Reverse fault occur in which the hanging wall block moves up relative to the footwall block.
The hanging wall has moved higher in relation to the footwall during a reverse or thrust fault. A reversal fault differs from a thrust fault in that it has a steeper dip—one that is greater than 30 degrees. Sectors of the crust that experience compression give rise to reverse and thrust faults. In this sense, a convergent plate boundary is a region with significant thrust and reverse faults. As a result, subduction zones are also referred to as mega-thrust faults.
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