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The convergence is a complex and turbulent area with seawater that has cooled dramatically around the Antarctic continent. As it became heavier, it starts to flow northwards along the seabed. As it unites with warmer subterranean water from equatorial regions, the convergence falls out in an outpouring sequence of the bottomless waters to the exterior...
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This gush carries out underwater nutrients, which is the key reason why areas in the southern part of this continent are astonishingly productive.
Ice formations are obviously common here. One of the common names of the bergs formed on the ice beds is "Pancake ice". This is formed when slabs of ice that are forming are jostled by the wind and movement of the sea which forces ice to bash against each other around the edges and start to curl upwards at the edges...
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