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6.1: Marine Sediments

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    Marine Sediments

    This chapter is about the origin and distribution of sedimentary deposits (sediments and sedimentary rocks) with a focus on marine sediments.

    The word “sedimentary” refers to materials consisting of sediments or formed by deposition; the word sedimentary also applies to both the processes and the products of deposition (Figure 6.1).

    The Rock Cycle
    Figure 6.1. Sediments, sedimentary rocks and sedimentary processes are part of the Rock Cycle.

    Sediment: Solid material that has settled from a state of suspension. Sediments are transported and deposited by water (rivers, lakes, and oceans), ice (glaciers), and wind.

    Sedimentary rock
    is rock that has formed through the deposition and consolidation and solidification of sediment. Sedimentary rocks are often deposited in layers, and frequently contain fossils. Studies of sedimentary deposits can help tell the geologic history of an area.

    Classification of Sediments and Sedimentary Rocks

    Sediments (and sedimentary rocks) are classified in by origin of source material and by grain size.

    There are 4 sources of sediments (and sedimentary rocks):
    a) Cosmogenous:
    material that falls to the Earth surface from outer space.
    b) Hydrogenous: material precipitated directly seawater.
    c) Lithogenous: material derived from erosion of other rocks, typically from continental sources.
    d) Biogenous: material formed from the accumulation of remains of living organism.

    This page titled 6.1: Marine Sediments is shared under a not declared license and was authored, remixed, and/or curated by Miracosta Oceanography 101 (Miracosta)) via source content that was edited to the style and standards of the LibreTexts platform; a detailed edit history is available upon request.

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