an aqueduct to Birmingham (q.v.).

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  • The watershed consequently keeps close to the western seaboard, and indeed in some places is not above a mile and a half from the shore.

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  • On the southern side of the watershed, in Dumfriesshire and Galloway, the valleys run generally transversely from north-west to south-east.

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  • The breakdown of the watershed between the Firths of Clyde and Forth exposes southern Perthshire, the counties of Clackmannan and Kinross, and nearly the whole of Fife to the clouds and rains of the west, and their climates are consequently wetter than those of any others of the eastern slopes of the country.

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  • The watershed of this system is so placed that from two-thirds to three-fourths of the country is on its western side.

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  • East of the watershed are a number of valleys running to the Ghor; the most remarkable of these are the Wadi el-Bireh and the Wadi Jalud, the latter containing the river that flows from the fine spring called 'Ain Jalud.

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  • For the greater part the principal mountains are near the watershed; they include Jebel Fuku`a (Gilboa), a range that forms the watershed at the eastern extremity of the plain of Esdraelon.

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  • On the eastern side of the watershed the most important feature is perhaps the great valley system that connects the Mukhnah (the plain south of Nablus) with the Ghor - beginning with the impressive Wadi Bilan and proceeding through the important and abundantly watered Wadi Far`a.

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  • On the west side of the watershed the mountainous district extends about half way to the sea, broken by deep valleys and passes.

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  • The main watershed of the peninsula lies towards the east coast; therefore such elevated ground as exists is found on the east, while the western slope is gentle and consists of a low sandy plain of slight undulation.

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  • With the exception of the Dniester, which skirts its northern border, Bukovina belongs to the watershed of the Danube.

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  • From Nushki it crosses the Helmund desert, touching the crest of a well-defined mountain watershed for a great part of the way, and, leaving Chagai to Baluchistan, it strikes nearly west to the Persian frontier, and joins it on the Koh-i-Malik Siah mountain, south of Seistan.

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  • At a point which is not far east of the Kabul meridian an offshoot is directed southwards, which becomes the water-parting between the Kurram and the Logar at Shutargardan, and can be traced to a connexion with the great watershed of the frontier dividing the Indus basin from that of the Helmund.

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  • This main watershed retains its high altitude far to the south.

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  • These beds are conformably succeeded, along the Central Asian watershed, by a continuous series of strata which apparently represent the Permian, Trias and Jurassic of Europe.

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  • The Jurassic beds are followed, generally with perfect conformity, by the Cretaceous, which covers a large part of Afghan Turkestan and probably forms the greater part of the ranges which run south and south-west from the principal watershed.

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  • It rises very gradually from the sea at either end; the lowest point of the watershed between the Punjab rivers and the Ganges is about 924 ft.

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  • Near the watershed it is generally more; but there is here no ridge of high ground between the Indus and the Ganges, and a very trifling change of level would often turn the upper waters of one river into the other.

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  • From the gorge of the Indus to that of the Brahmaputra, a distance of 1400 m., the Himalayas form an unbroken watershed, the northern flank of which is drained by the upper valleys of these two rivers; while the Sutlej, starting from the southern foot of the Kailas Peak, breaks through the watershed, dividing it into two very unequal portions, that to the north-west being the smaller.

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  • It comprises the valleys of the Brahmaputra and Surma rivers, together with the mountainous watershed which intervenes between them.

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  • The difficulty of ascertaining the true line of the watershed had been very great, but the result was eminently successful.

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  • The watershed between the Rhine and the Eem is formed by a plateau of sand and gravel hills which extend from the southeast corner on the Rhine to Zeist near Utrecht, and also northwards to Huizen on the Zuider Zee.

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  • On the east the watershed of the Caspian gradually increases in breadth, the foot of the scarp extending considerably to the north of the south-eastern angle of that sea, three degrees east of which it turns to the south-east, parallel to the axis of the Kopet Dagh.

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  • Four rivers belonging essentially to Persia, in reference to the Caspian watershed, are the Seafid Rud or Kizil Uzain on the southwest, the Herhaz on the south and the Gurgan and Atrek at the south-eastern corner of that inland sea.

