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Subduction zones
Transform boundaries
Spreading centers
Continent-continent convergence
Normal faults
Reverse faults
Crustal thickening
Thrust faults
Subduction zones
Transform faults
Terrain boundaries
Divergent boundaries
Two units experiencing compression breaks easily
The two units undergoing compression will collide
When two units undergoes compression, it will just slide past each other along the plane of contact
When two units collide, the one who is closer to the contact will experience more compressive stress
Earthquake can happen because of fault
Faults are evidences of ductile deformation in rocks
Faults are fractures in rocks with no observable movement
The process of mountain building is associated with faults
The Sun's gravity
Gravity slap pull
Convection currents
Movement of the plates
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