It creates a mountain
when at least two or more crust(continental crust) collide together then they push together
A conversion boundary is a place where 2 tectonic plates are mving toward each other. There are 3 types of convergent boundaries OCEANIC CRUST-OCEANIC CRUST OCEANIC CRUST-CONTINENTAL CRUST CONTINENTAL CRUST-CONTINENTAL CRUST They are classified according to their crust
Mountain ranges are formed when plates with continental crust collide. The immense pressure causes the crust to buckle, fold, and uplift, creating mountainous terrain such as the Himalayas or the Alps.
continental-continental collision I think. When I got down to the last one, that was the only answer left.
When two plates collide, or come together, the plates will push upward, forming a mountain. If one plate is continental crust and the other is oceanic crust, the less dense crust (this being the oceanic) will actually move under the more dense crust, in a process called subduction, to form a deep-ocean trench.
When two plates collide, or come together, the plates will push upward, forming a mountain. If one plate is continental crust and the other is oceanic crust, the less dense crust (this being the oceanic) will actually move under the more dense crust, in a process called subduction, to form a deep-ocean trench.
When plates with continental crust push together, they form convergent boundaries. The collision results in the crumpling and uplift of the crust, leading to the formation of large mountain ranges like the Himalayas. Subduction may also occur where one plate is forced beneath the other, creating deep oceanic trenches and volcanic activity.
convergent boundary
Volcanoes or sometimes earthquake!
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When plates with continental crust collide, they can create mountain ranges through the process of continental collision. The rocks get deformed and uplifted, leading to the formation of large mountain chains like the Himalayas. Subduction zones may also develop, where one plate is forced beneath the other, leading to intense volcanic activity.
When two continental plates push together, they can create mountain ranges through a process known as orogeny. The immense pressure from the collision causes the crust to buckle and fold, leading to the formation of high peaks and complex geological structures. A prime example of this is the Himalayas, which formed from the collision of the Indian and Eurasian plates.