Plizio Visual Lab
Turgai Hollow
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The Turgai Hollow is a prominent geological erosion channel stretching approximately 800 kilometers from north to south, connecting the West Siberian Plain with the Turan Lowland. This feature is widely regarded as a remnant of an ancient waterway that likely facilitated the drainage of massive glacial lakes during the Pleistocene epochs. The relief is characterized by a broad, flat valley floor, reaching widths of up to 300 kilometers, flanked by plateaus rising 100 to 200 meters above the valley. Today, the hollow is traversed by sluggish rivers like the Turgai and Ubagan, which often drain into chains of saline and freshwater lakes. The semi-arid continental climate supports a landscape of steppes and semi-deserts, serving as a critical migration corridor for the endangered Saiga antelope and various migratory birds. Geologically, the region is noted for its significant deposits of iron ore and coal, though its agricultural utility is limited by low precipitation to seasonal livestock grazing.
Best time to visit & climate
The most pleasant time to visit is Jun–Aug.
| Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Avg °C | -17 | -14 | -5 | 6 | 15 | 20 | 22 | 21 | 13 | 4 | -5 | -14 |
| Rain mm | 17 | 19 | 29 | 32 | 41 | 32 | 39 | 29 | 24 | 31 | 26 | 22 |
📋 Practical info
Geography
Facts
- The Turgai Hollow extends for a total distance of about 800 kilometers.
- The width of the hollow varies from 20 to a maximum of 300 kilometers.
- The valley floor lies at an average elevation of 100 to 125 meters.
- During glacial periods, it served as a spillway for the Arctic-flowing rivers.
- The hollow is a major habitat and migration route for the Saiga antelope.
- Geologically, it acts as a boundary between the Urals and the Kazakh Upland.
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Notable places around
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Frequently asked questions
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