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Geology of the Himalaya

The Geology of the Himalaya is a record of the most dramatic and visible creations of modern plate tectonic forces.

The Himalayas, which stretch over 2400 km are the result of an ongoing orogeny, the result of a collision between two continental tectonic plates.

This immense mountain range was formed by huge tectonic forces and sculpted by unceasing denudation processes of weathering and erosion.

The Himalaya-Tibet region is virtually the water tower of Asia: it supplies freshwater for more than one-fifth of the world population, and it accounts for a quarter of the global sedimentatary budget.

Topographically, the belt has many superlatives: the highest rate of uplift (nearly 1 cm/year at Nanga Parbat), the highest relief (8848 m at Mt.

Everest Chomolangma), the source of some of the greatest rivers and the highest concentration of glaciers outside of the polar regions.

Note: The above text is excerpted from the Wikipedia article "Geology of the Himalaya", which has been released under the GNU Free Documentation License.

For more information, see the following related content on ScienceDaily:

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