The city stands on a rocky plateau, which projects southwards from the main line of hills.
Snows are frequent during the winter, and sometimes deep in the higher plateau and mountain districts.
The town is charmingly situated on a small plateau, 1680 ft.
There are many forests which clothe the slopes of the plateau.
The plateau was too small for it to land, but it hovered near the edge.
It is beautifully situated in the centre of a valley basin on a plateau 3500 ft.
The entire plateau area is drained by the Ohio river and its tributaries.
Petroleum and natural gas also occur in the plateau rocks in great quantities.
The Central Plateau has probably been a land mass ever since this period, but the rest of the country was flooded by the Palaeozoic sea.
Beginning with the Aptian and Albian the sea again gradually spread over the country and attained its maximum in the early part of the Senonian epoch, when once more the ancient massifs of the Central Plateau, Brittany and the Ardennes, alone rose above the waves.
at Fondu Corrongiu and San Sebastiano), like those of the Central Plateau of France.
of the city of Mexico, near the southern margin of the great Mexican plateau, 6398 ft.
The low shrub oak plateau to which the opposite shore arose stretched away toward the prairies of the West and the steppes of Tartary, affording ample room for all the roving families of men.
A little south of Samarra the stony plateau of Mesopotamia ends, and the alluvial plain of Irak, ancient Babylonia, begins.
This elevated region is known as the plateau of Matto Grosso, and its elevations so far as known rarely exceed 3000 ft.
The more important of the suburbs lie towards the east, where the promontory joins the main plateau, of which it forms the north-western extremity.
On the east the valley of the Kidron separates this plateau from the ridge of the Mount of Olives, which is 100 to 200 ft.
Rashki), a river which rises south of Erzerum, in the Bingeul-dagh, and flows east through the province of Erzerum, across the Pasin plateau, and then through Russian Armenia, passing between Mount Ararat and Erivan, and forming the Russo-Persian frontier.
The first industry was that of mining, gold having been discovered in the river valleys on the southern slopes of the plateau, and diamonds on the head-waters of the Paraguay, about Diamantino and in two or three other districts.
On the north their most noteworthy offshoots are, in the centre, the plateau of Lannemezan from which rivers radiate fanwise to join the Adour and Garonne; and in the east the Corbire.
The greater part of the state belongs to the western extension of the Brazilian plateau, across which, between the 14th and 16th parallels, runs the water-shed which separates the drainage basins of the Amazon and La Plata.
Towards the close of the Palaeozoic era France had become a part of a great continent; in the north the Coal Measures of the Boulonnais and the Nord were laid down in direct connection with those of Belgium and England, while in the Central Plateau the Coal Measures were deposited in isolated and scattered basins.
Rye, on the other hand, one of the least valuable of the cereals, is grown chiefly in the poor agricultural territories of the central plateau and western Brittany.
This ocean, already diminished in area, retreated after Oligocene times from the Iranian plateau, Turkestan, Asia Minor and the region of the north-west Alps.
The northern slope of this great plateau is drained by the AraguayaTocantins, Xingu, Tapajos and Guapore-Mamore-Madeira, which flow northward, and, except the first, empty into the Amazon; the southern slope drains southward through a multitude of streams flowing into the Parana and Paraguay.
Farther to the north a number of small rivers, the chief of which is the Svre Niortaise, drain the coast region to the south of the plateau of Gtine.
From this a gently-sloping plateau extends to almost due north of Spencer Gulf, at which point its height has fallen almost to sealevel.
8 Rocky Mountains and Plateau TO.
Along the flood-plains of the larger rivers are fertile " bottomlands," but the ruggedness of the plateau country as a whole has retarded the development of the state, much of which is still sparsely populated.
The poorer grazing lands on the upper levels of the Alps, Pyrenees, Jura and Vosges, the Landes, the more outlying regions of the central plateau, southern Brittany, Sologne, Berry, ChampagnePouilleuse, the Crau and the Carnargue, these districts being given over for the most part to sheep-raising.
The state is divided into two distinct physiographic provinces; the Alleghany Plateau on the west, comprising perhaps two-thirds of the area of the state, and forming a part of the great Appalachian Plateau Province which extends from New York to Alabama; and the Newer Appalachians or Great Valley Region on the east, being a part of the large province of the same name which extends from Canada to Central Alabama.
These minor ranges, excepting the Zenta, are separated from the Andean masses by comparatively low depressions and are usually described as distinct ranges; topographically, however, they seem to form a continuation of the ranges running southward from the Santa Victoria and forming the eastern rampart of the great central plateau of which the Puna de Atacama covers a large part.
are reached along the south-east margin of the plateau, which is known as the Alleghany Front.
The hilly regions of Limousin, Prigord and the Cvennes are the home of the chestnut, which in some places is still a staple food; walnuts grow on the lower levels of the central plateau and in lower Dauphin and Provence, figs and almonds in Provence, oranges and citrons on the Mediterranean coast, apricots in central France, the olive in Provcnce and the lower valleys of the Rhneand Durancc. Truffles arc found under Silk Cocoons.
ARGONNE, a rocky forest-clad plateau in the north-east of France, extending along the borders of Lorraine and Champagne, and forming part of the departments of Ardennes, Meuse and Marne.
The Alleghany Plateau consists of nearly horizontal beds of limestone, sandstone and shales, including important seams of coal; inclines slightly toward the north-west, and is intricately dissected by extensively branching streams into a maze of narrow canyons and steep-sided hills.
The Seine descends from the Langres plateau, flows northwest down to Mry, turns to the west, resumes its north-westerly direction at Montereau, passes through Paris and Rouen and discharges itself into the Channel between Le Havre and Honfleur.
The plateau portion of West Virginia is largely covered by hardwood forests, but along the Ohio river and its principal tributaries the valuable timber has been removed and considerable areas have been wholly cleared for farming and pasture lands.
On the north both summits are defended by cliffs; on the south the ground slopes away somewhat abruptly from the eastern summit towards the plateau on which the town stood, while the western summit is separated from this plateau by a valley traversed by a branch of the Hypsas [mod.
In Tertiary times the Central Plateau was the theatre of great volcanic activity from the Miocene, to the Pleistocene periods, and many of the volcanoes remain as nearly perfect cones to the present day.
The oldest rocks, the gneisses and schists of the Archean period, form nearly the whole of the Central Plateau, and are also exposed in the axes of the folds in Brittany.
at this point, three-fourths of which is a comparatively level alluvial plain, and the remainder an arid plateau broken by mountain ranges.
(a) Normandy, Perche, Cotentin and maritime Flanders, where horses are bred in great numbers; (b) the strip of coast between the Gironde and the mouth of the Loire; (c) the Morvan including the Nivernais and the Charolais, from which the famous Charolais breed of oxen takes its name; (d) the central region of the central plateau including the districts of Cantal and Aubrac, the home of the famous beef-breeds of Salers and Aubrac.1 The famous pre-sal sheep are also reared in the Vende and Cotentin.
Within the northern circle of the 8 lie the Mesozoic and Tertiary beds of the Paris basin, dipping inwards; within the southern circle lie the ancient rocks of the Central Plateau, from which the later beds dip outwards.
In the area of the Newer Appalachian Mountains, the eastern Panhandle region has a forest similar to that of the plateau district; but between these two areas of hardwood there is a long belt where spruce and white pine cover the mountain ridges.
slope of the central plateau.
below the general valley of the plateau.
South of this the country rises graudally to a high plateau with open campos.
to Mogilev; they form the central plateau, as also the slopes of the Urals and the Petchora region.
From a central plateau, which comprises the governments of Tver, Moscow, Smolensk and Kursk, and projects E.
In general the climate is dry and bracing all over the plateau.
to encircle the plateau of the Donets.
In the Valdai plateau there are only a few beds of mediocre coal.
At Kufstein, down to which point it has still pursued a north-easterly direction, it breaks through the north Tirol limestone formation, and, now keeping a northerly course, enters at Rosenheim the Bavarian high plateau.
