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  2. Body of water - Wikipedia

    en.wikipedia.org/wiki/Body_of_water

    The process of creating an "impoundment" of water is itself called "impoundment". Ice cap: A body of frozen water less than 50,000 km 2 not constrained by topographical features (i.e., they will lie over the top of mountains) Ice field: A body of frozen water constrained by topographical features: Ice sheet: A body of frozen water more than ...

  3. Sea ice - Wikipedia

    en.wikipedia.org/wiki/Sea_ice

    Furthermore, sea ice affects the movement of ocean waters. In the freezing process, much of the salt in ocean water is squeezed out of the frozen crystal formations, though some remains frozen in the ice. This salt becomes trapped beneath the sea ice, creating a higher concentration of salt in the water beneath ice floes.

  4. Outline of oceanography - Wikipedia

    en.wikipedia.org/wiki/Outline_of_oceanography

    The following outline is provided as an overview of and introduction to Oceanography.. Thermohaline circulation. Oceanography (from Ancient Greek ὠκεανός (ōkeanós) 'ocean' and γραφή (graphḗ) 'writing'), also known as oceanology, sea science, ocean science, and marine science, is the scientific study of the ocean, including its physics, chemistry, biology, and geology.

  5. Seabed - Wikipedia

    en.wikipedia.org/wiki/Seabed

    The seabed (also known as the seafloor, sea floor, ocean floor, and ocean bottom) is the bottom of the ocean. All floors of the ocean are known as 'seabeds'. The structure of the seabed of the global ocean is governed by plate tectonics. Most of the ocean is very deep, where the seabed is known as the abyssal plain. Seafloor spreading creates ...

  6. 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.

  7. AOL Mail

    mail.aol.com

    Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!

  8. Brinicle - Wikipedia

    en.wikipedia.org/wiki/Brinicle

    The brine-rich water remains liquid, and its increased density causes this water to sink, setting the stage for the creation of a "brinicle". Its outer edges begin accumulating a layer of ice as the surrounding water, cooled by this jet to below its freezing point, ices up in a tubular or finger shape and becomes self-sustaining. The down ...

  9. The only living core member of 'The Jeffersons' cast made a ...

    www.aol.com/entertainment/only-living-member...

    Marla Gibbs, the last living original core cast member from "The Jeffersons," made a surprise cameo this week during ABC's "Live in Front of a Studio Audience: Norman Lear's 'All in the Family ...