Location
The lake is located at above sea level. It formed due to the melting of the Lhonak glacier.Rapid growth
The lake is rapidly growing in size in an abnormally rapid manner due to the melting of the lake's associated South Lhonak glacier and additional melt water from the adjacent North Lhonak and main Lhonak glaciers. According to the declassified CORONA data from 1962, which was then collected by the Central Intelligence Agency and the United States Air Force between 1960 and 1972 as a part of America's first space reconnaissance program, the lake first appeared as a supraglacial lake at the glacier's snout on November 24, 1962. The first occurrence of a separate lake was identified in the 1977 Landsat program's multispectral scanner (MSS) data. The lake's area was also traced using MSS data and the glacier's retreat. The lake had an area of 17.54 hectares in 1977 and was connected to the glacier terminal. Later, the lake's areal extent was determined using 1989, 2002, and 2008 temporal satellite data. Between 1977 and 2008, the lake's surface area rose by 81.1 hectares.2023 outburst flood
In October 2023, heavy rains caused the swollen lake to breach its embankments and cause a severe flood in the Teesta river basin, causing widespread property damage and killing at least 40 people.Further reading
* Hazra, P., & Krishna, A. P. (2021, July). AHP Based Assessment of Glof Susceptibility of South Lhonak Glacial Lake, Sikkim Himalaya, India. In ''2021 IEEE International Geoscience and Remote Sensing Symposium IGARSS'' (pp. 5489-5492). IEEE. .See also
* Lonak GlacierReferences
Glacial lakes of India Lakes of Sikkim {{Sikkim-geo-stub