Selenga

The Selenga (SEL-eng-GAH) or Selenge is a major river in Mongolia and Buryatia, Russia. Originating from its headwater tributaries, the Ider and the Delger mörön, it flows for 992–1,024 kilometres (616–636 mi) before draining into Lake Baikal. The Selenga therefore makes up the most distant headwaters of the Yenisey-Angara river system. Carrying 935 cubic metres per second (33, 000 cu ft/s) of water into Lake Baikal, it makes up almost half of the riverine inflow into the lake, and forms a wide delta of 680 square kilometres (260 mi2) when it reaches the lake. Periodic annual floods are a feature of the Selenga River. The floods can be classified as “ordinary”, “large” or “catastrophic” based on the degree of impact. Of the twenty-six documented floods that occurred between 1730 and 1900, three were “catastrophic”. The three “catastrophic” floods were the floods of 1830, 1869 and 1897. The Selenga River basin is a semi-arid region occupying 280,000 square kilometres (110, 000 mi2). It is part of the Arctic Ocean Basin and mainly located in northern Mongolia. Stone implement artifacts found on the Selenga River at the end of the 19th century have been used to form a link between Native Americans and their ancestors in East Asia. The climate of the Selenga basin is influenced by the Siberian High, a powerful anti-cyclone, and consists of harsh winters, with the river freezing from November to April, and warm summers. The Selenga River delta is a Ramsar site, surrounded by marshl

Flows through: Mongolia, Russia.

River data from Wikidata (CC0); lengths normalised to a common unit.