Rock Deformation: Folds, Faults, and Crustal Structures
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Geological Deformation of Earth's Crust
The Earth's crust undergoes various types of deformation due to tectonic forces. These deformations can be categorized based on how the material responds to stress:
- Plastic Deformation: Undergoes permanent change, resulting in Folds.
- Elastic Deformation: Undergoes temporary change, returning to its original shape once stress is removed. No permanent deformation occurs.
- Brittle Deformation: Undergoes fracture, resulting in Faults and Joints.
Geological Folds: Structure and Classification
Folds are bends in rock strata or other planar structures, typically resulting from compressional forces.
Parts of a Fold
- Flank:
- Each of the areas that form the fold, extending outwards from the hinge.
- Hinge:
- The line joining the