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Indian Himalayas
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Uttaranchal Glaciers >>
Uttaranchal Glaciers
Indian scientists studying Himalayan glaciers
fear an acute shortage of natural drinking water in Himachal Pradesh state based
on studies of the Beas and Baspa basins from 1962 to 2001.
About 67 percent of the nearly 12,124 square
miles of Himalayan glaciers are receding and in the long run as the ice
diminishes, glacial runoffs in summer and river flows will also go down, leading
to severe water shortages in the region.
The Gangotri glacier, the source of the Ganga,
India's holiest river, is retreating 75 feet a year. And the Khumbu Glacier in
Nepal, where Edmund Hillary and Tenzing Norgay began their ascent of Everest,
has lost more than 3 miles since they climbed the mountain in 1953.
Dokriani
|
Region : |
Garhwal, Uttaranchal |
|
Local Name |
Bamak |
|
Altitude Variation : |
5,600m To 6,000m |
|
Best Time to Go |
Throughout Summer And Autumn
Season. |
Doriani or 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.
Bandar Punch Glaciers
|
Region : |
Garhwal, Uttaranchal |
|
Significance |
Important Glacier of The Yamuna River Basin |
|
Altitude Variation : |
6,316m To 6,387m |
|
Best Time to Go |
Throughout Summer And Autumn
Season. |
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.
Khatling Glacier
|
Region : |
Garhwal, Uttaranchal |
|
Local Name |
Bamak |
|
Altitude Variation : |
6,316m To 6,387m |
|
Best Time to Go |
Throughout Summer And Autumn
Season. |
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
|
Region : |
Garhwal, Uttaranchal |
|
Lake Formed by Glacier |
Bamak |
|
Altitude Variation : |
600m To 3,800m |
|
Best Time to Go |
Throughout Summer And Autumn
Season. |
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.
Dunagiri Glacier
|
Region |
Garhwal, Uttaranchal |
|
Significance |
Important Glacier
Of Dhauli Ganga System |
|
Altitude Variation |
5,150m To 4,240m |
|
Best Time to Go |
Throughout Summer And Autumn
Season. |
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. b
More Glaciers in Uttaranchal
b
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