The shores of the lake are slightly sloping and smooth, without bays or peninsulas. Several rivers flow into the lake, but most are intermittent. The largest river with a constant flow is the Khari River, which flows into the northwest of the lake. Swamp-type shrubs and swamps grow near the mouth of the Khari River. The lake water is salty due to high evaporation and no outflow.[4]
The Üüreg Lake depression is a desert, so there is a lot of evaporation from the water surface. The average annual evaporation is 800-900 mm. In addition to the inflow of rivers, this water loss is offset by rainfall and groundwater. The general salinity of the water is 4.17 g/L.