Fault The Hanging Wall Moves Downward Relative To The Footwall

The hanging wall moves up relative to the foot wall. In dip slip faults if the hanging wall block moves downward relative to the footwall read more. A downthrown block between two normal faults dipping towards each other is a graben.

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Fault Types

It is caused by tension.

Fault the hanging wall moves downward relative to the footwall.

There is a normal fault which happens at a divergent boundary. Formed by compressional stress rocks are pushed towards each other thrust fault. These usually occur when tectonic forces cause tension that pulls rocks apart. The hanging wall moves down relative to the foot wall.

Low angle normal faults with regional tectonic significance may be designated detachment faults. To the dip is called dip slip faulting. In this fault the hanging wall moves down relative to the footwall. It is caused by tension.

An upthrown block between two normal faults dipping away from each other is a horst. There is a normal fault which happens at a divergent boundary. In a normal fault the hanging wall moves downward relative to the footwall. Strike slip faults are right lateral or left lateral depending on whether the block on the opposite side of the fault from an observer has moved to the right or left.

Special type of reverse fault that is nearly horizontal angle has less than 45 degrees strike slip fault. When the hanging wall moves down in relative to the footwall it is called a fault. When the hanging wall moves up in relative to the footwall it is called a fault. In this fault the hanging wall moves down relative to the footwall.