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  2. General Bathymetric Chart of the Oceans - Wikipedia

    en.wikipedia.org/wiki/General_Bathymetric_Chart...

    The GEBCO chart series was initiated in 1903 by an international group of geographers and oceanographers, under the leadership of Prince Albert I of Monaco.At that time there was an explosion of interest in the study of the natural world and this group recognized the importance of a set of maps describing the shape of the ocean floor.

  3. Marine geology - Wikipedia

    en.wikipedia.org/wiki/Marine_geology

    When the Earth turns on its axis, the metals release electrical currents which generate magnetic fields. [17] These fields can then be measured to reveal geological subseafloor structures. [ 18 ] This method is especially useful in marine exploration and geology as it can not only characterize geological features on the seafloor but can survey ...

  4. Marine sediment - Wikipedia

    en.wikipedia.org/wiki/Marine_sediment

    Marine sediment, or ocean sediment, or seafloor sediment, are deposits of insoluble particles that have accumulated on the seafloor.These particles either have their origins in soil and rocks and have been transported from the land to the sea, mainly by rivers but also by dust carried by wind and by the flow of glaciers into the sea, or they are biogenic deposits from marine organisms or from ...

  5. Vine–Matthews–Morley hypothesis - Wikipedia

    en.wikipedia.org/wiki/Vine–Matthews–Morley...

    Harry Hess proposed the seafloor spreading hypothesis in 1960 (published in 1962 [1]); the term "spreading of the seafloor" was introduced by geophysicist Robert S. Dietz in 1961. [2] According to Hess, seafloor was created at mid-oceanic ridges by the convection of the Earth's mantle, pushing and spreading the older crust away from the ridge. [3]

  6. Hypsometry - Wikipedia

    en.wikipedia.org/wiki/Hypsometry

    Hypsometry (from Ancient Greek ὕψος (húpsos) 'height' and μέτρον (métron) 'measure') [1] [2] is the measurement of the elevation and depth of features of Earth's surface relative to mean sea level. [3] On Earth, the elevations can take on either positive or negative (below sea level) values.

  7. Seafloor spreading - Wikipedia

    en.wikipedia.org/wiki/Seafloor_spreading

    The idea that the seafloor itself moves and also carries the continents with it as it spreads from a central rift axis was proposed by Harold Hammond Hess from Princeton University and Robert Dietz of the U.S. Naval Electronics Laboratory in San Diego in the 1960s. [1] [2] The phenomenon is known today as plate tectonics. In locations where two ...

  8. Fort Worth elementary students watch in awe of solar eclipse ...

    www.aol.com/fort-worth-elementary-students-watch...

    Fifth-grade students at Alice Carlson Applied Learning Center in Fort Worth who helped organize lesson plans and activities for the school in preparation for the solar eclipse show off their “UV ...

  9. Wilson Cycle - Wikipedia

    en.wikipedia.org/wiki/Wilson_cycle

    The Wilson cycle theory is based upon the idea of an ongoing cycle of ocean closure, continental collision, and a formation of new ocean on the former suture zone.The Wilson Cycle can be described in six phases of tectonic plate motion: the separation of a continent (continental rift), formation of a young ocean at the seafloor, formation of ocean basins during continental drift, initiation of ...