5 Written questions
4 Multiple choice questions
- location of two normal faults that dip towards each other, horst is the ridge, graben is the valley
- located in areas where oceanic lithosphere is being subducted beneath the leading edge of the continent
- Forms when a normal faults uplift a block of rock.
- a type of fault where the hanging wall slides upward; caused by compression in the crust
4 True/False questions
syncline → an upward fold in rock formed by compression of Earth's crust
fold mountains → Formed when magma collects and pushes the rock layers above it into a rounded-dome shape.
anticline → a downward fold in rock formed by compression in earth's crust
strike slip fault → break in rock caused by shear forces, where rocks move past each other without much vertical movement