they hug each other
It is called subduction. When subduction occurs one plate slips beneath the other and sinks into the Earth's mantle and creates a trench.
A convergent plate movement occurs when two tectonic plates collide with each other. This typically happens at subduction zones, where one plate is forced beneath the other due to differences in density. This can create mountains, earthquakes, and volcanic activity.
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.
Subduction occurs when one tectonic plate moves underneath another plate at a convergent boundary. This typically happens at deep ocean trenches where the denser oceanic plate is forced beneath the less dense continental plate. Subduction is a key process in the cycle of plate tectonics, leading to the formation of volcanic arcs and earthquakes.
When plates collide, one plate is typically forced beneath the other in a process known as subduction. This can create mountain ranges, volcanic arcs, and deep ocean trenches above the subduction zone as a result of the intense geological activity generated by the collision and subduction of the plates.
Where two plates collide
when two oceanic plates collide they create a deep-ocean trench, at deep-ocean trenches subduction occurs.
It is called subduction. When subduction occurs one plate slips beneath the other and sinks into the Earth's mantle and creates a trench.
Subduction.
When that happens a earthquake is produced.
A convergent plate movement occurs when two tectonic plates collide with each other. This typically happens at subduction zones, where one plate is forced beneath the other due to differences in density. This can create mountains, earthquakes, and volcanic activity.
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.
Subduction is when two plates collide, and one moves underneath the other, or subducts. The denser one is the one that subducts. Subduction is caused by the collision of two plates.
When two plates collide with enough force, faulting occurs, breaking the crust. Faulting (Apex)
Subduction occurs when one tectonic plate moves underneath another plate at a convergent boundary. This typically happens at deep ocean trenches where the denser oceanic plate is forced beneath the less dense continental plate. Subduction is a key process in the cycle of plate tectonics, leading to the formation of volcanic arcs and earthquakes.
When plates collide, one plate is typically forced beneath the other in a process known as subduction. This can create mountain ranges, volcanic arcs, and deep ocean trenches above the subduction zone as a result of the intense geological activity generated by the collision and subduction of the plates.
Earthquakes are caused when this happens.