Oceanic plates move under continental plates when they converge together because the oceanic plate is more denser than the continental plate.
The oceanic plate subduct under the continental because oceanic is made from basalt(rock) which is denser than andesite and granite(continental)
When oceanic plates collide and slide under continental plates, they can form volcanic mountain ranges called continental volcanic arcs. These arcs result from the melting of the descending oceanic plate, which then feeds magma to the Earth's surface. Examples include the Andes in South America and the Cascades in North America.
Oceanic plates are denser than continental plates due to their composition and age. When two plates collide and one is denser, the denser plate will subduct beneath the less dense plate. This is why oceanic plates subduct beneath continental plates in a process known as subduction.
When oceanic and continental plates collide, the oceanic plate is usually forced under the continental plate in a process called subduction. This can result in the formation of mountain ranges on the continental plate and can lead to the creation of volcanic arcs. The collision can also cause earthquakes and tsunamis.
When dense oceanic plates collide with a continental plate, the denser oceanic plate is usually subducted beneath the less dense continental plate due to the difference in density. This can lead to the formation of deep ocean trenches, volcanic arcs, and mountain ranges on the continental plate. Subduction zones are also associated with earthquakes and volcanic activity.
The oceanic plate subduct under the continental because oceanic is made from basalt(rock) which is denser than andesite and granite(continental)
When oceanic plates collide and slide under continental plates, they can form volcanic mountain ranges called continental volcanic arcs. These arcs result from the melting of the descending oceanic plate, which then feeds magma to the Earth's surface. Examples include the Andes in South America and the Cascades in North America.
The oceanic plate subducts under the continental because it is denser. The Andes are being formed in this way and the Himalayas started that way also.
This phenomenon, known as subduction, occurs because oceanic plates are denser and thinner than continental plates. When the two plates collide, the denser oceanic plate is forced beneath the less dense continental plate due to gravitational pull. This process results in the oceanic plate descending into the mantle, leading to the formation of deep ocean trenches and volcanic arcs.
Oceanic plates are denser than continental plates due to their composition and age. When two plates collide and one is denser, the denser plate will subduct beneath the less dense plate. This is why oceanic plates subduct beneath continental plates in a process known as subduction.
Tectonic plates.Tectonic plates are plates underneath Earth's surface that move very slowly. There are oceanic and continental plates. Of course, oceanic plates are plates under the ocean, and continental plates are plates underneath ground, or continents. Each of the plates carry the things above them, land or ocean. When two continental or oceanic plates collide, it causes a fold in Earth's surface, and an earthquake. Now, when a continental plate draws near and nearly collides with an oceanic plate, something called subduction occurs. Subduction is basically when the oceanic plate dips down below the continental plate, causing a trench.
When oceanic and continental plates collide, the oceanic plate is usually forced under the continental plate in a process called subduction. This can result in the formation of mountain ranges on the continental plate and can lead to the creation of volcanic arcs. The collision can also cause earthquakes and tsunamis.
is means under the oceanic crust the tectonicplate collide
the oceanic plates are denser than continental plates, therefore, when oceanic plates and continental plates converge, the oceanic will go under the continental plates. But when two oceanic converge either both will rise to form moutains, or both will sink and cause a trench.
When dense oceanic plates collide with a continental plate, the denser oceanic plate is usually subducted beneath the less dense continental plate due to the difference in density. This can lead to the formation of deep ocean trenches, volcanic arcs, and mountain ranges on the continental plate. Subduction zones are also associated with earthquakes and volcanic activity.
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The density of the plates and the angle of the collision can determine which plate comes out on top when two plates collide. The denser plate tends to sink beneath the less dense plate, while the angle of collision can influence the direction of movement. Additionally, the presence of features like oceanic crust and continental crust can also impact which plate is subducted.