The Sicilian-Ionian basin has a mean depth of 885 fathoms, and the Levant basin, 793 fathoms. Deep water is found close up to the coast of Sicily, Greece, Crete and the edge of the African plateau.
by the Ante and the Aisne, which rises in its southern plateau.
Thence he at last ascended upon the Iranian plateau.
at the western extremity of the Pyrenees), and nearly as much in the Vosges, Morvan, Cvennes and parts of the central plateau.
As the tableland runs northward it decreases both in height and width, until it narrows to a few miles only, with an elevation of scarcely 1500 ft.; under the name of the Blue Mountains the plateau widens again and increases in altitude, the chief peaks being Mount Clarence(4000 ft.), Mount Victoria (3525 ft.), and Mount Hay (3270 ft.).
Australia is essentially the fragment of a great plateau land of Archean rocks.
They are also preserved in basins on the western plateau, as shown by brown coal deposits passed through in the Lake Phillipson bore.
The second and marine type of the Jurassics occurs in Western Australia, on the coastal plain skirting the western foot of the western plateau.
The sea does not appear to have extended completely across Australia, breaking it into halves, for a projection from the Archean plateau of Western Australia extended as far east as the South Australian highlands, and thence probably continued eastward, till it joined the Victorian highlands.
Tasmania and Victoria were separated by the foundering of Bass Strait, and at the same time the formation of the rift valley of Spencer Gulf, and Lake Torrens, isolated the South Australian highlands from the Eyre Peninsula and the Westralian plateau.
Towards its northern end the ridge widens and rises to the plateau of the Azores, and in about 50° N.
it merges with the " Telegraph Plateau," which extends across nearly the whole ocean from Ireland to Newfoundland.
On both sides of the central ridge deep troughs extend southwards from the Telegraph plateau to the Southern Ocean, the deep water coming close to the land all the way down on both sides.
On the hills the baobab and hyphaene palm are characteristic; on the plateau are stretches of open savanna, and park-like country with clumps of silk cotton and shea-butter trees.
In the interior cattle and sheep are plentiful, on the plateau horses and donkeys.
beneath the plateau, runs across the plain towards the mountains; it is at this point that the traveller coming from Shechem now ascends the hill to the village of Sebusteh, which occupies only the extreme E.
It is well situated on a hill forming part of the plateau of la Goole, and is known as Dammartin-en-Goole to distinguish it from Dammartin-sousTigeaux, a small commune in the same department.
It collects nearly all the drainage of the Udaipur plateau with that of the eastern slopes and hill-tracts of the Aravallis, and joins the Chambal a little beyond the northeastern extremity of the Bundi state, after a course of about 300 m.
Geologically considered, the country may be divided into three regions - a central, and the largest, comprising the whole width of the Aravalli system, formed of very old sub-metamorphic and gneissic rocks; an eastern region, with sharply defined boundary, along which the most ancient formations are abruptly replaced by the great basin of the Vindhyan strata, or are overlaid by the still more extensive spread of the Deccan trap, forming the plateau of Malwa; and a western region, of very ill-defined margin, in which, besides some rocks of undetermined age, it is more or less known or suspected that Tertiary and Secondary strata stretch across from Sind, beneath the sands of the desert, towards the flanks of the Aravallis.
This plateau region is watered by numerous tributaries of the Parnahyba, chief of which are the Urussuhy, the Caninde and its tributary the Piauhy, the Gurgueia and its tributary the Parahim, which drains the large inland lake of Parnagua, the Longa, and the Poty, which has its source in the state of Ceara.
On the 28th of March 1888 the negus indeed descended from the Abyssinian high plateau in the direction of Saati, but finding the Italian position too strong to be carried by assault, temporized and opened negotiations for peace.
Menelek, by means of Count Antonelli, resident in the Shoa country, requested Italy to execute a di version in his favor by occupying Asmar and other points on the high plateau.
of the high plateau, with the positions of Halai, Saganeiti and Asmar.
Bath-Agos, the native chieftain who ruled the Okul-Kusai and the cis-Mareb provinces on behalf of Italy, intrigued with Mangash, ras of the trans-Mareb province of Tigr, and with Menelek, to raise a revolt against Italian rule on the high plateau.
of the high plateau and ceding to Abyssinia the fertile provinces of Sera and Okul-Kusai.
Groningen is connected with the Drente plateau by the sandy tongue of the Hondsrug which extends almost up to the capital.
The rivers of Groningen descending from the Drente plateau meet at the capital, whence they are continued by the Reitdiep to the Lauwers Zee (being discharged through a lock), and by the Ems canal (1876) to Delfzyl.
m.) is a thickly wooded mountainous region, shut off from the Persian plateau by the Talysh range (7000-8000 ft.
For example, in southern Algeria, a region of steppes is situated on a flat plateau, about 3000 ft.
The third part is the north, which belongs to the central plateau, still much higher, and therefore rough and very cold in the winter.
He appears to have ascended from Kabul to the plateau of the Pamir, and thence onwards by Yarkand, Khotan and Aksu.
The continental plateau might for purposes of detailed study be divided into the continental shelf from - 660 ft.
on the other, the higher enclosing a plateau shut in by tinents mountains.
It comprises a comparatively narrow coastal zone, a high inland plateau, and an intermediate zone formed by the terraces and slopes between the two.
The rivers of the state include a number of small plateau streams flowing southward to the Sao Francisco River, and several large streams in the eastern part flowing eastward to the Atlantic. The former are the Moxoto, Ema, Pajehu, Terra Nova, Brigida, Boa Vista and Pontai, and are dry channels the greater part of the year.
The general slope of the plateau is toward the N., and the drainage of the state is chiefly through the above-named rivers - the principal tributaries of the Araguaya being the Grande and Vermelho, and of the Upper Tocantins, the Manoel Alves Grande, Somno, Paranan and Maranhao.
there is a well-defined chain of mountains, of which the Pyreneos, Santa Rita and Santa Martha ranges form parts, but their elevation above the plateau is not great.
The surface of the plateau is generally open campo and scrubby arboreal growth called caatingas, but the streams are generally bordered with forest, especially in the deeper valleys.
The climate of the plateau is usually described as temperate, but it is essentially sub-tropical.
of the great plateau formation of the old continent - the backbone of Asia - which stretches with decreasing altitude and width from of Asia.
Thus it consists of the immense plains and flat lands which extend between the plateau formation and the Arctic Ocean, including the series of parallel chains and hilly spurs which skirt the former region on the N.W.
of Lake Baikal that it climbs up on to the plateau, from which it descends again before it reaches the Pacific.
higher portions of the plateau formation the empire has only comparatively recently planted its foot on the Pamir, and it was only a few years earlier that it established itself firmly on the highlands of Armenia.
A broad belt of hilly tracts - in every respect alpine in character, and displaying the same variety of climate and organic life as alpine tracts usually do - skirts the plateau formation throughout its entire length on the N.
and N.W., forming an inter mediate region between the plateau and the plains.
- all these belong to the same alpine belt that borders the plateau from end to end of the series.
The picturesque Bureya Mountains above the Amur, the forest-clad Sikhota-alin on the Pacific, and the volcanic chains of Kamchatka belong, however, to quite another orographical construction, being the border-ridges of the terraces by which the great plateau formation descends to the depths of the Pacific Ocean.
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.
A broad depression - the Aral-Caspian desert - has arisen where the plateau formation reaches its greatest altitude, and at the same time suddenly changes its direction from N.W.
The round flattened summits of the Valdai plateau do not rise above 1100 ft., and they present the appearance of mountains only in consequence of the depths of the valleys - the rivers which flow towards the depression of Lake Peipus being only 200 to 250 ft.
The same elevation is reached by a very few flat summits of the plateau about Kursk, and farther E.
The depressions which gap the borders of the central plateau thus acquire a greater importance than the small differences in its vertical elevation.
above the sea, still filled by Lakes Peipus, Ladoga, Onega, Byelo-ozero, Lacha, Vozhe, and many thousands of smaller lakes, skirts the central plateau on the N., and follows the same E.N.E.
the central plateau slopes gently towards the S., and we find there a fourth depression stretching W.
