Plate boundaries

Deformation occur along their boundaries

Seafloor mountain

Collision of two continental plates

Destructive plate

margins where

oceanic crust are

being consumed in the mantle are

called

continental

plate converges with

an oceanic plate

When two oceanic slabs converge, one descends beneath the other

initiating volcanic activity

the

continued subduction eventually

brings the two continents

together

where two plates

grind past each other

without the production

or destruction of

lithosphere

The fracture zone that

forms a transform plate

boundary is known as a

where two plates move apart, resulting in upwelling of material from the mantle to from the mantle to create seafloor