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  2. Fold (geology) - Wikipedia

    en.wikipedia.org/wiki/Fold_(geology)

    In structural geology, a fold is a stack of originally planar surfaces, such as sedimentary strata, ... Ramsay classification scheme for folds Class Curvature C

  3. Folk classification - Wikipedia

    en.wikipedia.org/wiki/Folk_classification

    Folk's carbonate rock classification details the relative proportions of allochems in the rock and the type of matrix. The classification scheme covers most common carbonate rocks, however the more inclusive although less precise alternative, Dunham classification, may be preferred in some instances. Folk classification consists of one or two ...

  4. Chevron (geology) - Wikipedia

    en.wikipedia.org/wiki/Chevron_(geology)

    Chevron folds with flat-lying axial planes, Millook Haven, North Cornwall, UK. Chevron folds are a structural feature characterized by repeated well behaved folded beds with straight limbs and sharp hinges. Well developed, these folds develop repeated set of v-shaped beds. [1] They develop in response to regional or local compressive stress.

  5. Vergence (geology) - Wikipedia

    en.wikipedia.org/wiki/Vergence_(geology)

    To better understand the importance of this use, it is important to understand the different classifications of folds, based on their geometry. The most commonly used terms to describe and classify folds, based on their geometry, are the terms antiforms and synforms, as well as anticlines and synclines. Although these terms sound similar, they ...

  6. Structural geology - Wikipedia

    en.wikipedia.org/wiki/Structural_geology

    If there are folds, these are numbered as F 1, F 2, etc. Generally the axial plane foliation or cleavage of a fold is created during folding, and the number convention should match. For example, an F 2 fold should have an S 2 axial foliation. Deformations are numbered according to their order of formation with the letter D denoting a ...

  7. Mountain formation - Wikipedia

    en.wikipedia.org/wiki/Mountain_formation

    Illustration of mountains that developed on a fold that thrusted. Mountain formation occurs due to a variety of geological processes associated with large-scale movements of the Earth's crust (tectonic plates). [1] Folding, faulting, volcanic activity, igneous intrusion and metamorphism can all be parts of the orogenic process of mountain ...

  8. 3D fold evolution - Wikipedia

    en.wikipedia.org/wiki/3D_Fold_Evolution

    In geology, 3D fold evolution is the study of the full three dimensional structure of a fold as it changes in time. A fold is a common three-dimensional geological structure that is associated with strain deformation under stress .

  9. Geologic map - Wikipedia

    en.wikipedia.org/wiki/Geologic_map

    A geologic map or geological map is a special-purpose map made to show various geological features. Rock units or geologic strata are shown by color or symbols. Bedding planes and structural features such as faults , folds , are shown with strike and dip or trend and plunge symbols which give three-dimensional orientations features.