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  2. Anticline - Wikipedia

    en.wikipedia.org/wiki/Anticline

    If the angle between the limbs is large (70–120 degrees), then the fold is an "open" fold, but if the angle between the limbs is small (30 degrees or less), then the fold is a "tight" fold. [4] If an anticline plunges (i.e., the anticline crest is inclined to the Earth's surface), it will form V s on a geologic map view that point in the ...

  3. File:Clitheroe Beginners (Non-patronising edition) .pdf

    en.wikipedia.org/wiki/File:Clitheroe_Beginners...

    You are free: to share – to copy, distribute and transmit the work; to remix – to adapt the work; Under the following conditions: attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made.

  4. Fold (geology) - Wikipedia

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

    Folds can have a fold axis. A fold axis "is the closest approximation to a straight line that when moved parallel to itself, generates the form of the fold". [2] (Ramsay 1967). A fold that can be generated by a fold axis is called a cylindrical fold. This term has been broadened to include near-cylindrical folds.

  5. Folding endurance - Wikipedia

    en.wikipedia.org/wiki/Folding_endurance

    where F is the folding endurance and d the number of double folds. Folding endurance is especially applicable for papers used for maps, bank notes, archival documents, etc. The direction of the grain in relation to the folding line, the type of fibres used, the fibre contents, the calliper of the test piece, etc., as well as which type of ...

  6. File:Structure of accretionary prism and land or seaward ...

    en.wikipedia.org/wiki/File:Structure_of...

    Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts.

  7. Vergence (geology) - Wikipedia

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

    The vergence of a fold lies parallel to the surrounding surfaces of a fold, so if these surrounding surfaces are not horizontal, the vergence of the fold will be inclined. For a fold, the direction and the extent to which vergence occurs can be calculated from the strike and dip of the axial surfaces, along with that of the enveloping surfaces ...

  8. Fold number - Wikipedia

    en.wikipedia.org/wiki/Fold_number

    where f is the fold number, F i is the folding endurance for each test piece and n is total number of test pieces used. In the introduction of ISO 5626:1993 it is emphasized that fold number, as defined in that very International Standard, does not equal the mean number of double folds observed.

  9. 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 ...