Retrieving "Folds" from the archives

Cross-reference notes under review

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1. Geological Strata

   Linked via "folds"

   Principle of Original Horizontality
   Sediments are generally deposited in horizontal layers parallel to the Earth’s surface, dictated by the initial gravitational settling relative to the geoid. Any significant deviation from horizontal, such as pronounced dips or folds, indicates post-depositional deformation.
   Principle of Lateral Continuity