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Normal faults are characterized by the hanging wall moving down relative to the footwall, while reverse faults are characterized by the hanging wall moving up relative to the footwall. Both faults are caused by compressional forces in the Earth's crust, but their movements are opposite in direction.
The three major types of faults are normal faults, reverse faults, and strike-slip faults. Synclines are not faults but rather geological structures that describe the folding of rock layers.
Normal faults occur when the hanging wall moves down relative to the footwall due to extensional forces, while reverse faults occur when the hanging wall moves up relative to the footwall due to compressional forces. Normal faults are associated with divergent plate boundaries, while reverse faults are associated with convergent plate boundaries.
Thrust faults and reverse faults are essentially the same, the only difference being the angle: thrust faults have a shallow angle of 45 degrees or less from horizontal. Reverse (thrust) faults and folds usually indicate rock being compressed. In many cases folds develop along reverse faults as one fault block is dragged along another, with an anticline forming in the hanging wall.
The three main types of fault lines are normal faults, reverse faults, and strike-slip faults. Normal faults occur when rocks are pulled apart, reverse faults form when rocks are pushed together, and strike-slip faults happen when rocks slide past each other horizontally.
The main direction of the stress on blocks of rock at normal faults, reverse faults and the strike slip faults usually happens at the weak areas.
Normal faults are characterized by the hanging wall moving down relative to the footwall, while reverse faults are characterized by the hanging wall moving up relative to the footwall. Both faults are caused by compressional forces in the Earth's crust, but their movements are opposite in direction.
reverse fault
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The three main types of faults are normal faults, reverse (or thrust) faults, and strike-slip faults. Normal faults occur when the crust is extended, causing one block of rock to move downward relative to another. Reverse faults happen when the crust is compressed, pushing one block up over another. Strike-slip faults involve horizontal movement, where two blocks slide past each other laterally.
reverse faults move from compression when the hanging wall moves up
compression
The three major types of faults are normal faults, reverse faults, and strike-slip faults. Synclines are not faults but rather geological structures that describe the folding of rock layers.
An uplifted block bounded by two reverse faults is known as a horst. It is a raised area of land between two parallel faults where the central block has moved upward relative to the blocks on either side. Horsts are common features in regions where tectonic forces cause the Earth's crust to compress and deform.
the best answer is reverse boundary
-Normal Faults form when the hanging wall moves down. -Reverse Faults form when the hanging wall moves up. -Strike-Slip Faults have walls that moce sideways, instead of up or down.
Reverse failts are caused by compression. Normal faults however are formed by tension.