sinks
sinks
sinks
Yes, it "dives" under the continental crust and back into the mantle.
Oceanic plates are denser than continental plates, so when they collide at a convergent boundary, the denser oceanic plate is forced to subduct beneath the less dense continental plate. This subduction is driven by the force of gravity pulling the denser plate downward. This process can lead to the formation of volcanic arcs and deep ocean trenches.
is forced below the less dense continental plate in a process called subduction. This can lead to the formation of deep ocean trenches, volcanic arcs, and earthquakes along the subduction zone.
When oceanic plates collide with continental plates, the denser oceanic plate is subducted beneath the lighter continental plate. This process leads to the formation of deep ocean trenches and volcanic arcs on the continental side. Additionally, intense seismic activity and mountain building may occur along the boundary.
This phenomenon, known as subduction, occurs because oceanic plates are denser and thinner than continental plates. When the two plates collide, the denser oceanic plate is forced beneath the less dense continental plate due to gravitational pull. This process results in the oceanic plate descending into the mantle, leading to the formation of deep ocean trenches and volcanic arcs.
When tectonic plates collide with oceanic plates, the denser oceanic plate is usually forced beneath the less dense continental plate in a process called subduction. This can lead to the formation of volcanic arcs and deep ocean trenches. The collision can also cause earthquakes and crustal deformation.
When dense oceanic plates collide with a continental plate, the denser oceanic plate is usually subducted beneath the less dense continental plate due to the difference in density. This can lead to the formation of deep ocean trenches, volcanic arcs, and mountain ranges on the continental plate. Subduction zones are also associated with earthquakes and volcanic activity.
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.
this depends on the two plates that collide. Ocean plates are much heavier than continental plates. If an ocean and continental plate collide, the ocean plate sinks underneath and creates a trench. If two ocean plates or two continental plate collide, it creates a mountain range/ oceanic ridge depending on the type.
A convergent boundary is formed when plates collide. At this type of boundary, the denser plate sinks beneath the less dense plate in a process known as subduction. This collision often results in the formation of mountain ranges, volcanoes, and deep ocean trenches.