there is tremendous heat and pressure and this drives slow circular called convectioncurrents within the mantle layer
Different tectonic plates meet each other at their boundaries which are known PLATE MARGINS
There are 3 types of plate margins:
Constructive (divergent)
Destructive (convergent)
Conservative (transform)
Constructive (divergent) two plates MOVEAWAY from each other
This movement forms a gap between plates which allows to magma to see through and cool for new geological features such a volcanoes (CONSTRUCTIVE)(DIVERGENT)
The mid Atlantic ridge under the Atlantic ocean is an example of divergent
Destructive (convergent) two plates MOVE TOWARDS FROM EACH OTHER