Satopanth Glacier
| Satopanth | |
|---|---|
 Balkun Peak dividing Satopanth Glacier in the left and Bhagirath Kharak Glacier in the right. | |
  Satopanth Location in India  Satopanth Satopanth (India) | |
| Type | Mountain glacier |
| Location | Uttarakhand, India |
| Coordinates | 30°45′12.2″N 79°21′51.1″E / 30.753389°N 79.364194°E |
 | |
The Satopanth glacier is situated in the
Alaknanda, one of the primary headstreams of the Ganges, has its origin in the Satopanth glacier. The glacier is one of the most popular glaciers in Uttarakhand
among tourists. Mountaineers consider it somewhat challenging to scale.
Name origin
The term ‘Satopanth’ is perhaps derived from two words – ‘Sat-o’ meaning of truth, and ‘Panth’ meaning path or way. So its literal meaning is the path of truth.
Geography
Satopanth glacier lies on the northwest side of
Garhwal division of the Himalayas
. It sits below a 2,500 m (8,200 ft) face of the peak.
Originating at a height of 7000 meters from the peaks of the Chaukhamba (7068m) and the Badrinath (6974m) mountains, the glacier spreads over a vast expanse of 13 km, this glacier melts into water at an altitude of 3810 meters. The Narayan Parvat and the foot of Balkun or Balakun peak, touches the glacier.
Scientists claim that the Satopanth Glacier is retreating, though not as fast as the
Indo-Tibet Border
, photography is strictly prohibited.
Tourist Information
The Satopanth Glacier can be approached from
Alaknanda River. On the route, you will come across a waterfall named Vasudhara Falls, lying on the right bank of the Alaknanda River. The snout of Satopanth Glacier opens at about 5 km upwards from Vasudhara Falls
. Two kilometers down the valley, the left bank of the river offers good conditions for camping.
Satopanth Glacier can only be approached in summer months. Treks to this glacier is a very sought-after adventure, for tourists in Uttarakhand.
The nearest airport is at
See also
- List of glaciers of India
References
- ^ "Frozen Delights - Glaciers". Archived from the original on 24 June 2001. Retrieved 9 June 2010.
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