hanging wall
Quick Summary
In geology, the hanging wall refers to the upper or overhanging wall of an inclined vein, fault, or other geologic structure. It is the block of rock that lies above an inclined fault plane. This is in contrast to the footwall, which is the block of rock below the fault plane. The hanging wall is also referred to as the hanging side. When rocks slip past each other along a fault, the hanging wall moves relative to the footwall. In normal dip-slip faults, the hanging wall slides down relative to the footwall, often occurring as Earth's crust lengthens.123
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