Subduction.
this is a destructive plate boundary. An earthquake and a vocano is created
when you are floating and then you start moving and then you fall beneth water when you are floating and then you start moving and then you fall beneth water
The lithosphere sinking into the mantle occurs at a convergent plate boundary, specifically in subduction zones. In these regions, one tectonic plate is forced beneath another, typically an oceanic plate descending beneath a continental plate or another oceanic plate. This process leads to the formation of deep ocean trenches and volcanic arcs. The subduction of the lithosphere is a key driver of tectonic activity and geological phenomena associated with plate interactions.
Subduction
Subduction occurs when one tectonic plate slides beneath another into the Earth's mantle at convergent plate boundaries. This process is commonly associated with the formation of deep oceanic trenches and volcanic arcs, and it is a key mechanism driving plate tectonics and shaping the Earth's surface.
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.
Subduction is the process where one tectonic plate moves beneath another plate at a convergent boundary. This occurs because the denser plate sinks into the mantle, creating a subduction zone. The sinking plate can cause earthquakes, volcanic activity, and the formation of mountain ranges.
squat-thrust
When one plate sinks under the other, it is callled subduction, no matter what kind of plate it is. When two oceanic plates collide, they form trenches(i.e. the mariana trench). Hope this answers your question!!!
The pacific oceanic plate is sinking beneath conential plate
The principle behind this phenomenon is known as plate tectonics, where lithospheric plates float on the semi-fluid asthenosphere. When one plate subducts beneath another, it forms a convergent boundary. This process can lead to the formation of deep ocean trenches, volcanic arcs, and seismic activity.
When two oceanic plates or two plates both containing oceanic crust collide or converge, the convergent boundary will form a trench. The plate which has the higher density will plunge beneath the other plate forming a trench.