An ice shelf is a thick, floating platform of ice that forms where a
glacier or
ice sheet flows down to a coastline and onto the ocean surface. Ice shelves are found in
Antarctica,
Greenland and
Canada only. The boundary between the floating ice shelf and the grounded (resting on bedrock) ice that feeds it is called the grounding line. When the grounding line retreats inland, water is added to the ocean and
sea level rises.
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