The answer would be convergent
A divergent boundary is where tectonic plates move away from each other, creating new crust. A convergent boundary is where plates collide, leading to the formation of mountains or subduction zones.
Divergent boundaries occur when tectonic plates move away from each other, creating new crust, while convergent boundaries happen when plates collide, leading to the destruction or subduction of crust.
The three main types of plate boundaries are divergent, convergent, and transform. Divergent boundaries occur where plates move apart, creating new crust. Convergent boundaries occur where plates collide and can result in subduction zones or mountain formation. Transform boundaries occur where plates slide past each other horizontally.
convergent boundary -rift valley divergent boundary -mid-ocean ridge
divergent plate boundary- a boundary where two plates move apart from each other. convergent plate boundary- a boundary where two plates move towards each other so that one plate can sink beneath the other. transform plate boundary- a boundary where one plate slips along side another plate.
Subduction is a process that takes place at convergent boundaries.
No, subduction is not common at divergent plate boundaries. Divergent plate boundaries are characterized by plates moving away from each other, which creates new oceanic crust. Subduction occurs at convergent plate boundaries where plates collide and one descends beneath the other.
It is neither, because plate is not being made or destroyed. Divergent is constructive. Convergent is destructive. Subduction is constructive.
That is easy there are acctuaslly 4 they are convergent,covergent subduction, divergent, and transform.
The antonym for divergent boundary is convergent boundary. In a divergent boundary, tectonic plates move away from each other, while in a convergent boundary, they move towards each other. This can result in subduction zones, mountain formation, or continental collision.
Paricutin is located on a convergent boundary. The volcano formed as a result of the subduction of the Cocos Plate beneath the North American Plate in Mexico.
Yes, volcanism is found at both convergent and divergent boundaries of tectonic plates. At convergent boundaries, subduction zones can result in the formation of volcanoes due to the melting of subducted crust. At divergent boundaries, magma rises to the surface to create new crust, leading to volcanic activity as seen in mid-ocean ridges.
The four types of plate boundaries are divergent boundaries (plates moving apart), convergent boundaries (plates moving together), transform boundaries (plates sliding past each other), and subduction zones (one plate sinking beneath another).
A divergent boundary is where tectonic plates move away from each other, creating new crust. A convergent boundary is where plates collide, leading to the formation of mountains or subduction zones.
Krakatoa is located at a convergent boundary, where the Indo-Australian Plate is being subducted beneath the Eurasian Plate. This subduction zone can lead to intense volcanic activity due to the melting and rising of magma from the subducted plate.
Divergent boundaries occur when tectonic plates move away from each other, creating new crust, while convergent boundaries happen when plates collide, leading to the destruction or subduction of crust.
A continent to continent convergent boundary does not have a subduction zone.