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Reverse faults form when the hanging wall moves up.
Hanging wall and footwall reverse fault. Reverse faults indicate compressive shortening of the crust. In a reverse fault the hanging wall right slides over the footwall left due to compressional forces. In a strike slip fault they slide past each other the foot wall and hanging wall are not there because it has. A n fault forms when the hanging wall moves down relative to the footwall a.
If you imagine undoing the motion of a reverse fault you will undo the compression and thus lengthen the horizontal distance between two points on either side of the fault. The dip of a reverse fault is relatively steep greater than 45. The forces creating reverse faults are compressional pushing the sides together. The hanging wall moves up and over the footwall.
A reverse fault is the opposite of a normal fault the hanging wall moves up relative to the footwall. If the hanging wall rises relative to the footwall you have a reverse fault. Mike dunning dorling kindersle getty images. Reverse faults occur in areas undergoing compression squishing.
A reverse fault is one in which the hanging wall block has moved up relative to the footwall block along an inclined fault in layered sedimentary rocks are evidence for horizontal compression and shortening. They are common at convergent boundaries. Thrust faults are reverse faults that dip less than 45. Thrust faults with a very low angle of dip read more.
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