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1 Fault-block mountains-Fault-block mountains are formed along faults where some large blocks of rock are forced upwards while others are forced down. 2  The higher area is sometimes called a horst and the lower a graben (see the picture below).
The fault block above the fault is the hanging wall. The fault block below the fault is the footwall. Normal faults: the hanging wall moves down relative to the other side of the fault, while the footwall moves up relative to the other side of the fault. Rule of. thumb â puts younger rocks against older rocks.