It is located 7 km south of the Lake Shira, in a deep basin, at around 390 m above sea level.

There is sulfate-chloride and sodium-magnesium in its composition, very similar to the Shirin moisture.

The composition of both only differs in the percentage of anions and cations.

[2] In the early stages of development, the lake was considered as a source of salt.

In the 20th century, the peloid was largely expended by the visitors, what has caused that at present the thickness of the peloid layer is of about a meter.