Antarctic Ice is the oceanic ice folder would be considered an ice shelf.
An ice shelf is a sizable ice platform that develops where a glacier or ice sheet slides down to the ocean's surface along a shoreline.
Only Antarctica, Greenland, Northern Canada, and the Russian Arctic have ice shelves.
The grounding line separates the floating ice shelf from the anchor ice that feeds it, which is supported by bedrock. Ice shelves can be between 100 meters (330 feet) and 1,000 meters thick (3,300 ft).
In contrast, sea ice forms all over the Arctic Ocean, is significantly thinner (usually less than 3 m (9.8 ft)), and is produced on water. It can also be found in the Southern Ocean, near the Antarctic continent.
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