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  • The sources of the Taia, and those of the Great Bum, are near to those of the Niger, the watershed between the coast streams and the Niger basin here forming the frontier.

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  • The greater part of the Serra da Estrella constitutes the watershed between the Mondego and Zezere.

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  • Of the ranges extending south from the Cordillera Real and branching out between the 18th and 19th parallels, the more prominent are the Frailes which forms the eastern rampart of the great central plateau and which is celebrated for its mineral deposits, the Chichas which runs south from the vicinity of Potosi to the Argentine frontier, and the Livichuco which turns south-east and forms the watershed between the Cachimayo and Pilcomayo.

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  • Bohemia belongs to the watershed of the Elbe, which rises within the territory and receives on the right the Iser and the Polzen, and on the left the Adler; the Eger with its affluent the Tepl; the Biela and the Moldau.

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  • They form the principal watershed not only of the province of Bauchi, but of the protectorate of Northern Nigeria.

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  • The other strange feature is that from near Isola in the upper Tinee valley southwards the political frontier does not coincide with the physical frontier, or the main watershed of the Alpine chain; the reason (it is said) is that in 1860 all the higher valleys of the Maritime Alps (on both sides of the watershed) were expressly excepted from the treaty of cession, in order that Victor Emmanuel II.

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  • Watersheds are rarely used as boundaries for any distance; but, although slightly overlapping the watershed on all sides, Yorkshire is very nearly coincident with the basin of the Ouse.

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  • East of Adai-khokh, by what seems a strange freak of nature, the granitic [main] range is rent over and over again to its base by gorges, the watershed being transferred to the parallel chain of clay slates.

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  • Lumber is floated down the rivers of the Carpathian watershed to the Danube, and so exported to Turkey and Bulgaria; casks, shaped planks and petroleum drums go chiefly to Austria and Russia.

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  • A few rivers belong to the Atlantic side of the watershed, the chief being the Loire, which rises on the western borders of the department, and the Allier, which for a short distance separates it from Lozere.

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  • The first of these extends from the southern border at Markelo to the Lemeler hill (262 ft.) near the confluence of the Vecht and Regge, and forms the watershed between the Regge and the Salland streams (Sala, whence Salis, Isala, Ysel), which unite at Zwolle to form the Zwarte Water.

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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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  • It divides on the Panama frontier, the easterly branch forming the watershed between the Atrato and the rivers of eastern Panama, and serving as the frontier between the two republics.

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  • The two main objects of the expedition were the suppression of slavery by means of civilizing influences, and the ascertainment of the watershed in the region between Nyasa and Tanganyika.

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  • The inner chain of mountains forms the watershed of the colony.

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  • In English it has been called indifferently the " catchment basin," the " gathering ground," the " drainage area " and the " watershed."

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  • Thus the figure and area of a surface watershed may not be coincident with that of the corresponding underground watershed; and the flow in any watercourse, especially from a small watershed, may, by reason of underground flow from or into other watersheds, be disproportionate to the area apparently drained by that watercourse.

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  • When no reservoir exists, the volume of continuous supply from any watershed area Dry is evidently limited to the minimum, or, so-called, extreme dry weather flow of the stream draining it.

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  • The neglect of these facts has led to many errors in estimating the mean rainfall on watershed areas from the fall observed at gauges in particular parts of those areas.

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  • In the simplest case of a single mountain valley to be used for the supply of an impounding reservoir, the rainfall should be known at five points, three being in the axis of the valley, of which one is near the point of intersection of that axis with the boundary of the watershed.

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  • If, therefore, instead of regarding only the mean rainfall of several gauges over a series of years, we compare the relative falls in short intervals of time among gauges yielding the same general averages, the discrepancies prove to be very great, and it follows that the maximum possible intensity of discharge from different areas rapidly increases as the size of the watershed decreases.

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  • As an example, assume that we can conveniently construct a reservoir to contain, in addition to bottom water not to be used, 200,000 gallons for each acre of the watershed above the point of interception by the proposed dam.

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  • In the same manner it will be found that by means of a reservoir having an available capacity of only 118,000 gallons per acre of the watershed, we may with the same rainfall and evaporation secure a daily supply of 1085 gallons per acre.

