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  2. Torridon Group - Wikipedia

    en.wikipedia.org/wiki/Torridon_Group

    This formation is similar to the Applecross formation except that the sandstones are fine to medium-grained and there are very few pebbles. Almost all of these sandstone beds show the contortions shown by the older formation. The Applecross and Aultbea Formations together consist of an overall fining-upward sequence of sandstones.

  3. Lithic fragment (geology) - Wikipedia

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

    Lithic fragments, or lithics, are pieces of other rocks that have been eroded down to sand size and now are sand grains in a sedimentary rock.They were first described and named (in their modern definitions) by Bill Dickinson in 1970. [1]

  4. QFL diagram - Wikipedia

    en.wikipedia.org/wiki/Qfl_diagram

    As sandstones, these are known as lithic sandstones. Arc sands plot along the F and L line, with sometimes significant Q components. Clustering near the F pole indicates a dissected arc, and clustering near the L pole indicates an undissected, or new arc. As sandstones, these are known as arkoses and/or lithic sandstones.

  5. List of sandstones - Wikipedia

    en.wikipedia.org/wiki/List_of_sandstones

    Steenpan (also Flatpan or Klippan), Free State province, near Wolvehoek Table Mountain Sandstone Western Cape province, various quarry sites numerous types, some without trade names, from the Karoo Supergroup in many quarries near Graaff-Reinet , Cradock , Queenstown , Aliwal North , Burgersdorp and Sterkstroom

  6. Sandstone - Wikipedia

    en.wikipedia.org/wiki/Sandstone

    Framework grains are sand-sized (0.0625-to-2-millimeter (0.00246 to 0.07874 in) diameter) detrital fragments that make up the bulk of a sandstone. [16] [17] Most framework grains are composed of quartz or feldspar, which are the common minerals most resistant to weathering processes at the Earth's surface, as seen in the Goldich dissolution ...

  7. Conglomerate (geology) - Wikipedia

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

    They are closely related to sandstones in origin, and exhibit many of the same types of sedimentary structures, such as tabular and trough cross-bedding and graded bedding. [ 1 ] [ 2 ] [ 3 ] Fanglomerates are poorly sorted, matrix-rich conglomerates that originated as debris flows on alluvial fans and likely contain the largest accumulations of ...

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  9. Folk classification - Wikipedia

    en.wikipedia.org/wiki/Folk_classification

    Folk's philosophy is that the name of a rock must convey as much information as possible without being a complete description. For this, he proposed five important properties of sandstones to use as defining characteristics.