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Growth of a post-Little Ice Age submarine fan, Glacier Bay, Alaska

January 1, 1999

A small Holocene fan is forming where Queen Inlet, a hanging valley, enters West Arm fjord, Glacier Bay, Alaska. Queen fan formed in the last 80 years following retreat of the Little Ice Age glacier that filled Glacier Bay about 200 yr BP. It was built mainly by a turbidite system originating from Carroll Glacier delta, as the delta formed in the early 1900s at the head of Queen Inlet. The Late Holocene Queen fan is comparable to large Pleistocene fans that formed in the Gulf of Alaska and differs from trough-mouth fans formed by cooler climate glacier systems.

Publication Year 1999
Title Growth of a post-Little Ice Age submarine fan, Glacier Bay, Alaska
DOI 10.1007/s003670050113
Authors P. R. Carlson, E. A. Cowan, R. D. Powell, J. Cai
Publication Type Article
Publication Subtype Journal Article
Series Title Geo-Marine Letters
Index ID 70020912
Record Source USGS Publications Warehouse