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  • The church was rebuilt outside the watershed, and the remains from the old churchyard were removed to a new cemetery adjoining it.

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  • Between the Katonga and the Nile outlet, the rivers which rise close to the lake drain away northward, the watershed being the lake shore.

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  • It is the southern watershed of a tortuous, low chain of mountains running, roughly, east and west.

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  • Thessaly was further subdivided into four districts, of which Pelasgiotis embraced the lower plain of the Peneius, and Hestiaeotis and Thessaliotis respectively the northern and the southern portions of the upper plain; while the fourth, Phthiotis, which lies towards the south-east, was geographically distinct from the rest of the country, being separated from it by a watershed.

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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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  • To the north is an intervening watershed between Bajour and the small state of Dir; and it is over this watershed and through the valley of Dir that the new road from Malakand and the Punjab runs to Chitral.

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  • The country is a moderately elevated plateau sloping northward from the higher ground marking the Congo-Nile watershed.

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  • This western chain forms a secondary watershed separating the basin of the Yei, a large river, some 400 m.

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  • All these ranges, except the Uskoken Gebirge, constitute the central watershed of the kingdom, between the Drave and Save.

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  • It is joined by the Sotla, Krapina, Lonja, Ilova, Pakra and Oljana, which drain the central watershed; but its only large tributaries are the Una, a Bosnian stream, which springs in the Dinaric Alps, and skirts the Croatian border for 40 m.

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  • The main line eastward from Agram passes through Brod, where it meets the Bosnian system, and on to Belgrade; throwing out two branch lines to Brcka and Samac in Bosnia, and several branches on the north, which traverse the central watershed, and cross the Hungarian frontier.at ZAkAny, Barcs, Esseg, Erdar and Peterwardein.

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  • As the highlands of Austria form part of the great watershed of Europe, which divides the waters flowing northward into the North Sea or the Baltic from those flowing southward or eastward into the Mediterranean or the Black Sea, its rivers flow in three different directions - northward, southward and eastward.

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  • It would appear that either Libyan (Fula) or, less probably, Hamitic, blood enters into the composition of the Zandeh peoples on the Nile-Congo watershed.

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  • A narrow watershed separates it from the headwaters of the o P streams flowing south-west through Sierra Leone.

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  • The Douro (485 m.) and the Ebro (466 m.) flow respectively south-west to the Atlantic at Oporto, and south-east to the Mediterranean at Cape Tortosa, from their sources in the great northern watershed.

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  • The latter is buttressed against hills at a much higher elevation than the Kharan desert, which is separated from the great expanse of the Helmund desert within the borders of "Afghanistan by a transverse band of serrated hills forming a distinct watershed from Nushki to Seistan.

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  • The plateau has a gradual fall from the watershed near Yarim, 8500 ft.

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  • Beyond the Kaukkwe there is a ridge of hills, which starts at Leka, near Mogaung, and diverges to the south, the eastern ridge dividing the Kaukkwe from the Mosit, and the western forming the eastern watershed of the Nam Yin and running south into Katha.

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  • The range of hills which runs between Ajmere and Nasirabad marks the watershed of the continent of India.

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  • These form the continental watershed, but in this region erosion is taking place so rapidly that the day is not far distant when Lakes La Plata and Fontana, situated to the east at a height of 3000 ft.

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  • To the north of this mountain, situated at the watershed of the Andes, extends a lofty region comprising peaks such as Chimbote (18,645 ft.) and Mount Polleras (20,266 ft.).

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  • Karl Marx as Watershed As we all know, Latin American liberation theologians are deeply engaged with Marxism.

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  • The road crosses a minor watershed in its short journey between the two stations.

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  • The end of Dental school represents a watershed in the life of many Dentists.

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  • What's more, having reached a watershed in my personal life I was ready for a career change anyway.

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  • It includes the entire watershed of the South Alligator River, also the East Alligator, West Alligator and Wildman Rivers.

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  • Scheduling Family Viewing Policy This fixes the nine o'clock watershed.

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  • Junk food advertising could be banned till the 9pm watershed.

