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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 Block Mountains, on the other hand, break up into chunks which either move up or down or end up getting stacked on one another. The mountains are characterized by a steep front side which is in contrast to the sloping back side. A notable example of Block Mountains is the Sierra Nevada, a block stretching 80 km wide and 650 km long.