If you are talking about plate tectonics, the action you're referring to is called subduction.
The process involved in the sinking of cold oceanic plates into the mantle is called subduction. This occurs at convergent plate boundaries where the denser oceanic plate is forced beneath the less dense continental plate. As the oceanic plate sinks into the mantle, it undergoes partial melting, causing volcanic activity along the subduction zone.
The colder, denser plate sinks beneath the less dense plate during subduction due to gravity. The older plate has had more time to cool and become denser, while the less dense plate is usually younger and has not had as much time to cool. This density contrast is a major driving force for subduction.
The force on the lithosphere from the asthenosphere below due to cooling and sinking rock is called slab pull. This force is one of the driving mechanisms behind plate tectonics, where the denser oceanic lithosphere sinks into the mantle, pulling the rest of the plate along with it.
A subduction zone forms when one tectonic plate moves beneath another plate. This happens because the denser oceanic plate sinks below the less dense continental plate. The key processes involved in the creation of a subduction zone include the convergence of tectonic plates, the sinking of the denser plate into the mantle, and the generation of earthquakes and volcanic activity along the subduction zone.
Subduction
No, the denser plate sinks under the less dense plate in a process called subduction.
The process is called subduction. It occurs when one tectonic plate is forced beneath another due to differences in density, typically in convergent plate boundaries. This subduction process is a key driver of plate tectonics.
The process involved in the sinking of cold oceanic plates into the mantle is called subduction. This occurs at convergent plate boundaries where the denser oceanic plate is forced beneath the less dense continental plate. As the oceanic plate sinks into the mantle, it undergoes partial melting, causing volcanic activity along the subduction zone.
The process is called subduction. Subduction occurs when one tectonic plate slides beneath another plate due to differences in density, often leading to the formation of deep ocean trenches and volcanic activity.
The colder, denser plate sinks beneath the less dense plate during subduction due to gravity. The older plate has had more time to cool and become denser, while the less dense plate is usually younger and has not had as much time to cool. This density contrast is a major driving force for subduction.
The plate motion due to higher densities is called subduction. This occurs when a denser oceanic plate is forced underneath a less dense continental plate at convergent plate boundaries.
This is called a destructive plate boundary. It occurs due to the fact that the oceanic crust is far denser than the continental crust. As a result it subducts into the mantle and is incenerated. Hope it helped:)
Subduction is the term used to describe the process of one tectonic plate sinking beneath another at a deep-ocean trench. This occurs when a denser oceanic plate slides under a less dense continental plate, leading to the formation of deep-sea trenches and volcanic arcs.
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.
The less dense plate would override the more dense plate during a collision, as it is not as heavy and will ride up over the denser plate. This could lead to the less dense plate being forced to subduct beneath the more dense plate due to the heavier weight of the latter.
Oceanic plates are denser than continental plates due to their composition, so when they collide, the denser oceanic plate is forced to dive (subduct) beneath the less dense continental plate. This process occurs due to the difference in density between the two types of plates, leading to the oceanic plate sinking into the mantle.
The force on the lithosphere from the asthenosphere below due to cooling and sinking rock is called slab pull. This force is one of the driving mechanisms behind plate tectonics, where the denser oceanic lithosphere sinks into the mantle, pulling the rest of the plate along with it.