The rhomboidal peninsula of the Crimea, connected by only a narrow isthmus with the continent, is occupied by an arid plateau sloping gently N.
of the central plateau) so close to one another that they may be said to radiate from the same centre.
By their means the plains of the central plateau - the very heart of Russia, whose natural outlet was the Caspian - were brought into water-communication with the Baltic, and the Volga basin was connected with the Gulf of Finland.
parts of the central plateau, in the same marshy lakes.
of the central plateau.
slopes of the central plateau and those of the Carpathian and Lublin mountains, and the Carpathian plateau, that is, the governments of Podolia, Volhynia, Poltava, and Kiev.
is not conspicuously uplifted, being plateau, rather than mountain.
The plateau "lowlands" in the centre of the Basin are approximately 5000 ft.
The whole Basin is marked by three features of elevation - the Utah basin, the Nevada basin and, between them, the Nevada plateau.
The Falkland Islands form essentially a part of Patagonia, with which they are connected by an elevated submarine plateau, 1 See B Stechele, in'Milnchener geographische Studien, xx.(1906), and Geographical Journal (December 1907).
This plateau, however, is not a plain, but contains many buttes and mesas and isolated mountain ranges rising from 1000 to 8000 ft.
From this depression eastward the general level of the plateau gradually rises to an elevation of 6000 ft.
From the valley of the Humboldt river southward the plateau gradually rises until the divide between this stream and the Colorado river, in the vicinity of the White Pine Mountains, is reached.
At a distance from the central core the radiating ridges become less abrupt and descend with a gentle gradient, finally passing somewhat abruptly, at a height of some 7000 ft., into the level plateau.
Its territory is divided into two nearly equal parts by the eastern branch of the Sierra Madre Occidental, the northern part belonging to the great central plateau region, and the southern to an extremely broken region formed by the diverging branches of the Sierra Madre, with their wooded terraces and slopes and highly fertile valleys.
Though the plateau region was settled soon after the arrival of the Spaniards in Mexico, there are large districts on the southern and Pacific slopes that still belong almost exclusively to the Indians.
until it is merged in the great Central American plateau.
The c nquest of the peninsula was undertaken in 1527 by Francisco de Montejo, who en-, countered a more vigorous opposition than Cortes had on the high plateau of Anahuac. In 1549 Montejo had succeeded in establishing Spanish rule over barely one-half of the peninsula, and it was never extended further.
The " Fall Line," the boundary between the Coastal Plain and the Piedmont Plateau, has a very irregular course across North Carolina, but lies in a general S.W.
The Piedmont Plateau Region extends from this line to the Blue Ridge Escarpment, toward which its mean elevation increases at the rate of about 32 ft.
or more above the Piedmont Plateau, forms the S.E.
of E., then, finding a passage across one of the ridges of the Piedmont Plateau, turn to.
part of the Piedmont Plateau Region, and a little to the N.
part of the Piedmont Plateau Region, have their S.E.
In the Mountain Region and in the Piedmont Plateau Region the rivers have numerous falls and rapids which afford a total water power unequalled perhaps in any other state than Maine on the Atlantic Coast, the largest being on the Yadkin, Roanoke and Catawba; and in crossing some of the mountains, especially the Unakas, the streams have carved deep narrow gorges that are much admired for their scenery.
In the Piedmont Plateau Region oaks, hickories and elms are the most common.
The species of fauna that are at all characteristic of this part of the United States are found in the Piedmont Plateau Region and the western portion of the Coastal Plain Region.
For the Coastal Plain Region it is 61° F.; for the Piedmont Plateau Region, 60° F.; for the Mountain Region, 56° F.; for Southport, in the S.E.
on the Piedmont Plateau, and of 44° F.
on both the Coastal Plain and the Piedmont Plateau and 74° F.
For the Coastal Plain Region it is 54 in.; for the Piedmont Plateau Region, 48 in.; and for the Mountain Region, 53 in.
Throughout much of the Piedmont Plateau and Mountain regions the decomposition of felspar and of other aluminous minerals has resulted in a deep soil of clay with which more or less sand is mixed.
Farmers of the Piedmont Plateau formerly kept large numbers of horses and cattle from April to November in ranges in the Mountain Region, but with the opening of portions of that country to cultivation the business of pasturage declined, except as the cotton plantations demanded an increased supply of mules; there were 25,259 mules in 1850, 110,011 in 1890, 138,786 in 1900, and 181,000 in 1910.
portion of the Piedmont Plateau and in a few counties along or near the W.
portion of the Piedmont Plateau and in the central and N.W.
portion of the Piedmont Plateau and in the Mountain Region; vegetables and small fruits in the middle and S.
At the beginning of the 20th century a great number of minerals were found in the Piedmont Plateau and Mountain regions, but most of them in such small quantities as to be of little or no commercial value, and in 1902 the total value of the products of the mines and quarries was only $927,376; but in 1907 their value was $2,961,381, and in 1908, $2,145,947.
portion of the Piedmont Plateau.
The cotton mills are mostly in the Piedmont Plateau Region; durham|Durham, Durham county, and Winston, Forsyth county, are leading centres of tobacco manufacture; and High Point (pop. in 1900, 4163) in Randolph is noted for its manufacture of furniture.
upon the great Brazilian plateau.
It rises near the peak of Itatiaya, on the northern slopes of the Mantiqueira, and flows north-west and west across the Minas plateau, receiving several large tributaries from the south.
All these rivers of the Brazilian plateau are interrupted by falls and rapids.
Such lakes (in common with all the plateau hamuns of south-west Baluchistan and Persia) change their form and extent from season to season, and many of them are impregnated with saline deposits from the underlying strata.
China lies between the eastern flank of the Tibetan plateau and the North Pacific, having its northern and southern limits about on 40° and 20° N.
The portion of Asia west of British India, excluding Arabia and Syria, forms another extensive plateau covering an area as large as that of Tibet, though at a much lower altitude.
The western part of the range, which received the name of Paropamisus Mons from the ancients, diminishes in height west of the 65th meridian and constitutes the northern face of the Afghan and Persian plateau, rising abruptly from the plains of the Turkoman desert, which lies between the Oxus and the Caspian.
West of Ararat high hills extend along the Black Sea, between which and the Taurus range lies the plateau of Asia Minor, reaching to the Aegean Sea; the mountains along the Black Sea, on which are the Olympus and Ida of the ancients, rise to 6000 or 7000 ft.; the Taurus is more lofty, reaching 8000 and 10,000 ft.; both ranges decline in altitude as they approach the Mediterranean.
This great plateau, extending from the Mediterranean to the Indus, has a length of about 2500 m.
The north-western extremity of the elevated Tibeto-Himalayan mountain plateau is situated about on 73° E.
From it the Oxus, or Amu, flows off to the west, and the Jaxartes, or Syr, to the north, through the Turki state of Khokand, while to the east the waters run down past Kashgar to the central desert of the Gobi, uniting with the streams from the northern slope of the Tibetan plateau that traverse the principalities of Yarkand and Khotan, which are also Turki.
The central area bounded on the north and north-west by the Yablonoi Mountains and their western extension in the Tian-shan, on the south by the northern face of the Tibetan plateau, and on the east by the Khingan range before alluded to, forms the great desert of central Asia, known as the Gobi.
It includes an immense high and broken plateau which spreads from south-west to north-east, losing in width and altitude as it advances north-east.
Bonvalot, accompanied by Prince Henri d'Orleans, crossed the Tibetan plateau from north to south, but failed to enter Lhasa.
The great highland plateau which tion stretches from the Himalaya northwards to Chinese Turkestan, and from the frontier of Kashmir eastwards to China, has now been defined with comparative geographical exactness.
The great central depression of the continent which reaches from the foot of the Pamir plateau on the west through the Tarim desert to Lop Nor and the Gobi has yielded up many interesting Chinese secrets.
South and east of the Palaeozoic plateau is an extensive area consisting chiefly of Archean rocks, and including the greater part of Mongolia north of the Tian-shan.
