When one plate slides beneath another it is said to subduct. This is called a subduction zone. However, a continental plate cannot subduct, only an oceanic plate can. When two continental plates collide the land between them is squeezed horizontally, forming mountain ranges. Eventually the continental land masses will fuse together.
material from the Earth's surface is returned to the interior.
NO that would mean we are making heaps of tetonic plates although this scenario can cause an earthquake and for rocks to slide under or above the plates and the mantle
Subduction (where one plate is forced beneath another less dense plate - may occur at oceanic-oceanic and oceanic-continental boundaries), obduction (where oceanic plate is forced over a continental plate) and orogenesis where two continental plates collide and mountains are formed (e.g. the Himalayas).
Mountains are formed in this way. The Himalayan mountains were formed this way; in fact, they are still growing today as one plate slides under another.
earthquake
A subduction zone is formed.
When an oceanic plate and a continental plate collide, it forms a volcano. The oceanic plate subducts underneath the continental plate. As the oceanic plate slides underneath, a magma chamber is formed. This magma chamber is what feeds the volcano.
When oceanic plates slide under continental plates they form subduction zones. Subduction zones always occur at convergent boundaries where one plate slides beneath another plate.
material from the Earth's surface is returned to the interior.
the oceanic plate is less bouyant so it slides under the continental plate
The Himalayas were formed by the collision of the Eurasian plate (continental) and the Indo-Australian plate (continental).
NO that would mean we are making heaps of tetonic plates although this scenario can cause an earthquake and for rocks to slide under or above the plates and the mantle
adwadadada
well it's simple: an earthquake that can kill and destroy cars, trees, and buildings and they can cause tsunamies
The Himalayas are formed from a continental to continental plate convergence.
A subduction zone, with a whole host of other geological features such as an Island arc, volcanoes and a mountain range.
Mt. Pinatubo is in a subduction zone. subduction is when one tectonic plate slides under another. In the Mt. Pinatubo area the Eurasian Plate slides under the Philippine Sea Plate at the Manila Trench.