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Expedition to East
Greenland 1962 A party of four (David Sugden, Brian John, Sandy Hall and Svend Wurm) spent part of August 1962 on a reconnaissance survey of the glacier, which at that time was not heavily crevassed apart from one distinct icefall. In their glaciological studies they noticed ice
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Two climbing parties, one in 1976 and the other in 2013, found that the glacier was heavily crevassed and impassable in places. The neighbouring glacier, Løberen, is renowned as one of the fastest-flowing surging glaciers in
Greenland.
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temperature anomalies which were difficult to explain. They did not know it at the time, but they had discovered some of the earliest evidence of surging behaviour.
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Please help improve this article by looking for better, more reliable sources. Unreliable citations may be challenged and removed.
197:"AAC Publications - Oxford Glacier, Island Peak, East Face and South Ridge; Snow Dome, North Ridge; Panorama Peak, South Ridge"
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John, BS and Sugden, DE. 1963. Report of the OU Expedition to East
Greenland, 1962. OU Expedition Club Bulletin 12, 16 pp.
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118:. On older maps it is referred to as Uranus Glacier. It was named in recognition of the work of the
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155:"Stonehenge and the Ice Age: Oxford Gletscher -- the surface thermal regime of a surging glacier"
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Sugden, DE. 2008. "OU Expedition to East
Greenland, 1962: David Sugden's Diary", 67 pp.
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Traverse of the
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