Farther south, in the Chinese provinces of Shansi and Shensi, the geological succession is similar in some respects to that of the Siberian Palaeozoic plateau, but the sequence is more complete.
The city of Ayacucho, capital of the department of that name and of the province of Guamanga, is situated on an elevated plateau, 8911 ft.
The department of Ayacucho extends across the great plateau of central Peru, between the departments of Huancavelica and Apurimac, with Cuzco on the E.
It consists chiefly of an extensive plateau between the Eastern and Western Ghats, of a height varying from Boo to 1000 ft.
The disturbances among the underlying rocks of Ohio have been slight, and originally the surface was a plain only slightly undulating; stream dissection changed the region to one of numberless hills and valleys; glacial drift then filled up the valleys over large broken areas, forming the remarkably level till plains of northwestern Ohio; but at the same time other areas were broken by the uneven distribution of the drift, and south-eastern Ohio, which was unglaciated, retains its rugged hilly character, gradually merging with the typical plateau country farther S.E.
Its southern extremity penetrates into the high plateau of Asia, and the lake lies entirely in the Alpine zone which fringes that plateau on the north-west.
The deepest part is in the south-east, at the foot of the Khamardaban border-ridge of the high plateau.
With the exception of the extreme north (Commagene), which is shut off by a barrier of hills and belongs to foreign hydrographic systems, the whole country is roughly a gable-shaped plateau, falling north and south from a medial ridge, which crosses Syria at about its central point.
Thereafter it broadens out and becomes the high table-land of Galilee, Samaria and Judaea, and gradually sinks into the plateau of north Sinai.
The Drakensberg forming the buttress of the plateau seaward, attain their highest elevation on the BasutoNatal border.
It is commonly said to take its origin in some small lakes a little south of the summit plateau of the Mont Genevre Pass.
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.
The city was built by the state on an open plateau, and provided with all necessary public buildings, gas, water and tramway services before the seat of government was transferred from Ouro Preto.
has gigantic cryptomerias and chamoecyparis; then follow pines; then, at a height of 9500 ft., a broad plateau, and then alternate stretches of grass and forest up to the top, which consists of several small peaks.
The state occupies an elevated plateau, extending from two spurs of the Sierra Madre, called the Sierra Fria and Sierra de Laurel, eastward to the rolling fertile plains of its eastern and south-eastern districts.
These railway communications, and the situation of the city (on the Piedmont Plateau) on the water-parting between the streams flowing into the Atlantic Ocean and those flowing into the Gulf of Mexico, have given Atlanta its popular name, the "Gate City of the South."
As is shown by its name the province is situated in the centre of the Indian peninsula, comprising a large proportion of the broad belt of hill and plateau country which separates the plains of Hindustan from the Deccan.
plateau, and districts south of the Satpuras.
The, 6th century saw the establishment of a powerful Gond kingdom by Sangram Sah, who succeeded in 1480 as the 47th of the petty Gond rajas of Garha-Mandla, and extended his dominions so as to include Saugor and Damoh on the Vindhyan plateau, Jubbulpore and Narsinghpur in the Nerbudda valley, and Seoni on the Satpura highlands.
In the 17th century Chhatarsal, the Bundela chieftain, deprived the Mandla principality of part of the Vindhyan plateau and the Nerbudda valley.
The whole region is characterized by a remarkable degree of physical uniformity, and may be broadly described as a vast plateau of an average elevation of 3000 ft., bounded westwards by the Ethiopian and Galla highlands and northwards by an inner and an outer coast range, skirting the south side of the Gulf of Aden in its entire length from the Harrar uplands to Cape Guardafui.
The plateau, known as the Ogaden plateau, everywhere presents the same monotonous aspect of a boundless steppe clothed with a scanty vegetation of scrubby plants and herbaceous growths.
- The Somaliland plateau is chiefly composed of gneiss and schist.
In the north the plateau is overlain by red and purple unfossiliferous sandstones, capped near its edge by a cherty limestone also unfossiliferous but possibly of Lower Cretaceous age.
The plains inland from Berbera, and the maritime margins between the coast and foot of the plateau, consist of limestones of Lower Oolitic age with Belemnites subhastatus.
On an average the coast-belt temperatures are some 10 0 higher than those of the plateau.
In consequence of the elevation of the plateau and the dryness of the air, the heat is less oppressive than is indicated by the temperatures recorded.
On the plateau many forms common elsewhere in East Africa, such as the Borassus palm and the baobab tree, are missing.
high, and thickets of tamarisk along the river beds, and on either side the jungle is high and more luxuriant than on the open plateau.
The antelopes include the beisa oryx, fairly common and widely distributed; the greater and lesser kudu (the greater kudu is not found on the Ogaden plateau); the Somali hartebeest (Bubalis Swaynei), found only in the Haud and Ogo districts; waterbuck, rare except along the Webi Shebeli and the Nogal; the dol or Somali bushbuck; the dibatag or Clarke's gazelle; the giraffe-like gerenuk or Waller's gazelle, very common; the aoul or Soemmering's gazelle, widely distributed; the dero (Gazella Speki); and the small dikdik or sakaro antelope, found in almost every thicket.
The Hawiya domain comprises the Ogaden plateau and the region generally between the Nogal and Webi-Shebeli rivers.
Between the Harrar plateau and Cape Guardafui the coast ranges maintain a mean altitude of from 4000 to 5000 ft., and fall generally in steep escarpments down to the narrow strip of sandy lowlands skirting the Gulf of Aden.
South of the Golis the ground falls gradually to the central plateau known as the Haud, a waterless but not unfertile district.
Its waters are lost in the arid stony plateau of the Sorl.
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.
The region between the lines of the two coastal systems is a much dissected plateau, imperfectly explored.
It first flows in a valley bounded, especially towards the west, by the escarpments of a high plateau, and containing the towns of Lugh (in 3° 50' N., the centre of active trade), Bardera, 387 m.
Its summit consists of a plateau too acres in area, with a slight slope to the south, terminating on its north-eastern side in a sheer fall of more than 1500 ft.
They comprise the geographically distinct regions of the Anatolian plateau (Asia Minor), the Armenian and Kurdish highlands, the Mesopotamian lowlands, the hilly and partly mountainous territory of Syria and Palestine and the coast lands of west and north-east Arabia.
The main body were between Weimar and Apolda during the 12th, and the Saxons duly effected their junction with Hohenlohe in the vicinity of Vierzehnheiligen, whilst the latter had withdrawn his troops all but some outposts from Jena to the plateau about Capellendorf, some 4 m.
Hohenlohe now brought up the remainder of his command, but in the meanwhile the French had poured across the neck between the Landgrafenberg and the main plateau, and the troops of Soult and Augereau were working up the ravines on either hand.
Davout in obedience to his orders of the previous morning was packed on the narrow plateau of the mountain, whilst, below in the ravines on either flank, Soult on the right, and Augereau on the left, were getting into position.
The latter with at least 50,000 men was marching in two columns, and ought therefore to have delivered its men into line of battle twice as fast as the French, who had to deploy from a single issue, and whose columns had opened out in the passage of the Kosen defile and the long ascent of the plateau above.
in width along the coast, and of a mountainous tract, falling steeply on the west and merging into a highland plateau which slopes gradually to the N.E.
The city commands pleasant views from its position on a plateau, which, at places on bluffs along the shore, has elevations of about 75 ft.
Situated on the northern border of the Central Plateau, the department slopes from south to north.
Plains alternating with forests occupy the northern zone of the department, while the central and western regions form an undulating and well-watered plateau.
SELENGA-ORKHON, a river of Central Asia, which rises in two principal head-streams, the Selenga and the Orkhon, on the plateau of N.W.
The village is picturesquely situated on a plateau within a rampart of hills on the E.
The harbour town is Adamanta; from this there is an ascent to the plateau above the harbour, on which are situated Plaka, the chief town, and Kastro, rising on a hill above it, and other villages.
Holdich, India (” Regions of the World " series, 1903); Ryder, Geographical Journat, 1905; Rawlings, The Great Plateau (1906).
