Hanging Wall Geology Definition
Hanging Wall Geology Definition. The block below the fault plane or, in other words, beneath the fault plane is called the footwall. A mass of rock overhanging a fault plane.
The underside of the wall rock overlying a vein or bed of ore. Is that hangingwall is while footwall is (geology) the section of rock that extends below a diagonal fault line (the corresponding upper. The mass of rock overlying a mineral deposit in a mine.
Compare Footwall (Sense 1) 2.
A mass of rock overhanging a fault plane. A mass of rock overhanging a fault plane. Moves down in normal faulting, up in reverse faulting.
Meaning Of Hanging Wall For The Defined Word.
The block below the fault plane or, in other words, beneath the fault plane is called the footwall. Most material © 2005, 1997, 1991 by. Hanging valleys are typically formed when the main valley has been widened.
Hanging Valley [ Hăng ′Ĭng ] A Side Valley That Enters A Main Valley At An Elevation High Above The Main Valley Floor.
The mass of rock underlying a mineral deposit in a mine. Such a fault in which hanging wall has apparently moved down with respect to foot wall is classified as a normal fault. Noun [ edit] hanging wall ( plural hanging walls ) ( geology) the section of rock that extends above a diagonal fault line (the corresponding lower section being the footwall ).
Geologic Structures Influence The Shape Of The Landscape, Determine The Degree Of Landslide Hazard, Bring Old Rocks To The Surface, Bury Young Rocks, Trap Petroleum And Natural.
The section of rock that extends above a diagonal fault line. The overlying block of a fault having an inclined fault plane. A mass of rock overhanging a fault plane.
American Heritage® Dictionary Of The.
The underside of the wall rock overlying a vein or bed of ore.compare footwall (def. On a dipping fault, the side that is on top of the fault plane. The mass of rock overlying a mineral deposit in a mine.
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