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  2. 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 ...

  3. 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]

  4. 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 ]

  5. Breakwater (structure) - Wikipedia

    en.wikipedia.org/wiki/Breakwater_(structure)

    Breakwaters create safer harbours, but can also trap sediment moving along the coast. Breakwater under construction in Ystad , Sweden (2019) A breakwater in Haukilahti , Espoo , Finland A breakwater is a permanent structure constructed at a coastal area to protect against tides, currents, waves, and storm surges.

  6. Sediment transport - Wikipedia

    en.wikipedia.org/wiki/Sediment_transport

    Coastal sediment transport takes place in near-shore environments due to the motions of waves and currents. At the mouths of rivers, coastal sediment and fluvial sediment transport processes mesh to create river deltas. Coastal sediment transport results in the formation of characteristic coastal landforms such as beaches, barrier islands, and ...

  7. Turbidity current - Wikipedia

    en.wikipedia.org/wiki/Turbidity_current

    A buoyant sediment-laden river plume can induce a secondary turbidity current on the ocean floor by the process of convective sedimentation. [24] [4] Sediment in the initially buoyant hypopycnal flow accumulates at the base of the surface flow, [25] so that the dense lower boundary become unstable. The resulting convective sedimentation leads ...

  8. What You Need To Do Before It Gets Ridiculously Cold

    www.aol.com/gets-ridiculously-cold-103500516.html

    It is recommended that a winter survival kit includes: Jumper cables, flares and flashlights. Shovel, ice scraper and a basic toolkit. Sand or cat litter. First aid kit, blankets and a change of ...

  9. Longshore drift - Wikipedia

    en.wikipedia.org/wiki/Longshore_drift

    Longshore drift from longshore current is a geological process that consists of the transportation of sediments (clay, silt, pebbles, sand, shingle, shells) along a coast parallel to the shoreline, which is dependent on the angle of incoming wave direction.