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  • In 1881 a treaty was signed which provided that the boundary line should follow the highest crests of the Andes forming the watershed as far south as the 52nd parallel,thence east to the 10th meridian and south-east to Cape Dungeness at the eastern entrance to the Straits of Magellan.

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  • But the 18th degree of latitude had been reached, where the watershed divided the rivers of the Gulf of Carpentaria from the Victoria river, flowing towards the north-west coast.

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  • The whole of the land which directs drainage towards one river is known as its basin, catchment area or drainage area - sometimes, by an incorrect expression, as its valley or even its watershed.

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  • The boundary line between one drainage area and others is rightly termed the watershed, but on account of the ambiguity which has been tolerated it is better to call it water-parting or, as in America, divide.

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  • The inner slopes and ranges of the Elburz south of the principal watershed, generally the central one of the three principal ranges which are outside of the fertilizing influence of the moisture brought from the sea, have little or no natural vegetation, and those farthest south are, excepting a few stunted cypresses, completely arid and bare.

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  • Upper Austria belongs to the watershed of the Danube, which flows through it from west to east, and receives here on the right the Inn with the Salzach, the Traun, the Enns with the Steyr and on its left the Great and Little Mühl rivers.

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  • Throughout the whole of the Thames watershed, and especially in the 3800 sq.

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  • The lake really lies on the watershed between the two, and is probably a glacial relic. Its contribution to either infant stream appears to depend on conditions of overflow determined by the blocking of ice masses towards one end.

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  • Already in 1884 a protocol had been signed between the contending parties, by which it was agreed that the frontier should follow the line where " the highest peaks of the Andine ranges divide the watershed."

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  • Difference of opinion, therefore, arose as to the interpretation of the protocol, the Argentines insisting that the boundary should run from highest peak to highest peak, the Chileans that it should follow the highest points of the watershed.

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  • But this gives no correct idea of the true character of the Darling, for it can hardly be said to drain its own watershed.

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  • From the sources of its various tributaries to the town of Bourke, the river may be described as draining a watershed.

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  • Below this the watershed of the Apennines is too near to the sea on that side to allow the formation of any large streams. Hence the rivers that flow in the opposite direction into the Adriatic and the Gulf of Taranto have much longer courses, though all partake of the character of mountain torrents, rushing down with great violence in winter and after storms, but dwindling in the summer into scanty streams, which hold a winding and sluggish course through the great plains of Apulia.

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  • North and parallel with its course is a low watershed, which separates its drainage basin both from that of the Sao Francisco and from that of the Parnahyba, the northern confluent of the Parana.

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  • There are considerable spaces where the strike, or axis, of the main ranges is transverse to the water-parting, which is then represented by intermediate highlands forming lacustrine regions with an indefinite watershed.

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  • In its course through Eastern Manchuria it forms the watershed of the Sungari, Usuri and other rivers, and in the south that of the Ya-lu and many smaller streams. it also forms the eastern boundary of the great plain of Liao-tung.

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  • In the Tagharat pass Mr Maw was the only one of the party who reached the watershed; but from Jebel Tezah a good view was obtained southward across the great valley of the Sias to the Anti-Atlas, which appeared to be from 9000 to io,000 ft.

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  • It is a swift clear river, fed in its upper reaches by numerous mountain streams. The Mogaung river, rising in the watershed which divides the Irrawaddy and the Chindwin drainages, flows south and south-east for 180 m.

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  • The basin of the Ghazal is a large one, extending north-west to Darfur, and south-west to the Congo watershed.

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  • In 1859 a Venetian, Giovanni Miani, penetrated the southern regions of the Ghazal basin and was the first to bring back reports of a great river (the Welle) flowing west beyond the Nile watershed.

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  • Georg Schweinfurth between 1869 and 1871 traversed the whole of the southern district, and crossing the watershed discovered the Welle.

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  • The Sahyadri range stretches from north to south; the watershed is formed by the Chander range, which runs east and west.

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  • To the north of the watershed, the Girna and its tributary the Mosam flow through fertile valleys into the Tapti.

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  • Along the centre lies the watershed between the basins of the Main and the Saale, belonging to the systems of the Rhine and Elbe respectively.

