Hanging Wall Fault Definition

When working a tabular ore body the miner stood with the footwall under his feet and with the hanging wall above him.

Hanging wall fault definition.

The dip of a fault plane is its angle of inclination measured from the horizontal. It is a flat surface that may be vertical or sloping. Edges of horsts and grabens. Structural analysis indicates the presence of down to basin footwall and hanging wall faults associated with rollover anticlines and horst block back to back fault.

The block below the fault plane or in other words beneath the fault plane is called the footwall. Hanging wall down footwall up. The american heritage science dictionary copyright 2011. The fault strike is the direction of the line of intersection between the fault plane and earth s surface.

A wall of smoke. The hanging wall occurs above the fault plane and the footwall occurs below it. The block of rock lying above an inclined geologic fault plane. Definition of hanging wall.

Basin and range region. The fault plane is where the action is. Published by houghton mifflin harcourt publishing company. Hanging wall and footwall.

Type of fault map symbol definition type of regional stress geologic associations. A wall of prejudice. The upper block or in other words the block above the fault plane is called hanging wall. Hanging wall the upper wall of an inclined fault inclined fault a geological fault in which one side is above the other wall anything that suggests a wall in structure or function or effect.

In fault fault plane is called the hanging wall or headwall. This terminology comes from mining. Hanging wall and footwall. The main components of a fault are 1 the fault plane 2 the fault trace 3 the hanging wall and 4 the footwall.

In models without a plastic sheet numerous secondary normal faults form in the hanging wall of the master normal fault. Negotiations ran into a brick wall. The block below is called the footwall. The line it makes on the earth s surface is the fault trace.

See more at fault. The upper or overhanging wall of an inclined vein fault or other geologic structure opposed to footwall. Zones of crustal extension. Low angle normal fault footwall gneiss hanging wall shallow crust rocks.