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  2. Body of water - Wikipedia

    en.wikipedia.org/wiki/Body_of_water

    a water feature usually consisting of a shallow pool of water, undisturbed by fountain jets, for a reflective surface. Reservoir: a place to store water for various uses, especially drinking water, which can be a natural or artificial (see lake and impoundment). Rill: a shallow channel of running water. These can be either natural or human-made.

  3. Shallow water - Wikipedia

    en.wikipedia.org/wiki/Shallow_water

    Shallow water may refer to: Waves and shallow water. Shallow water equations; Shallow water marine environment; Shallow Water; Shallow Water, Kansas, unincorporated ...

  4. Waves and shallow water - Wikipedia

    en.wikipedia.org/wiki/Waves_and_shallow_water

    When waves travel into areas of shallow water, they begin to be affected by the ocean bottom. [1] The free orbital motion of the water is disrupted, and water particles in orbital motion no longer return to their original position. As the water becomes shallower, the swell becomes higher and steeper, ultimately assuming the familiar sharp ...

  5. Depression (geology) - Wikipedia

    en.wikipedia.org/wiki/Depression_(geology)

    Panhole: a shallow depression or basin eroded into flat or gently sloping, cohesive rock. [2] Collapse-related: Sinkhole: a depression formed as a result of the collapse of rocks lying above a hollow. This is common in karst regions. Kettle: a shallow, sediment-filled body of water formed by melting glacial remnants in terminal moraines. [3]

  6. Shallow water marine environment - Wikipedia

    en.wikipedia.org/wiki/Shallow_water_marine...

    Many shallow marine environments are associated with carbonate factory zones, where processes that remove CO 2 from the water change bicarbonate ions into carbonate ions, supporting lime precipitation. These processes include increasing temperature, intense evaporation, and mixing water that is high in CO 3 and low in calcium cations with seawater.

  7. Shallow water equations - Wikipedia

    en.wikipedia.org/wiki/Shallow_water_equations

    Shallow-water equations, in its non-linear form, is an obvious candidate for modelling turbulence in the atmosphere and oceans, i.e. geophysical turbulence. An advantage of this, over Quasi-geostrophic equations , is that it allows solutions like gravity waves , while also conserving energy and potential vorticity .

  8. Neritic zone - Wikipedia

    en.wikipedia.org/wiki/Neritic_zone

    All photosynthetic life needs light to grow and how far out into the ocean light can still penetrate through the water column to the floor or benthic zone is what defines the neritic zone. That photic zone, or area where light can penetrate through the water column, is usually above ~100 meters (~328 feet). Some coastal areas have a long area ...

  9. Shallow (underwater relief) - Wikipedia

    en.wikipedia.org/wiki/Shallow_(underwater_relief)

    Shallow is an elevation of the bottom in the sea, river, lake, which impedes navigation. It is a type of an underwater relief where the depth of the water is low compared to that of the surrounding points. Usually formed by sand or pebble deposits, can also be of volcanic origin or the result of human or animal activities.