Russia | Page 3

the great rivers of the old continent are comprised within the limits of the Russian empire. Taking rise on the plateau-belt, or in its Alpine outskirts, they flow first, like the upper Rhone and Rhine, along high longitudinal valleys formerly filled up with great lakes; next they find their way through the rocky walls; and finally they enter the lowlands, where they become navigable, and, describing great curves to avoid here and there the minor plateaus and hilly tracts, they bring into water-communication with one another places thousands of miles apart. The double river-systems of the Volga and Kama, the Obi and Irtish, the Angara and Yenisei, the Lena and Vitim on the Arctic slope, the Amur and Sungari on the Pacific slope, are instances. They were the true channels of Russian colonization.
A broad depression--the Aral-Caspian desert--has arisen where the plateau-belt has reached its greatest height and suddenly changes its direction from a north-western into a north-eastern one; this desert is now filled only to a small extent by the salt waters of the Caspian, Aral and Balkash inland seas; but it bears unmistakable traces of having been during Post-Pliocene times an immense inland basin. There the Volga, the Ural, the Sir Daria, and the Oxus discharge their waters without reaching the ocean, but continue to bring life to the rapidly drying Transcaspian Steppes, or connect by their river network, as the Volga does, the most remote parts of European Russia.
The above-described features of the physical geography of the empire explain the relative uniformity of this wide territory, in conjunction with the variety of physical features on the outskirts. They explain also the rapidity of the expansion of Sclavonic colonization over these thinly-peopled regions; and they also throw light upon the internal cohesion of the empire, which cannot fail to strike the traveller as he crosses this immense territory, and finds everywhere the same dominating race, the same features of life. In fact, as their advance from the basins of the Volkhoff and Dnieper to the foot of the Altai and Sayan mountains, that is, along nearly a quarter of the earth's circumference, the Russian colonizers could always find the same physical conditions, the same forest and prairies as they had left at home, the same facilities for agriculture, only modified somewhat by minor topographical features. New conditions of climate and soil, and consequently new cultures and civilizations, the Russians met with, in their expansion towards the south and east, only beyond the Caucasus in the Aral-Caspian region, and in the basin of the Usuri on the Pacific coast. Favoured by these conditions, the Russians not only conquered northern Asia--they colonized it.
The Russian Empire falls into two great subdivisions, the European and the Asiatic, the latter of which, representing an aggregate of nearly 6,500,000 square miles, with a population of only sixteen million inhabitants may be considered as held by colonies. The European dominions comprise European Russia, Finland, which is, in fact, a separate nationality treated to some extent as an allied state, and Poland, whose very name has been erased from official documents, but which nevertheless continues to pursue its own development. The Asiatic dominions comprise the following great subdivisions:--Caucasia, under a separate governor-general; the Transcaspian region, which is under the governor-general of Caucasus; the Kirghiz Steppes; Turkestan under separate governors-general, Western Siberia and Eastern Siberia; and the Amur region, which last comprises also the Pacific coast region and Kamchatka.
Climate of Russia in Europe.--Notwithstanding the fact that Russia extends from north to south through twenty-six degrees of latitude, the climate of its different portions, apart from the Crimea and the Caucasus, presents a striking uniformity. The aerial currents--cyclones, anti-cyclones and dry south-east winds--extend over wide surfaces and cross the flat plains freely. Everywhere we find a cold winter and a hot summer, both varying in their duration, but differing little in the extremes of temperature recorded.
Throughout Russia the winter is of long continuance. The last days of frost are experienced for the most part in April, but also in May to the north of fifty-five degrees. The spring is exceptionally beautiful in central Russia; late as it usually is, it sets in with vigour and develops with a rapidity which gives to this season in Russia a special charm, unknown in warmer climates; and the rapid melting of snow at the same time raises the rivers, and renders a great many minor streams navigable for a few weeks. But a return of cold weather, injurious to vegetation, is observed throughout central and eastern Russia between May 18 and 24, so that it is only in June that warm weather sets in definitely, reaching its maximum in the first half of July (or of August on the Black Sea coast). The summer is much warmer than might be supposed; in