Up to the year 1862 not only was the fortress of Belgrade garrisoned by Turkish troops, but the Danubian slope of the town was inhabited by Turks, living under a special Turkish administration, while the modern part of the town (the plateau of the ridge and the western slope) was inhabited by Servians living under their own authorities.
American plateau in Brazil from Pernambuco to Rio de Janeiro, at a height of 3000 to 5000 ft.
Like other plateaus, the great plateau of the centre of Asia, stretching from the Himalayas to Bering Strait, 2 has on its surface a number of gentle eminences (angehaufte Gebirge of K.
On the margins of the plateau there are several gaps or indentations, which can best be likened to gigantic trenches, like railway cuttings, as with an insensible gradient they climb to a higher level.
These trenches have for successive geological periods been the drainage valleys of immense lakes (probably also of glaciers) which formerly extended over the plateau or fiords of the seas which surrounded it.
And it is along these trenches that the principal commercial routes have been made for reaching the higher levels of the plateau itself.
In the plateau there are in reality two terraces - a higher and a lower, both very well defined in Transbaikalia and in Mongolia.
Several low chains of mountains have their base on the lower terrace and run from south-west to north-east; they are known as the Nerchinsk Mountains in Transbaikalia, and their continuations reach the northern parts of the Gobi.4 The great plateau is fringed on the north-west by a series of lofty border-ranges, which have their southern base on the plateau and their northern at a much lower level.
There are, however, among these border-ranges several breaches of continuity - broad depressions or trenches leading from Lake Balkash and Lake Zaisan to the upper parts of the plateau.
On the other hand, there are on the western outskirts of the plateau a few mountain chains which take a direction at right angles to the above (that is, from north-west to south-east), and parallel to the great line of upheavals in south-west Asia.
But around and north-east of this lake the same wellmarked ranges fringe the plateau and turn their steep north-western slope towards the valleys of the Irkut, the Barguzin, the Muya and the Chara, while their southern base lies on the plateaus of the Selenga (nearly 4000 ft.
The orography of the Aldan region is little known; but travellers who journey from the Aldan (tributary of the Lena) to the Amur or to the Sea of Okhotsk have to cross the same plateau and its border-range.
A typical feature of the north-eastern border of the high plateau is a succession of broad longitudinal 5 valleys along its outer base, ' The wide area between the middle Lena and the Amur, as well as the hilly tracts west of Lake Baikal, and the Yeniseisk mining region are in this condition.
2 The great plateau of North America, also turning its narrower point towards Bering Strait, naturally suggests the idea that there was a period in the history of our planet when the continents turned their narrow extremities towards the northern pole, as now they turn them towards the southern.
The south-eastern slope of the great plateau of Asia cannot properly be reckoned to Siberia, although parts of the province of Amur and the Maritime Province are situated on it; - they have quite a different character, climate and vege- eastern, tation, and ought properly to be reckoned to the Manslope of, churian region.
To the east of the Yablonoi border-range p l ateau: lies the lower terrace of the high plateau, reaching 2000 to 2500 ft.
Two such folds maybe distinguished, corresponding on a smaller scale to the belt of alpine tracts which fringe the plateau on the north-west.
This conformation is seen in the valley of the Us in West Sayan, in that of the upper Oka and Irkut in East Sayan, in the valley of the Barguzin, the upper Tsipa, the Muya and the Chara, at the foot of the Vitim plateau, as also, probably, in the Aldan.
in breadth, fringes the plateau on the N.
Volcanic formations, so far as is known, occur chiefly along the north-western border-range of the great plateau.
Ejections of basaltic lava have been observed on the southern slope vo of this range, extending over wide areas on the plateau itself, over a stretch of more than 600 m.
- namely, in East Sayan about Lake Kosso-gol and in the valley of the Tunka (river Irkut), in the vicinity of Selenginsk, and widely distributed on the Vitim plateau (rivers Vitim and Tsipa).
Gold-dust is found in almost all the alpine regions fringing the great plateau.
Gold is found on the high plateau in the basin of the upper Vitim, on the lower plateau in the Nerchinsk district, and on the upper tributaries of the Amur (especially the Oldoi) and the Zeya, in the north-east continuation of the Nerchinsk Mountains.
The three principal rivers - the Ob, the Yenisei, and the Lena - take their rise on the high plateau or in the alpine regions fringing it, and, after descending from the plateau and piercing the alpine regions, flow for many hundreds of miles across the high plains and lowlands before they reach the Arctic, Ocean.
being, however, much shorter, as in these latitudes the plateau approaches nearer to the Arctic Ocean.
The Amur, the upper tributaries of which rise on the eastern border-range of the high plateau, is similar.
There are wide areas on the plains of West Siberia and on the high plateau of East Siberia, which, virtually, are still passing through the Lacustrine period; but the total area now under water bears but a trifling proportion to the vast surface .which the lakes covered even at a very recent period, when Neolithic man inhabited Siberia.
This arises chiefly from the orographical structure; the vast plateau of Central Asia prevents the moderating influence of the sea from being felt.
The Cevennes proper are formed by a folded belt of Palaeozoic rocks which lies along the south-east border of the central plateau of France.
The overthrust came from the south-east, and the Palaeozoic beds were crushed and crumpled against the ancient massif of the central plateau.
The Secondary and Tertiary beds of the Languedoc were crushed against the central plateau and were frequently overfolded.
The shore consists of a central plateau descending to the water in three terraces, each with its "tread" and "rise."
The central plateau is a plain whose surface presents "rounded, flat-topped hills and low ridges and reefs of limestone," with narrow intervening valleys.
This region is the smallest of the chapadao divisions of the great plateau, and might be considered either a southward extension of the Sao Francisco or an eastward extension of the Parana chapadao.
Its rivers flow easterly into the Atlantic and drain a triangular-shaped area of the plateau lying between the northern frontier and the southern and western watersheds of the Araguary, whose extreme limits are about o° 30' N.
The rivers of the great Brazilian plateau which flow directly to the Atlantic coast may be divided into two classes: those of its northward slope which flow in - a northerly and north-easterly direction to the north-east coast of the republic, and those which drain its eastern slope and flow to the sea in an easterly direction.
The latter descend from the plateau much nearer the coast, and are in most cases navigable for short distances only.
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.
The Sao Francisco, which belongs to the inland plateau region, is the largest river of the eastern coast of Brazil and exists by virtue of climatic conditions wholly different from those of the coast where it enters the Atlantic. The tributaries of the lower half of this great river, which belong to the Atlantic coast region, are small and often dry, but the upper river where the rainfall is heavier and more regular receives several large affluents.
From the Sao Francisco to Cape Frio there are many short rivers rising on the slopes of the plateau and crossing the narrow coastal plain to the sea.
There are also a few of greater length which rise far back on the plateau itself and flow down to the plain through deeply cut, precipitous courses.
The navigable channels of these rivers are restricted to the coastal plain, except where a river has excavated for itself a valley back into the plateau.
This river system drains a large part of the northern mountainous region of the state, and has a considerable extension of navigable channels between the plateau margin and the lake.
Though the Uruguay plays a less important part, its relations to the country are similar to those of the Parana, and its tributaries from the plateau region are similarly broken by falls and rapids.
In general terms, it is a tropical country, with sub-tropical and temperate areas covering its three southern states and a great part of the elevated central plateau.
The climatic conditions of the Brazilian plateau are widely different from those of the coast in many respects.
The Brazilian Guiana plateau, lying immediately north of the equator, is in great part a hot, stony desert.
It lies in the north-east trade winds belt, but the mountain chain on its northern frontier robs these winds of their moisture and leaves the greater part of the Brazilian plateau rainless.
South of the Amazon valley and filling a great part of the eastern projection of the continent, is another arid, semi-barren plateau, lying within the southeast trade winds belt, and extending from Piauhy southward to southern Bahia.
In winter the plateau is less heated, and cold currents of air from the west and south-west cause precipitation over a part if not all of this region.
The scene of the most important fighting was the Pratzen plateau.
