How Himalayan Moutains form

There is a lot of visual evidence that can be seen while examining the Himalayan mountain ranges. Many mountain ranges feature evident creasing around their sides. The sides begin bending around the bottom and lean against highest crests of the mountain. The sides are soft and that implies that their location was somewhere near a body of water. Also, researchers discovered a number of fossilized sea creatures near the northern part of India. This creatures were formed with a hard outer layer on their bodies. During the formation of the Himalayas, the "Ammonites" lost their natural habitat, or a body of water and became extinct. The discovery of the sea creatures leads us to the conclusion that there was a body of water in the place of the colossal mountains of India. There are many finding of soft rocks, near the highest peaks of the Himalayas, that were created below a body of water. There are many mountain ranges that still deposit such rocks. This finding verifies the hypothesis of a huge collision of soft edged South Asia and, in contrast, rigid and hard North India Visual Evidence. The Himalayan mountains towers between India and Tibet. The mountain were buckled up by the collision of two continental plates the Indian plate and the Eurasian plate. Since both are made of lightweight continental rock, they crunched together and pushed up mountains. Most of the growth, of the Himalayas and Tibetan plateau has taken place in the last 10 million years and continues to this day. The Himalaya's formed when the sub continent of India broke away from Gondwanalandand from memory 55 million years ago. Gondwanaland was comprised of the continents we now know as Antarctica, Australia, South America and Africa. The Indian piece travelled north and collided with Asia ie where India now is. This caused uplift of the collision forming the Himalaya's. The himalaya’s pushed together to form mountains.