Lofty lines of fold mountains form the " backbones " of North America in the Rocky of Mountains and the west coast systems, of South America in the Cordillera of the Andes, of Europe in the Pyrenees, Alps, Carpathians and Caucasus, and of Asia in the mountains of Asia Minor, converging on the Pamirs and diverging thence in the Himalaya and the vast mountain systems of central and eastern Asia.
And the Maanselka heights in the N.W.; the Baltic coast-ridge and spurs of the Carpathians in the W., with a broad depression between the two, occupied by Poland; the Crimean and Caucasian mountains in the S.; and the broad but moderately high swelling of the Ural Mountains in the E.
It is only in the S.W., where spurs of the Carpathians enter the governments of Volhynia, Podolia and Bessarabia, that ridges reaching 1 100 ft.
Of these the black-earth region - about 150,000,000 acres - which reaches from the Carpathians to the Urals, from the Pinsk marshes in the S.W.
(Great, Little and White Russians), it will be seen that, with the exception of some 3,000,000 Little Russians, now settled in East Galicia and in Poland, and of a few on the southern slope of the Carpathians, the whole of the E.
CURTEA DE ARGESH (Rumanian, Curtea de Arges; also written Curtea d'Argesh, Curtea d'Ardges, Argish and Ardjish), the capital of the department of Argesh, Rumania; situated on the right bank of the river Argesh, where it flows through a valley of the lower Carpathians; and on the railway from Pitesci to the Rothenthurm Pass.
The town rises from a marshy plain, east of the Carpathians, and west of the cornlands of southern Moldavia.
Parallel to the Carpathians are the Marsgebirge (1915 ft.) and its continuation, the Steinitzer Wald (1450 ft.).
Forestry is greatly developed; the breed of sheep in the Carpathians is of an improved quality, and the horses bred in the plain of the Hanna are highly esteemed.
TIRGU JIU (often incorrectly written Tergu Jiu), the capital of the department of Gorjiu, Rumania; situated among the lower slopes of the Carpathians, on the left bank of the river Jiu, and at the terminus of a branch railway which joins the main Walachian line between Turnu Severin and Craiova.
These mountains belong to the Carpathians and the Alps, which are separated by the valley of the Danube.
Towards the close of this period great earth movements took place and the gap between the Alps and the Carpathians was formed.
If Transylvania be excepted, three separate zones are roughly 'distinguishable: the " highland," comprising the counties in the vicinity of the Northern and Eastern Carpathians, where the winters are very severe and continue for half the year; the " intermediate " zone, embracing the country stretching northwards from the Drave and Mur, with the Little Hungarian Plain, and the region of the Upper Alfold, extending from Budapest to Nyiregyhaza and Sarospatak; and the " great lowland " zone, including the main portion of the Great Hungarian Plain, and the region of the lower Danube, where the heat during the summer months is almost tropical.
The Sla y s, the most numerous race after the Magyars, are divided into several groups: the Slovaks, mainly massed in the mountainous districts of northern Hungary; the Ruthenians, established mainly on the slopes of the Carpathians between Poprad and Maramaros Sziget; the Serbs, settled in the south of Hungary from the bend of the Danube eastwards across the Theiss into the Banat; the Croats, overwhelmingly preponderant in Croatia-Slavonia, with outlying settlements in the counties of Zala, Vas and Sopron along the Croatian and Styrian frontier.
'RAMNICUVALCEA(Rimnicu' Valcea), or Rymnik, an episcopal city and the capital of the department of Valcea, Rumania; situated at the foot of the Carpathians, on the right bank of the river Olt, and on the railway from Caracal to Hermannstadt in Transylvania.
1 -142), the country of the Scythae or the country over which the nomad Scythae were lords, that is, the steppe from the Carpathians to the Don.
The dominance from the Yenisei to the Carpathians of a distinct style of art which, whatever its original elements may have been, seems to have taken shape as far east as the Yenisei basin is an additional argument in favour of a certain movement of population from the far north-east towards the south Russian steppes.
The Hungarians, severed from their kindred and their rulers, migrated to the Carpathians, whilst Oleg, the Russ prince of Kiev, passed through the Slav tribes of the Dnieper basin with the cry "Pay nothing to the Khazars" (884).
TATRA MOUNTAINS (Hungarian Tarczal) or the High Tatra, the highest group in the central Carpathians, and the central group of the whole Carpathian system.
On the northern frontier of the empire he kept the Avars in check by inducing the Serbs to migrate from the Carpathians to the Balkan lands so as to divert the attention of the Avars.
With the exception of the extreme southern and south-eastern ramifications, which belong to Rumania, the Carpathians lie entirely within Austrian and 2 The name is derived from the Slavonic word Chrb, which means mountain-range.
In official Hungarian documents of the 13th and 14th centuries the Carpathians are named Thorchal or Tarczal, and also Monies Nivium.
The total length of the Carpathians is over Boo m., and their width varies between 7 and 230 m., the greatest width of the Carpathians corresponding with its highest altitude.
