Ladakh himalayas General Info · Villages · Valleys and plateaus · Lakes · Passes · Glaciers Siachen · Baltoro · Hispar · Nubra · Biafo · Chong Kumdan · Gasherbrum · Rakaposhi · Saltoro · Rivers · People · Religion · Fairs and festivals · Other places of interest | |||
Large tributary glaciers like the Shelkar Chorten and Mamostang open into the main glacier from both sides of its trough. The trunk glacier and its tributaries are in the form of a vast icefield, particularly during the winter season when there is continuous snowfall for several weeks at a stretch.
Numerous icefalls have been formed at the junction of small valley glaciers and the trunk glacier. Lateral moraines occur at the confluence of larger tributary glaciers and the trunk glacier. The side walls of the glacial trough are steeply sloping. Avalanches roll down these slopes quite often, particularly in winter. This glacier encompasses a vast are in winter. There are virtually no signs of recession. This tract is more or less devoid of a vegetative cover due to its high elevation as well as its latitude. The bulk of the total annual precipitation is in the form of snow. The Siachen glacier can be approached via Skardu in Ladakh. To the east of the Siachen lies the Rimo glacier group, a group of three glaciers -- North , Central and South -- located at an altitude of between 6,000 and 7000 m above sea level. Between them, these glaciers have almost 700 square kilometers of ice which at places is 100 m deep. Thus the Siachen glacier empire contains about 2,000 square kilometers of ice surface and almost 200 cubic kilometers of ice. |
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