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  2. Sediment transport - Wikipedia

    en.wikipedia.org/wiki/Sediment_transport

    The sediments entrained in a flow can be transported along the bed as bed load in the form of sliding and rolling grains, or in suspension as suspended load advected by the main flow. [16] Some sediment materials may also come from the upstream reaches and be carried downstream in the form of wash load.

  3. Marine geology - Wikipedia

    en.wikipedia.org/wiki/Marine_geology

    Sediment transportation and coastal erosion is a complex subject that is necessary to understand to protect infrastructure and the environment. [70] Coastal erosion is the process of sediment and materials breaking down and transported due to the effects of the sea . [ 71 ]

  4. Coastal sediment transport - Wikipedia

    en.wikipedia.org/wiki/Coastal_sediment_transport

    Coastal sediment transport (a subset of sediment transport) is the interaction of coastal land forms to various complex interactions of physical processes. [1] [2] The primary agent in coastal sediment transport is wave activity (see Wind wave), followed by tides and storm surge (see Tide and Storm surge), and near shore currents (see Sea#Currents) . [1]

  5. 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 ...

  6. Coastal sediment supply - Wikipedia

    en.wikipedia.org/wiki/Coastal_sediment_supply

    Coastal sediment supply is the transport of sediment to the beach environment by both fluvial and aeolian transport. While aeolian transport plays a role in the overall sedimentary budget for the coastal environment, it is paled in comparison to the fluvial supply which makes up 95% of sediment entering the ocean. [1]

  7. Sediment–water interface - Wikipedia

    en.wikipedia.org/wiki/Sedimentwater_interface

    Physical movement of water and sediments alter the thickness and topography of the sediment-water interface. Sediment resuspension by waves, tides, or other disturbing forces (e.g. human feet at a beach) allows sediment pore water and other dissolved components to diffuse out of the sediments and mix with the water above. [5]

  8. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    Since liquid water flows, ocean waters cycle and flow in currents around the world. Since water easily changes phase, it can be carried into the atmosphere as water vapour or frozen as an iceberg. It can then precipitate or melt to become liquid water again. All marine life is immersed in water, the matrix and womb of life itself. [7]

  9. Category:Water transportation in the Philippines - Wikipedia

    en.wikipedia.org/wiki/Category:Water...

    Ferry transportation in the Philippines (2 C, 1 P) L. ... Pages in category "Water transportation in the Philippines" The following 5 pages are in this category, out ...