When two plates carrying oceanic crust collide, the result
is that one goes underneath the other - probably causing
a tsunami - or an underwater earthquake.
When the continental plates collide the oceainc cust gets stuck and eventually evaporates
When oceanic lithosphere and continental lithosphere collide, the continental lithosphere may be obducted over the oceanic lithosphere or the oceanic lithosphere may be subducted under the continental lithosphere. The latter is thought to be more common. This subduction and obduction generally results in tectonic activity such as volcanoes and earthquakes.
oceanic crust and continental crust collide, with the continental crust subducting under the oceanic
subduction zone
A subduction zone
When two oceanic crusts collide, the older plate is forced under the younger one and is pulled under it, forming a subduction zone. This leads to the formation of chains of volcanic islands known as island arcs.
When two oceanic crusts collide, the older plate is forced under the younger one and is pulled under it, forming a subduction zone. This leads to the formation of chains of volcanic islands known as island arcs.
Tectonic plates are oceanic plates. But when tectonic plates collide and a convergent boundary earthquakes occur.
the older crust is subducted and later pushed up to form oceanic arcs
When the continental plates collide the oceainc cust gets stuck and eventually evaporates
It makes a mountain.
The contiental cdrust is forced under the continental crust in a process called subduction.
When a trench or volcano comes.
When oceanic lithosphere and continental lithosphere collide, the continental lithosphere may be obducted over the oceanic lithosphere or the oceanic lithosphere may be subducted under the continental lithosphere. The latter is thought to be more common. This subduction and obduction generally results in tectonic activity such as volcanoes and earthquakes.
oceanic
this is because the oceanic plate is much denser than the continental plate so when they collide the oceanic plate will sink easily
At this type of convergent boundary the oceanic plate will be subducted, or sink into the mantle underneath the continental plate. Volcanoes often form near these boundaries.