Russia

From the Catholic Encyclopedia

GEOGRAPHY

Russia (Rossiiskaia Imperiia; Russkoe Gosudarstvo) comprises the greater part of Eastern Europe, and a third of Asia; its area is one-sixth of the land surface of the globe. In the reign of Alexander II the total area of the empire was 8,689,945 sq. miles, of which only 2,156,000 were in Europe. The greatest length of Russia from east to west is 6666 miles, and its greatest breadth is 2666 miles; it lies between 35º 45' and 79º N. lat., and 17º 40' and 191º E. long. (i. e., 169 W. long.). The boundaries of Russia are: on the north, the Arctic Ocean; on the west, Sweden, Norway, the Baltic Sea, Germany, Austria-Hungary, and Rumania; on the south, the Black Sea, Turkey, Persia, the Caspian Sea; Afghanistan, and China; on the east, the Pacific Ocean. Russia forms a vast, compact territory, the area of its islands being only 107,262 sq. miles, which was greatly reduced by the cession of the southern part of Sakhalin to Japan. Geographers usually divide Russia into European and Asiatic Russia, regarding the natural boundary to be the Ural Mountains, the Ural River, the Don, and the Volga; this division is based neither on natural nor on political grounds. The Ural Mountains form a chain of wooded highlands, which may be compared to the central axis of the empire rather than to a dividing barrier; moreover there is no natural boundary line between the southern extremity of these mountains and the Caspian Sea. The division between European and Asiatic Russia can best be established ethnologically, and this method is frequently used in Russian geographies.

SEAS

The coasts of Russia are washed by many seas; the Arctic Ocean, the White Sea, the Bay of Tcheskaya, the Bay of Kara, the Gulf of Obi, the Baltic Sea, the Gulfs of Bothnia, Finland, and Riga, the Black Sea, the Sea of Azof, the Caspian Sea, the Pacific Ocean, Behring Sea, the Sea of Okhotsk, and the Sea of Japan. But Russia is not destined to become a great maritime power, because for the most part the seas of Russia are in regions where navigation is impossible in winter; for periods of six months in the Arctic Ocean, and from fifteen days to one month at some points in the Black Sea. And the future of Russia as a maritime power is moreover obstructed by political difficulties; the way from the Black Sea to the Mediterranean is closed by the Bosphorus and the Dardanelles; the way from the Baltic to the Atlantic is closed by Sweden, Germany, Norway, and Denmark. The Arctic Ocean washes the extreme northern coasts of Russia, sterile, uninhabited regions, over which there hangs a winter of nine months, paralyzing the activities of life. The ice, whether fixed or floating, blocks the way of ships; these ply however in the White Sea, which is free of ice for three months of the year, and the waters of which form the Gulfs of Mezen, the Dwina, Onega, and Kandalak, the latter being the most frequented. There are but few islands in this immense extent of ice; the more important ones are the islands of Kolguet, Vaigatch, Nova Zembla, New Siberia, and the islands of Solovka, on one of which is a famous monastery founded in the fifteenth century by St. Sabbatius and the Blessed Germanus. Among the most important peninsulas may be cited that of Kola or Russian Lapland. Russia shares the possession of the Baltic Sea with Sweden, Germany, and Denmark, and its waters have been the highway of Russian commerce since the time of Peter the Great, although their shores are rugged and reefs numerous. The Gulfs of Bothnia, Finland and Riga are frozen for several months of the year, while the Gulf of Livadia is frozen for six weeks, although it sometimes remains free of ice through the whole year. Notwithstanding these natural obstacles, Russian commerce has been developed on the Baltic, the shortest route for the exportation of Russian products to European countries and America. The Baltic Sea is studded with islands, of which the following belong to Russia: the numerous Aland group, eighty of which are inhabited; the Islands of Dago, Oesel, Mohn, Wornes, and Kotlin; on the last is built the formidable fortress of Kronstadt.

CLIMATE

In European Russia the climate is severe, both in winter and summer, the rains are scanty, and the temperature is not as mild as in Western Europe. The coasts of the Baltic and the shores of the Vistula have a climate similar to that of Western Europe. European Russia presents graduated variations of climate between 40º and 70º N. lat., and also from east to west. At Nova Zembla the lowest winter temperature is 16º F., while at the south of the Crimea it rises to 56.3º in summer. The isothermal lines of European Russia are not coincident with the parallels of latitude, but diverge towards the southeast. There are places situated on the same parallel presenting considerable differences in mean temperature, e. g. Libau, 49.1º; Moscow, 39.2º; Kazan, 37.4º; Yekaterinburg, 32.9º. In the valley of the Rion in the Caucasus, cotton and sugar-cane are grown, while the tundras of the Kola Peninsula are sparsely covered with moss. In Western Russia, the cold of winter is never greater than 31º below zero, while the heat of summer is never in excess of 86º; but in Eastern Russia the thermometer falls to 40º below zero in winter, and rises to 109º in summer. European Russia may be divided into four climatic zones: the cold zone, which includes the coasts of the Arctic Ocean and their adjacent islands, and extends beyond the Arctic Circle; its winter lasts nine months, and its summer three; the cold-temperate zone, from the Arctic Circle to 61º N. lat.; its winter Lasts six months, and each of the other seasons two months; the temperate zone, extending from 61º to 48º N. lat.; each season lasts three months, the winter being longer towards the north, and summer longer towards the south; the warm zone, between 48º N. lat. and the southern frontier of Russia; the summer lasts six months, and the other three seasons two months each. European Russia is not unhealthy, although in the cold zone scurvy is frequent, and near the Gulf of Finland ailments of the throat and the respiratory organs; plica polonica infects the marshy regions of Lithuania and Russian Poland; and there is the so-called Crimean fever in the neighbourhood of the Sivash and in a region on the coast of the Black Sea.

The climate of the Caucasus is not of a uniform character; it belongs in the north to the cold-temperate zone, and in Transcaucasia to the warm zone. In the north, summer lasts six months, and the other seasons two months each. In Transcaucasia the summer lasts nine months, and the other three months of the year are like spring. Nevertheless the irregularity of the mountain system of the Caucasus produces differences of temperature in places separated by short distances. On the coast of the Black Sea between Batum and Sukhum, the temperature seldom falls below 32º; in January the temperature rises as high as 43º. Western Transcaucasia receives warm and humid winds, while the eastern part is exposed to dry winds from the north-east.

The part of Siberia that borders on the Arctic Ocean lies entirely within the cold zone; the winter lasts nine months, and the summer is like the beginning of spring in European Russia. The portion of Siberia between the Arctic Circle and 60º N. lat. has a winter that lasts six months; the region below the parallel of 60º N. lat. has a winter a little longer than the summer. In proportion to the distance from the Ural Mountains the climate of Western Siberia experiences greater extremes of temperature, the winter and the heat of summer becoming more severe; and the same is true of Eastern Siberia in relation to the Pacific Ocean. The greatest variations of temperature in Eastern Siberia are observed at Irkutsk, Yakutsk, and Verkhoyansk, where the thermometer registers at times 59.6º below zero in winter, and 49.46º in summer. In midwinter the northern extremity of Siberia resembles the polar regions; during several days the sun does not rise, and the vast plain of snow is lit up by the Aurora Borealis, while at times the region of the tundras is swept by violent snowstorms. The climate of Turkestan is similar to Siberia. Those regions are far from the sea, and have cold winters and very warm summers, a sky that is always clear, a dry atmosphere, and strong northerly and north-easterly winds. The north winds develop violent snowstorms. The summer is unbearable; in the shade, the thermometer rises to 104º, and even to 117.5º, while the ground becomes heated to 158º.