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  2. Hemipelagic sediment - Wikipedia

    en.wikipedia.org/wiki/Hemipelagic_sediment

    Hemipelagic sediment, or hemipelagite, is a type of marine sediment that consists of clay and silt-sized grains that are terrigenous and some biogenic material derived from the landmass nearest the deposits or from organisms living in the water.

  3. Hip prosthesis zones - Wikipedia

    en.wikipedia.org/wiki/Hip_prosthesis_zones

    After hip replacement, hip prosthesis zones are regions in the interface between prosthesis material and the surrounding bone. These are used as reference regions when describing for example complications including hip prosthesis loosening on medical imaging .

  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. Hip replacement - Wikipedia

    en.wikipedia.org/wiki/Hip_replacement

    Hip replacement is a surgical procedure in which the hip joint is replaced by a prosthetic implant, that is, a hip prosthesis. [1] Hip replacement surgery can be performed as a total replacement or a hemi/semi(half) replacement. Such joint replacement orthopaedic surgery is generally conducted to relieve arthritis pain or in some hip fractures.

  6. Zona orbicularis - Wikipedia

    en.wikipedia.org/wiki/Zona_orbicularis

    The zona orbicularis and proximal hip joint capsule are poorly understood. Recent studies seem to confirm that the proximal to middle part of the articular capsule, including the zona orbicularis, acts biomechanically as a locking ring wrapped around the femoral neck and thus is a key structure for hip stability in distraction.

  7. Continental rise - Wikipedia

    en.wikipedia.org/wiki/Continental_rise

    Because the continental rise lies below the continental slope and is formed from sediment deposition, it has a very gentle slope, usually ranging from 1:50 to 1:500. [1] As the continental rise extends seaward, the layers of sediment thin, and the rise merges with the abyssal plain, typically forming a slope of around 1:1000.

  8. Accretionary wedge - Wikipedia

    en.wikipedia.org/wiki/Accretionary_wedge

    The mountains began to form about 35 million years ago when the Juan de Fuca plate collided with and was forced (subducted) under the North American plate. [ 14 ] Kodiak Shelf in the Gulf of Alaska – The geology of the Chugach National Forest is dominated by two major lithologic units, the Valdez Group (Late Cretaceous) and the Orca Group ...

  9. Nankai Trough - Wikipedia

    en.wikipedia.org/wiki/Nankai_Trough

    Distribution of identified gas hydrate locations, in green and the location of selected subduction zones, red lines, modefied from Collet, 2002. Drill cores from the seaward edge of the Nankai Trough (where the heat flow is one of the highest in the region) reveal that sediments there only reach pre-oil window to early oil window thermal ...

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