When the fault plane is vertical there is no hanging wall or footwall.
Hanging wall and footwall geology.
When working a tabular ore body the miner stood with the footwall under his feet and with the hanging wall above him.
The fault strike is the direction of the line of intersection between the fault plane and earth s surface.
The leo pargil shear zone defines the west flank of the dome and separates the footwall rocks of the dome from the haimanta group and the overlying metasedimentary rocks in the hanging wall to the west thiede et al 2006.
Hintersberger et al 2010 in press.
Hanging wall definition the underside of the wall rock overlying a vein or bed of ore.
The hanging wall moves up and over the footwall.
Any fault plane can be completely described with two measurements.
This terminology comes from mining.
Draw a normal and reverse fault label the hanging wall and footwall for each also show how they move for each fault.
The block below is called the footwall.
In fault fault plane is called the hanging wall or headwall.
Block below is called the footwall.
Hanging wall and footwall the two sides of a non vertical fault are known as the hanging wall and footwall.
Footwall synonyms footwall pronunciation footwall translation english dictionary definition of footwall.
The mass of rock underlying a mineral deposit in a mine.
Foot wall fo ot wôl the block of rock lying under an inclined fault.
The dip of a fault plane is its angle of inclination measured from the horizontal.
Thrust faults are reverse faults that dip less than 45.
Metamorphism melting and exhumation of the leo pargil dome nw india.
The fault separates hanging wall serpentinite from the footwall.
The dip of a fault plane is its angle of inclination measured from the horizontal.
The fault strike is the direction of the line of intersection between the fault plane and earth s surface.
Thrust faults with a very low angle of dip and a very large total displacement are called overthrusts or detachments.
Its strike and its dip.
These are often found in intensely deformed mountain belts.