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  2. Seafloor spreading - Wikipedia

    en.wikipedia.org/wiki/Seafloor_spreading

    Plates that are not subducting are driven by gravity sliding off the elevated mid-ocean ridges a process called ridge push. [4] At a spreading center, basaltic magma rises up the fractures and cools on the ocean floor to form new seabed. Hydrothermal vents are common at spreading centers. Older rocks will be found farther away from the ...

  3. 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 ...

  4. Open ocean convection - Wikipedia

    en.wikipedia.org/wiki/Open_ocean_convection

    Open ocean convection is a process in which the mesoscale ocean circulation and large, strong winds mix layers of water at different depths. Fresher water lying over the saltier or warmer over the colder leads to the stratification of water, or its separation into layers. Strong winds cause evaporation, so the ocean surface cools, weakening the ...

  5. Downwelling - Wikipedia

    en.wikipedia.org/wiki/Downwelling

    Buoyancy-forced downwelling, often termed convection, is the deepening of a water parcel due to a change in the density of that parcel.Density changes in the surface ocean are primarily the result of evaporation, precipitation, heating, cooling, or the introduction and mixing of an alternate water or salinity source, such as river input or brine rejection.

  6. Scientists Discovered a Secret Ocean Floor Between Earth’s ...

    www.aol.com/scientists-discovered-secret-ocean...

    Scientists believe they’ve discovered an ancient ocean floor comprising a new layer between Earth’s mantle and core.

  7. Vine–Matthews–Morley hypothesis - Wikipedia

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

    Magnetic anomalies off west coast of North America. Dashed lines are spreading centers on mid-ocean ridges. The Vine–Matthews-Morley hypothesis correlates the symmetric magnetic patterns seen on the seafloor with geomagnetic field reversals. At mid-ocean ridges, new crust is created by the injection, extrusion, and solidification of magma.

  8. The source of the mysterious 'ocean buzzing' may have finally ...

    www.aol.com/news/2016-02-24-the-source-of-the...

    New research from the University of California, San Diego could solve a mystery that scientists have puzzled over for several years.

  9. Ocean Explorers Discovered a Massive Underwater ... - AOL

    www.aol.com/ocean-explorers-discovered-massive...

    Oceanographers explored an area around the Pacific Ocean’s Nazca Ridge and found a massive underwater mountain. ... Of the 71 percent of the Earth’s surface that is ocean floor, only 26 ...