West Siberian Glacial Lake
The West Siberian Glacial Lake, also known as West Siberian Lake, or Mansiyskoe Lake (Russian: Мансийское озеро), was a periglacial lake formed when the Arctic Ocean outlets for each of the Ob and Yenisei rivers were blocked by the Barents-Kara Ice Sheet during the Weichselian Glaciation, approximately 80,000 years ago. At its maximum extent, the lake's surface area was more than twice that of the present-day Caspian Sea.
It is theorized that while drainage to the Arctic Ocean basin (e.g. by the Ob and Yenisei Rivers) was prevented, the lake would eventually overflow to the Mediterranean Sea through a circuitous route that would include the Aral Sea, the Caspian Sea, and the Black Sea. This would have resulted in water from the Selenga River and Lake Baikal draining over a course of some 6,000 miles (9600 km), considerably longer than any river's course today.
See Mangerud et al. (2004) for diagrams and descriptions of the lake as well as postulated drainage patterns.
- Nerpa, a freshwater seal of Lake Baikal probably related to Caspian seals.
- Turgai Straits or West Siberian Sea, a Cretaceous to Eocene extension of the Tethys Sea separating Europe and Asia
- Dutch, Steve, Professor of Natural and Applied Sciences, University of Wisconsin-Green Bay. "Pleistocene Glaciers and Geography" webpage (accessed 30 November 2006)
- Mangerud, J. et al. (2004). Ice-dammed lakes and rerouting of the drainage of northern Eurasia during the Last Glaciation. Quaternary Science Reviews 23 (2004), pp. 1313–1332.  (accessed 30 November 2006)
|This palaeogeography article is a stub. You can help Wikipedia by expanding it.|