a reverse fault
thrust
The movement of the Hanging wall in the normal fault downward with the gravity whereas in the Reverse fault the hanging wall moved upward against the gravity
A normal fault.
The hanging wall block slips downward along the thrust fault
In terms of Science it is the land mass above the fault.
a reverse fault
When a fault is not vertical, a hanging wall and footwall are formed. The hanging wall is the block of rock above the fault plane, while the footwall is the block of rock below the fault plane. These terms help geologists describe the displacement and movement along the fault.
thrust
No. With a fault there are two different blocks of rock moving against one another. If the fault is not vertical then the block on top is the hanging wall and the block on the bottom is the footwall.
Yes! The HANGING WALL is usually associated with / occurs on, the upper face of a near-vertical fault. It is evidenced when a mineral vein which follows a fault has been worked out and then can produce a danger of fall where the rock is fractured
In a non-vertical fault (where the fault plane dips), the footwall is the section of the fault that lies under the fault, while the hanging wall lies over the fault.The names come about from the mining industry because important ore minerals were commonly deposited along fault planes. In a mine along a fault, the miner would be standing on the block lower block and hanging his lantern from the upper block (hence, foot wall and hanging wall).In perfectly vertical faults, you cannot designate a footwall or a hanging wall.
its when a hotdog becomes mush when it gets eaten
Hanging Wall
In a normal fault, the hanging wall moves downward relative to the footwall, creating extensional forces. In a reverse fault, the hanging wall moves upward relative to the footwall, generating compressional forces.
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.
When the hanging wall of a fault slips downward relative to the footwall, the result is a normal fault. This type of fault typically occurs in extensional tectonic settings, where the Earth's crust is being pulled apart. Normal faults are characterized by a vertical displacement, causing the hanging wall to move downwards, which can lead to the formation of rift valleys or basins.
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