Kutusovwaspursuing this march to the southwest when he was surprised by the swift advance of Soult's men on the plateau itself.
The French did not win the plateau without a severe struggle.
The Russians in Sokolnitz surrendered, an opportune cavalry charge further discomfited the allied left, and the Pratzen plateau was now in full possession of the French.
The last serious attempt of the allies in the centre led to some of the hardest fighting of the day; the Russian Imperial Guard under the grand-duke Constantine pressed closely upon St Hilaire and Vandamme on the plateau, and only gave way when the French Guard and the Grenadiers came into action.
No further attempt was made on the plateau, which was held by the French from Pratzen to the Olmiitz road.
The fighting in Telnitz was perhaps the hardest of the whole battle, but the inevitable retreat, every part of which was now under the fire of the French on the plateau, was terribly costly.
28 sqq., led southwards from Ai over an undulating plateau to Michmash.
On the north the crag is crowned by a sort of plateau sloping backwards into a round-topped hill.
Many of the inhabitants are nominally Moslems. The greater part of the province may be said to consist of an extensive plateau, generally from 5000 to 7000 ft.
The climate is generally healthy and equable; on the plateau the summer heat seldom exceeds 86°, and in winter there is little snow.
The state belongs to the elevated plateau region, with its semi-arid conditions.
and 20° 47' N., at an altitude of about 5000 ft., in a depressed plateau on the crest of the Sintaung hills.
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.
Geographically it is a table-land, forming the north-east corner of the great plateau of Asia Minor, edged on the north by a lofty mountain rim, along the foot of which runs a fringe of coast-land.
The inhabitants of Baden are of various origin - those to the north of the Murg being descended from the Alemanni and those to the south from the Franks, while the Swabian plateau derives its name and its population from another race.
above sea-level on the right bank of the Ve]ino (a torrent subtributary to the Tiber), which at this point issues from the limestone plateau; the old town occupies the declivity and the new town spreads out on the level.
Nuevo Leon lies partly upon the great Mexican plateau and partly upon its eastern slopes, the Sierra Madre Oriental crossing the state N.W.
YAK, the wild (and domesticated) ox of the Tibetan plateau; a species nearly allied to the bison group. The yak, Bos (POephagus) grunniens, is one of the finest and largest of the wild oxen, characterized by the growth of long shaggy hair on the flanks and under parts of the body and the well-known bushy tail.
None of such halfbreeds can compare with the magnificent half-tamed animals kept by the natives of the elevated Rupsu plateau, S.
at the shoulder, and is absolutely confined to the arid central plateau of Tibet.
It is built for the most part on a plateau about 50 ft.
After the execution he sought a secluded retreat on the Plateau de Satory at Versailles and took exercise after nightfall.
by the inland plateau of Syria, mainly steppe-land.
The country is an elevated plateau, with hills in the southern and central parts.
It stands on a narrow plateau of ground supported on the south-east by a terrace wall.
MORELOS, an inland state of Mexico on the southern slope of the great Mexican plateau, lying S.
The Carpathians separate Hungary and Transylvania from Lower Austria, Moravia, Silesia, Galicia, Bukovina and Rumania, while its ramifications fill the whole northern part of Hungary, and form the quadrangular mass of the Transylvanian plateau.
The eastern part of Bastar is a flat elevated plateau, from 1800 to 2000 ft.
On the plateau there are but few hills; the streams run slowly and the country is a mixture of plain and undulating ground covered by dense sdl forests.
There are also indications of another series of faults roughly parallel to the south-east coast, which point to the islands being fragments of a former extensive plateau.
TEGEA, an ancient Greek city of Arcadia, situated on a plateau which is enclosed by Mts.
and W., and by two transverse ranges which separate it from the plateau of Orchomenus and the Eurotas valley respectively.
above the sea, and occupies the southern end of the great central rift-valley, which terminates suddenly at its southern point, the line of depression being represented farther south by the more easterly trough of Lakes Nyasa and Rukwa, from which Tanganyika is separated by the Fipa plateau, composed of old granitoid rocks; though even here traces of old valley-walls are said by Dr Kohlschiitter to exist.
The latter almost at once encountered the heads of the 6th cavalry division, at that moment just clearing the defile leading up to the Rezonville plateau from Gorze.
Without pausing to fire, the men raced onward, but the French striking their outer wing rolled up the whole line in succession, the actual collision occurring in and near the Bruville ravine, a deep-cut natural trench which, starting from the Tronville copses, here intersects the plateau from west to east.
The same idea had, however, occurred to Ladmirault, and he had called on the two nearest French cavalry divisions to put it into execution, and as the Prussians began to reach the plateau west of Mars-la-Tour and the Yron brook from the south, the French were deploying across it some two thousand yards to the north.
- The position on to which the French army fell back from the field of Vionville is formed by a ridge some six miles long running from Rozerieulles almost due north to Roncourt, a little village overhanging the steep and wooded banks of the Orne, and connected with the general plateau between the Meuse and Moselle by a gentle saddle running from about Amanvillers nearly due west through the Bois de la Cusse towards Doncourt.
Corps succeeded in reaching the plateau between St Hubert and Point du Jour, where the debris of the VII.
The Paropamisus forms the southern face of the Turkestan plateau, which contains the sources of the Murghab river; the northern face of the same plateau is defined by the Band-i-Turkestan.
On the south of the plateau we find a similar succession of narrow valleys dividing parallel flexures, or anticlinals, formed under similar geological conditions to those which appear to be universally applicable to the Himalaya, the Hindu Kush, and the Indus frontier mountain systems. From one of these long lateral valleys the Hari Rud receives its principal tributary, which joins the main river below Obeh, 180 m.
The city is built in a bowllike depression of the great central plateau, and the drainage from the surrounding hillsides has produced a dangerously insanitary condition, from which one or two virulent fever epidemics have resulted.
HOLGUIN, a town of the high plateau country in the interior of Oriente province, Cuba, about 65 m.
The town is near the Maranon and Jigue rivers, on a plain from which hills rise on all sides except the E., on which side it is open to the winds of the plateau.
Viewed from the floor of the ocean the continental block would thus appear as a great plateau rising to a height of 14,360 ft.
troughs and basins in the middle of the ocean, (2) the steeply sloping ridge which interposes a narrower barrier between two depressions, and (3) the plateau or wide elevation rising steeply on all sides from a depression.
it widens into what was called by Maury the Telegraph Plateau.
Continuing southwards the rise joins the Azores Plateau, which has in parts a very marked relief, and runs thence southward almost exactly in the middle of the ocean, becoming gradually lower as it goes.
is only from 3 2.2° to 32.7° F., and the same low temperature continues throughout the Brazil Basin to the equator; but in the North American Basin from the West Indies to the Telegraph Plateau no satisfactory bottom temperature lower than 35.6° F.
These mountains, which have in the northern part an altitude of 2700 ft., slope down towards the south-east near Tokaj in a hilly plateau of about 1500 ft.
The hills in the south of the duchy are a continuation of the Lorraine plateau, and the northern districts are crossed in all directions by outrunners from the Ardennes.
Besides the iron furnaces, situated in the south near the Lorraine plateau, there are tanneries, weaving and glove-making factories, paper-mills for all sorts of paper, breweries and distilleries, and sugar refineries.
The Great Plains (really a plateau) comprise the W.
from the high plateau or from the mountains in the W.
boundary of New Mexico the Great Plains province is known as the Edwards Plateau; between the Edwards Plateau and the valley of the Canadian river, as the Llano Estacado, or Staked Plains; and N.
parts of the Edwards Plateau and the E.
corner of the Trans-Pecos Province is a smaller plain known as the Stockton Plateau, but the remaining portion of this province is traversed from N.E.
of the Pecos Valley, and in the Staked Plain and Edwards Plateau; and the widely extending Lower Austral zone, covering most of the state and subdivided into the Lower Sonoran or arid western part, the Austroriparian, or humid eastern, and the narrow Gulf Strip, which is semi-tropical.
