A geologic fault which the hanging wall has moved downward relative to the footwall is called normal fault.
A crack or cluster of cracks separating two rock blocks is referred to as a fault. Due to problems, the block could move in relation to one another. Faults can range in length from a few millimeters to thousands of kilometers. The majority of faults result in repeated displacements over geologic time. During an earthquake, the rock on one side of the fault quickly shifts in proportion to the other. The fault surface could be at any arbitrary angle or could be vertical or horizontal. - a dip-slip fault in which the block above the fault has moved downward in proportion to the block below. The Basin and Range Province of the Western United States as well as along oceanic ridge typically exhibit this type of faulting, which is caused by extension.
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