Normal Fault Footwall Hanging Wall

The fault plane is where the action is.
Normal fault footwall hanging wall. If you imagine undoing the motion of a normal fault you will undo the stretching and thus shorten the horizontal distance between two points on either side of the fault. A reverse fault is the opposite of a normal fault the hanging wall moves up relative to the footwall. With compressional forces the hanging wall moves upward relative to the footwall. They bound many of the mountain ranges of the world and many of the rift valleys found along spreading margins.
The hanging wall slides down relative to the footwall. Other articles where normal fault is discussed. Normal faults occur in areas undergoing extension stretching. If the hanging wall drops relative to the footwall you have a normal fault.
Normal dip slip faults are produced by vertical compression as earth s crust lengthens. Edges of horsts and grabens. The dip of a reverse fault is relatively steep greater than 45. The term footwall is derived from miners finding mineral deposits where inactive faults have been filled in with mineral deposits at their feet.
It is a flat surface that may be vertical or sloping. Where the fault plane is sloping as with normal and reverse faults. Hanging wall down footwall up. Boundaries of metamorphic core complexes.
The main components of a fault are 1 the fault plane 2 the fault trace 3 the hanging wall and 4 the footwall. The motion between the two is not always smooth and sometimes the walls get caught on each other. Boundaries of metamorphic core complexes. This type of fault is referred to as a fault.
Normal fault with the fault blocks on the right dropping downward myrna martin footwalls and hanging walls. Zones of crustal extension. Reverse faults indicate compressive shortening of the crust. Low angle normal fault footwall gneiss hanging wall shallow crust rocks.
The line it makes on the earth s surface is the fault trace. Hanging wall down footwall up. Low angle normal fault footwall gneiss hanging wall shallow crust rocks. Normal faults are common.
Zones of crustal extension. Edges of horsts and grabens. A normal fault occurs when the hanging wall moves relative to the footwall. Hanging wall up footwall down.
In this picture of a normal fault the valley is the hanging wall and the mountain is the footwall. Basin and range region. Basin and range region.