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A basic mountain should be formed from the collision of continental crust and oceanic crustAnswerWhen an oceanic and a continental crust collide, the heavier oceanic crust tends to subduct under the lighter continental crust. Because of the collision and corresponding compression and also because of volcanism related to dehydration and melting of the subducted plate a mountain range is formed. The Andes mountain range is a, if not the, most typical example.
He said that it was due to plate tectonics, a theory which he is famous for. Two plates, either continental-continental, oceanic-continental or oceanic-oceanic collide at plate boundaries, causing an uplift of land. The oceanic plate or the denser plate will subduct. These uplifts will result in the formation of mountains, mountain ranges, volcanoes and islands.
A mountain range can be formed by the collision of an oceanic plate and a continental plate. This creates a subduction zone which eventually leads to the formation of a range of mountains.
Because the oceanic crust is under water in the ocean and a continental crust is land such as the continents
The continental crust is the land. The oceanic is under the ocean.
A basic mountain should be formed from the collision of continental crust and oceanic crustAnswerWhen an oceanic and a continental crust collide, the heavier oceanic crust tends to subduct under the lighter continental crust. Because of the collision and corresponding compression and also because of volcanism related to dehydration and melting of the subducted plate a mountain range is formed. The Andes mountain range is a, if not the, most typical example.
There are three types of convergent boundaries: Oceanic, continental, and continental-oceanic convergent boundaries. Continental-continental convergent boundaries form mountain ranges. Continental-oceanic boundaries result in subduction zones and the recycling of lithosphere. The continental side of the boundary may form a mountain range. Oceanic-oceanic form deep oceanic trenches and sometimes volcanoes.
Andean
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A convergent boundary with no subduction is a continental-continental boundary. Because oceanic crust is denser than continental crust, it is always the subducting plate in a oceanic-continental boundary. In an oceanic-oceanic boundary, one of the plates will subduct, depending on several factors. Continental plates are thicker and less dense than oceanic plates, and when they converge, they push up the area where the plates meet, forming mountain ranges (note that this is not the only, or even the predominant, method of mountain formation). The Himalayas are being formed as a result of a continental-continental boundary.
The oceanic plate subduct under the continental because oceanic is made from basalt(rock) which is denser than andesite and granite(continental)
Oceanic-Oceanic.
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Because continental plates are denser than oceanic. That is why oceanic and continental plates cause subduction zones.
He said that it was due to plate tectonics, a theory which he is famous for. Two plates, either continental-continental, oceanic-continental or oceanic-oceanic collide at plate boundaries, causing an uplift of land. The oceanic plate or the denser plate will subduct. These uplifts will result in the formation of mountains, mountain ranges, volcanoes and islands.
A mountain range can be formed by the collision of an oceanic plate and a continental plate. This creates a subduction zone which eventually leads to the formation of a range of mountains.
It's because the oceanic plate is more dense than the continental plate.