The Drift River Lobe of the Double Glacier. The bare ice of the lower Double Glacier appears gray due to its thin mantle of Redoubt ash. This ash will accelerate melting of the glacier surface. ***AVO research technician Max Kaufman took these images during 3 days of campaign GPS work on and around Redoubt volcano: June 6,8,10 2009.
Image courtesy of the AVO/UAF-GI.
Please cite the photographer and the Alaska Volcano Observatory / University of Alaska Fairbanks, Geophysical Institute when using this image.
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