25,289. . Welcome to CK-12 Foundation | CK-12 Foundation The aforesaid Gazetteer states in pages 520 and 364 that "The eastern (Kuenlun) range forms the southern boundary of Khotan", "and is crossed by two passes, the Yangi or Elchi Diwan, .. and the Hindutak (i.e. It resulted in China's withdrawing from the disputed territory following suit by Pakistan. 2. (a) Indus . The duration of each surge has a large range of uncertainty as does the exact position of the glacier front at the beginning and end of the surges, so the terminus advance rates (145-75ma −1) have an even larger range of uncertainty. Highest Mountain: K2 (8611m) Topography and Climate: Due to the low temperature of the area, precipitation generally takes place in the form of snow. 2. Its Southern boundary is defined by the Gilgit, Indus and the Shyok Rivers which separate it from the Himalayan Range in the South. The Karakoram are generally considered separate from the Himalayas.. This range extends from the Pakistan-Afghanistan region into Tibet.Formation of this great mountain chain began when India drifted away from Gondwanaland (a land mass that consisted of all the southern continents of Pangea) and moved northwards colliding into Asia (as seen in The Break . K2 rising up above the rest of the Karakoram Range. The southern boundary of the Karakoram, from west to east, is formed by the Gilgit, Indus, and Shyok rivers. To the south of the Indus before merger and to the East after merger are the Himalayas Since it could not sink, the Indian Plate pushed the crust upward and also downward, because of this, the Himalayas were formed! 2. Non-volcanic mountain ranges may be found along convergent boundaries of tectonic plates. mountains formed on Asian palates are known as trans Himalayas e.g karakoram . When was the karakoram range formed? From about 50-40 Ma the rate of northward drift of the Indian continental plate slowed to around 4-6 cm per year. cal data show that the Karakoram Range was a dynamic active mountain range with semi-continuous crustal thickening, deforma- tion, metamorphism and partial melting for at least the last 63 mil-.
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