When an oceanic plate and a continental plate collide, the oceanic plate is always subducted. Oceanic plates are denser than continental plates, and they have a higher iron content. Since they are denser, oceanic plates always sink below the continental plate in the event of a collision.
When an oceanic plate collides with a continental plate, the oceanic plate is usually subducted because it is denser and thinner than the continental plate. This density difference causes the oceanic plate to sink beneath the continental plate into the mantle, forming a subduction zone. This process can lead to the formation of deep ocean trenches and volcanic arcs on the continental side. Additionally, the subduction of the oceanic plate contributes to geological activity such as earthquakes and volcanic eruptions.
The crust is subducted and destroyed at convergent plate boundaries, where an oceanic plate collides with a continental plate or another oceanic plate. In these zones, the denser oceanic plate is forced beneath the lighter continental crust into the mantle, leading to volcanic activity and the formation of deep ocean trenches. As the subducted material melts and is recycled, it contributes to geological processes such as magma formation and the creation of mountain ranges.
The Oceanic plate is subducted under the Continental plate because oceanic crust is much more dense than continental crust. The average density of the oceanic crust is 3g/cm^3 while the average density of continental crust is 2.7g/cm^3.
When the oceanic plate collides with a continental plate, it is typically subducted underneath the continental plate due to its higher density. This subduction process can lead to the formation of deep oceanic trenches and volcanic arcs on the overriding continental plate. It also contributes to the recycling of oceanic crust back into the mantle.
subduction
When an oceanic plate collides with a continental plate, the denser oceanic plate is subducted beneath the continental plate due to its weight. This subduction can lead to the formation of deep ocean trenches, volcanic arcs, and seismic activity.
When an oceanic plate collides with a continental plate, the oceanic plate is usually subducted because it is denser and thinner than the continental plate. This density difference causes the oceanic plate to sink beneath the continental plate into the mantle, forming a subduction zone. This process can lead to the formation of deep ocean trenches and volcanic arcs on the continental side. Additionally, the subduction of the oceanic plate contributes to geological activity such as earthquakes and volcanic eruptions.
The oceanic plate is made of denser (and thinner) rock than the continental crust, so the oceanic plate gets subducted (pushed underneath) where it descends and gets melted by geothermal heat.
The oceanic plate is made of denser (and thinner) rock than the continental crust, so the oceanic plate gets subducted (pushed underneath) where it descends and gets melted by geothermal heat.
The crust is subducted and destroyed at convergent plate boundaries, where an oceanic plate collides with a continental plate or another oceanic plate. In these zones, the denser oceanic plate is forced beneath the lighter continental crust into the mantle, leading to volcanic activity and the formation of deep ocean trenches. As the subducted material melts and is recycled, it contributes to geological processes such as magma formation and the creation of mountain ranges.
The Oceanic plate is subducted under the Continental plate because oceanic crust is much more dense than continental crust. The average density of the oceanic crust is 3g/cm^3 while the average density of continental crust is 2.7g/cm^3.
When the oceanic plate collides with a continental plate, it is typically subducted underneath the continental plate due to its higher density. This subduction process can lead to the formation of deep oceanic trenches and volcanic arcs on the overriding continental plate. It also contributes to the recycling of oceanic crust back into the mantle.
Continental plates are lighter (less dense) than oceanic plates.
it forms a trench
subduction
At some convergent boundaries, an oceanic plate collides with acontinental plate. Oceanic crust tends to be denser and thinner thancontinentalcrust, so the denser oceanic crust gets bent and pulled under, or subducted, beneath the lighter and thicker continental crust. This forms what is called a subduction zone.
When a oceanic plate collides with a continental plate, the denser oceanic plate is usually subducted beneath the lighter continental plate. This can result in the formation of mountain ranges, volcanic arcs, and deep ocean trenches. The collision can also lead to earthquakes and the release of magma.