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Glaciers Flow into a Greenland Valley
This page contains archived content and is no longer being updated. At the time of publication, it represented the best available science. However, more recent observations and studies may have rendered some content obsolete.
Small glaciers spill into a mostly dry valley in western Greenland in this picture from August 29, 2009. The Advanced Land Imager (ALI) on NASA’s Earth Observing-1 (EO-1) satellite acquired this natural-color image. The top view shows the wider area and the bottom view is a close-up of two glacier snouts.
The close-up image allows a clear view of both snouts’ rough surfaces. While ice at the bottom of a glacier generally flows smoothly, the ice overhead is often brittle. As a result, the glacier’s movement causes ruptures on the ice surface, which can be exacerbated by surface melting. Foehn winds—warm, dry, down-slope winds—may contribute to glacier melt, and also keep the underlying valley mostly dry. The shallow, blue-green water in the valley bottom is likely laced with rock flour left over from earlier glacial grinding of Greenland’s rocks.
Multiple glaciers frequently flow into straight valleys in Greenland. The valleys result from earlier glaciations that carved the bedrock. The smaller glaciers that flow into the valley may take advantage of weak joints in the bedrock.
NASA image created by Jesse Allen, using EO-1 ALI data provided courtesy of the NASA EO-1 Team. Caption by Michon Scott based on image interpretation by Ian Howat of the Byrd Polar Research Center and Ted Scambos of the National Snow and Ice Data Center.
These true-color images show wide-area and close-up views of glaciers flowing into a largely dry, linear valley in western Greenland on August 29, 2009.