The Totonacs inhabit northern Vera Cruz and speak a language related to that of the Mayas; the Tarascos form a small group living in Michoacan; the Matlanzingos, or Matlaltzincas, live near the Tarascos, the savage Apaches, a nomadic group of tribes ranging from Durango northward into the United States; the Opata-Pima group, inhabiting the western plateau region from Sonora and Chihuahua south to Guadalajara, is sometimes classed as a branch of the Nahuatlaca; the Seris, a very small family of savages, occupy Tiburon Island and the adjacent mainland of Sonora; and the Guaicuros, or Yumas, are to be found in the northern part of the peninsula of Lower California.
It is celebrated because of the difficulties overcome on the precipitous eastern slopes of the Sierra Madre, the beauties of the mountain scenery through which it passes, and the rapid transition from the hot, humid coastal plain to the cool, arid plateau, 7924 ft.
The next important line is the F.C. Internacional Mexicano, running from Ciudad Porfirio Diaz, on the Rio Grande, south-westward across the plateau to Durango, and is to be extended to Mazatlan, on the Pacific coast.
and below, is that of some of the mountain tops of northern Georgia; from the mountain-sides to the Piedmont Plateau this mean temperature varies from 45° to 60'; on the Piedmont Plateau from 60° to 65°; and on the Coastal Plain from 60° to 70°.
In the Cumberland Plateau and Great Valley Regions are a red or brown loam, rich in decomposed limestone and calcareous shales, and sandy or gravelly loaTns.
In the Piedmont Plateau and Appalachian Mountains Regions the surface soil is generally sandy, but in considerable areas the subsoil is a red clay derived largely from the decomposition of hornblende.
In the north the ground rises gradually to a plateau some 2000 ft.
The helo hovered near the edge of the plateau.
It receives from the north several intermittent streams, the chief, usually carrying a fair amount of water, being the Khulu or Kolimbine, coming from the Kaarta plateau.
The value per acre of land, which exceeds 48 in the departments of Seine, Rhne and those fringing the north-west coast from Nord to Manche inclusive, is on the average about 29, though it drops to 16 and less in Morbihan, Landes, Basses-Pyrnes, and parts of the Alps and the central plateau.
The western trough extends northwards into Davis Strait, forming a depression in the Telegraph plateau; to the south of Newfoundland and Nova Scotia are Sigsbee Deep, Libbey Deep and Suhm Deep, each of small area; north-east of the Bahamas Nares Deep forms the largest and deepest depression in the Atlantic, in which a sounding of 4561 fathoms was obtained (70 m.
An elevation of great extent which rises at a very gentle angle from a surrounding depression is termed a " rise," one which is relatively narrow and steep-sided a " ridge," and one which is approximately equal in length and breadth but steep-sided a " plateau," whether it springs direct from a depression or from a rise.
The upper Euphrates consists of two arms, which, rising on the Armenian plateau, and flowing west in long shallow valleys parallel to Mount Taurus, eventually unite and force their way southward through that range to the level of Mesopotamia.
from the Persian Gulf, separated from it by a couple of small spurs of the Syrian plateau, and may be said to mark the beginning of the lower Euphrates.
The state lies wholly within the great Brazilian plateau region, but its surface is much broken towards the N.
The general elevation of the plateau is estimated to be about 2700 ft., and the highest elevation was reported in 1892 to be the Serra dos Pyreneos (5250 ft.).
Finally, in the S.E., towards the Caspian, on the slopes of the southern Urals and the plateau of Obshchiy Syrt, as also in the interior of the Crimea, and in several parts of Bessarabia, there are large tracts of real desert, buried under coarse sand and devoid of vegetation.
On reaching the Tibetan plateau, with the increased dryness the flora assumes many features of the Siberian type.
Little, The Far East (Oxford, 1905); Captain Rawling, The Great Plateau (London, 1905); Journal of the Royal Geogl.
The Rio Grande de Lerma, or Santiago, is the principal river, whose sources are to be found on the high plateau in the state of Mexico.
The capital of the territory is Tepic (pop. 1900, 15,488), attractively situated on a small plateau 2 9 50 ft.
in the Stavropol "plateau," which stretches northwards, separating the tributaries of the Kuban from those of the Terek and the Kuma.
But the uniformity of the slope is interrupted by a plateau (2000-3000 ft.
The Armenian highlands, which run generally parallel to the Caucasus, though at much lower elevations (5000-6000 ft.), are a plateau region, sometimes quite flat, sometimes gently undulating, clothed with luxuriant meadows and mostly cultivable.
North of the Caucasus ranges the water-divide between these two seas descends from Mount Elbruz along the Sadyrlar Mountains (11,000 ft.), and finally sinks into the Stavropol "plateau" (1600 ft.).
After acquiring the northern edge of the Armenian plateau, partly from Persia in 1828 and partly from Turkey in 1829, Russia crushed a rising which had broken out in the Caspian coast districts of Daghestan on the north of the Caucasus.
The state lies on the borderland between the Prairie Plains and the Alleghany Plateau.
Owing to the fact that the great plateau separates the Lena from the Amur, no easy water communication can be established between the latter and the other Siberian rivers.
The tributaries of the Amur (the Shilka with its affluent the Ingoda) become navigable only on the lower terrace of the plateau.
But the trench of the Uda, to the east of Lake Baikal, offers easy access for the Great Siberian railway up to and across the high plateau.
On the high plateau the larch predominates over all other species of conifers or deciduous trees; the wide, open valleys are thickly planted with Betula nana and B.
The Siberian larch predominates also in the alpine tracts fringing the plateau on the north, intermingled with the fir, stone-pine, aspen and birch.
The lower plateau exhibits, of course, new characteristics.
The high plains of the west slope of the plateau are also rich prairies diversified with woods.
On the whole, we may say that the arctic and boreal faunas of Europe extend over Siberia, with a few additional species in the Ural and Baraba region - a number of new species also appearing in East Siberia, some spreading along the high plateau and others along the lower plateau from the steppes of the Gobi.
On the lower terrace of the great plateau we find an 1 In Vega Exped.
The Mongols (less than 300,000) extend into West Siberia from the high plateau - nearly 20,000 Kalmucks living in the eastern Altai.
The Tunguses (nearly 70,000) occupy as their hunting-grounds an immense region on the high plateau and its slopes to the Amur, but their limits are yearly becoming more and more circumscribed both by Russian gold-diggers and by Yakut settlers.
On the high plateau all attempts to grow cereals have failed, the wide trenches alone (Uda, Selenga, Jida) offering encouragement to the agriculturist.
On the lower plateau, in Transbaikalia, grain is successfully raised in the Nerchinsk region, with serious risks, however, from early frosts in the valleys.
During the great migrations in Asia from east to west many populations were probably driven to the northern borders of the great plateau and thence compelled to descend into Siberia; succeeding waves of immigration forced them still farther towards the barren grounds of the north, where they melted away.
It is situated upon a lofty plateau, the highest point of which (823 ft.), projecting to the W., was the ancient citadel, and is occupied by the well-preserved castle erected by Frederick II., and rebuilt by Pierre d'Angicourt about 1280.
The long straight lines of works which stretched to the plateau of the Michelsberg and formed the outworks of the main fortress on the left bank of the Danube were purchased in 1900 by the municipal authorities, in order to be levelled and laid out in streets for the extension of the town in this direction.
EUSKIRCHEN, a town of Germany, in the Prussian Rhine province, on a plateau lying to the E.
North of this line is the low hilly country, known as the Waldviertel, which lies at the foot and forms the continuation of the Bohemian and Moravian plateau.
Cebenna or Gehenna), a mountain range of southern France, forming the southern and eastern fringe of the central plateau and part of the watershed between the Atlantic and Mediterranean basins.
On its northern aspect this plateau has a raised rim having all the appearances of being once the margin of an atoll.
The Orange here enters the great inner plateau of South Africa, which at Aliwal North, the first town of any size on the banks of the river, 80 m.
The Brazilian plateau slopes southward and eastward, traversed by broken ranges of low mountains and deeply eroded by river courses.
