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This is true of normal faults. In thrust or reverse faults, the hanging wall moves up relative to the footwall and in strike slip faults, it moves horizontally relative to the footwall.
In a non-vertical fault (where the fault plane dips), the footwall is the section of the fault that lies under the fault, while the hanging wall lies over the fault.The names come about from the mining industry because important ore minerals were commonly deposited along fault planes. In a mine along a fault, the miner would be standing on the block lower block and hanging his lantern from the upper block (hence, foot wall and hanging wall).In perfectly vertical faults, you cannot designate a footwall or a hanging wall.
Reverse and thrust faults are both under compressive stress.
In geology, a fault or fault line is a planar fracture in rock in which the rock on one side of the fracture has moved with respect to the rock on the other side. Large faults within the Earth's crust are the result of differential or shear motion and active fault zones are the causal locations of most earthquakes. Earthquakes are caused by energy release during rapid slippage along a fault. A fault that runs along the boundary between two tectonic plates is called a transform fault.Since faults do not usually consist of a single, clean fracture, the term fault zone is used when referring to the zone of complex deformation that is associated with the fault plane. The two sides of a non-vertical fault are called the hanging wall and footwall. By definition, the hanging wall occurs above the fault and the footwall occurs below the fault. This terminology comes from mining. When working a tabular ore body the miner stood with the footwall under his feet and with the hanging wall hanging above him.
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Fault-block mountains
Normal faults are when you have hanging walls that slide down relative to and below the footwall. Dip-slip faults are normal faults.
Reverse faulting is found in the Himalayas. With a reverse fault, the hanging wall moves up relative to the footwall.
This is true of normal faults. In thrust or reverse faults, the hanging wall moves up relative to the footwall and in strike slip faults, it moves horizontally relative to the footwall.
A reverse fault is a fault in which the hanging wall moves up relative to the footwall.
Normal faults are when you have hanging walls that slide down relative to and below the footwall. Dip-slip faults are normal faults.
In a non-vertical fault (where the fault plane dips), the footwall is the section of the fault that lies under the fault, while the hanging wall lies over the fault.The names come about from the mining industry because important ore minerals were commonly deposited along fault planes. In a mine along a fault, the miner would be standing on the block lower block and hanging his lantern from the upper block (hence, foot wall and hanging wall).In perfectly vertical faults, you cannot designate a footwall or a hanging wall.
Normal faults have a hanging wall and footwall Normal Faults are common at mid-ocean ridges Normal Faults occur where the crust is being pulled apart at the divergent plate boudary. Sorry i only have 3 facts, but I anyone with the question
The two types of faults that can result in mountains are reverse faults and normal faults.
In a normal fault, the fault is at an angle, so one block of rock lies above the fault while the other lies below it. The rock above it is the hanging wall and the rock below it is the footwall. In a normal fault, the hanging wall moves downwards relative to the footwall.
Reverse and thrust faults are both under compressive stress.
-Normal Faults form when the hanging wall moves down. -Reverse Faults form when the hanging wall moves up. -Strike-Slip Faults have walls that moce sideways, instead of up or down.