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Photographer’s Note

The Tâterât Glacier is fed directly from the Sukkertoppen (Sugar Loaf) ice pack which is an extension of the central ice cap.

Greenland’s ice cap contains 2.85 million cubic km of ice, in places over 3 km thick, 1/8th of the global total ice mass. The weight of the ice has depressed the center of Greenland so that if the ice were to melt, Greenland would appear as a ring of mountains surrounding a new sea and the global sea level would rise by 6 to 7 meters.

The ice of Greenland has been accumulating for 3 million years. Drilling cores in the ice reveals the history of ancient climates and changes in the earth’s atmosphere.

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Additional Photos by Peter Jennings (Geo) Gold Star Critiquer/Gold Star Workshop Editor/Gold Note Writer [C: 213 W: 57 N: 186] (1239)
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