Amber has indeed a very wide distribution, extending over a large part of northern Europe and occurring as far east as the Urals.
Only in the Urals, the Caucasus, the Timan Mountains, the region of the Donets coalfield, and the Kielce Hills is there any sign of the great folding from which nearly the whole of the rest of Europe has suffered at one time or another.
The Finland rappa-kivi, the Serdobol gneiss, and the Pargas and Rustiala marble (with the so-called Eozoon canadense) yield good building stone; while iron, copper and zinc-ore are common in Finland and in the Urals.
Russia, as a narrow strip on the Urals, and in the Dnieper ridge.
slope of the Urals; in the Pai-kho ridge; and in the islands of the Arctic Ocean.
to Mogilev; they form the central plateau, as also the slopes of the Urals and the Petchora region.
Europe, represented in Poland and in the Urals, is missing in N.W.
Russia has three large coalbearing regions - the Moscow basin, the Donets region and the Urals.
Several smaller coalfields on the slopes of the Urals and on the Timan ridge may be added to the above.
In the Urals the marine facies is more fully developed and the fauna shows affinities with that of the Productus limestone of the Central Asian mountain belt.
of the Urals, but the question as to the glaciation of the Urals still remains open.
l Bibliography: Memoirs, Izvestia and Geological Maps of the Committee for the Geological Survey of Russia; Memoirs and Sborniks of the Mineralogical Society, of the Academy of Science and of the Societies of Naturalists at the Universities; Mining Journal; Murchison's Geology of Russia; Helmersen's and MSller's Geological Maps of Russia and the Urals; Inostrantsev in Appendix to Russian translation of Reclus's Geogr.
Urals, as well as to some of the steppe governments.
it has the Asiatic dominions of the empire, Siberia and the Kirghiz steppes, from both of which it is separated by the Ural Mountains, the Ural river and the Caspian - the administrative boundary, however, partly extending into Asia on the Siberian slope of the Urals.
Urals, and enters the ocean by a large estuary at the Gulf of Pechora.
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.
Isolated black-earth islands, though less fertile, occur also in Courland and Kovno, in the OkaVolga-Kama depression, on the slopes of the Urals, and in a few patches in the N.
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.
Russia, though it does reach as far as the Urals and beyond.
It does not, however, prevail for long, and in the first half of September frosts begin on the middle Urals.
The temperature drops so rapidly that a month later, about October the oth on the middle Urals and November the 15th throughout Russia, the thermometer ceases to rise above the freezing-point.
on the Urals, 71° in W.
The silver fir does not extend over Russia, and the oak does not cross the Urals.
of Archangel, and the limit is still lower towards the Urals.
Europe have held their ground; while in the Urals only a few - now Siberian, but formerly also European - are met with.
The sable has quite disappeared, being found only on the Urals; the beaver may be trapped at a few places in Minsk, and the otter is very rare.
(1884); Regel, Flora Rossica (1884); Brown, Forestry in the Mining Districts of the Urals (1885); Reports by Commissioners of Woods and Forests in Russia (1884) birds, even to hazel-hen (Tetrao bonasa), capercailzie (T.
Bogdanov, Birds and Mammals of the Black-Earth Region of the Volga Basin (in Russian, Kazan, 1871); Karelin for the southern Urals; Kessler for fishes; Strauch, Die Schlangen des Russ.
of Vyatka, the Permyaks in Perm, the Syryenians or Zyryans in Vologda, Archangel, Vyatka and Perm; (e) the Ugrians, or Trans-Uralian Finns, including the Voguls on both slopes of the Urals, the Ostiaks in Tobolsk and partly in Tomsk, and the Magyars, or Ugrians.
Urals, that is, the steppes of Ufa and Orenburg, extend also into Perm and Samara.
One section of them crossed the Urals and occupied the steppes between the Urals and the Volga; the remainder belong to Turkestan and Siberia.
