Answer
The formation of fault-block mountains differs from the processes that generate most other major mountain belts, such as fold mountains like the Himalayas or volcanic mountains like the Andes. In fault-block mountains, the uplift and topography are primarily a result of vertical movements along faults, leading to the creation of elongated mountain ranges with steep slopes. On the other hand, most other major mountain belts are formed through complex tectonic interactions, including compressional forces, crustal folding, and volcanic activity.
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