All three of Newton's laws apply in all cases.
The subducted plate descends into the mantle at subduction zone
Subduction is part of the geological process of plate tectonics. A subduction zone is a place where the oceanic plate is sinking back in to the mantle (usually at the edge of a continental plate.
Subduction Zone
It is known as subduction.
Convergent plate boundariesDestructive plate boundaries
It is called subduction and only occurs in oceanic to oceanic or oceanic to continental plate collisions.
The subducted plate descends into the mantle at subduction zone
The subducted plate descends into the mantle at subduction zone
Subduction is part of the geological process of plate tectonics. A subduction zone is a place where the oceanic plate is sinking back in to the mantle (usually at the edge of a continental plate.
subduction zone
Subduction Zone
Subduction into the upper mantle and melting.
The process in which the ocean floor sinks into the mantle is called subduction. This occurs at convergent plate boundaries, where one tectonic plate slides beneath another. Subduction zones are associated with deep-sea trenches and volcanic activity.
It is known as 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.
Subduction is the process when one tectonic plate moves beneath another plate at a convergent boundary. This movement can lead to the recycling of old oceanic crust back into the mantle.
Newton's first law of motion applies in this scenario. The rock that gets stuck while the plate is subducting into the mantle remains at rest until an external force acts upon it, in this case, the force from the movement of the tectonic plate.