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  2. Bay - Wikipedia

    en.wikipedia.org/wiki/Bay

    The bay of Baracoa, Cuba. A bay is a recessed, coastal body of water that directly connects to a larger main body of water, such as an ocean, a lake, or another bay. [1] [2] [3] A large bay is usually called a gulf, sea, sound, or bight. A cove is a small, circular bay with a narrow entrance. A fjord is an elongated bay formed by glacial action ...

  3. Oceanic basin - Wikipedia

    en.wikipedia.org/wiki/Oceanic_basin

    Sea level is affected not only by the volume of the ocean basin, but also by the volume of water in them. Factors that influence the volume of the ocean basins are: Plate tectonics and the volume of mid-ocean ridges: the depth of the seafloor increases with distance to a ridge, as the oceanic lithosphere cools and thickens.

  4. Category:Landforms by sea or ocean - Wikipedia

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

    Landforms of the Pacific Ocean (26 C, 3 P) Landforms of the Persian Gulf (2 C) R. Landforms of the Red Sea (4 C, 5 P) S. Landforms of the Sea of Azov (4 C, 1 P)

  5. Glossary of landforms - Wikipedia

    en.wikipedia.org/wiki/Glossary_of_landforms

    Barrier island – Coastal dune landform that forms by wave and tidal action parallel to the mainland coast; Bay – Recessed, coastal body of water connected to an ocean or lake; Baymouth bar – low and narrow strip of alluvial land made from sand or pebbles

  6. Oceanic plateau - Wikipedia

    en.wikipedia.org/wiki/Oceanic_plateau

    However, when a plate carrying oceanic crust subducts under a plate carrying an igneous oceanic plateau, the volcanism which erupts on the plateau as the oceanic crust heats up on its descent into the mantle erupts material which is more felsic than the material which makes up the plateau. This represents a step toward creating crust which is ...

  7. Geology of the Pacific Ocean - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Pacific_Ocean

    The Farallon plate subducted under North America from the late Mesozoic, while spreading between the Pacific and Farallon plates was initiated 190 Ma and lasted until the break-up of the Farallon plate 23 Ma. During the Cenozoic the Farallon plate broke up along the eastern Pacific margin into the Kula, Vancouver/Juan de Fuca, and Cocos plates.

  8. Category:Coastal and oceanic landforms - Wikipedia

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

    Аԥсшәа; العربية; Asturianu; Azərbaycanca; تۆرکجه; বাংলা; Башҡортса; Беларуская; Беларуская ...

  9. Marine geology - Wikipedia

    en.wikipedia.org/wiki/Marine_geology

    Plate tectonics is a scientific theory developed in the 1960s that explains major land form events, such as mountain building, volcanoes, earthquakes, and mid-ocean ridge systems. [26] The idea is that Earth's most outer layer, known as the lithosphere , that is made up of the crust and mantle is divided into extensive plates of rock.