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Sample Term Paper on Himalaya Mountains of South Asia

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Sample Term Paper on Himalaya Mountains of South Asia

The Himalayas is one the highest points in South Asia with over 110 peaks. Its formation was as a result of the collision between two continental tectonic plates: the Indo-Australian and the Eurasian plates. The collision’s resultant pressure caused the skyward thrusting of plates; hence, the jagged Himalayan peaks were formed. There are two types of plate boundaries that are and were in existence in the region. Currently, scientists believe that there are divergent plate boundaries that exist in the region. Scientists have the belief that some parts of the Eurasian plate are now stretching away from the Indo-Australian plate rather than thrusting up, and this has caused the shaping up of the divergent plate boundaries seen in the region today. However, in other parts, India is seen to move towards the Asian continents, and the collision between the two has contributed in one way or another to the shaping up of the region’s convergent plate boundaries. In the past, it is believed that when the two large landmasses met, India and Eurasia, there was skyward thrusting owed to the region’s Himalayas peaks; hence, the collision between the two landmasses was crucial in the convergent plate boundaries’ formation.

The diverse plate interactions in the region resulted in the formation of various geological structures that are of significance in modern Geography. Arguably, the collision between the plates, as said earlier, resulted in a skyward thrusting whose effects are evident in the peaks that later became mountains of which a perfect example of a mountain in the region is Mount Everest, which is irrefutably the highest mountain on the planet. It is also notable that the existence of the region’s plateaus owes to the collision of the plates, and a perfect example is the Tibetan plateau. In addition, the interactions between the plates saw the rise of hilly landscapes such as the Sivalik Hills. After the formation of peaks, they were later covered with glacier that resulted in the formation of valley glaciers in the region. The world’s famous rivers such as Indus, Ganges, and the Brahmaputra owe their formation to the plate interactions in the South Asia region.

Owing to their mode of formation, there are specific types of rocks that one would expect to find in the mountains of South Asia. A common type of rock in the region is sedimentary rocks that are formed because of the deposition of materials within or at the surface of the earth, as well as in water bodies. During the plate interactions, materials were deposited in the Tethys Ocean, and these later formed sedimentary rocks. An evidence of this is the presence of limestone that makes up the summit of Mount Everest. The marine limestone found at the summit of Mount Everest was from the ancient Tethys Ocean. In addition, metamorphic rocks are found in the region, and they are rocks that result from the transformation of pre-existing rocks after the latter are introduced to intense heat or pressure. During the collision of the Indian and Eurasian plate, due to the same rock density, it was impossible for one to be sub-ducted under another. Thus, there was existing pressure that was mounted on pre-existing rocks thus resulting in metamorphic rocks. Additionally, the existent volcanic rocks in the region are attributed to the formation of eruptive volcanic mountains in the region such as Mount Everest.

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