Baikal Rift Zone
Quick Summary
The Baikal Rift Zone is a geological region in Siberia, Russia, characterized by extensive block faulting. This geological activity creates a deep structural hollow where Lake Baikal, the world's oldest and deepest freshwater lake, is situated. The rift valley is marked by steep slopes and deep basins, with sedimentary layers up to 20,000 feet thick on the lake floor. This region experiences occasional severe earthquakes, indicating ongoing tectonic activity. The Baikal Rift Zone is one of the most significant continental rift valleys, comparable to the East African Rift System.1234
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mountainThe Himalayan chainThe Baikal Rift Zone in Siberia and the Shansi Graben in northern China seem to have resulted from the east-southeastward extrusion of material out of Indiaās path. Moreover, crustal thickening in the Tibetan Plateau has ceased, and now eastāwest extension of the plateau contributes to theā¦
Read MoreThe Baikal Rift Zone in Siberia and the Shansi Graben in northern China seem to have resulted from the east-southeastward extrusion of material out of Indiaās path. Moreover, crustal thickening in the Tibetan Plateau has ceased, and now eastāwest extension of the plateau contributes to theā¦
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tectonic basins and rift valleysRift valleysSimilarly, the Baikal Rift in Siberia, which contains the deepest lake in the world, Lake Baikal, has a very steep northwestern edge and a gentler southeastern margin.
Read MoreSimilarly, the Baikal Rift in Siberia, which contains the deepest lake in the world, Lake Baikal, has a very steep northwestern edge and a gentler southeastern margin.
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