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Drift ice

Drift ice, also called brash ice, is sea ice that is not attached to the shoreline or any other fixed object. Unlike fast ice, which is "fastened" to a fixed object, drift ice is carried along by winds and sea currents, hence its name. When drift ice is driven together into a large single mass, it is called pack ice. Wind and currents can pile up that ice to form ridges up to dozens of metres in thickness. These represent a challenge for icebreakers and offshore structures operating in cold oceans and seas.

Gallery
Image:Kontio towing.jpg|The icebreaker Kontio, which in this picture became stuck in drift ice while towing a cargo ship in pack ice in the northern Baltic Sea Image:IceNomenclature-2LightPack.jpg|Ice floes / pack ice Image:Wrangelisland.jpg|Satellite image of drift ice in the Arctic Ocean around Wrangel Island Image:Icebreaker Aurora on drift ice at Sea of Okhost.jpg|Drift ice in the Sea of Okhotsk Image:Aboard Aurora Icebreaker at Sea of Okhost.jpg|Aboard the Aurora icebreaker in the Sea of Okhotsk ==See also==
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