Wiki User
∙ 12y agoA normal fault
Wiki User
∙ 12y agoThe result is a normal fault, where the hanging wall moves down relative to the footwall due to extensional forces pulling the rock layers apart.
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.
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.
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.
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.
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.
A normal fault
Normal Fault
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.
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.
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.
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.
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.
thrust
A strike-slip fault does not have a hanging wall or footwall because the movement is primarily horizontal, with the two sides sliding past each other horizontally.
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
No, a thrust fault is a type of reverse fault, where the hanging wall moves up and over the footwall. In contrast, a normal fault is a type of fault where the hanging wall moves down relative to the footwall.