Комментарий к фотографии от автора: Since the Central Paleozoic epoch the Baikal mountain area has experienced sustainable and continuous rising. It has been accompanied with block dislocations, renewal of ancient deep faults and formation of new interblock faults. In the picture: in the mountain tundra of the Baikal Mountain Ridge, which underwent the process of tectonic and magmatic activization. | |||
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