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Is a hanging wall the same as a footwall?

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.


What is the result When a hanging wall of a fault slips down with respect to the footwall?

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.


When the hanging wall of a fault slips down with respect to the footwall the result is a?

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.


What is the type of fault where a hanging wall block moves down relative to the footwall block?

The type of fault where the hanging wall block moves down relative to the footwall block is called a normal fault. This occurs due to extensional forces that pull the crust apart, causing the hanging wall to descend. Normal faults are commonly found in regions experiencing tectonic stretching, such as rift zones.


How does the hanging wall in a normal fault move in relation to a reverse 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.

Related Questions

When the hanging wall moves down relative to the footwall what is that called?

It is called a Normal Fault.


How does the rock move on a normal fault?

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.


How does a rock move on a normal fault?

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.


Is a hanging wall the same as a footwall?

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.


What type of motion is found along a reverse fault?

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In A Blank Fault The Hanging Wall Moves Up Relative To The 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.


What is the result When a hanging wall of a fault slips down with respect to the footwall?

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.


What happens along a fault?

the hanging wall moves down relative to the footwall


In normal fault what happens to the foot wall?

In a normal fault, the hanging wall moves down relative to the footwall. This results in the footwall being pushed up and becoming uplifted relative to the hanging wall.


When the hanging wall of a fault slips down with respect to the footwall the result is a?

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.


What the hanging wall of a fault slips down with respect to the footwall the result is a?

Normal Fault


When the hanging wall of a fault slips down with respect to the footwall the result is a?

A normal fault