Final answer:
In a typical fault-block mountain, large blocks of crust are uplifted along normal faults due to compressional stresses, and thrust faulting plays a significant role in its formation.
Step-by-step explanation:
In a typical fault-block mountain, large blocks of crust are uplifted along normal faults. The major forces involved are compressional stresses. Thrust faulting plays an important part in its formation.
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