Ice streams and lakes under the Greenland Ice Sheet

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The Greenland ice sheet is not a static body of ice but instead a dynamic body of dense, flowing and deforming ice. Snow deposited on the central parts of the ice sheet is gradually compressed to ice that slowly flows towards the ice margin.

Greenland ice sheet - Wikipedia

Greenland's ice is melting from the bottom up and far faster than previously thought

A check on runaway lake drainage, MIT News

Greenland ice sheet melting could expose 400 million people to flooding by end of century, study says - ABC News

Greenland-wide inventory of ice marginal lakes using a multi-method approach

Meltwater is infiltrating Greenland's ice sheet through millions of hairline cracks – destabilizing its structure

Archive photos reveal Greenland's contribution to sea level rise - Carbon Brief

Research - Cryo-Hydrologic Remote Sensing

NASA Continues to Research Greenland Ice Sheet Melt and Sea Level Rise

Buried remnants of the Laurentide Ice Sheet and connections to its surface elevation

Frontiers The Influence of Hydrology on the Dynamics of Land-Terminating Sectors of the Greenland Ice Sheet