The law of Russia prohibits them from entering Great Russia, only the wealthiest and best educated enjoying this privilege; nevertheless they are met with everywhere, even on the Urals.
The two principal mining centres of European Russia are the Urals, Ekaterinoslav, Kharkov and the Don Cossacks territory.
The minerals chiefly produced in the Urals are iron, coal, gold, platinum, copper, salt and precious stones.
The amount of iron and steel produced in the Urals is not quite 20% of the total in all European Russia and Poland.
The output of coal in the Urals is, altogether, less than 3% of the total for all the empire and 4% of the output of European Russia (exclusive of Poland) alone.
Gold has been mined in the Urals since 1820; but since 1892 the output has fallen off very considerably.
No less than 96% of the world's supply of platinum comes from the Urals; but the total output only ranges between 10,000 and 16,000 lb annually.
At one time all Russia was supplied with salt from the Urals, but at the present time the output is extremely small, less than 350 tons annually.
Chelyabinsk was linked by a transverse line with the middle Urals railway, which connects Perm, the head of navigation in the Volga basin, with Tyumen, the head of navigation on the Ob and Irtysh, passing through Ekaterinburg and other mining centres of the middle Urals.
The Urals indicate no real division of races, and in both Greek and Turkish times Asia Minor has been connected with the opposite shores of Europe rather than with the lands lying to the east.
Large ore-bodies of granular and compact magnetite occur as beds and lenticular masses in Archean gneiss and crystalline schists, in various parts of Norway, Sweden, Finland and the Urals; as also in the states of New York, New Jersey, Pennsylvania and Michigan, as well as in Canada.
Trade with Persia and India, as also with the Khazars and the Russians, and undoubtedly with Biarmia (Urals), was, however, their chief occupation, their main riches being furs, leather, wool, nuts, wax and so on.
Since the researches of Schrenk it may be regarded as settled that in historical times the Samoyedes were inhabitants of the so-called Ugria in the northern Urals, while Radlov considers that the numberless graves containing remains of the Bronze Period which are scattered throughout W.
The more important iron-works of the Urals are situated on the Siberian slope of the range.
The Ekaterinburg stone-polishing works in the Urals and those of Kolyvan in the Altai are well known.
At the present day steamers ply from Tyumen, at the foot of the Urals, to Semipalatinsk on the border of the Kirghiz steppe and to Tomsk in the very heart of West Siberia.
The oak, elm, hazel, ash, apple, lime and maple disappear to the east of the Urals, but reappear in new varieties on the eastern slope of the border-ridge of the great plateau.
The Russians, issuing from the middle Urals, have travelled as a broad stream through south Siberia, sending branches to the Altai, to the Ili river in Turkestan and to Minusinsk, as well as down the chief rivers which flow to the Arctic Ocean, the banks of which are studded with villages 15 to 20 m.
It starts from Perm on the Kama, and, crossing the Urals, reaches Ekaterinburg - the centre of mining industry - and Tyumen on the Tura, whence steamers ply via Tobolsk to Tomsk.
used to strike off from the Kama eastwards, and Ekaterinburg, on the eastern slope of the Urals.
It was supposed at that time that this line would form part of the projected trans-Siberian railway; but it was finally decided, in 1885, to give a more southerly direction to the railway and to continue the Moscow-Samara line to Ufa, Zlatoust in the Urals, and Chelyabinsk on the west Siberian prairies, at the head of one of the tributaries of the Ob.
In the beginning of the 16th century Tatar fugitives from Turkestan subdued the loosely associated tribes inhabiting the lowlands to the east of the Urals.
These were united by Khan Ediger, and conflicts with the Russians who were then colonizing the Urals brought him into collision with Moscow; his envoys came to Moscow in 1555 and consented to a yearly tribute of a thousand sables.
As early as the nth century the Novgorodians had occasionally penetrated into Siberia; but the fall of the republic and the loss of its north-eastern dependencies checked the advance of the Russians across the Urals.
