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Convergent
Contiental- oceanic
Ocean plate sub ducts under the land plate
Trench formed
Convergent- ocean to ocean
More dense oceanic plate sub ducts under the other one
A volcanic island arch is formed
Convergent
Contiental to contiental
No subduction, plates gets pushed up
Folded/non-explosive mountains
Divergent
Magma pops up in the crack that is formed
Mid-ocean ridge and rift valleys
Transform boundary
The plates slide by each other
Fault zone formed
Hot spot
Magma reaches the surface NOT at a plate boundary
Volcanos and volcanic island chain formed
Convection currents
Hot liquids rise, cool liquids sink in the mantle
Slab pull
DOING MOST OF THE WORK
Subduction causes a pulling force on the plate
Ridge push
Creation of new crust pushing exciting rock out of the way