If two plates of different densities collide, the more dense one is forced downwards and eventually becomes part of the mantle. This is usually an oceanic plate. The less dense, continental, plate is pushed up and mountains form along the edge.
This is known as subduction. The subducting plate introduces volatiles into the mantle which acts to cause melting and the formation of magma. This rises to the surface promoting volcanism in the overlying plate.
No, the denser plate sinks under the less dense plate in a process called subduction.
No. The more dense plate will subduct under the less dense plate in a convergent plate setting.
Assuming the denser plate is composed of oceanic crust, then it will subduct into the mantle.
8% equalls the inner out
During subduction, one tectonic plate is forced beneath another plate into the Earth's mantle. This typically occurs at convergent plate boundaries where two plates collide. As the subducting plate sinks into the mantle, it can cause various geological phenomena such as earthquakes, volcanic activity, and the formation of mountain ranges.
Subduction of nazca plate beneath TE south American plate since nazca plate is an oceanic plate, which means it is more dense than the south American plate, which is continental. Oceanic plates have 3.0g/cm^3 of density. Continental have 2.8g/cm^3 of density. Denser plate always sinks beneath less dense plates :)
A tectonic boundary where two oceanic lithospheric plates are either moving away from one another and new crust is formed, or moving toward each other, in which the more dense oceanic plate will subduct beneath the less dense plate.
subduction boundary!!!
a big wave
It was formed by the pacific plate sub ducting beneath the Australian plate. The pacific plate slides into the earths mantle, where it melts. the molten rock then rises to the surface because it is less dense and forms a volcano
SubductionThe Magma Forms And Makes A Volcano
SubductionThe Magma Forms And Makes A Volcano
A subduction zone, with a whole host of other geological features such as an Island arc, volcanoes and a mountain range.
During subduction, one tectonic plate is forced beneath another plate into the Earth's mantle. This typically occurs at convergent plate boundaries where two plates collide. As the subducting plate sinks into the mantle, it can cause various geological phenomena such as earthquakes, volcanic activity, and the formation of mountain ranges.
The downward movement of the more dense plate beneath the less dense plate in a convergent plate scenario is called subduction.Conversely, the over thrusting of one plate onto another is known as obduction.
A convergent plate boundary is where one of the plates is sinking beneath another, and the other one is being pushed on top of the subducting plate. This is called a subduction zone. This happens when denser, heavier oceanic crust meets less dense, thicker, continental crust.When two plates converge, and one is less dense, that plate goes under the more dense plate into the mantle, this is called subduction.subduction will happen and a volcano will be formed. when one plate slides beneath another one magma from earths mantle is being pushed up on earths surface.
Subduction of nazca plate beneath TE south American plate since nazca plate is an oceanic plate, which means it is more dense than the south American plate, which is continental. Oceanic plates have 3.0g/cm^3 of density. Continental have 2.8g/cm^3 of density. Denser plate always sinks beneath less dense plates :)
A tectonic boundary where two oceanic lithospheric plates are either moving away from one another and new crust is formed, or moving toward each other, in which the more dense oceanic plate will subduct beneath the less dense plate.
subduction boundary!!!
In a process called subduction, the more dense plate is drawn under the less dense plate and creates an angular path downward toward the mantle. The presence of water in the subducting plate can cause melting which leads to rising plumes of magma and possible volcanism.
Dense oceanic crust slides under less dense continental crust