On the defeat of the adventurer Stenka Razin (1667-1671) many who were unwilling to submit to the iron rule of Moscow made their way to the settlements of Stroganov in Perm, and tradition has it that, in order to get rid of his guests, Stroganov suggested to their chief, Yermak, that he should cross the Urals into Siberia, promising to help him with supplies of food and arms. Yermak entered Siberia in 1580 with a band of 1636 men, following the Tagil and Tura rivers.
From this region started an important trade route eastward by the Thyssagetae among the southern Urals, the Iyrcae on the Tobol and Irtysh to the Kirgiz steppe, where dwelt other Scyths, regarded as colonists of those in Europe: then by the Argippaei in the Altai and the Issedones in the Tarym basin, to the one-eyed Arimaspi on the borders of China, who stole their gold from the watchful griffins, and who marched with goat-footed men and Hyperboreans reaching to the sea.
In this leisurely journey Pallas went by Kasan to the Caspian, spent some time among the Kalmucks, crossed the Urals to Tobolsk, visited the Altai mountains, traced the Irtish to Kolyvan, went on to Tomsk and the Yenisei, crossed Lake Baikal, and extended his journey to the frontiers of China.
The western portion of Kotelnyi is built up of Middle Devonian limestones and slates, folded the same way, of which the fossil fauna is similar to that of the Urals.
At the beginning of the 16th century the illimitable steppe of south-eastern Europe, extending from the Dnieper to the Urals, had no settled population.
Volcanic rocks are also present but they are not so extensively developed as in the islands of the Javan arc. The Permian beds consist chiefly of limestone and contain numerous fossils similar to those of the middle and upper divisions of the Productus limestone of northern India and the Artinsk stage of the Urals.
At the same time it must be remembered that there is in India, South Africa, the Urals, in Australasia and parts of North America an important series of rocks, with a " Permo-Carboniferous " fauna, which constitutes a passage formation between the Carboniferous, sensu stricto, and Jurassic rocks.
There are also important ore beds in the Urals, near the border of Finland, and at the south of Moscow.
Humboldt searched for them in the Urals on account of the similarity of the gold and platinum deposits to those of Brazil, and small diamonds were ultimately found (1829) in the gold washings of Bissersk, and later at Ekaterinburg and other spots in the Urals.
BEREZOVSK, a village of east Russia, in the government of Perm, on the eastern slope of the Urals, 8 m.
Again the Finnish languages spoken in various parts of Russia and more or less allied to Magyar must have spread gradually westwards from the Urals, and their development and diffusion seem to postulate a long period (for the history of the Finns shows that they were not mobile like the Turks and Mongols), so that the ancestral language from which spring Finnish and Magyar can hardly have been brought across Asia after the Christian era.
The whole of the iron production of the Urals depends also on the same fair.
by the Caspian Sea and the government of the Urals.
From Russia, too, there is a stream of colonization across the Urals into western Siberia, and amongst the western Mediterranean populations there is constant migration to North Africa The greatest drain from Europe, however, has been across the sea to the United States, Canada and Australasia, especially to the first-named.
But in the meantime a flow of Novgorodian colonization had moved eastward, along the upper portions of the left-bank tributaries of the Volga, and had reached the Urals.
They seem to have held the southern end of the Urals about Ufa and Orenburg.
I have recently obtained, from my contact in the Urals, a large plate of muscovite mica.
on the Urals, 71Ã‚° in W.
The fauna of Siberia is closely akin to that of central Europe; and the Ural Mountains, although the habitat of a few species which warrant the naturalist in regarding the southern Urals as a separate region,, are not so important a boundary zoologically as they are botanically.
on the Urals, 62Ã‚° at Yakutsk, 61 Ã‚° at Aldansk, 54Ã‚° 30' at Udskoi, and 53Ã‚° to 54Ã‚° in the interior of Kamchatka (Middendorff, Sibirische Reise, vol.
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