The table-topped hills of Almeyrin (or Almeirim) and Erere, which lie near the lower Amazon and rise to heights of 800 and 900 ft., are generally considered the southernmost margin of this plateau, though Agassiz and others describe them as remains of a great sandstone sheet which once covered the entire Amazon valley.
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.
In general, Brazilian Guiana, as this plateau region is sometimes called, is one of the least attractive parts of the republic.
The great Brazilian plateau, which is the most important physical division of Brazil, consists of an elevated tableland moo to 3000 ft.
This range forms the true backbone of the maritime mountainous belt and rises from the plateau itself, while the Coast Range rises on its eastern margin and forms a rim to the plateau.
deep, has been excavated northward from the centre of the plateau.
The plateau breaks down abruptly toward the sea, and slopes gradually some hundreds of feet toward the south and west.
The northern and western parts of this plateau have an average elevation a little less than that of the Atlantic margin, and their slopes are toward the south and east, those of Goyaz and Matto Grosso being abrupt and deeply eroded.
This region is well wooded along the river courses of Minas Geraes, the lower Atlantic slopes of Bahia, which are perhaps outside the plateau proper, and on the weather side of some of the elevated ridges where the rainfall is heavy and regular.
Its general elevation is less than that of the Sao Francisco region, owing to the slope of the plateau surface toward the Amazon depression and to denudation.
The Amazonian chapadao, which includes the remainder of the great Brazilian plateau west of the Sao Francisco and Parnahyba regions and which appears to be the continuation of these tablelands westward, is much the largest of these plateau divisions.
South and south-west of this arid plateau lie the inhabited tablelands of Rio de Janeiro, Sao Paulo and Minas Geraes, where the climate is greatly modified by a luxuriant vegetation and southerly winds, as well as by the elevation.
The rainfall throughout this region is abundant, except in northern Minas Geraes, where the climatic conditions are influenced to some extent by the arid eastern plateau.
There is no absolutely dry season in this part of the great Brazilian plateau, though the year is customarily divided into a dry and wet season, the latter running from September to April in Goyaz, and from November to April in Matto Grosso.
The Amazon region is frequented by the giboia (boa constrictor), and the central plateau by the sucurid (Eunectes murinus), both distinguished for their enormous size.
Besides these, the flora of the Paraguay basin varies widely from that of the inland plateau, and that of the Brazilian Guiana region is essentially distinct from the Amazon.
The coast and tide-water rivers are fringed with mangrove, and the sandy plain reaching back to the margin of the inland plateau is generally bare of vegetation, though the carnahuba palm (Copernicia cerifera) and some species of low-growing trees are to be found in many places.
The slopes of the plateau, which receive a better rainfall, are more heavily forested, some districts being covered with deciduous trees, forming catingas in local parlance.
Then come the catinga tracts, and, beyond these, the open campos of the elevated plateau, dotted with clumps of low growing bushes and broken by tracts of carrasco, a thick, matted, bushy growth 10 to 12 ft.
In general, the carrasco growth extends over the whole central plateau, and heavy forests are found only in the deep river valleys.
The development of railway construction in Brazil has been impeded to a great extent by two unfavourable conditions-by the chain of mountains or plateau escarpments which follow the coast line and obstruct communication with the interior, and by the detached positions of the settlements along the Atlantic, which compel 1 The areas are reduced from the planimetrical calculations made at Gotha and used by A.
Cruls's exploration of a section of the Goyaz plateau in 1892 in search of a site for the future capital of the republic, and from some of the river and railway surveys.
ChalybonBeroea), situated on a plateau in the valley of the Kuwaik (anc. Charus) about 10 m.
One series of its numerous headstreams traverses the Kikuyu plateau north of the Athi, while others flow down the southern and eastern slopes of Kenya.
Hyde Park is a plateau almost in the centre of the city, which in the early days of Sydney was used as a race-course.
Ranges of hills lead to the first plateau, which has an average elevation of 2000 ft.
The second plateau, reached by a steep ascent, has an elevation of from nearly 4000 to fully 5000 ft.
Thence it turns north-west, following the Great Wall for over 300 m.; it then crosses the plateau so as to separate Mongolia from the Chinese province of Sin-Kiang (Hari-su-sin-tsiang, which includes the Nan-shan highlands and eastern Turkestan), and from Dzungaria, reaching the Chinese or Ektagh Altai in 46° 30' N., 92° 50' E.
Geographically, Mongolia may thus be said to occupy both terraces of the great plateau of east Asia, which stretches in the south of Siberia, between the Sailughem range of the Great Altai and the Great Khingan - with the exception of the Dzungarian depression.
From Manchuria and China it is separated by the border ridge of the plateau - the Great Khingan, while in the south-west it runs up to the foot of the high northern border ridges of the Tibetan plateau - an artificial frontier separating it from east Turkestan and Dzungaria.
Broadly speaking, Mongolia may be divided naturally into three parts: (1) north-western Mongolia, which occupies the high terrace of the plateau; (2) the Gobi, in its wide sense, covering the lower terrace of the plateau, together with a slightly more elevated and better-watered zone along the western slope of the Great Khingan and its south-western continuation; and (3) southeastern Mongolia, on the eastern slope of the Khingan.
It appears, however, from Russian explorations during the last third of the 19th North- century, that it has all the characteristics of an elevated western plateau, of a rhomboid shape (like Bohemia), bounded by four mountain ranges; namely, the Russian Altai on the N.W., the Sayans on the N.E., the Kentei range on the S.E., and the Ektagh Altai on the S.W.
above the general level of the plateau.
in 94° E., its north-eastern foot rests on the high plateau, i.e.
Thus the Ektagh Altai is a true border-rangethat is, a lofty and steep escarpment facing the Dzungarian depression, with a gentle and relatively short slope towards the plateau.
to E.S.E., border another slightly higher terrace of the same great plateau of north-west Mongolia, upon which Lake Kossogol lies, at an altitude of 5320 ft.
representing the northern counterpart of the plateau of Tibet.
The Kobdo river, which rises in the Dain-gol (7060 ft.) in the Ektagh Altai, winds in great curves across the plateau, and enters Lake Kara-usu (3840 ft.), which also receives the Buyantu, an outflow from Lake Kobdo, and is connected by a small river with another large lake, Durga-nor, situated a score of miles to the east.
The plateau is built up of granites, gneisses and crystalline schists of Archean and probably Primary age.
The Hindu Kush represents the southern edge of a great central upheaval or plateau.
To the north the plateau gradually slopes away towards the Oxus,, falling from an average altitude of 15,000 ft.
Its surface is a roughly broken plateau, traversed N.W.
Lemberg is situated on the small river Peltew, an affluent of the Bug, in a valley in the Sarmatian plateau, and is surrounded by hills.
That part of the plateau east of Johannesburg is from 5000 to 6400 ft.
The northern edge of the plateau follows an irregular line from somewhat north of Mafeking on the west to the Mauchberg on the east.
The banken veld, formed by the denudation of the plateau, is much broken up and is rich in romantic scenery.
Thence issue many streams which in their way to the ocean have forced their way through the ranges of hills which mark the steps in the plateau, forming the narrow passes or poorts characteristic of South African scenery.
West and north of the Drakensberg the general level of the low veld is not much below that of the lowest altitudes of the middle veld, though the climatic 1 By the Boers the western and less elevated part of the plateau is known as the middle veld.
in the year, but it diminishes rapidly towards the centre of the plateau where it averages, at Johannesburg about 30 in., 2 while in the extreme west as the Kalahari is approached it sinks to about 12 in.
In the eastern part of the plateau snow occasionally falls, and frost at night is common during winter.
The rainfall in the low country is more erratic than on the plateau, and in some districts, a whole year will pass without rain.
The wild seringa (Burkea africana) is also characteristic of the low veld and, extends up the slopes of the plateau.
The Sierra Madre crosses the southern part of the state parallel with the coast, separating the low, humid, forested districts on the frontier of Tabasco from the hot, drier, coastal plain on the Pacific. The mountain region includes a