In terms of Earth Science it is the land mass below the fault.
The word footwall is a term which is used in Geology. It is the piece of rock that is under a mineral deposit.
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.
Astrike-slip fault it when the hanging wall and the footwall slide past each other.
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 two main types of faulting are normal faulting, where the hanging wall moves down relative to the footwall, and reverse faulting, where the hanging wall moves up relative to the footwall.
The answer would be upward
The footwall
No
The hanging wall is the upper block in a fault where movement has occurred, while the footwall is the lower block that has not moved. The hanging wall moves over the footwall in response to stress within the Earth's crust.
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.
footwall
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.
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.
Astrike-slip fault it when the hanging wall and the footwall slide past each other.
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.
normal fault
Thrust
When the hanging wall of a fault slips down with respect to the footwall, it results in a normal fault. This type of faulting is associated with extensional tectonic forces, where the hanging wall moves downward in relation to the footwall, creating space between the two blocks.