Reverse Fault Hanging Wall And Footwall

This is a landform made from volcanism.

Reverse fault hanging wall and footwall.

Its also called a reverse fault because a normal fault has the foot wall going up and the hanging wall. These either merge into the detachment fault at depth or simply terminate at the detachment fault surface without shallowing. The line it makes on the earth s surface is the fault trace. The hanging wall composed of extended thinned and brittle crustal material can be cut by numerous normal faults.

This is the result of tension built up. The unloading of the footwall can lead to isostatic uplift and doming of the more ductile material beneath. In a non vertical fault where the fault plane dips the footwall is the section of the fault that lies under the fault while the hanging wall lies over the fault. The hanging wall will slide upwards right.

You probably noticed that the blocks that move on either side of a reverse or normal fault slide up or down along a dipping fault surface. Where the fault plane is sloping as with normal and reverse faults the upper side is the hanging wall and the lower side is the footwall. 2 1 volcanism is the process by which molten rock reaches the earth s surface in order to make new landforms. The main components of a fault are 1 the fault plane 2 the fault trace 3 the hanging wall and 4 the footwall.

The movement along the thrust fault is the foot wall goes down and the hanging wall goes up. Plutonism is the result of the magma as it has reached the earth s surface into pre existing rock. When the fault plane is vertical there is no hanging wall or footwall. It is a flat surface that may be vertical or sloping.

When movement along a fault is the reverse of what you would expect with normal gravity we call them reverse faults. The fault plane is where the action is. If we hold the foot wall stationary where would the hanging wall go if we reversed gravity.