The effect of subduction at the boundary of two plates is the movement of one tectonic plate under another tectonic plate. This creates a subduction zone, which often occurs in convergent boundaries.
Convergent on the western perimeter, divergent on the Easter perimeter.
divergent boundary
The mid-ocean ridge system is the longest continuous divergent plate boundary on Earth.
The Divergent Boundaries.
The southeast Indian Ridge is a divergent plate boundary, where two tectonic plates are moving away from each other. This movement causes magma to rise from the mantle, creating new crust as the plates separate.
It is called a divergent plate boundary.
Convergent on the western perimeter, divergent on the Easter perimeter.
Divergent boundary is formed
divergent boundary
The mid-ocean ridge system is the longest continuous divergent plate boundary on Earth.
The Divergent Boundaries.
A divergent plate boundary.
Convergent plate boundary, divergent plate boundary and strike-slip (transform) plate boundary.
Divergent refers to a plate boundary where plates are moving apart. Plates are not referred to in terms of their boundary movements.
The Mid-Atlantic Ridge separates the North American plate from the African plate. This ridge runs through the Atlantic Ocean and marks the boundary where the two plates are moving apart.
The southeast Indian Ridge is a divergent plate boundary, where two tectonic plates are moving away from each other. This movement causes magma to rise from the mantle, creating new crust as the plates separate.
A rift valley is evidence of a divergent plate boundary, where two tectonic plates are moving away from each other. This movement creates a gap in the Earth's crust, resulting in the formation of a rift valley.