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The answer would be upward
In a normal fault, the hanging wall moves down relative to the footwall due to tensional forces pulling the plates apart. This type of fault is associated with divergent plate boundaries or areas where the Earth's crust is being pulled apart.
This is called a reverse fault. It occurs when compressional forces cause the hanging wall to move up relative to the footwall along a steeply inclined fault plane. Reverse faults are commonly found in areas where tectonic plates are colliding or converging.
In a lateral fault, the hanging wall moves horizontally in relation to the footwall. This type of fault occurs when the blocks of rock on either side of the fault move horizontally past each other. The hanging wall moves in the direction of the fault line, while the footwall remains relatively stationary.
In a normal fault, the hanging wall moves down relative to the footwall due to tensional stress pulling the plates apart. This movement creates a dip in the fault plane, with the hanging wall located below the footwall. The divergent motion between the plates along the fault line leads to extension and crustal thinning in the region.
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.
The answer would be upward
thrust
In a normal fault, the hanging wall moves down relative to the footwall due to tensional forces pulling the plates apart. This type of fault is associated with divergent plate boundaries or areas where the Earth's crust is being pulled apart.
normal fault
This is called a reverse fault. It occurs when compressional forces cause the hanging wall to move up relative to the footwall along a steeply inclined fault plane. Reverse faults are commonly found in areas where tectonic plates are colliding or converging.
In a lateral fault, the hanging wall moves horizontally in relation to the footwall. This type of fault occurs when the blocks of rock on either side of the fault move horizontally past each other. The hanging wall moves in the direction of the fault line, while the footwall remains relatively stationary.
A normal fault results from tensional forces pulling rocks apart, causing the hanging wall to move downward relative to the footwall. A reverse fault is caused by compressional forces pushing rocks together, resulting in the hanging wall moving up relative to the footwall. A strike-slip fault is produced by horizontal shearing forces causing rocks to move horizontally past each other.
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.
In a normal fault, the hanging wall moves down relative to the footwall due to tensional stress pulling the plates apart. This movement creates a dip in the fault plane, with the hanging wall located below the footwall. The divergent motion between the plates along the fault line leads to extension and crustal thinning in the region.
A reverse fault is in a zone of compressional faulting, rocks in the hanging wall are pushed up relative to rocks in the footwall. A normal fault is in a zone of tensional faulting, rocks in the hanging wall drop down relative to those in a footwall forming a normal fault.
The San Andreas fault is a strike-slip fault, where two tectonic plates move horizontally past each other. It is not a reverse fault, where the hanging wall moves up relative to the footwall due to compression.