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  2. Monocline - Wikipedia

    en.wikipedia.org/wiki/Monocline

    A monocline (or, rarely, a monoform) is a step-like fold in rock strata consisting of a zone of steeper dip within an otherwise horizontal or gently dipping sequence.

  3. Monoclinic crystal system - Wikipedia

    en.wikipedia.org/wiki/Monoclinic_crystal_system

    Monoclinic crystal An example of the monoclinic crystal orthoclase. In crystallography, the monoclinic crystal system is one of the seven crystal systems.A crystal system is described by three vectors.

  4. Fold (geology) - Wikipedia

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

    Monocline: linear, strata dip in one direction between horizontal layers on each side. Recumbent: linear, fold axial plane oriented at a low angle resulting in ...

  5. List of geological folds in Great Britain - Wikipedia

    en.wikipedia.org/wiki/List_of_geological_folds...

    A monocline (or, rarely, a monoform) is a step-like fold, one limb of which is roughly horizontal. Both domes and periclines are anticlines in which the strata fall away about equally in all directions.

  6. Purbeck Monocline - Wikipedia

    en.wikipedia.org/wiki/Purbeck_Monocline

    The Purbeck Monocline is a geological fold in southern England. The term 'fold' is used in geology when one or more originally flat sedimentary strata surfaces are bent or curved as a result of plastic (i.e. permanent) deformation. A monocline is a step-like fold, in which one limb is roughly

  7. Homocline - Wikipedia

    en.wikipedia.org/wiki/Homocline

    Homocline near Lulworth Cove, England Diagram of a homocline Homocline in Aberdeenshire, Scotland. In structural geology, a homocline or homoclinal structure (from old Greek: homo = same, cline = inclination), is a geological structure in which the layers of a sequence of rock strata, either sedimentary or igneous, dip uniformly in a single direction having the same general inclination in ...

  8. Hogback (geology) - Wikipedia

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

    Oblique aerial photo of a hogback located between Gallup and Ramah in western New Mexico.. In geology and geomorphology, a hogback or hog's back is a long, narrow ridge or a series of hills with a narrow crest and steep slopes of nearly equal inclination on both flanks.

  9. Syncline - Wikipedia

    en.wikipedia.org/wiki/Syncline

    A syncline is a fold of rocks with younger rock layers closer to the center of the structure, whereas an anticline is the inverse of a syncline.