Hanging Wall Up Footwall Down

The hanging wall moves down relative to the footwall.

Hanging wall up footwall down.

The hanging wall moves up relative to the footwall. 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. Zones of crustal extension. The crust experiences extension.

Combination of dip and strike slip focus and epicenter focus. Then there is also a reverse fault which happens at a convergent boundary. Hanging wall right side is at the bottom reverse. 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.

Low angle normal faults with regional tectonic significance may be designated detachment faults. In a reverse fault the hanging wall moves up and the footwall moves down. Hanging wall up footwall down. A downthrown block between two normal faults dipping towards each other is a graben.

San andreas fault 3. Low angle normal fault footwall gneiss hanging wall shallow crust rocks. Edges of horsts and grabens. Boundaries of metamorphic core complexes.

In a strike slip fault they slide past each other the foot wall and hanging wall are not there because it has. Movement is left and right horizontal example. Hanging wall down footwall up. Movement is up and down vertical normal.

Type of regional stress. Basin and range region. In a normal fault the hanging wall moves downward relative to the footwall. Where the displacement of the plates takes place aka hypocenter epicenter.

The footwall moves down relative to the hanging wall. The motion of the crustal blocks is referred to as strike slip. Zones of crustal extension. Footwall left side is at the bottom 2.

An upthrown block between two normal faults dipping away from each other is a horst. Directly above earth s. Hanging wall down footwall up. But that is when the foot wall moves down the hanging wall moves up.

It is caused by compression.