In structural geology, a fold is a stack of originally planar surfaces, such as sedimentary strata, that are bent or curved during permanent deformation. A fault is a fracture in rock where there has been movement and displacement.
In structural geology, a fold is a stack of originally planar surfaces, such as sedimentary strata, that are bent or curved during permanent deformation. A fault is a fracture in rock where there has been movement and displacement.