डिस्क्राइब हाउ द हिमालयाज वेयर फॉर्म्ड
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The Indian Peninsula drifted towards the north and finally collided with the much larger Eurasian Plate. As a result of this collision, the sedimentary rocks which were accumulated in the geosynclines (known as Tethys) got folded and formed the mountain systems of the West Asia and Himalayas.
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