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The formation of the Himalayan mountains

The Himalayas are located just at the junction of two tectonic plates between the South of Asia and its center. Length area of about 2400 km and width of 350km. The mountains here young and pointed their average height of about 6,000 meters. There are peaks over 8,000 metres.
Himalaya perhaps the most poorly understood area on the planet. Mountains and valleys, mountains and valleys, sometimes from one valley to another except on the helicopter. In these places its authentic nature and unique conditions for life. Scientists have always been interested in the Himalayan mountains because of constant seismic activity in the area. To predict earthquakes need to know what breeds and at what depths lie. If there are faults, where they are and at what depth.
Until that these data science, scientists have only made a map of the most seismically active zones in the Himalayas. Yet little data, but something that can already be said on the nature of the given district. How and under what conditions appeared so imposing value mountains. It will take some time and mystery of the Himalayas will be fully revealed by scientists from France, Nepal, and China.
In ancient times, the two tectonic plates moving at a meeting one another formed the so-big mountain peaks. One plate was from India, the other side of Eurasia. The Indian plate submerged under the Eurasian plate and thus raised. So actually got this mountain structure.
Had the Himalayas in the tertiary period is referred to as a time of Alpine orogeny. This time though it was far away, but for the mountains is a very long period. Mountains can say young and folded from shale, granite and other different species. Some where sandstones and in these places pronounced erosion.

Record made 2013-11-01

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