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Movement: Lateral - blocks of crust slide past each other horizontally. Associated stress: Shear.

Movement: Combination of vertical and horizontal - showing features of both strike-slip and dip-slip. Associated stress: Shear and either tensional or compressional.

Movement: Similar to reverse faults but with a lower angle - the hanging wall moves up over the footwall. Associated stress: Compressional.

Movement: Divergent - hanging wall moves downward while sedimentary layers continue to deposit on the footwall. Associated stress: Tensional.

Movement: Divergent - the hanging wall moves downward relative to the footwall. Associated stress: Tensional.

Movement: Lateral - when facing across the fault line, the other side moves to the right. Associated stress: Shear.

Movement: Convergent - the hanging wall moves upward relative to the footwall. Associated stress: Compressional.