a normal fault
parallel normal faults.
The hanging wall is the block of rock located above the fault plane. It moves downward in a normal fault and upward in a reverse fault during faulting events. It is named "hanging" because in underground mining, it appears to hang over the miners' heads.
This is described as a normal 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.
In a normal fault the hanging wall moves downward. With this type of fault, the hanging wall also shifts horizontally away from the fault line.
This kind of fault is called a normal fault and is usually a sign of crustal extension.
A normal fault occurs when rock is pulled apart, causing one block of rock to move downward relative to the other. This displacement is due to tensional forces acting on the earth's crust, causing the hanging wall to drop relative to the footwall along the fault plane.
A normal fault occurs when a portion of rock moves downward relative to the other in place. This type of fault is caused by tensional forces pulling the rock mass apart, resulting in the hanging wall moving down relative to the footwall.
It moves downward.. the force behind it is tension
reverse
parallel normal faults.
parallel normal faults.
A block of rock below the plane of a fault is known as the hanging wall. It is the rock mass that is located above the fault plane and typically moves downward relative to the footwall during fault movement.
That type of fault is known as Synclinal fault.
Seismic waves are released when rock moves along a fault. These waves are the ones that cause earthquakes.
The hanging wall is the block of rock located above the fault plane. It moves downward in a normal fault and upward in a reverse fault during faulting events. It is named "hanging" because in underground mining, it appears to hang over the miners' heads.
This is described as a normal fault.