zone of subduction
Oceans do not collide but oceanic crustal plates can collide, and when they do collide, island arcs are formed along the subduction zone.
A subduction zone, that includes a ocean trench. This is only possible if one of the plates are oceanic, because if two continental plates collide a mountain range is formed.
Both Plates are pushed upwards and rocks are folded and faulted to form mountain ranges. For Example this occurred in Europe when the Eurasian and African plates collided to form the Alps. And a Subduction zone is formed when a continental and Oceanic plates collide as the oceanic plate is forced downwards into the mantle.
Subduction zones usually refer to convergent tectonic plate boundaries. A convergent boundary indicates two plates that are moving together, or colliding. Oceanic plates that collide with other oceanic plates will create deep trenchs, such as the Marianas Trench, earthquakes, and/or volcanic islands. As oceanic plates collide with continental plates, the oceanic plate will always be subducted by the continental plate because oceanic plates are more dense. This type of collision yields a good deal of heat, resulting in volcanic mountains. Continental plates that collide with other continental plates will crumple on impact producing large mountain ranges, such as the Alps or Himalayas.
mountais
Oceans do not collide but oceanic crustal plates can collide, and when they do collide, island arcs are formed along the subduction zone.
subduction zone
A subduction zone, that includes a ocean trench. This is only possible if one of the plates are oceanic, because if two continental plates collide a mountain range is formed.
Both Plates are pushed upwards and rocks are folded and faulted to form mountain ranges. For Example this occurred in Europe when the Eurasian and African plates collided to form the Alps. And a Subduction zone is formed when a continental and Oceanic plates collide as the oceanic plate is forced downwards into the mantle.
coenvergent 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 tectonic plates collide and the direction of the forces is primarily perpendicular, the plates push up forming a mountain. The Himalayan Mountains are formed by the collision of two plates and are still growing. The summit of Mount Everest is, in fact, marine limestone.
Most notable is the so-called 'Ring of Fire', an area encircling the Pacific Ocean where oceanic crustal plates are subducting under continental plates and less dense oceanic plates.
Subduction zones usually refer to convergent tectonic plate boundaries. A convergent boundary indicates two plates that are moving together, or colliding. Oceanic plates that collide with other oceanic plates will create deep trenchs, such as the Marianas Trench, earthquakes, and/or volcanic islands. As oceanic plates collide with continental plates, the oceanic plate will always be subducted by the continental plate because oceanic plates are more dense. This type of collision yields a good deal of heat, resulting in volcanic mountains. Continental plates that collide with other continental plates will crumple on impact producing large mountain ranges, such as the Alps or Himalayas.
mountais
A subduction zone is a convergent boundary where two tectonic plates collide.