Himalayas - Himalayas - People: Of the four principal language families in the Indian subcontinent—Indo-European, Tibeto-Burman, Austroasiatic, and Dravidian—the first two are well represented in the Himalayas. In ancient times, peoples speaking languages from both families mixed in varying proportions in different areas. Their distribution is the result of a long history of penetrations.
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Himalayas - Himalayas - Physical features: The most characteristic features of the Himalayas are their soaring heights, steep-sided jagged peaks, valley and alpine glaciers often of stupendous size, topography deeply cut by erosion, seemingly unfathomable river gorges, complex geologic structure, and series of elevational belts (or zones) that display different ecological associations of flora.
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 between the Namche Barwa syntaxis in Tibet and the Nanga Parbat syntaxis in Pakistan, are the result of an ongoing orogeny — the result of a collision of the continental crust of two tectonic plates.
Himalayas Facts: The Himalayas are the youngest of the mountains in the world, which was created some 50 million years ago by the collision of the Indian plate with the Eurasian plates. The impact was so profound that the mountains stretched out to 2400 kilometers and now encompasses countries namely Afghanistan, Pakistan, India, Nepal, Tibet and Bhutan.