An Area in the World Where Two Plates Are Interacting: Himalayan Mountains

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In the world, there are currently multiple areas in which the interaction of tectonic plates can be represented. I am going to discuss how, as well as provide scientific reasoning to justify the features provided on the surface of the earth due to the Himalayan mountains.

The phrase Himalaya, comes from a Sanskrit word meaning Abode of Snow. Due to such snow on the mountain. The Nepalese meanings for hima from ‘snow’ and ālaya for ‘abode meaning home. But for buddhists cases, the himalayan area is known for by various names such as Himava and Himavanta. The Himalayas are known as the result of tectonic plate motions that collided India into Tibet many years ago. Due to the great amount of tectonic motion still occurring at the site today, the Himalayas have a proportionally high number of earthquakes and tremors. The Himalayas are one of the youngest mountain ranges on the planet currently. The 14 mountains are well over 8,000 metres high in length, comparing to, Nanga Parbat and Mount Everest, at 8,848 meters the world’s highest mountain. The Himalayas extend over 1,500 miles “2,400 km” from the Indus Valley in the west to the Brahmaputra Valley in the east. They are between 100 and 250 kilometres wide.

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There are only three kinds of plate tectonic boundaries: divergent, convergent, and transform plate boundaries. Plates move towards one another at convergent boundaries, meaning that one plate is forced below another plate in a process called we call subduction. Earthquakes and composite volcanoes are really common at this type of boundary. Plates move past one another at transform boundaries.

Because of the great amount of tectonic motion still occurring at the site, between collisions from india tinto Tibet. the Himalayas have a high amount of earthquakes and tremors today. The Himalayas are one of the youngest mountain ranges on our planet. Earthquakes are mainly caused when a rock underground suddenly breaks along a fault. This sudden release of energy causes the seismic waves that make the ground shake and gives us data to know how strong it is. When two blocks of rock or two plates are rubbing against each other, they stick a little but later when the pressure is too much the rocks later break and the earthquake occurs. The major feature of a composite volcano is a system in where magma from a reservoir deep in the Earth’s crust rises to the surface. The range of this began to form between 40 and 50 million years ago, when two large landmasses, India and Eurasia, were moved by plate movement, and collided. At present, the movement of India continues to put big pressure on the Asian continent.

Everything has an origin. The highest and youngest mountain range in the world, the Himalayas are a geologic marvel that occurred when the Indo Australian plate collided into the underbelly of the Eurasian plate, nearly about 70 million years ago. The Himalayas, which stretch over 2400 km are the result of an ongoing in which a section of the earth’s crust is folded and deformed by lateral compression to form a mountain range. The result of a such a collision between two continental tectonic plates. This huge mountain range was formed by multiple huge tectonic forces and sculpted by unceasing denudation processes of weathering and erosion. The Himalaya Tibet area is the water tower of Asia as it supplies freshwater for more than one fifth of the world population today. The Himalayan Mountains are still growing higher every year, at a rate of about 2.4 in/6.1cm per year. That’s twice as fast as previously thought and recorded. A growth rate of 2.4 in/6.1cm per year doesn’t sound like very much to you. But, if you think about it, that means in the last 26,000 years the Himalayans have risen almost a mile into the upper reaches of the earth’s atmosphere. Meaning, that over the years it has grown soo much due to interacting plates. With all events currently happening, the mountains are able to grow every year and maintain shape. Today, the plates continue to press against each other, causing the mountains in the range to still rise for the past 50 million years. Everest grows about 0.16 inch (0.41 centimeters) per year.

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