Hanging Wall Down Geology

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