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The appearance of a fault typically features a visible fracture or displacement in the Earth's crust, often characterized by a linear or zigzag pattern. The surrounding rock may show signs of stress, such as fault breccia or slickensides, where surfaces have been ground smooth. Additionally, there may be vertical or horizontal offsets in geological layers, creating a clear distinction between adjacent rock formations. In some cases, the fault line may be marked by vegetation changes or surface features like fissures or cracks.

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4mo ago

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