Hanging Wall Up Footwall Down

Then there is also a.

Hanging wall up footwall down.

Directly above earth s. Hanging wall up footwall down. Low angle normal faults with regional tectonic significance may be designated detachment faults. The hanging wall moves down relative to the footwall.

In a normal fault the hanging wall moves downward relative to the footwall. Basin and range region. It is caused by compression. San andreas fault 3.

But that is when the foot wall moves down the hanging wall moves up. 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. In a reverse fault the hanging wall moves up and the footwall moves down. Hanging wall right side is at the bottom reverse.

Combination of dip and strike slip focus and epicenter focus. Movement is left and right horizontal example. 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. An upthrown block between two normal faults dipping away from each other is a horst.

Boundaries of metamorphic core complexes. Edges of horsts and grabens. Movement is up and down vertical normal. The hanging wall moves up relative to the footwall.

A downthrown block between two normal faults dipping towards each other is a graben. Low angle normal fault footwall gneiss hanging wall shallow crust rocks. Zones of crustal extension. Edges of horsts and grabens.

Hanging wall down footwall up. In a strike slip fault they slide past each other the foot wall and hanging wall are not there because it has. Type of regional stress. Footwall left side is at the bottom 2.

The footwall moves down relative to the hanging wall. The motion of the crustal blocks is referred to as strike slip. Then there is also a reverse fault which happens at a convergent boundary. The crust experiences extension.

Hanging wall down footwall up.