a normal fault
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 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 reverse fault, the hanging wall moves up relative to the footwall due to compressional stress in the Earth's crust. Reverse faults are typically associated with convergent plate boundaries where tectonic forces push rocks together, causing them to thrust upwards.
normal fault
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
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.
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.
A normal fault is a product of tension so the hanging wall of the fault slides down the footwall. If you look into the fault plane, and it slopes from lower left to top right, the (over)hanging wall is on the left and you will see its younger rocks have slid down to meet older ones on the footwall opposite.
A normal fault is a product of tension so the hanging wall of the fault slides down the footwall. If you look into the fault plane, and it slopes from lower left to top right, the (over)hanging wall is on the left and you will see its younger rocks have slid down to meet older ones on the footwall opposite.
A reverse fault forms when a hanging wall moves upward due to compressional forces. This type of fault occurs in areas where the crust is being pushed together, causing the hanging wall to move up and the footwall to move down.
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 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.