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Geography of the Lake Baikal

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The Baikal, the world’s deepest lake, stretches 391 mile (636 kilometer) long and nearly 50 mile (80 kilometer) wide. On the northeastern borders of central Asia, it lies at an altitude of 1,494 foot (455.6 meter) above the Pacific Ocean sea level. With an area of 12,162 square mile (31,500 square kilometer), the Baikal ranks seventh in the world after the Caspian and Aral seas, the North American Huron, Michigan, and Superior lakes and Victoria in Africa.

The lake is surrounded by the vast mountains of the Eastern Sayan massif with an absolute altitude of 11,453 foot (3,491 meter). Many of the Sayan mountain rivers flow into the Baikal, like the Irkut and other tributaries of the Angara. The Baikal region is characterized by a continental climate. In winter, the mean temperature falls to 1 to -13 degrees F (-17 to -25 degrees C), the absolute minimum is -35 to -40 degrees F (-37 to -40 degrees C). The mean summer temperature of July, normally the warmest month in the Baikal region, is 66 to 68 degrees F (19 to 20 degrees C), with a maximum of 100 degrees F (38 degrees C).

The underwater slopes of the Baikal depression show a distinct ancient relief of the coastline. Down to depths of 1,640 to 1,968 foot (500 to 600 m ), it uncovers submerged mouths of rivers and ancient valleys. The Baikal was born by a rift when the Eurasian and Indian plates collided. Tectonically, the lake consists of 3 deep basins, each separated by underwater uplifts. Winds and changes in the atmospheric pressure have an influence on the water level. The mean perennial level stands normally at 1,494 foot (455 meter). The highest level, measured on October 2, 1869, was 1,499 foot (457 meter); the lowest, 1,492 foot (455 meter), was observed in April 1904.

The first research on the Baikal was done in the 18th century by the German explorers I.E. Gmelin, P.S. Pallas, and I.G. Georgi. Systematical studies on the Baikal were encouraged in the 19th century by the Russian Geographical Society. W. Dybowsky distinguished in 1912 2 complexes of the Baikalian fauna: the general Siberian fauna and the endemic fauna. In response to the ecological conditions, these 2 species are developing completely differently. Ordinary Siberian fauna do only colonize the areas of mild temperatures, that is, near the shores. In contrast, indigenous Baikalian fauna can be found in the depth of the lake. Therefore, the temperature of the water presents an ecological barrier. The greatest enigma for scientists is the presence of seals in Baikal. Alexander von Humboldt suggested in 1843 that the presence of seals in the Caspian Sea and the Baikal was evidence of a past connection between these 2 lakes.

The German explorer O. Peschel believed in 1878 that Baikal was directly connected with the Arctic Ocean and that seals migrated from the north. Others, like V.P. Garyayev (1901) and German paleontologist M. Neimeier (1886), thought that the fauna of Baikal was a relict of an old marine fauna. The Baikal environment is very sensitive to ecological changes. When in 1957 the Soviet government planned to build a cellulose plant at Baikal’sk, local scientists, citizens, and writers like Valentin Rasputin launched a protest campaign that succeed after thirty years. In April 1987, the Soviet government issued a decree protecting Lake Baikal. Nevertheless, the cellulose plant is still producing industrial waste and dumping it into the lake.


Mikhail Kozhov, Lake Baikal and Its Life (W. Junk Publishers, 1963); Koji Minoura, ed., Lake Baikal: A Mirror in Time and Space for Understanding Global Change Processes (Elsevier, 2000).



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