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  2. Coastal path - Wikipedia

    en.wikipedia.org/wiki/Coastal_path

    A coastal path (or a littoral path) is a trail along a sea shore or a lake shore for pedestrians, and sometimes for cyclists or equestrians. Some coastal paths were originally created for use by customs or coastguard officials looking out for smugglers landing illicit goods. In modern times some routes have been developed for tourists, with ...

  3. Neritic zone - Wikipedia

    en.wikipedia.org/wiki/Neritic_zone

    Definition (marine biology), context, extra terminology [ edit ] In marine biology , the neritic zone , also called coastal waters , the coastal ocean or the sublittoral zone , [ 3 ] refers to that zone of the ocean where sunlight reaches the ocean floor , that is, where the water is never so deep as to take it out of the photic zone .

  4. Marine coastal ecosystem - Wikipedia

    en.wikipedia.org/wiki/Marine_coastal_ecosystem

    A marine coastal ecosystem is a marine ecosystem which occurs where the land meets the ocean. Worldwide there is about 620,000 kilometres (390,000 mi) of coastline. Coastal habitats extend to the margins of the continental shelves, occupying about 7 percent of the ocean surface area.

  5. Marine geology - Wikipedia

    en.wikipedia.org/wiki/Marine_geology

    Marine geology or geological oceanography is the study of the history and structure of the ocean floor. It involves geophysical, geochemical, sedimentological and paleontological investigations of the ocean floor and coastal zone.

  6. Coastal biogeomorphology - Wikipedia

    en.wikipedia.org/wiki/Coastal_biogeomorphology

    Coastal biogeomorphology looks at the interaction between marine organisms and coastal geomorphic processes. [2] Biogeomorphology is a subdiscipline of geomorphology. This can include not only microorganisms and plants, but animals as well.

  7. Marine habitat - Wikipedia

    en.wikipedia.org/wiki/Marine_habitat

    Primary coasts are shaped by non-marine processes, by changes in the land form. If a coast is in much the same condition as it was when sea level was stabilised after the last ice age, it is called a primary coast. [27] "Primary coasts are created by erosion (the wearing away of soil or rock), deposition (the buildup of sediment or sand) or ...

  8. Priest Cove - Wikipedia

    en.wikipedia.org/wiki/Priest_Cove

    Priest Cove (Cornish: Porth Ust, meaning St Just's Cove) or Priest's Cove is a small cove one mile (1.6 km) west of St Just, Cornwall, UK. [1] The name is from the Cornish Porth Ust, the port or cove of St Just, which was shortened to Por’ Ust. The apostrophised name "Priest’s" is a spelling mistake and the site has no connection with the ...

  9. 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]