In a reverse fault, compression (plates crashing together) causes the hanging wall to move up. In a normal fault, tension ( plates pulling apart) causes the footwall to push up.
Tension, a pulling force that causes the plates to move apart, can create a normal fault. The rocks above a normal fault move downward as the plates below the fault move upward.
There is a hanging wall and a foot wall and the hanging wall moves downward and
causes it to look like a hill, in a way.
There is a hanging wall and a foot wall and the hanging wall moves downward and causes it to look like a hill, in a way.
A geological fault in which the upper side appears to have been pushed upward by compression.
This is described as a normal fault.
Reverse Fault
epicenter.
valcano valcano valcano valcano
The footwall is the block that is below the fault. The hanging wall is the fault block that is above the fault.
This is described as a normal fault.
Hanging Wall
This is described as a normal fault.
hanging wall
This is described as a normal fault.
This kind of fault is called a normal fault and is usually a sign of crustal extension.
This is described as a normal fault.
Reverse Fault
This kind of fault is called a normal fault and is usually a sign of crustal extension.
Reverse Fault
probably because those are the definitions.
hanging wall