As a result of pressure, friction, and plate material melting in the mantle, earthquakes and volcanoes are common near convergent bouther, they form either a subduction zone or a continental collision.
When two plates move towards one another, they form either a subduction zone or a continental collision. As a result of pressure, friction, and plate material melting in the mantle, earthquakes and volcanoes are common near convergent boundaries.
As a result of pressure, friction, and plate material melting in the mantle, earthquakes and volcanoes are common near convergent boundaries. When two plates move towards one another, they form either a subduction zone or a continental collision.
As a result of pressure, friction, and plate material melting in the mantle, earthquakes and volcanoes are common near convergent boundaries. When two plates move towards one another, they form either a subduction zone or a continental collision.