At a convergent boundary, tectonic plates are typically pushed together by the force of subduction where one plate is forced beneath the other, or by collision where the plates directly collide with each other. This movement can be driven by the force of mantle convection, where heat from the Earth's core causes the mantle to flow in a circular motion.
At a convergent boundary, plates move towards each other.
This is called a convergent boundary, because the two plates are converging, or coming together.
Convergent Boundary.
Convergent boundary.
Compression
At a convergent boundary, plates move towards each other.
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.
convergent boundary
A convergent boundary is where plates move together.
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, because the two plates are converging, or coming together.
convergent boundary
Convergent Boundary.
It is a divergent boundary when they move When they move -> together
divergent transform, or convergent
There are 3 types of Convergent boundaries, they are; 1. Continental-continental convergent boundary. 2. Continental-oceanic convergent boundary. 3. Oceanic-oceanic convergent boundary.
Convergent boundary.