Wiki User
∙ 12y agoSubduction
Wiki User
∙ 12y agoThis is known as a subduction zone. It is where one tectonic plate is forced beneath another due to tectonic forces, resulting in the recycling of crustal material back into the mantle. These zones are often associated with deep ocean trenches and volcanic arcs.
trenches
The crashing of the India plate into the Asia plate resulted in the thrusting up of the Himalayas. Another possibility is subduction, where one plate is pushed downwards into the mantle.
The India plate crashing into the Asia plate caused the formation of the Himalayas. It can also cause subduction, when one plate is pushed beneath the other plate and so pushed back into the molten mantle.
Subduction occurs at deep ocean trenches when one tectonic plate is forced beneath another plate. As the descending plate sinks into the mantle, it generates earthquakes and melts due to high temperature and pressure. This molten material can rise to the surface and form volcanic arcs on the overriding plate.
It is called subduction. Subduction occurs in tectonic plate boundaries, where one plate sinks into the mantle beneath another plate due to differences in density and thickness. This process can lead to the creation of deep ocean trenches and volcanic activity.
trenches
When one tectonic plate is pushed beneath another plate, it is called subduction. This process occurs at convergent plate boundaries where one plate is denser than the other, causing it to sink into the mantle. Subduction zones are associated with deep ocean trenches and can lead to volcanic activity and earthquakes.
One plate tectonic, or fragment, is pushed underneath another plate which causes the other one to go nowhere else but up.
This process is known as subduction, where one tectonic plate is forced beneath another plate in the Earth's lithosphere. Subduction zones are often associated with the formation of deep ocean trenches and volcanic arcs due to the intense heat and pressure created by the descending plate melting the mantle.
The crashing of the India plate into the Asia plate resulted in the thrusting up of the Himalayas. Another possibility is subduction, where one plate is pushed downwards into the mantle.
Oceanic plates are pushed down into the upper mantle in a process known as subduction. This occurs at convergent plate boundaries where one tectonic plate is forced beneath another due to differences in density. Subduction zones are associated with earthquakes and volcanic activity.
Subduction zones are formed where an oceanic plate is forced beneath another plate, typically a continental plate. This process typically leads to the formation of deep oceanic trenches, volcanic arcs, and seismic activity due to the subduction of the oceanic plate into the mantle.
The India plate crashing into the Asia plate caused the formation of the Himalayas. It can also cause subduction, when one plate is pushed beneath the other plate and so pushed back into the molten mantle.
subduction boundary!!!
At this type of convergent boundary the oceanic plate will be subducted, or sink into the mantle underneath the continental plate. Volcanoes often form near these boundaries.
Subduction occurs at deep ocean trenches when one tectonic plate is forced beneath another plate. As the descending plate sinks into the mantle, it generates earthquakes and melts due to high temperature and pressure. This molten material can rise to the surface and form volcanic arcs on the overriding plate.
It is called subduction. Subduction occurs in tectonic plate boundaries, where one plate sinks into the mantle beneath another plate due to differences in density and thickness. This process can lead to the creation of deep ocean trenches and volcanic activity.