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  • In the north, beside `Ain Faluj, it is connected by a low watershed with the Buka'a; from the gorge of the Litany it is separated by the ridge of Jebel ed-Dahr.

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  • Unlike the other wings of the great central system of Europe, the Carpathians, which form the watershed between the northern seas and the Black Sea, are surrounded on all sides by plains, namely the great Hungarian plain on the south-west, the plain of the Lower Danube (Rumania) on the south, and the Galician plain on the north-east.

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  • The direct passes across it from Herat (the Baba and the Ardewan) wind amongst masses of disintegrating sandstone for some miles on each side of the dividing watershed, but farther west the rounded knolls of the rain-washed downs may be crossed almost at any point without difficulty.

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  • The Brenner, too, being on the main watershed of the Alps, separates the two main river systems of which Tirol is composed.

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  • From a point about midway between the two rivers, and near the town of Dehra, runs a ridge which forms the watershed of the valley.

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  • Its democratic constitution, which seems to have been entirely congenial to the population of small freeholders, and its ambition to gain control over the Alpheus watershed and both the Arcadian high roads to the isthmus, frequently estranged Mantineia from Sparta and threw it into the arms of Argos.

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  • The watershed between the Vaal and Caledon is formed by chains of hills, which, leaving the main range of the Drakensberg at Mont aux Sources, sweep in semicircles west and south.

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  • Cabra is built in a fertile valley between the Sierra de Cabra and the Sierra de Montilla, which together form the watershed between the rivers Cabra and Guadajoz.

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  • The main watershed follows a tortuous course which crosses the mountainous belt just north of New river in Virginia; south of this the rivers head in the Blue Ridge, cross the higher Unakas, receive important tributaries from the Great Valley, and traversing the Cumberland Plateau in spreading gorges, escape by way of the Cumberland and Tennessee rivers to the Ohio and Mississippi, and thus to the Gulf of Mexico; in the central section the rivers, rising in or beyond the Valley Ridges, flow through great gorges (water gaps) to the Great Valley, and by southeasterly courses across the Blue Ridge to tidal estuaries penetrating the coastal plain; in the northern section the water-parting lies on the inland side of the mountainous belt, the main lines of drainage running from north to south.

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  • Two volcanic Cordilleras or mountain chains, separated from one another by the central plateau of San Jose and Cartago, traverse the interior of Costa Rica, and form a single watershed, often precipitous on its Pacific slope, but descending more gradually towards the Atlantic, where there is a broad expanse of plain in the north-east.

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  • It rises from the Indus basin near the village of Kiara, up to its watershed by Bruddur; thence it runs northwest by north to the point on the crest known as Chittabut.

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  • Running south-west to north-east, and united on the north with one of the offsets of the Pyrenees, is the range of the Sierra Llena, which bisects Catalonia, and forms its central watershed.

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  • The principal watershed is formed by the sierras of the state of Mexico, from which streams flow north-east to the Gulf of Mexico, northwest to the Pacific and south-west to the same coast below its great eastward curve.

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  • The wars of this nation with the Tepanecs, which went on into the 15th century, were merely destructive, but larger effects arose from the expeditions under the Culhua king Acamapichtli, where the Aztec warriors were prominent, and which extended far outside the valley of Anahuac. Especially a foray southward to Quauhnahuac, now Cuernavaca, on the watershed between the Atlantic and Pacific, brought goldsmiths and other craftsmen to Tenochtitlan, which now began to rise in arts, the Aztecs laying aside their rude garments of aloe-fibre for more costly clothing, and going out as traders for foreign merchandise.

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  • The Rotlagergebirge, Eggegebirge and Teutoburger Wald form with some intermediate ranges the watershed between the basin of the Weser and those of the Rhine and Ems. In the N.E.

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  • It forms the main watershed between the Pacific and Atlantic river systems. Its summit is not a well-defined crest, but is often rounded or flattened into a table-land.

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  • It is, however, impossible to subdivide the Sierra Madre into a northern and a volcanic chain; for the volcanoes are isolated by stretches of comparatively low countr y; at least thirteen considerable streams flow down between them, from the main watershed to the sea.

