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A thrust fault is a type of geological fault where the angle between the horizontal and the fault plane is small. It is also known as an overthrust fault.1

In geology, a fault is a fracture in the Earth's crust where rocks on opposite sides move relative to each other due to compressional or tensional forces. Thrust faults specifically result from horizontal compressional forces that shorten the Earth's crust. In this type of fault, the hanging wall (the block above the fault plane) moves up and over the footwall (the block below the fault plane). Thrust faults are a type of reverse fault with a dip less than 45 degrees and are commonly found in intensely deformed mountain ranges.2

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