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  2. Kurkar - Wikipedia

    en.wikipedia.org/wiki/Kurkar

    Kurkar is the regional name for an aeolian quartz sandstone with carbonate cement, [3] in other words an eolianite or a calcarenite (calcareous sandstone or grainstone), found on the Levantine coast of the Mediterranean Sea in Turkey, [3] Syria, Lebanon, Israel, [4] the Gaza Strip [5] and northern Sinai Peninsula. [6]

  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. 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

  5. Arenite - Wikipedia

    en.wikipedia.org/wiki/Arenite

    Other arenites include sandstones, arkoses, greensands, and greywackes. Arenites mainly form by erosion of other rocks or turbiditic re-deposition of sands. Some arenites contain a varying amount of carbonatic components and thus belong to the rock-category of carbonatic sandstones or silicatic limestones .

  6. Sandstone - Wikipedia

    en.wikipedia.org/wiki/Sandstone

    Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains, cemented together by another mineral. Sandstones comprise about 20–25% of all sedimentary rocks.

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    2. Control the temperature. Our body temperature fluctuates throughout the day. When it’s on the rise, we’re most likely to be alert (think post-workout) and when it’s falling it tells our ...

  8. Flysch - Wikipedia

    en.wikipedia.org/wiki/Flysch

    Flysch (/ f l ɪ ʃ /) is a sequence of sedimentary rock layers that progress from deep-water and turbidity flow deposits to shallow-water shales and sandstones. It is deposited when a deep basin forms rapidly on the continental side of a mountain building episode.

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