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Ch. 11 Mountain Building

Across
When a hanging wall slides down the foot wall of a fault line
Large masses of rock the arise up great distances and result from the forces of converging plates
Boundary between continental crust and ocean crust
When rock on opposite sides of the fault-line move horizontally past each other
Upfold of layered rock
Down
A down-flow of folded rock
A nearly circular folded mountain. Some are caused by magma intrusions or an uplifting force
When two or more plates collide and rock folds and crumbles to form mountains (Sierra Nevada or Himalayas)
A reverse fault where the fault plane dips less than 45 degrees
Opposite of a normal fault where the hanging wall moves up with respect to the foot walls
Similar to fault-line but present no apparent movement