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  2. Terrigenous sediment - Wikipedia

    en.wikipedia.org/wiki/Terrigenous_sediment

    Some 1.35 billion tons, or 8% of global river-borne sediment (16.5-17 billion tons globally), is transported by Ganges-Brahmaputra river system [5] annually according to decades old studies, it is unquantified how much variance year to year as well as the impact modern humans have on this amount by holding back sediment in dams, counteracted with increased development of erosion patterns.

  3. Continental shelf - Wikipedia

    en.wikipedia.org/wiki/Continental_shelf

    The continental shelves are covered by terrigenous sediments; that is, those derived from erosion of the continents. However, little of the sediment is from current rivers; some 60–70% of the sediment on the world's shelves is relict sediment, deposited during the last ice age, when sea level was 100–120 m lower than it is now. [21] [11]

  4. Bluff Downs fossil site - Wikipedia

    en.wikipedia.org/wiki/Bluff_Downs_fossil_site

    The fossils found at Bluff Downs fossil site consist of a diverse range of vertebrates dating to the Pliocene, found in the terrigenous sediments of the Allingham Formation. These include both broken and complete bones and skulls, though articulated skeletons (with the bones in the same position as upon the organism's death) are rare, and most ...

  5. Sediment Profile Imagery - Wikipedia

    en.wikipedia.org/wiki/Sediment_Profile_Imagery

    Portions of images in figure 14 are shown in panels 6, 7, and 8. Sediment texture is detailed in panel 6, a polychaete worm is evident in panel 7, and panel 8 shows Echinocardium (heart urchin) shell fragments in silt matrix. Panel 9 shows a diver giving the ‘thumbs up’ sign to the scanner to illustrate the limited depth of field of the ...

  6. Hemipelagic sediment - Wikipedia

    en.wikipedia.org/wiki/Hemipelagic_sediment

    The composition of Hemipelagic sediment directly depends on the composition of the adjacent land mass and geologic events such as volcanism that influence sediment input into the ocean. [ 7 ] [ 8 ] Hemipelagic sediments are mainly terrigenous but can also have biological oozes from marine organisms like Radiolarians or Diatoms .

  7. 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 ...

  8. Seabed - Wikipedia

    en.wikipedia.org/wiki/Seabed

    Terrigenous sediment is the most abundant sediment found on the seafloor. Terrigenous sediments come from the continents. These materials are eroded from continents and transported by wind and water to the ocean. Fluvial sediments are transported from land by rivers and glaciers, such as clay, silt, mud, and glacial flour. Aeolian sediments are ...

  9. Oceanic crust - Wikipedia

    en.wikipedia.org/wiki/Oceanic_crust

    Near the continental margins sediment is terrigenous, meaning derived from the land, unlike deep sea sediments which are made of tiny shells of marine organisms, usually calcareous and siliceous, or it can be made of volcanic ash and terrigenous sediments transported by turbidity currents.