Mountains form where continental and oceanic plates collide by the actions of the plates upon one another. Often one plate pushes up and over the other one, and the upper one creates a row of mountains.
The leading edge of the oceanic plate melts as it sinks deep into mantle. The melted rock becomes magma that forces its way up between the plates.
the same as mountains but with lava... daahhh
When continental plates collide one continental plate goes on top and the other on the bottom creating a mountain.
this is because the oceanic plate is much denser than the continental plate so when they collide the oceanic plate will sink easily
Oceanic plates move under continental plates when they converge together because the oceanic plate is more denser than the continental plate.
sinks
The oceanic plate subduct under the continental because oceanic is made from basalt(rock) which is denser than andesite and granite(continental)
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
this is because the oceanic plate is much denser than the continental plate so when they collide the oceanic plate will sink easily
Oceanic plates move under continental plates when they converge together because the oceanic plate is more denser than the continental plate.
sinks
When the continental plates collide the oceainc cust gets stuck and eventually evaporates
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
The oceanic plate subduct under the continental because oceanic is made from basalt(rock) which is denser than andesite and granite(continental)
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
When an oceanic plate and a continental plate collide, the oceanic plate is always subducted. Oceanic plates are denser than continental plates, and they have a higher iron content. Since they are denser, oceanic plates always sink below the continental plate in the event of a collision.
Oceans do not collide but oceanic crustal plates can collide, and when they do collide, island arcs are formed along the subduction zone.
When two continental plates collide they form mountains .