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  2. Ocean color - Wikipedia

    en.wikipedia.org/wiki/Ocean_color

    Ocean color is the branch of ocean optics that specifically studies the color of the water and information that can be gained from looking at variations in color. The color of the ocean , while mainly blue, actually varies from blue to green or even yellow, brown or red in some cases. [ 1 ]

  3. Ocean colonization - Wikipedia

    en.wikipedia.org/wiki/Ocean_colonization

    Ocean colonization (also blue colonization or ocean grabbing) [1] [2] is the exploitation, settlement or territorial claim of the ocean and the oceanic crust. Ocean colonization has been identified critically as a form of colonization and colonialism , particularly in the light of growing exploitive and destructive blue economy ocean ...

  4. Underwater environment - Wikipedia

    en.wikipedia.org/wiki/Underwater_environment

    The world ocean is the most visible part of Earth from space. Three quarters of the planet Earth are covered by water. Most of the planet's solid surface is abyssal plain, at depths between 4,000 and 5,500 metres (13,100 and 18,000 ft) below the surface of the oceans.

  5. Deep scattering layer - Wikipedia

    en.wikipedia.org/wiki/Deep_scattering_layer

    Lanternfish account for as much as 65 percent of all deep sea fish biomass and are largely responsible for the deep scattering layer of the world's oceans.. The phantom bottom is caused by the sonar misinterpreting as the ocean floor a layer of small seagoing creatures that congregate between 1,000 and 1,500 feet (300 and 460 m) below the surface.

  6. Geoid - Wikipedia

    en.wikipedia.org/wiki/Geoid

    If the ocean were of constant density and undisturbed by tides, currents or weather, its surface would resemble the geoid. The permanent deviation between the geoid and mean sea level is called ocean surface topography. If the continental land masses were crisscrossed by a series of tunnels or canals, the sea level in those canals would also ...

  7. Internal structure of Earth - Wikipedia

    en.wikipedia.org/wiki/Internal_structure_of_Earth

    The thin parts are the oceanic crust, which underlies the ocean basins (5–10 km) and is mafic-rich [9] (dense iron-magnesium silicate mineral or igneous rock). [10] The thicker crust is the continental crust , which is less dense [ 11 ] and is felsic -rich (igneous rocks rich in elements that form feldspar and quartz ). [ 12 ]

  8. Planetary oceanography - Wikipedia

    en.wikipedia.org/wiki/Planetary_oceanography

    Planetary oceanography, also called astro-oceanography or exo-oceanography, [1] is the study of oceans on planets and moons other than Earth.Unlike other planetary sciences like astrobiology, astrochemistry, and planetary geology, it only began after the discovery of underground oceans in Saturn's moon Titan [2] and Jupiter's moon Europa. [3]

  9. Waterphone - Wikipedia

    en.wikipedia.org/wiki/Waterphone

    Musician Thomas Bloch playing the waterphone, 19 September 2009 at the Mittersheim pond, France. A waterphone (also ocean harp) is a type of inharmonic acoustic tuned idiophone consisting of a stainless steel resonator bowl or pan with a cylindrical neck and bronze rods of different lengths and diameters around the rim of the bowl.

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