Divergent Boundary

Type 1 Ocean - Continental Collision

Convergence between the continents continues because the crust is still being pulled down by oceanic lithosphere sinking in the subduction zone to either side of the collision as well as beneath the impinging continent.

This collision can form Volcanoes, Mountains, a subduction zone etc.

Himalayan Mountain Range

Indo Australian plate and the Eurasian plate

Mount St Helens

Juan De Fuca Plate and North American Plate