Hanging Wall Down Geology

The block below is called the footwall.
Hanging wall down geology. Zones of crustal extension. Edges of horsts and grabens. When working a tabular ore body the miner stood with the footwall under his feet and with the hanging wall above him. Rift valleys are formed by the sliding of the hanging walls downward many thousands of metres where they then become the valley floors.
Low angle normal fault footwall gneiss hanging wall shallow crust rocks. The hanging wall slides down relative to the footwall. This terminology comes from mining. Normal faults are common.
ø such a fault in which hanging wall has apparently moved down with respect to footwall is classified as a normal fault. The fault strike is the direction of the line of intersection between the fault plane and earth s surface. Basin and range region. The dip of a fault plane is its angle of inclination measured from the horizontal.
Hanging wall down footwall up. A fault in which hanging wall has apparently gone up with respect to the footwall is termed as reverse fault. Boundaries of metamorphic core complexes. Hanging wall up footwall down.
A fault in which hanging wall hw has apparently come down with respect to the footwall fw is termed as normal fault. Fault plane is called the hanging wall or headwall. The hanging wall occurs above the fault plane and the footwall occurs below it. They bound many of the mountain ranges of the world and many of the rift valleys found along spreading margins of tectonic plates.