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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).
When two normal faults from parellel to each other a block of rock is left lying between them. As the hanging wall of each normal fault slips downward, the block in between moves upward forming a fault-block mountain.