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Continental Glacier
(i) they are confined to Polar Regions like Antarctica and Greenland.
(ii) They are thick ice sheets.
(iii) They are extensive and cover a large area and may extend up to 5000 km.
(iv) Their movement is extremely slow.
(v) They move due to pressure.
(vi) They break off at the edge of the continents and these big blocks float as icebergs in the sea.
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