Hanging Wall Fault Definition

In fault fault plane is called the hanging wall or headwall.

Hanging wall fault definition.

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. See more at fault. Zones of crustal extension. The block below is called the footwall.

Hanging wall deformation patterns differ signifi cantly when a basal plastic sheet imposes a con stant magnitude displacement distribution on the master normal fault. Low angle normal fault footwall gneiss hanging wall shallow crust rocks. Basin and range region. 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. It is a flat surface that may be vertical or sloping. Hanging wall and footwall. Published by houghton mifflin harcourt publishing company.

The block below the fault plane or in other words beneath the fault plane is called the footwall. Definition of 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. The dip of a fault plane is its angle of inclination measured from the horizontal.

A wall of prejudice. The fault strike is the direction of the line of intersection between the fault plane and earth s surface. The line it makes on the earth s surface is the fault trace. Hanging wall and footwall.

Hanging wall down footwall up. The upper or overhanging wall of an inclined vein fault or other geologic structure opposed to footwall. When working a tabular ore body the miner stood with the footwall under his feet and with the hanging wall above him. The upper block or in other words the block above the fault plane is called hanging wall.

This terminology comes from mining. The hanging wall occurs above the fault plane and the footwall occurs below it. Type of fault map symbol definition type of regional stress geologic associations. A wall of smoke.

The main components of a fault are 1 the fault plane 2 the fault trace 3 the hanging wall and 4 the footwall. The american heritage science dictionary copyright 2011. Edges of horsts and grabens. The two sides of a non vertical fault are known as the hanging wall and footwall.