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  2. Sedimentary rock - Wikipedia

    en.wikipedia.org/wiki/Sedimentary_rock

    Uluru (Ayers Rock) is a large sandstone formation in Northern Territory, Australia.. Sedimentary rocks can be subdivided into four groups based on the processes responsible for their formation: clastic sedimentary rocks, biochemical (biogenic) sedimentary rocks, chemical sedimentary rocks, and a fourth category for "other" sedimentary rocks formed by impacts, volcanism, and other minor processes.

  3. Sedimentology - Wikipedia

    en.wikipedia.org/wiki/Sedimentology

    Sedimentology encompasses the study of modern sediments such as sand, [1] silt, and clay, [2] and the processes that result in their formation (erosion and weathering), transport, deposition and diagenesis. [3] Sedimentologists apply their understanding of modern processes to interpret geologic history through observations of sedimentary rocks ...

  4. Sedimentary structures - Wikipedia

    en.wikipedia.org/wiki/Sedimentary_structures

    Sedimentary structures include all kinds of features in sediments and sedimentary rocks, formed at the time of deposition. Sediments and sedimentary rocks are characterized by bedding, which occurs when layers of sediment, with different particle sizes are deposited on top of each other. [1] These beds range from millimeters to centimeters ...

  5. Clastic rock - Wikipedia

    en.wikipedia.org/wiki/Clastic_rock

    Clastic rocks are composed of fragments, or clasts, of pre-existing minerals and rock. A clast is a fragment of geological detritus, [1] chunks, and smaller grains of rock broken off other rocks by physical weathering. [2] Geologists use the term clastic to refer to sedimentary rocks and particles in sediment transport, whether in suspension or ...

  6. Sedimentary basin - Wikipedia

    en.wikipedia.org/wiki/Sedimentary_basin

    Sedimentary basin. Sedimentary basins are region-scale depressions of the Earth's crust where subsidence has occurred and a thick sequence of sediments have accumulated to form a large three-dimensional body of sedimentary rock. [1][2][3] They form when long-term subsidence creates a regional depression that provides accommodation space for ...

  7. Limestone - Wikipedia

    en.wikipedia.org/wiki/Limestone

    Limestone. Limestone (calcium carbonate CaCO3) 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 CaCO3. Limestone forms when these minerals precipitate out of water containing dissolved calcium.

  8. 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. [1] Most sandstone is composed of quartz or feldspar, because they are the most resistant minerals to the weathering processes at the Earth's ...

  9. Diagenesis - Wikipedia

    en.wikipedia.org/wiki/Diagenesis

    Diagenesis (/ ˌdaɪ.əˈdʒɛnəsɪs /) is the process that describes physical and chemical changes in sediments first caused by water-rock interactions, microbial activity, and compaction after their deposition. Increased pressure and temperature only start to play a role as sediments become buried much deeper in the Earth's crust. [1]