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Bone growth of the epiphysis occurs at the
Normal Fault
A type of fault where the hanging wall slides downward relative to the footwall due to tensional forces.
Strike And Dip
Geological terms used to describe the orientation of rock layers, with strike indicating the direction of the layer's horizontal angle and dip indicating its vertical angle.
Horst And Graben
Geological features formed by the movement of the earth's crust, with a horst being a raised fault block and a graben being a lowered block, creating distinctive landscapes.
Footwall
The wall rock beneath an inclined fault.
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