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  • Owing to this unsymmetric development of North America the main structural watershed is towards its western side, on the south coinciding with the Rocky Mountains proper, but to the northward falling back to ranges situated further west in the same mountain region.

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  • The stretch from Samsat and Jeziret-ibn- 'Omar to the alluvial plain seems to divide itself naturally into three parallel belts, highland watershed district, un- Geography.

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  • All this drainage, collected into two rivers, the Belikh and the Khabur, is towards the left bank of the Euphrates, for the Mesopotamian watershed seems to be only some 15 m.

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  • It lies on the western side of the elevation of Stanedge, which here forms the watershed between streams flowing westward to the Irish Sea and eastward to the North Sea.

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  • As a whole the system forms the watershed between rivers flowing to the Indian Ocean - the Indus and its tributaries, Brahmaputra and its tributaries, and Salweenand the streams flowing into the undrained salt lakes to the north.

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  • The general structure of the trans-Himalayan chains appears to indicate that the main axis of upheaval of the whole vast mass of the Tibetan highlands is to be found on two approximately parallel lines, represented the one by the Kuen-lun and the other by a line which is more or less coincident with the watershed between India and the central lake region, extending from Lake Pangong to Tengri Nor, the plateau enclosed between the two being wrinkled by minor folds, of which the relative elevation is comparatively low, averaging from woo to 1500 ft.

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  • This watershed was found to lie much farther north than had been supposed, and to consist of very lofty mountains, in complicated ranges, from which large tributaries descend to the Tsangpo (Brahmaputra).

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  • In the ranges which rise above the high plateau in the north-west, in the vicinity of the Stanovoi watershed, gold mines of great richness are worked.

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  • A few defiles pass through this barrier to the other side of the north Greek watershed.

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  • Of course each of these semi-detached ranges has a watershed of its own, like the lateral ridges that branch off from the main watershed.

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  • Thus there are lofty ranges parallel to that which forms the main watershed.

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  • The Alps, therefore, are not composed of a single range (as shown on the old maps) but of a great " divide," flanked on either side by other important ranges, which, however, do not comprise such lofty peaks as the main watershed.

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  • In the following remarks we propose to follow the main watershed from one end of the Alps to the other.

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  • From the Rocher des Trois Eveques the watershed runs due north for a long distance, though of the two loftiest peaks of this region one, the Aiguille de Chambeyron (11,155 ft.), is just to the west, and the other, the Monte Viso (12,609 ft.), is just to the east of the watershed.

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  • Hence the main watershed extends eastwards, culminating in the Aiguille de Scolette (11,500 ft.), but makes a great curve to the north-west and back to the south-east before rising in the Rochemelon (11,605 ft.), which may be considered as a re-entering angle in the great rampart by which Italy is guarded from its neighbours.

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  • Thence the direction taken is north as far as the eastern summit (11,693 ft.) of the Levanna, the watershed rising in a series of snowy peaks, though the loftiest point of the region, the Pointe de Charbonel (12,336 ft.), stands a little to the west.

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  • A number of high peaks crown our watershed before it attains the Mont Dolent (12,543 ft.).

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  • It is in the portion of the watershed between the Great St Bernard and the Simplon that the main chain maintains a greater average height than in any other part.

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  • But, though it rises in a number of lofty peaks, such as the Mont Velan (12,353 ft.), the Matterhorn (14,782 ft.), the Lyskamm (14,889 ft.), the Nord End of Monte Rosa (15,132 ft.), and the Weissmies (13,226 ft.), yet many of the highest points of the region, such as the Grand Combin (14,164 ft.), the Dent Blanche (14,318 ft.), the Weisshorn (14,804 ft.), the true summit or Dufourspitze (15,217 ft.) of Monte Rosa itself, and the Dom (14,942 ft.), all rise on its northern slope and not on the main watershed.

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  • From the St Gotthard to the Maloja the watershed between the basins of the Rhine and Po runs in an easterly direction as a whole, though making two great dips towards the south, first to near the Vogelberg (10,565 ft.) and again to near the Pizzo Gallegione (10,201 ft.), so that it presents a broken and irregular appearance.

