The lake, fed by glaciers, is located to the north of the Kangchengyao range, in a high plateau area connected with the Tibetan Plateau.
It provides one of the source streams which joins the Tso Lahmu and then form the source of the Teesta River.
The lake remains completely frozen in the winter months, from November to Mid-May.

The lake has an area of 118 hectares (290 acres) and its peripheral length is 5.34 kilometres (3.32 mi).
However, the size of the lake appears small at the place where the devotees offer worship because the larger part of the lake is not visible due to hilly topography obstructing the view.
The area surrounding the lake, also known as Gurudongmar, is inhabited by Yaks, blue sheep and other wildlife of high altitude.

The lake is fresh water and used to be very clear; the bed of the lake could even be seen from the middle of the lake.
Pollution has muddied the waters in recent years, and the lake has taken on a white tinge and has obscured visibility.
The lake, fed by glaciers, is located to the north of the Kangchengyao range, in a high plateau area connected with the Tibetan Plateau. It provides one of the source streams which joins the Tso Lahmu and then form the source of the Teesta River. The lake remains completely frozen in the winter months, from November to Mid-May.
The lake has an area of 118 hectares (290 acres) and its peripheral length is 5.34 kilometres (3.32 mi). However, the size of the lake appears small at the place where the devotees offer worship because the larger part of the lake is not visible due to hilly topography obstructing the view. The area surrounding the lake, also known as Gurudongmar, is inhabited by Yaks, blue sheep and other wildlife of high altitude.
The lake is fresh water and used to be very clear; the bed of the lake could even be seen from the middle of the lake. Pollution has muddied the waters in recent years, and the lake has taken on a white tinge and has obscured visibility.
Gurudongmar Lake