Near the margins of the Greenland ice sheet,where glacial ice is forced between mountains so that it has an extremely high flow rate,it is called a surging glacier.

Name: Near the margins of the Greenland ice sheet,where glacial ice is forced between mountains so that it has an extremely high flow rate,it is called a surging glacier.
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A surging glacier is one that experiences short-lived episodes of rapid flow, not necessarily related to being near the margins or between mountains.

Near the Margins of the Greenland Ice Sheet,where Glacial Ice