The Plates form a Subduction zone. (look it up)
The three types of plate tectonic boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates collide; and transform boundaries, where plates slide past each other horizontally.
The three main types of plate boundaries are convergent boundaries, where plates move toward each other, divergent boundaries, where plates move away from each other, and transform boundaries, where plates slide past each other horizontally.
When 2 oceanic plates and 2 continental plates move towards each other, subduction occurs. The denser oceanic plate sinks beneath the less dense continental plate, creating deep ocean trenches and volcanic arcs. This process can lead to the formation of mountain ranges and earthquakes.
Convergent plates move towards each other, leading to a collision or subduction of the plates. This movement can result in the formation of mountain ranges, deep ocean trenches, and volcanic activity.
When continental plates move toward each other, it is called a convergent plate boundary. This can lead to the collision and subduction of the plates, causing mountain building and deep ocean trench formation.
When plates slide past each other, move toward each other, and move away from each other.
When crustal plates move toward each other, they can form convergent boundaries where one plate is forced beneath the other in a process called subduction. This can result in the formation of mountain ranges, deep ocean trenches, and volcanic activity in the area.
Convergence Boundary.
they move against one another
When plates of the earth move toward each other or collide they create compression, which can result in the formation of mountain ranges, seismic activity, and subduction zones.
When tectonic plates move toward each other, it is known as a convergent boundary. This movement can result in subduction, where one plate is forced beneath the other, or in the collision of two plates, leading to the formation of mountain ranges.
At a convergent boundary two plates move toward each other. At a transform boundary plates slide past each other.
This is called a convergent boundary. A divergent boundary is when plate move away from each other, and a transform boundary is when plates slide past each other.
Plates that move toasted each other are detractive plates meeting at a destructive margin. If a continental and an oceanic plate move towards each other, earthquakes and volcanoes occur, this is called a subduction margin, but if the plates are both continental then fold mountains form this is a collision margin
The three types of plate tectonic boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates collide; and transform boundaries, where plates slide past each other horizontally.
The three main types of tectonic plate boundaries are convergent boundaries, where plates move toward each other; divergent boundaries, where plates move away from each other; and transform boundaries, where plates slide past each other horizontally.
A convergent boundary occurs when two plates move toward each other. This movement can result in subduction, where one plate is forced beneath the other, or it can create mountain ranges and volcanic activity.