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In a normal fault the hanging wall moves downward. With this type of fault, the hanging wall also shifts horizontally away from the fault line.
Reverse Fault
A fault zone is created when directed stress (as opposed to isotropic stress that simply compacts materials) overcomes the physical strength of the rock to withstand pressure leading to a pervasive crack. If the stress that created the fault is pulling the rock apart, the block that lies above the fault (the hanging wall) is bound to sink and the rocks below the fault will move upwards relative to the hanging wall. This situation is termed a "normal fault" and occurs for example in rift zones all over the world. If confining pressure produces a fault, the hanging wall is pushed on top of the rocks below the fault. This is known as a "reverse fault" and is a common phenomenon in many mountain ranges. In a special type of stress regime, faults are created along which rocks are sliding past each other horizontally. They are called "transform faults".
I believe it is called a fault, like the San Andreas fault in California.
Normal fault. The fault itself does not cause the sinking but is part or an effectof the process. The sunken block between two faults is called a "graben".
In a normal fault the hanging wall moves downward. With this type of fault, the hanging wall also shifts horizontally away from the fault line.
transform
Reverse Fault
the upper wall of an inclined fault
its when the hanging and foot wall push together and the hanging wall goes upward a normal fault is the other way around when the walls are pulled apart and the hanging wall goes down Reverse-Convergent Normal- Divergent
A fault zone is created when directed stress (as opposed to isotropic stress that simply compacts materials) overcomes the physical strength of the rock to withstand pressure leading to a pervasive crack. If the stress that created the fault is pulling the rock apart, the block that lies above the fault (the hanging wall) is bound to sink and the rocks below the fault will move upwards relative to the hanging wall. This situation is termed a "normal fault" and occurs for example in rift zones all over the world. If confining pressure produces a fault, the hanging wall is pushed on top of the rocks below the fault. This is known as a "reverse fault" and is a common phenomenon in many mountain ranges. In a special type of stress regime, faults are created along which rocks are sliding past each other horizontally. They are called "transform faults".
goodluck.
A blind thrust fault is a geological term for a type of thrust fault which does not appear on the surface - where a hanging wall makes an angle with the horizontal of less than 45 degrees, but is hidden from view.
If a fault occurs in an area where rock layers have been folded, the type of fault it is likely to be is thrust faulting. This type of fault will have the ground on one side of the fault, move up and over adjacent ground.
Normal faults
This is a strike-slip fault.
This is a strike-slip fault.