It moves downward into the asthenosphere where it is partially melted. The melt may rise through the lithosphere and solidify, or flow onto the surface.
A deep oceanic trench forms where oceanic crust subducts beneath continental crust. The descending oceanic plate melts as it reaches greater depths, creating magma that can lead to volcanic activity. This process can also generate earthquakes due to the intense pressure and stress in the subduction zone.
Crust under the oceans is called oceanic crust.
When oceanic crust is pushed under continental crust in a subduction zone, a deep trench is formed at the boundary between the two plates. The oceanic crust then descends into the mantle, creating a convergent plate boundary. This process can lead to the formation of volcanic arcs on the overriding continental plate.
The oceanic crust is thinnest at mid-ocean ridges, where tectonic plates are moving away from each other and new crust is formed. These areas have thinner crust due to the upwelling of magma from the mantle, which creates new crust as it solidifies.
At a mid-ocean ridge, tectonic plates move apart, allowing magma from the mantle to rise and solidify, creating new oceanic crust. This process, known as seafloor spreading, contributes to the continuous formation of new oceanic crust and the expansion of the ocean floor.
A deep ocean trench is commonly formed at a plate boundary where oceanic crust converges with continental crust. The oceanic crust is denser and is forced beneath the lighter continental crust, creating a deep trench.
When heavier oceanic crust converges with lighter crust at a deep ocean trench, the heavier oceanic crust is usually forced under the lighter crust in a process known as subduction. This can create deep ocean trenches and volcanic arcs on the overriding plate. The subducting plate can also melt and cause volcanic activity.
They form when the oceanic crust goes under the Continental crust. The oceanic crust then forms the trenches through a process called subduction.
deep ocean trench.
An ocean trench is a deep canyon in the ocean floor that forms at a destructive plate margin where oceanic crust flows back into the Earth's mantle. An example would be the Mariana Trench is the deepest point in any ocean and is located in the Pacific Ocean
A deep oceanic trench forms where oceanic crust subducts beneath continental crust. The descending oceanic plate melts as it reaches greater depths, creating magma that can lead to volcanic activity. This process can also generate earthquakes due to the intense pressure and stress in the subduction zone.
continent-continent move together colliding making a mountain ocean-ocean or ocean-continent move together also but oceanic crust is denser so it will subduct and create a trench and one oceanic crust will be denser most likely than the other so it will also subduct and create a trench
When two plates collide, or come together, the plates will push upward, forming a mountain. If one plate is continental crust and the other is oceanic crust, the less dense crust (this being the oceanic) will actually move under the more dense crust, in a process called subduction, to form a deep-ocean trench.
Crust under the oceans is called oceanic crust.
Both the ocean trench and mid-ocean ridge are features found on the ocean floor as part of the oceanic crust. They are formed by tectonic processes, with ocean trenches created by the subduction of one tectonic plate beneath another, while mid-ocean ridges are formed by the divergence of tectonic plates, leading to the upwelling of magma and the creation of new oceanic crust.
When two plates collide, or come together, the plates will push upward, forming a mountain. If one plate is continental crust and the other is oceanic crust, the less dense crust (this being the oceanic) will actually move under the more dense crust, in a process called subduction, to form a deep-ocean trench.
When oceanic crust is pushed under continental crust in a subduction zone, a deep trench is formed at the boundary between the two plates. The oceanic crust then descends into the mantle, creating a convergent plate boundary. This process can lead to the formation of volcanic arcs on the overriding continental plate.