Hanging Wall Up Footwall Down

As rehemat explained in the reverse fault the hanging wall will move up with respect to the footwall and in a normal fault the hanging wall will move down with respect to the footwall.

Hanging wall up footwall down.

Zones of crustal extension. In a reverse fault the hanging wall moves up and the footwall moves down. Where the displacement of the plates takes place aka hypocenter epicenter. In a normal fault the hanging wall moves downward relative to the footwall.

Low angle normal fault footwall gneiss hanging wall shallow crust rocks. Low angle normal faults with regional tectonic significance may be designated detachment faults. Note that a vertical fault with one block moving up is neither a reverse or normal fault as there is no hanging wall or footwall. Hanging wall down footwall up.

Movement is up and down vertical normal. Combination of dip and strike slip focus and epicenter focus. Directly above earth s. In this fault the hanging wall moves down relative to the footwall.

Movement is left and right horizontal example. Edges of horsts and grabens. But that is when the foot wall moves down the hanging wall moves up. A downthrown block between two normal faults dipping towards each other is a graben.

Zones of crustal extension. The crust experiences extension. Edges of horsts and grabens. Then there is also a.

Hanging wall right side is at the bottom reverse. The footwall moves down relative to the hanging wall. Boundaries of metamorphic core complexes. The hanging wall moves down relative to the footwall.

The motion of the crustal blocks is referred to as strike slip. San andreas fault 3. Then there is also a reverse fault which happens at a convergent boundary. Hanging wall up footwall down.

An upthrown block between two normal faults dipping away from each other is a horst. It is caused by compression. In a strike slip fault they slide past each other the foot wall and hanging wall are not there because it has. Basin and range region.

Type of regional stress.