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  2. Limestone - Wikipedia

    en.wikipedia.org/wiki/Limestone

    Limestone (calcium carbonate CaCO 3) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of CaCO 3. Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place ...

  3. Chalk - Wikipedia

    en.wikipedia.org/wiki/Chalk

    Chalk is a soft, white, porous, sedimentary carbonate rock.It is a form of limestone composed of the mineral calcite and originally formed deep under the sea by the compression of microscopic plankton that had settled to the sea floor.

  4. Marine sediment - Wikipedia

    en.wikipedia.org/wiki/Marine_sediment

    Marine sediment, or ocean sediment, or seafloor sediment, are deposits of insoluble particles that have accumulated on the seafloor.These particles either have their origins in soil and rocks and have been transported from the land to the sea, mainly by rivers but also by dust carried by wind and by the flow of glaciers into the sea, or they are biogenic deposits from marine organisms or from ...

  5. Shallow water marine environment - Wikipedia

    en.wikipedia.org/wiki/Shallow_water_marine...

    The most common evaporite minerals found within modern and ancient deposits are gypsum, anhydrite, and halite. These minerals can occur as crystalline layers, isolated crystals, or clusters of crystals. [2] Approximately 75% of surface sediments are in shallow marine environments, holding most Phanerozoic and Precambrian sedimentary rock. [3]

  6. Marine biogenic calcification - Wikipedia

    en.wikipedia.org/wiki/Marine_biogenic_calcification

    The surface ocean engages in air-sea interactions and absorbs carbon dioxide (CO 2) from the atmosphere, making the ocean the Earth's largest sink for atmospheric CO 2. Carbon dioxide dissolves in and reacts with seawater to form carbonic acid. Subsequent reactions then produce carbonate (CO 3 2−), bicarbonate (HCO 3 −), and hydrogen (H ...

  7. Travertine - Wikipedia

    en.wikipedia.org/wiki/Travertine

    Travertine is found at Tivoli, 25 kilometers (16 mi) east of Rome, where the travertine has been quarried for at least 2,000 years. [40] Tivoli travertine was deposited in a body 20 square kilometers (7.7 sq mi) in area and 60 meters (200 ft) thick along a north-trending fault near the dormant Colli Albani volcano.

  8. List of types of limestone - Wikipedia

    en.wikipedia.org/wiki/List_of_types_of_limestone

    Caen Stone – Limestone quarried near Caen, France Lutetian limestone – Type of limestone from Paris, or "Paris stone" (city buildings are widely faced with it) Saint-Maximin – commune in Oise, France Pages displaying wikidata descriptions as a fallback , or Oise, limestone (variety of Lutetian)

  9. Oolite - Wikipedia

    en.wikipedia.org/wiki/Oolite

    The material consolidated and eroded during later exposure above the ocean surface. One of the world's largest freshwater lakebed oolites is the Shoofly Oolite, [ 5 ] a section of the Glenns Ferry Formation on southwestern Idaho 's Snake River Plain . 10 million years ago, the Plain formed the bed of Lake Idaho .