Glacial Landforms

Glacial Landforms in Relation to the Himalayas

Glaciers are represented by the flowing movement of a thick mass of ice and form as a result of the compaction or recrystallization of snow. Glaciers occur in areas whose climate favours the seasonal accumulation of snow in greater volumes than seasonal ablation. Here the seasonal accumulation of snow outpaces seasonal ablation that occurs due […]

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Himalaya | Seeking a Coordinated Approach in Glacier Research

The 2400 km long arcuate Himalaya-Hindu Kush mountain range supports largest accumulation of snow and ice following the Polar regions of Arctic and Antarctic and Greenland. Apart from the several peaks that attain more than 8000 m heights above mean sea level, the Himalaya also brings to life many major rivers that support ~1.3 billion […]

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Climate Change in the Himalayas

The Basic Possible Impacts of Climate Change in the Himalayas

Climate Change in the Himalayas is a major topic of worry for climate watchers in the Subcontinent and across the world. The Himalayas have the largest deposits of snow and ice in the world outside the Polar Regions and is often referred to as the ‘Third Pole’ and also as the ‘Water Tower of Asia’. […]

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