Another form of anchor ice may be observed at the mouths of Arctic rivers where fresh water seeps out of the river bed into the ocean up through the sediment.
12.
It is sometimes known as the "'Salisbury Avon "'or the "'Hampshire Avon "'in order to distinguish it from the various other Britain in which the phenomenon of anchor ice has been observed.
13.
These include : Anchor Red Crown 4.4 % ( similar in taste and branding to Anchor Smooth ), Anchor Lite 4.0 %, Anchor Classic 4.0 %, Anchor Ice 4.0 % and Anchor 97 4.0 %.
14.
Studies and observations of anchor ice formation in McMurdo Sound, Antarctica have shown that the phenomenon regularly causes the formation of ice on the seafloor to depths of approximately 15m, and rarely to depths of approximately 30m.
15.
Anchor ice that forms on the underside of sea ice is often referred to as platelet or congelation ice, and can be hard to distinguish from that formed due to the cooling of the sea ice cover by cold atmospheric conditions.
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