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 only found in
Antarctica,
Greenland and
Canada. The boundary between the floating ice shelf and the grounded (resting on bedrock) ice that feeds it is called the grounding line. The thickness of ice shelves ranges from about 100 to 1000 meters.