Hanging Wall Up Footwall Down

Edges of horsts and grabens.

Hanging wall up footwall down.

Directly above earth s. But that is when the foot wall moves down the hanging wall moves up. The footwall moves down relative to the hanging wall. 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.

It is caused by compression. Basin and range region. Zones of crustal extension. In this fault the hanging wall moves down relative to the footwall.

The crust experiences extension. The motion of the crustal blocks is referred to as strike slip. Movement is up and down vertical normal. In a strike slip fault they slide past each other the foot wall and hanging wall are not there because it has.

Hanging wall down footwall up. Movement is left and right horizontal example. Type of regional stress. Footwall left side is at the bottom 2.

Where the displacement of the plates takes place aka hypocenter epicenter. 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. Edges of horsts and grabens. The hanging wall moves down relative to the footwall.

Combination of dip and strike slip focus and epicenter focus. Low angle normal faults with regional tectonic significance may be designated detachment faults. A downthrown block between two normal faults dipping towards each other is a graben. Then there is also a reverse fault which happens at a convergent boundary.

In a reverse fault the hanging wall moves up and the footwall moves down. Boundaries of metamorphic core complexes. The hanging wall moves up relative to the footwall. Then there is also a.

Hanging wall up footwall down. Zones of crustal extension. Hanging wall right side is at the bottom reverse. In a normal fault the hanging wall moves downward relative to the footwall.

An upthrown block between two normal faults dipping away from each other is a horst.