terranes are attached to the edge of a continent
a trench will form
it forms a trench
subduction
When an oceanic plate collides with a continental plate, the denser oceanic plate is forced beneath the continental plate in a process called subduction. This creates a deep oceanic trench. As the oceanic plate sinks, it heats up, melts, and forms magma that rises to the surface, leading to volcanic activity.
terranes are attached to the edge of a continent
When a continental plate collides with an oceanic plate and overtakes it, the denser oceanic plate is forced underneath the continental plate in a process called subduction. This creates a deep ocean trench, volcanic arcs, and earthquakes along the boundary between the two plates. The subduction process can also lead to the formation of mountain ranges on the overriding continental plate.
When an oceanic plate collides with a continental plate, the denser oceanic plate is subducted beneath the continental plate due to its weight. This subduction can lead to the formation of deep ocean trenches, volcanic arcs, and seismic activity.
When an oceanic plate and a continental plate collide, the oceanic plate is always subducted. Oceanic plates are denser than continental plates, and they have a higher iron content. Since they are denser, oceanic plates always sink below the continental plate in the event of a collision.
the oceanic crust slides down and burns in the mantle and forms a volcano
When an oceanic plate collides with a continental plate, the oceanic plate is usually subducted because it is denser and thinner than the continental plate. This density difference causes the oceanic plate to sink beneath the continental plate into the mantle, forming a subduction zone. This process can lead to the formation of deep ocean trenches and volcanic arcs on the continental side. Additionally, the subduction of the oceanic plate contributes to geological activity such as earthquakes and volcanic eruptions.
When a continental plate collides with an oceanic plate, the denser oceanic plate is forced beneath the continental plate in a process called subduction. This leads to the formation of a subduction zone, which can create deep ocean trenches and volcanic arcs on the continental plate. As the oceanic plate sinks, it melts and can trigger earthquakes and volcanic eruptions. Over time, this interaction contributes to the recycling of the Earth's crust.
Volcanoes may form where two oceanic plates collide or where an oceanic plate collides with a continental plate.