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  • From the Maloja Pass the main watershed dips to the southeast for a short distance, and then runs eastwards and nearly over the highest summit of the Bernina group, the Piz Bernina (13,304 ft.), to the Bernina Pass.

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  • For some way beyond it the watershed runs eastwards over the highest crest of the Zillerthal Alps, which attains 11,559 ft.

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  • The eastward direction is maintained and the watershed (though not the chief Alpine watershed) continues through the Greater Tauern Alps, culminating in the Gross Venediger (12,008 ft.), for the Gross Glockner (12,461 ft.) rises to the south.

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  • Soon after our watershed makes a last bend to the south-east and culminates in the Terglou (9400 ft.), the highest point of the Julic Alps, though the Grintovc (8429 ft., the culminating point of the Karawankas Alps) stands more to the east.

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  • The watershed of the province runs from east to west across the middle of the province, along the line of the Orange canal.

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  • The watershed, too, is somewhat different.

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  • The watershed of the Southern Uplands is of much interest in relation to their geological history.

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  • Now it is perhaps timely to redress this situation and to undertake a systematic study of the earliest occupation of this key Wealden watershed.

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  • The month of October 1917 is a great historical watershed in the Russian revolution.

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  • Schrader, de St Sand and Wallon, that, taken as a whole, the range must be regarded, not as formed on the analogy of a fern-frond or fish-bone, with the lateral ridges running down to the two opposite plains, but rather as a swelling of the earth's crust, the culminating portion of which is composed of a series of primitive chains, which do not coincide with the watershed, but cross it obliquely, as if the ground had experienced a sidewise thrust at the time when the earth's crust was ridged up into the long chain under the influence of contraction.

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  • What 's more, having reached a watershed in my personal life I was ready for a career change anyway.

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  • We may now be at a key watershed moment where our fate hangs in the balance.

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  • This move is a compromise solution compared with the watershed ban on food and drink advertising that some parties are calling for.

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  • Disaster mitigation is another area where watershed protection is crucial.

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  • Reports include cost benefit analysis and watershed management manual.

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  • Watershed battle of decided to just los angeles based.

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  • The transfer of Army forces out of Germany is a watershed event.

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  • A watershed in history was just around the corner.

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  • Organic gardening is a great way to support San Diego County's watershed protection program.

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  • Not only will this add harmful chemicals to the watershed, it will also make plants grow faster than they need to grow.

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  • Though the conservative group Parents Television Center attempted to organize a campaign of FCC complaints, Lambert's performance was aired during FCC watershed hours and they refused to act.

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  • So complete is the watershed that no streams pass through these ranges, and there is hardly any communication in this direction between the interior of Asia Minor and the coast.

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  • The Andine sub-region extends from Peru to the Argentine and follows roughly the watershed of the Amazon.

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  • There is, however, a well defined watershed extending from the hills east of Stefanie to the Harrar range.

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  • A more or less continuous band of serpentine belonging to this series forms the principal watershed, although it nowhere rises to any great height.

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  • Hauran southward forms the main watershed of the peninsula is covered in places by deep beds of lava, which from their hardness have preserved the underlying sandstones from degradation, and now stand up consider ably above the general level.

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  • Arcadia, on the other hand, in the heart of Peloponnese, retained till a late date a quite different dialect, akin to the ancient dialect of Cyprus, and more remotely to Aeolic. This distribution makes it clear (r) that the Doric dialects of Peloponnese represent a superstratum, more recent than the speech of Arcadia; (2) that Laconia and its colonies preserve features alike, -n and -w which are common to southern Doric and Aeolic; (3) that those parts of " Dorian " Greece in which tradition makes the pre-Dorian population " Ionic," and in which the political structure shows that the conquered were less completely subjugated, exhibit the Ionic -a and -ov; (4) that as we go north, similar though more barbaric dialects extend far up the western side of central-northern Greece, and survive also locally in the highlands of south Thessaly; (5) that east of the watershed Aeolic has prevailed over the area which has legends of a Boeotian and Thessalian migration, and replaces Doric in the northern Doris.

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  • Here the main chain of the Alps (as marked by watershed) recedes so far to the north that it has never constituted the frontier.

