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  2. Elliott Bay - Wikipedia

    en.wikipedia.org/wiki/Elliott_Bay

    Grain is carried to docked cargo ships by passing over Elliott Bay Trail and a narrow shoreline park, which also features a public fishing pier [23] near Smith Cove. In the cove is Terminal 91, which has served a variety of purposes over the years, including storage for imported automobiles and fish, and most recently became a dock for Alaskan ...

  3. Beach cusps - Wikipedia

    en.wikipedia.org/wiki/Beach_cusps

    In the adjacent diagram, the two waves cancel each other out, creating a flat surface. However, this is a highly simplified version of events. The incoming wave has the same wave period as the edge wave, so the incoming wave changes from a peak to a trough over the same period as it takes the standing wave to change so they keep the same pattern.

  4. Puget Sound - Wikipedia

    en.wikipedia.org/wiki/Puget_Sound

    Puget Sound's shoreline is 1,332 miles (2,144 km) long, encompassing a water area of 1,020 square miles (2,600 km 2) and a total volume of 26.5 cubic miles (110 km 3) at mean high water. The average volume of water flowing in and out of Puget Sound during each tide is 1.26 cubic miles (5.3 km 3 ).

  5. Heavy surf causes coastal chaos across SLO County. See the ...

    www.aol.com/news/heavy-surf-causes-coastal-chaos...

    Waves crash against the cliffs in Shell Beach in a view from Shoreline Drive on Dec. 28, 2023. Storm driven high swells on the ocean combined with seasonal high tides combined to cause coastal ...

  6. Surf break - Wikipedia

    en.wikipedia.org/wiki/Surf_break

    A type of open ocean surf break, these occur where sand build ups occur well offshore to produce breaking waves in the open ocean, which are sometimes called 'Outer Banks', which are similar to open ocean reefs except that they are generally made of sand, and may disappear or change with storms. The 'Outer Banks' in North Carolina is an example.

  7. 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]

  8. How to turn ocean waves into renewable energy - AOL

    www.aol.com/turn-ocean-waves-renewable-energy...

    The power of the ocean could soon be used to power homes in the U.S. as scientists prepare to test an untapped form of renewable energy. The U.S. Department of Energy has invested $112.5 million ...

  9. Beach ridge - Wikipedia

    en.wikipedia.org/wiki/Beach_ridge

    A beach ridge is a wave-swept or wave-deposited ridge running parallel to a shoreline. It is commonly composed of sand as well as sediment worked from underlying beach material. The movement of sediment by wave action is called littoral transport. Movement of material parallel to the shoreline is called longshore transport.

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