A detailed analytical study of major cations (Ca2+, Mg2+, Na+, K+) and anions (SO2− 4 , HCO−3 , Cl−, NO−3 ) of meltwater draining from Gangotri Glacier was carried out to understand major ion chemistry and to get an insight into geochemical weathering processes controlling hydrochemistry of the glacier. In the meltwater, the abundance order of cations and anions varied as follows: Ca2+ > Mg2+ > K+ >Na+ and SO2− 4 > HCO−3 > Cl− > NO−3 , respectively. Calcium and magnesium are dominant cations while sulphate and bicarbonate are dominant anions.

After two decades of hardwork, on 5 February 2012, a team of Russian scientists began drilling at Lake Vostok, the largest of more than 140 sub-glacial lakes and the most deeply buried of the lakes hidden under the Antarctic ice cap.

Here the authors report the field evidences observed at Milam glacier, Goriganga basin, Kumaon Himalaya during the glaciological expedition carried out in July 2011 and the observations from Resourcesat-2 LISS IV data. (Correspondence)