Hanging Wall Up Footwall Down

Zones of crustal extension.

Hanging wall up footwall down. Hanging wall down footwall up. Hanging wall up footwall down. The crust experiences extension. Basin and range region.

In a normal fault the hanging wall moves downward relative to the footwall. In this fault the hanging wall moves down relative to the footwall. 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. 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.

The footwall moves down relative to the hanging wall. Then there is also a. Type of regional stress. In a strike slip fault they slide past each other the foot wall and hanging wall are not there because it has.

Combination of dip and strike slip focus and epicenter focus. Then there is also a reverse fault which happens at a convergent boundary. The hanging wall moves up relative to the footwall. It is caused by compression.

San andreas fault 3. Edges of horsts and grabens. But that is when the foot wall moves down the hanging wall moves up. Low angle normal faults with regional tectonic significance may be designated detachment faults.

Zones of crustal extension. Edges of horsts and grabens. Movement is left and right horizontal example. Hanging wall right side is at the bottom reverse.

Footwall left side is at the bottom 2. The hanging wall moves down relative to the footwall. Low angle normal fault footwall gneiss hanging wall shallow crust rocks. Directly above earth s.

Boundaries of metamorphic core complexes. The motion of the crustal blocks is referred to as strike slip. A downthrown block between two normal faults dipping towards each other is a graben. Hanging wall down footwall up.

In a reverse fault the hanging wall moves up and the footwall moves down.