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Abyssal (or submarine) fans are formed from turbidity currents. These currents begin when a geologic activity pushes sediments over the edge of a continental shelf and down the continental slope, creating an underwater landslide. A dense slurry of muds and sands speeds towards the foot of the slope, until the current slows. The decreasing ...
The longest turbidity current ever recorded occurred in January 2020 and flowed for 1,100 kilometers (680 mi) through the Congo Canyon over the course of two days, damaging two submarine communications cables. The current was a result of sediment deposited by the 2019–2020 Congo River floods. [54]
Turbidites provide a mechanism for assigning a tectonic and depositional setting to ancient sedimentary sequences as they usually represent deep-water rocks formed offshore of a convergent margin, and generally require at least a sloping shelf and some form of tectonism to trigger density-based avalanches. Density currents may be triggered in ...
The current is circumpolar due to the lack of any landmass connecting with Antarctica and this keeps warm ocean waters away from Antarctica, enabling that continent to maintain its huge ice sheet. Associated with the Circumpolar Current is the Antarctic Convergence , where the cold Antarctic waters meet the warmer waters of the subantarctic ...
[1] [3] A distinguishing characteristic of the CDW is that the water is not formed at the surface, but rather by a blending of other water masses. [1] CDW sits at a depth of around 500 meters, approximately at the depth of the continental shelf. [3] There are two types of CDW: Upper Circumpolar Deep Water (UCDW) and Lower Circumpolar Deep Water ...
An ocean current is generated by the forces such as breaking waves, temperature and salinity differences, wind, Coriolis effect, and tides caused by the gravitational pull of celestial bodies. In addition, the physical properties in a pycnocline driven by density gradients also affect the flows and vertical profiles in the ocean .
Cher's driver's license is registered exactly how fans would imagine it to be.. During an appearance on Jimmy Kimmel Live!on Tuesday, Jan. 7, the multi-hyphenate brainstormed ideas for the second ...
A geostrophic current is an oceanic current in which the pressure gradient force is balanced by the Coriolis effect. The direction of geostrophic flow is parallel to the isobars , with the high pressure to the right of the flow in the Northern Hemisphere , and the high pressure to the left in the Southern Hemisphere .