This is called a constructive plate boundry. The oceanic plate will be pushed under by the continental plate, as it as thinner and denser. The friction can result in earthquakes and the heat from the friction will melt some of the oceanic plate. The pressure in the mantle will push the magma up to the surface, creating a volcano (creating land, therefore "constructive"). Hope this helped, just recently did tectonics in geography class.
When two continental plates collide, they can crumple and fold to form mountain ranges. This process is known as continental collision or orogenesis. The collision can also lead to seismic activity such as earthquakes and the formation of deep crustal roots.
When continental plates collide, the denser oceanic crust is usually subducted beneath the less dense continental crust. This process can create subduction zones, where the oceanic crust is forced downward into the mantle. The oceanic crust may melt or be recycled back into the mantle in these subduction zones.
When two continental plates collide they form mountains .
When two plates carrying continental crust collide, both plates crumple and fold due to the immense pressure. This can lead to the formation of mountain ranges and earthquakes along the convergent boundary. The collision can also result in the subduction of one continental plate beneath the other, ultimately leading to the formation of a mountain belt.
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.
When two continental plates collide,fold mountains are formed.
When two continental plates collide, they can form mountain ranges due to the intense compression and uplift of the Earth's crust. This collision can also lead to the formation of earthquakes as the plates grind against each other. Over time, the collision can result in the merging of the two continental plates into a single larger landmass.
Mountains
Collision...
When two continental plates collide, they can crumple and fold to form mountain ranges. This process is known as continental collision or orogenesis. The collision can also lead to seismic activity such as earthquakes and the formation of deep crustal roots.
Landforms such as ocean trenches and mountain ranges are created.
Earthquake
sinks
When continental plates collide, the denser oceanic crust is usually subducted beneath the less dense continental crust. This process can create subduction zones, where the oceanic crust is forced downward into the mantle. The oceanic crust may melt or be recycled back into the mantle in these subduction zones.
When two continental plates collide they form mountains .
sinks
sinks