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Radda [10]
3 years ago
14

In a reverse fault, where does the hanging wall move relative to the footwall?

Geography
2 answers:
goldfiish [28.3K]3 years ago
7 0

The answer is;

The hanging wall rises above the footwall. This type of fault occurs due to compression tectonic movement that squishes the two crusts. This way the faulted section of rock shortens. This is the opposite of normal faults where the hanging wall falls below the footwall. This is due to extension tectonic movements that lengthen the faulted section.


monitta3 years ago
4 0

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

   brainly.com/question/1593688

2. Learn more about the earthquake

   brainly.com/question/1176195

3. Learn more about climate zones

  brainly.com/question/1600388

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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1. One side of the continents usually has a subduction zone, while the other side doesn't.

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It can be easily noticeable that some continents have high geological activity on one side, while they are much calmer on the opposite side. This is because of the different types of plate boundaries. Very often, one side of the continents has a subduction zone nearby, thus it is very active geologically. The other, opposite side, usually has another type of plate boundary, or the boundary is far away, making that side of the continent much less active.

  • The subduction zones are places where one plate moves below another plate.
  • The result of a subduction zone is intense volcanic activity and earthquakes.
  • The absence of plate boundary near a continent's edge results in geologically stable area.

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Explanation:

The majority of large plates on Earth's surface are continental tectonic plates. They are all different from each other though, be it in their size, their composition, the interaction with the other plates, the percentage of continental and oceanic crust they have etc. All continental plates have oceanic crust, thus their boundaries are strictly defined by the land mass. Some of continental plates have one boundary being further away in the ocean, while the other one actually to be roughly corresponding with the land mass.

  • The North American plate is an example where one side of the plate has its boundary along the edge of the land mass, while the other one is further away in the ocean.
  • The western boundary of the North American plate is with the Juan de Fuca and the Pacific plates, where there is subduction zones, and the boundary is roughly the same as the coastline.
  • The eastern boundary is with the Eurasian and slightly with the African plate. It is a divergent boundary, found in the middle of the Atlantic Ocean.

(b) The west coast of Africa is geologically relatively calm, while the west coast of South America is geologically very active.

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  • The subduction zone and the intense geological activity along the west coast of South America contribute to lot of earthquakes, which can easily be seen by Chile's earthquake record.

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