volcanos formed igneous rock that builded up past the ocean surface.
The process is called "subduction." It occurs when one tectonic plate moves beneath another at a convergent boundary, where the oceanic plate is forced down into the mantle at a subduction zone. This process leads to the recycling of old oceanic crust back into the mantle.
Yes, oceanic crust can slide under oceanic crust during subduction at convergent plate boundaries. This process occurs when a more dense oceanic plate descends beneath another oceanic plate, leading to the formation of a subduction zone.
Minerals
A steep slide is commonly referred to as a "chute" or a "slope." These terms describe a sharply inclined surface that allows objects or individuals to slide quickly downhill.
The soft, weak layer of rock below the lithosphere is called the asthenosphere. It is semi-molten and behaves plastically, allowing the tectonic plates of the lithosphere to move and slide on top of it.
they are related because they all have to do with the oceanic lithosphere.The convection causes the lithosphere to move sideways and away from the midocean ridges.The ridge push makes the oceanic lithosphere slide downhill under the force of gravity. The slab pull:the old lithosphere is denser than asthenosphere so, the edge of the tectonic plates that contains oceanic lithosphere sinks and plls the rest of the tectonic plate.
they are related because they all have to do with the oceanic lithosphere.The convection causes the lithosphere to move sideways and away from the midocean ridges.The ridge push makes the oceanic lithosphere slide downhill under the force of gravity. The slab pull:the old lithosphere is denser than asthenosphere so, the edge of the tectonic plates that contains oceanic lithosphere sinks and plls the rest of the tectonic plate.
gravity
snowboarding
Oceanic plates are sections of the Earth's lithosphere that are found beneath the oceans. These plates are denser and thinner than continental plates and are typically composed of basaltic rock. Oceanic plates are constantly moving due to the process of plate tectonics, where they can collide with, slide past, or be forced beneath other plates.
The recycling of the lithosphere primarily occurs at convergent plate boundaries, where one tectonic plate is forced beneath another in a process known as subduction. This leads to the recycling of oceanic lithosphere back into the mantle. Additionally, some recycling may occur at transform boundaries where lithospheric plates slide past each other.
The process is called "subduction." It occurs when one tectonic plate moves beneath another at a convergent boundary, where the oceanic plate is forced down into the mantle at a subduction zone. This process leads to the recycling of old oceanic crust back into the mantle.
depression, trough, downhill, slide, recession
you slide downhill over the ice.
Yes, oceanic crust can slide under oceanic crust during subduction at convergent plate boundaries. This process occurs when a more dense oceanic plate descends beneath another oceanic plate, leading to the formation of a subduction zone.
Subduction zones are formed when oceanic plates slide beneath continental plates. The process leads to the oceanic plate being forced into the Earth's mantle. This can result in the formation of deep oceanic trenches and volcanic activity at the surface.
Minerals