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Crandell, Dwight Raymond

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Album Caption: Mount Rainier National Park, Washington. These arcuate end moraines of a former small cirque glacier are the type locality of the McNeeley Drift. The cirque is on the north slope of the Sourdough Mountains seven-tenths of a kilometer south of McNeeley Peak and almost directly north of the Sunrise Visitor Center at Yakima Park. Pumice layer R, which is more than 8,750 years old, overlies the outermost McNeeley moraine at this locality. Circa 1964. Pierce County, Washington. Published in U.S. Geological Survey Professional paper 847, figure 23. 1974.
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Album Caption: Mount Rainier National Park, Washington. Forested McNeeley and bare Garda moraines of a former cirque glacier at the north end of Old Desolate, north of Mount Rainier. The McNeeley glacier reached about 300 meters farther than did the Garda glacier. Circa 1964. Pierce County, Washington. Published in U.S. Geological Survey Professional paper 847, figure 24. 1974.
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Album Caption: Mount Rainier National Park, Washington. Four curved recessional moraines are spread over a distance of 2,000 feet on the valley floor of Fryingpan Creek. They were formed within the last few hundred years as Fryingpan Glacier lost volume and shrank back toward its present position above a line of cliffs. Circa 1967. Published in U.S. Geological Survey Bulletin 1292, figure 15. Published in U.S. Geological Survey Bulletin 1292, figure 14. (revised edition).
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Album Caption: Mount Rainier National Park, Washington. Rubble rill on the south side of a ridge 1.5 kilometers north of Mount Fremont, northeast of Mount Rainier. Man in center shows relative scale. Circa 1964. Pierce County, Washington. Published in U.S. Geological Survey Professional paper 847, figure 40. 1974.
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