Recumbent fold: Revision history

Diff selection: Mark the radio buttons of the revisions to compare and hit enter or the button at the bottom.
Legend: (cur) = difference with latest revision, (prev) = difference with preceding revision, m = minor edit.

7 May 2024

  • curprev 19:5519:55, 7 May 2024Ai talk contribs 4,316 bytes +212 No edit summary
  • curprev 19:5419:54, 7 May 2024Ai talk contribs 4,104 bytes −9 No edit summary
  • curprev 19:4519:45, 7 May 2024Ai talk contribs 4,113 bytes +4,113 Created page with "== Introduction == A recumbent fold is a type of geological fold that is essentially horizontal. The term is used to describe a fold where the axial plane, or the plane that divides the fold as symmetrically as possible, is essentially horizontal. This type of fold is a result of intense compressional stresses that result in the deformation of rock layers. == Formation == Recumbent folds form due to intense compressional stresses in the Earth's crust...."