The Carpathians do not form an uninterrupted chain of mountains, but consist of several orographically and geologically distinctive groups; in fact they present as great a structural variety as the Alps; but as regards magnificence of scenery they cannot compare with the Alps.
The Carpathians, which only in a few places attain an altitude of over 8000 ft., lack the bold peaks, the extensive snow-fields, the large glaciers, the high waterfalls and the numerous large lakes which are found in the Alps.
They are nowhere covered by perpetual snow, and glaciers do not exist, so that the Carpathians, even in their highest altitude, recall the middle region of the Alps, with which, however, they have many points in common as regards appearance, structure and flora.
The Danube separates the Carpathians from the Alps, which they meet only in two points, namely, the Leitha Mountains at Pressburg, and the Bakony Mountains at Vacz (Waitzen), while the same river separates them from the Balkan Mountains at Orsova.
The valley of the March and Oder separates the Carpathians from the Silesian and Moravian chains, which belong to the middle wing of the great central mountain system of Europe.
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.
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.
The Carpathian system can be divided into two groups: the Carpathians proper, and the mountains of Transylvania.
The Carpathians proper consist of an outer wall, which forms the frontier between Hungary and the adjacent provinces of Austria, and of an inner wall which fills the whole of Upper Hungary, and forms the central group. The outer wall is a complex, roughly circular mass of about 600 m.
Extending from Pressburg to the valley of the Viso, and the Golden Bistritza, and is divided by the Poprad into two parts, the western Carpathians and the eastern or wooded Carpathians.
Orographically, therefore, the proper Carpathians are divided into: (a) the western Carpathians, (b) the eastern or wooded Carpathians, and (c) the central groups.
(a) The western Carpathians, which begin at the Porta Hungarica on the Danube, just opposite the Leitha Mountains, and extend to s.
The Poprad river, are composed of four principal groups: the Little Carpathians (also called the Pressburg group) with the highest peak Bradlo (2670 ft.); the White Carpathians or Miava group, with the highest peak Javornik (3325 ft.), and the Zemerka (3445 ft.); the Beskid proper or western Beskid group, which extends from a little west of the Jablunka pass to the river Poprad, with the highest peaks, Beskid (3115 ft.), Smrk (4395 ft.), Lissa Hora (4350 ft.) and Ossus (5106 ft.); and the Magura or Arva Magura group, which extends to the south of Beskid Mountains, and contains the Babia Gora (5650 ft.), the highest peak in the whole western Carpathians.
(b) The eastern or wooded Carpathians extend from the river Poprad to the sources of the river Viso and the Golden Bistritza, whence the Transylvanian Mountains begin, and form the link between these mountains and the central groups or High Carpathians.
To the eastern Carpathians belongs also the range of mountains extending between the Laborcza and the Upper Theiss, called Vihorlat, which attains in the peak of the same name an altitude of 3495 ft.
(c) The central groups or the High Carpathians extend from the confluence of the rivers Arva and Waag to the river Poprad, and include the highest group of the Carpathian system.
The Matra group is of volcanic origin, rising abruptly in the great Hungarian plain, and constitutes one of the most beautiful groups of the Carpathians; lastly, to its east extend the thicklywooded Biikk Mountains (3100 ft.).
The western and central Carpathians are much more accessible than the eastern Carpathians and the Transylvanian Mountains.
The principal passes in the western Carpathians are: Strany, Hrozinkau, Wlara, Lissa and the Jablunka pass (1970 ft.), the principal route between Silesia and Hungary, crossed by the Breslau-Budapest railway; and the Jordanow pass.
In the central Carpathians are: the road from Neumarkt to Kesmark through the High Tatra, the Telgart pass over the Kralova Hola from the Poprad to the Gran, and the Tylicz pass from Bartfeld to Tarnow.
In the eastern Carpathians are: the Dukla pass, the Mezo-Laborcz pass crossed by the railway from Tokaj to Przemysl; the Uszok pass, crossed by the road from Ungvar to Sambor; the Vereczke pass, crossed by the railway from Lemberg to Munkacs; the Delatyn or Korosmezo pass (3300 ft.), also called the Magyar route, crossed by the railway from Kolomea to Debreczen; and the Stiol pass in Bukovina.
The Carpathians consist of an outer zone of newer beds and an inner zone of older rocks.
It is visible only in the west and in the east, while in the central Carpathians, between the Hernad and the headwaters of the Theiss, it is lost beneath the modern deposits of the Hungarian plain.
In the western Carpathians the inner zone consists of a foundation of Carboniferous and older rocks, which were folded and denuded before the deposition of the succeeding strata.
In the eastern Carpathians also, the Permian and Mesozoic beds are not much folded except near the outer margin of the zone.
The Carpathians, like the Alps, form a protective wall to the regions south of them, which enjoy a much milder climate than those, situated to the north.
As regards the fauna, the Carpathians still contain numerous bears, wolves and lynxes, as well as birds of prey.