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  2. Oceanic crust - Wikipedia

    en.wikipedia.org/wiki/Oceanic_crust

    Oceanic crust is the uppermost layer of the oceanic portion of the tectonic plates. It is composed of the upper oceanic crust, with pillow lavas and a dike complex, and the lower oceanic crust, composed of troctolite, gabbro and ultramafic cumulates. [1] [2] The crust overlies the rigid uppermost layer of the mantle.

  3. Benthic zone - Wikipedia

    en.wikipedia.org/wiki/Benthic_zone

    The benthic boundary layer, which includes the bottom layer of water and the uppermost layer of sediment directly influenced by the overlying water, is an integral part of the benthic zone, as it greatly influences the biological activity that takes place there. Examples of contact soil layers include sand bottoms, rocky outcrops, coral, and ...

  4. Ocean stratification - Wikipedia

    en.wikipedia.org/wiki/Ocean_stratification

    Stratified layers are a barrier to the mixing of water, which impacts the exchange of heat, carbon, oxygen and other nutrients. [1] The surface mixed layer is the uppermost layer in the ocean and is well mixed by mechanical (wind) and thermal (convection) effects. Climate change is causing the upper ocean stratification to increase.

  5. Internal structure of Earth - Wikipedia

    en.wikipedia.org/wiki/Internal_structure_of_Earth

    Earth's crust ranges from 5 to 70 kilometres (3.1–43.5 mi) [7] in depth and is the outermost layer. [8] 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]

  6. Sheeted dyke complex - Wikipedia

    en.wikipedia.org/wiki/Sheeted_dyke_complex

    A sheeted dyke complex, or sheeted dike complex, is a series of sub-parallel intrusions of igneous rock, forming a layer within the oceanic crust. [1] At mid-ocean ridges , dykes are formed when magma beneath areas of tectonic plate divergence travels through a fracture in the earlier formed oceanic crust, feeding the lavas above and cooling ...

  7. Oceanic zone - Wikipedia

    en.wikipedia.org/wiki/Oceanic_zone

    The oceanic zone is typically defined as the area of the ocean lying beyond the continental shelf (e.g. the neritic zone), but operationally is often referred to as beginning where the water depths drop to below 200 metres (660 ft), seaward from the coast into the open ocean with its pelagic zone.

  8. 80 Secondhand Finds That Are As Strange As They Are Wonderful

    www.aol.com/lifestyle/80-weird-wonderful...

    It now hangs in my castle room and reminds me of dragon scales lol and collecting a new layer of dust. Image credits: Weird and Wonderful Secondhand Finds #59 Found And Left At Goodwill In Lady ...

  9. Isopycnal - Wikipedia

    en.wikipedia.org/wiki/Isopycnal

    Isopycnal mixing and diapycnal mixing work together to mix and ventilate the entire ocean. Isopycnal mixing is when surface waters moving into the interior of the ocean typically run horizontally, along the isopycnal layers, settling into their correct density-dependent layer [2]. This process is important for ventilating the ocean with oxygen.