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  • There is a large staff of inspectors constantly visiting the various parts of the watershed, and in spite of many difficulties arising from vested interests, the work of purification is attaining completion, with a correspondingly great improvement in the quality of the river water.

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  • This watershed includes the ranges running eastward and northward under the names of Imeri, Tapiira-peco, Curupira, Parima and Pacaraima, the Venezuelan section terminating at Mt.

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  • This watershed slopes gently to the south, to the valley of the Dnieper, which enters the government from the north-east and flows due south.

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  • South of the watershed the whole aspect of the landscape is as hideous and disappointing as scenery in Afghanistan.

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  • Upper Austria belongs to the watershed of the Danube, which flows through it from west to east, and receives here on the right the Inn with the Salzach, the Traun, the Enns with the Steyr and on its left the Great and Little Mühl rivers.

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  • The lake really lies on the watershed between the two, and is probably a glacial relic.

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  • Thus new land forms are created - valleys of curious complexity, for example by the " capture " and diversion of the water of one river by another, leading to a change of watershed.'

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  • With the exception of the Idria and the Wippach, which as tributaries of the Isonzo belong to the basin of the Adriatic, Carniola belongs to the watershed of the Save.

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  • The Salmonidae are entirely absent from the waters of southern Asia, though they exist in the rivers that flow into the Arctic Ocean and the neighbouring parts of the northern Pacific, extending perhaps to Formosa; and trout, though unknown in Indian rivers, are found beyond the watershed of the Indus, in the streams flowing into the Caspian.

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  • The others, which terminate streams, are the Bahr el-Ateiba, which receives the waters of Damascus; the Mat, into which the Kuwaik flows below Kinnesrin; and the Ak Deniz, or Bahrat Antakia, the ancient Lake of Antioch, which collects the waters of the Kara Su and Afrin, the southward from the watershed which shuts off Commagene.

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  • Bosnia belongs wholly to the watershed of the Save, and its rivers to the Danubian system, no large stream finding a way to the Adriatic. The Save flows eastward along the northern frontier for 237 m.

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  • North of the Sao Francisco the watershed projecting from the plateau eastward toward Cape St Roque, known as the Serra da Borborema in Parahyba and Rio Grande do Norte where its direction becomes north-east, leaves a triangular section of the easterly slope in which the river courses are short and much broken by rapids.

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  • They formed important settlements at various points on the Mekong, notably Luang Prabang, Wieng Chan (Vien-Tiane) Ubon and Bassac; and, heading inland as far as Korat on the one side and the Annamite watershed in the east, they drove out the less civilized Kha peoples, and even the Cambodians, as the Lao Pong Dam did on the west.

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  • On the east the Kachin, Shan and Karen hills, extending from the valley of the Irrawaddy into China far beyond the Salween gorge, form a continuous barrier and boundary, and tail off into a narrow range which forms the eastern watershed of the Salween and separates Tenasserim from Siam.

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  • Eastwards of this the great Kashgar depression, which includes the Tarim desert, separates Russia from the vast sterile highlands of Tibet; and a continuous series of desert spaces of low elevation, marking the limits of a primeval inland sea from the Sarikol meridional watershed to the Khingan mountains on the western borders of Manchuria, divide her from the northern provinces of China.

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  • In the north it is occupied by the watershed which separates the basins of the Dvina and the Dnieper, an undulating tract 650 to goo ft.

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  • Lower Austria belongs to the watershed of the Danube, which with the exception of the Lainsitz, which is a tributary of the Moldau, receives all the other rivers of the province.

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  • This edge is marked by ranges of hills such as the Witwatersrand, Witwatersberg and Magaliesberg; the Witwatersrand, which extends eastward to Johannesburg, forming the watershed between the rivers flowing to the Atlantic and Indian Ocean.

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  • The only river communication with foreign countries is furnished by the Danube, on the one hand towards Austria and Germany, and on the other towards the Black Sea, All the rivers belong to the watershed of the Danube, with the exception of the Poprad in the north, which as an affluent of the Dunajec flows into the Vistula, and of a few small streams near the Adriatic. The Danube enters Hungary through the narrow defile called the Porta Hungarica at Deveny near Pressburg, and after a course of 585'.m.

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