In a reverse fault, the hanging wall moves upward relative to the footwall.
Further Explanation:
Fault: It is a fracture or rupture in the earth's outer layer. The faults are caused by the tectonic forces forming large boundaries between the plates. The faults are of following types:
• Strike-slip faults
• Dip-slip faults
• Oblique-slip faults
• Listric fault
• Ring fault
The dip-slip can be of two types normal or reverse fault. A non-vertical fault has two sides namely the footwall and hanging wall.When the hanging wall movement is in downward direction, with respect to the footwall is referred as normal fault but when the hanging wall movement is in upward direction, with respect to the footwall is referred as reverse fault. This movement results from compression and is commonly seen where the boundaries made of tectonic plate. The example of reverse fault is San Andreas Fault in California.
Learn more:
1. Learn more about layers of Earth
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Answer details:
Grade: High School
Subject: Geology
Chapter: Landforms
Keywords: In a reverse fault, where does the hanging wall move relative to the footwall, landforms, strike-slip faults, dip-slip faults, oblique-slip faults, listric fault, ring fault
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