what kind of convergent plate boundary movement formed the mount himalayas?
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The Himalayan mountain range and Tibetan plateau have formed as a result of the collision between the Indian Plate and Eurasian Plate which began 50 million years ago and continues today.
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The image shows the Convergent plate boundary. Explanation: Convergent boundaries occur wherever the Earth's tectonic plates move or collide toward each other.
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The Himalayan mountain range and Tibetan plateau have formed as a result of the collision between the Indian Plate and Eurasian Plate which began 50 million years ago and continues today. ... From about 50-40 Ma the rate of northward drift of the Indian continental plate slowed to around 4-6 cm per year.
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Convergent boundaries form strong earthquakes, as well as volcanic mountains or islands, when the sinking oceanic plate melts. The third type is transform boundaries, or boundaries where plates slide past each other, forming strong earthquakes.
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Another event that can occur at a convergent boundary, usually one between two plates bearing continental crust, is continental collision. When two landmasses collide, they push into each other, deforming and creating tall, folded mountains.
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convergent plate boundary. [ kən-vûr′jənt ] A tectonic boundary where two plates are moving toward each other. If the two plates are of equal density, they usually push up against each other, forming a mountain chain.
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Continental crust is too buoyant to subduct. When two continental plates converge, they smash together and create mountains. The amazing Himalaya Mountains are the result of this type of convergent plate boundary. The Appalachian Mountains resulted from ancient convergence when Pangaea came together.
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Answer and Explanation: The three types of convergent plate boundaries include oceanic-continental convergence, oceanic-oceanic convergence, and continental-continental...
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Continental/Continental: The Himalayas. The Himalayan mountain range and Tibetan plateau have formed as a result of the collision between the Indian Plate and Eurasian Plate which began 50 million years ago and continues today.
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Each of these types of plate boundaries is associated with different geological features. Typically, a convergent plate boundary—such as the one between the Indian Plate and the Eurasian Plate—forms towering mountain ranges, like the Himalaya, as Earth's crust is crumpled and pushed upward.
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convergent plate boundary. [ kən-vûr′jənt ] A tectonic boundary where two plates are moving toward each other. If the two plates are of equal density, they usually push up against each other, forming a mountain chain. If they are of unequal density, one plate usually sinks beneath the other in a subduction zone.
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The oceanic plate pushes into the land, and coastal mountains go up. That's a standard convergent plate boundary. It doesn't explain why the highest parts of the Rocky Mountains are more than 1000 km away from the plate boundary.
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Most divergent plate boundaries are underwater and form submarine mountain ranges called oceanic spreading ridges. While the process of forming these mountain ranges is volcanic, volcanoes and earthquakes along oceanic spreading ridges are not as violent as they are at convergent plate boundaries.
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These are also known as constructive boundaries. Convergent boundaries are areas where plates move toward each other and collide. These are also known as compressional or destructive boundaries. Subduction zones occur where an oceanic plate meets a continental plate and is pushed underneath it.
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Continental collisions result in the creation of mountains and fold belts as the rocks are forced upwards. Plates can move towards each other at a boundary. This type of is called a convergent boundary. This type of boundary is dominated by reverse faulting although other types of faulting may be observed.
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The three main types are convergent, divergent and conservative. Divergent plate boundaries are where new crust is created. Mid ocean ridges are the main type. Convergent plate boundaries are where two plates collide.
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The Andes mountains were formed as a result of a convergence of plate tectonics. The Nazca Plate moved eastwards, towards the South American Plate finally colliding and forming the Andes about 45 million years ago.