Formation of Himalayas :- In this blog let us understand about the formation of Himalayas . There are two theories which explain formation of Himalayas :- One is "The Geosyncline Theory " and the second one is " The Plate Tectonic Theory " Let us understand the first one which is explained by a German Scientist Kober, according to this theory About 541 millions to 252 million years ago from the end of Plaeozoic Era there was Tethys ocean containing salt water. View of Tethys ocean On either side of this Tethys ocean there was Gondwana Land (Indic Plate ) and India was also the part of Gondwana land and on the other side there was Laurasia ( Urasiayee Plate )or Eurasia means Europe and Asia was connected together which was called Angara Land. At that time the rivers flowing from both sides deposited huge muck , sand , boulders and silt in the Tethys ocean The pressure on Angara Land and Gondwana Land caused movement on both in opposite directions and t
Himalaya:- Lesser Himalayas or Mid Himalayas :- Beautiful View of Lesser Himalayas Previously we have studied about the Great Himalayas or Himadri , in this post we will see the Himachal or Lesser Himalayas . It is also called Mid Himalayas . The Mid Himalayas or the lesser Himalayas is the Himalayan mountains range which exists in between Shiwalik range in the south and the Greater Himalayas in the North. It almost runs parallel to Greater Himalayas and Shiwalik range. Mount Makalu Nepal Himalayas The elevations of Mid Himalayas ranges from about 3500 metres to 4500 metres above mean sea level . The total length of Mid Himalayas is about 2400 Kms and width varies between 60 km to 80 kms. In the middle Himalayas some peaks are more than 5050 metres above mean sea level and remains under snow throughout the year . Mid Himalayas The main ranges of Lesser Himalayas are 1. Pir Panjal Range , The Dhaoladhar . 3. The Mussoorie and Nag Tiba range in Uttarakhand and Pir Panjal and Dh
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