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The movement of crustal plates is driven by heating from within the mantle, as the separate plates sit atop the fluid asthenosphere. The difference in rock motion means that plates can be pushed into, over, and under each other.
False. A rift valley forms when continental plates diverge or pull apart. When two continental plates collide the result is a mountain range.
Oceans do not collide but oceanic crustal plates can collide, and when they do collide, island arcs are formed along the subduction zone.
When oceanic plates collide with continental plates, The oceanic plate goes under the Continental plate, creating friction deep in the earth, where the plates are rubbing against each other, creating magma, which rises to the surface and creates volcanic mountain ranges. The Andes mountain range is an example. I don't know if this will help you at all.
Meteor impacts in the ocean basins
Mountain buildup.
the plates will push each other up and form a mountain range.
The movement of crustal plates is driven by heating from within the mantle, as the separate plates sit atop the fluid asthenosphere. The difference in rock motion means that plates can be pushed into, over, and under each other.
When two continental plates collide, the crust is thickened, buckled and deformed--gaining elevation. Mountain chains are the result; their creation occurring over periods of millions of years.
Trolled
False. A rift valley forms when continental plates diverge or pull apart. When two continental plates collide the result is a mountain range.
When two tectonic plates collide, it is called compressional stress at convergent boundaries. Rocks and plates usually have stronger compressional strength than tensional strength (which would happen at divergent boundaries). This means the higher the likelihood of developing mountains for continent-continent convergence or being subducted for oceanic-oceanic/oceanic-continental boundaries.
Oceans do not collide but oceanic crustal plates can collide, and when they do collide, island arcs are formed along the subduction zone.
They form high range mountain becuase there is no subduction zone. This is usually a good place to find regional Metamorphic rock.
When oceanic plates collide with continental plates, The oceanic plate goes under the Continental plate, creating friction deep in the earth, where the plates are rubbing against each other, creating magma, which rises to the surface and creates volcanic mountain ranges. The Andes mountain range is an example. I don't know if this will help you at all.
Its When Tectonic plates either collide Or Move Apart. Examples Of Tectonic Plates moving Together are mountains and volcanoes.
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.