Khatling Glacier
This lateral glacier situated in Tehri district is the source of river Bhilangna. Snow peaks of the Jogin group, Sphetic Pristwar, Barte Kauter Kirti Stambh and Meru surround the glacier. The moraines on the side of the glaciers look like standing walls of gravel mud.

Chorbari Bamak Glacier
Chorbari Bamak glacier is situated in Rudraprayag district of Uttaranchal the glacier is 6-km. Long and originates from the southern slope of Kedar-dome, Bhartekhunta and Kirti Stambh and this hill range is the water divide which separates the gangotri group of glaciers and the Chorbari glacier. Several hanging glaciers and avalanche chutes feed the glacier. The lower part of the glacier is covered by thick debris and bounded by huge deposits of lateral moraines. The glacier starts from its accumulation zone (600m) and terminates at an elevation of 3,800 m, from where a snow/ ice melt stream originates, called “Mandakini” and merges into the Alaknanda River at Rudraprayag.

Dokriani Glacier
Dokriani ‘Bamak’ is a well-developed medium sized glacier of the Bhagirathi basin. The glacier is formed by two cirques, originating at the northern slope of Draupadi Ka Danda and Jaonli Peak, 5,600 m and 6,000 m respectively. The glacier is 5-km long and flows in the northwest direction terminating at an elevation of 3,800m.
The stream originating from the glacier’s melted water is called “Dingad”, which later joins many other snow/ice-melted streams and finally merges into Bhagirathi River near Bukki village. There are several well-developed meadows and proglacial lakes located 2 km below the snout of the glacier. These meadows, lakes and other formations themselves tell their past history and behaviour of the glacier and also provide good camping sites.

Bandarpunch Glacier
Bandarpunch is an important glacier of Yamuna river basin. The glacier is 12-km long situated on the northern slopes of Bandarpunch Peak (6,316m), Bandarpunch West (6,102 m) and Khatling peak (6387 m). The glacier is formed by three cirque glaciers and later joins the Yamuna River. It lies on a gentle slope and is bounded by lateral moraines, which indicate the last surface level of the glacier.
Doonagiri Glacier
Doonagiri glacier is one of the important glaciers of Dhauli Ganga system of glaciers where more than 500 glaciers, of different shapes and sizes lie in the deep and narrow valleys. The important glaciers here are: Changbang, Girthi, Hoti and Niti glaciers. Doonagiri glacier is 5.5-km long, extending between an elevation from it head 5,150m to the snout 4,240m, which is the terminal point of the glacier. A stream originating from the glacier merges into Dhauli Ganga near the Juma village.