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The typical prokaryotic flagellum features
Joints
Natural fractures or separations in rocks without displacement, often resulting from the rock's response to stress.
Folds
Structures formed by the bending and warping of rocks under pressure during geological processes, often seen in mountain ranges.
Joints
Natural fractures or separations in rocks without displacement, often formed by stresses such as contraction, expansion, or tectonic activities.
Faults
Fractures in the Earth's crust along which there has been significant displacement as a result of rock-mass movement.
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