The type of fault that occurs when the hanging wall moves up relative to the footwall is called a reverse fault. This movement is typically associated with compressional forces in the Earth's crust, often resulting from tectonic plate convergence. Reverse faults can also lead to the formation of mountain ranges and other geological features. A specific subtype of reverse fault is known as a thrust fault, where the angle of the fault plane is relatively low.
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.
No, a hanging wall and a footwall are not the same in geology. The hanging wall is the block of rock above a fault line that moves down relative to the footwall, which is the block of rock below the fault line that moves up.
That geological structure is called a normal fault, where the hanging wall moves down relative to the footwall. If the hanging wall slides up and over the footwall, it is known as a reverse fault.
The type of fault characterized by the hanging wall moving upward relative to the footwall is called a reverse fault. In a reverse fault, the movement occurs due to compressional forces, which push the rock masses together, causing the hanging wall to be thrust up over the footwall. This movement is opposite to that of a normal fault, where the hanging wall moves downward. Reverse faults are commonly associated with mountain-building processes and tectonic collisions.
The result is a normal fault, where the hanging wall moves down relative to the footwall due to extensional forces pulling the rock layers apart.
A normal fault.
Reverse Fault
In a normal fault, the hanging wall moves down relative to the footwall, whereas in a reverse fault, the hanging wall moves up relative to the footwall.
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.
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.
thrust
Reverse Fault
Thrust
Thrust
Yes, when the hanging wall moves up relative to the footwall along a fault, it is known as a reverse fault. Reverse faults are caused by compressional forces in the Earth's crust, leading to the hanging wall moving up and over the footwall.
The answer would be upward
A reverse fault is a fault in which the hanging wall moves up relative to the footwall.