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In addition to the input of old reworked carbon by eolian processes, the late Pleistocene sediments were also influenced by old carbon delivered by deglacial meltwater.
In western languages, the city at that time was most often referred to as Urga (from Mongolian: , Örgöö, "Palace").
Both radiocarbon and optically stimulated luminescence (OSL) dating methods were applied to test their suitability for establishing a chronology of arid-zone lacustrine sediments using a 5.88-m-long core drilled from Lake Ulaan, southern Mongolia.
Although the radiocarbon and OSL ages agree in some samples, the radiocarbon ages are older than the corresponding OSL ages at the 550-cm depth horizon (late Pleistocene) and in the 100–300-cm interval (early to late Holocene).
Selenga brings into the lake about 30 cubic kilometres (7 cubic miles) of water per year, exerting a major influence on the formation of the lake water and its sanitary condition.
Selenga is the habitat of the most valuable fish species such as Omul, Siberian sturgeon, Siberian taimen, Thymallus and Coregonus. The length of the watercourse is 467 kilometres (290 miles).
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