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Slab Pull
Oceanic crust subducts
Pulls the plate with it
Ridge Pull
New crust hot, buoyant and elevated
Slides away from the mid-ocean ridge
Rift Valleys
Constructive boundary
Continental areas
Plates move apart
Crust drops between faults
Upstanding block is called a horst
E.g. Rift Valley in Eastern Africa
Deep Sea Trenches
Destructive boundary
Oceanic and continental plates
Down warping of the oceanic plate forms a deep part of the ocean
Subduction zone
E.g. Marianas Trench (Pacific and Philippines plate)
Island Arcs
Destructive boundary
Oceanic and continental plates
Material rises to the surface forming volcanoes
After eruption, island arcs form
E.g. Marianas Islands and Guam
Parallel to the Marianas Trench
Young Fold Mountains
Collision boundary
2 continental plates
Crusts are forced together
Sediment is forced together up and down
Up = young fold mountains
Down = deep mountain roots