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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).
Often fault-block mountains have a steep front side and a sloping back side. Examples of fault-block mountains include: the Sierra Nevada mountains in North America; the Harz Mountains in Germany ; Dome Mountains. Dome mountains are the result of a great amount of melted rock (magma) pushing its way up under the earth crust.