Skip to main content
Article
The Most Extensive Holocene Advance in the Stauning Alper, East Greenland, Occurred in the Little Ice Age
Polar Research
  • Brenda L. Hall, University of Maine - Main
  • Carlo Baroni
  • George H. Denton, University of Maine - Main
Document Type
Article
Rights and Access Note
This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. In addition, no permission is required from the rights-holder(s) for educational uses. For other uses, you need to obtain permission from the rights-holder(s).
Publication Date
8-1-2008
Disciplines
Abstract/ Summary

We present glacial geologic and chronologic data concerning the Holocene ice extent in the Stauning Alper of East Greenland. The retreat of ice from the late-glacial position back into the mountains was accomplished by at least 11 000 cal years B.P. The only recorded advance after this time occurred during the past few centuries (the Little Ice Age). Therefore, we postulate that the Little Ice Age event represents the maximum Holocene ice extent in this part of East Greenland.

Citation/Publisher Attribution
Hall, BL, Baroni, C, and Denton, GH, 2008, The Most Extensive Holocene Advance in the Stauning Alper, East Greenland, Occurred in the Little Ice Age: Polar Research, v. 27, p. 128-134.
DOI
10.1111/j.1751-8369.2008.00058.x
Version
publisher's version of the published document
Citation Information
Brenda L. Hall, Carlo Baroni and George H. Denton. "The Most Extensive Holocene Advance in the Stauning Alper, East Greenland, Occurred in the Little Ice Age" Polar Research Vol. 27 Iss. 2 (2008) p. 128 - 134
Available at: http://works.bepress.com/brenda_hall/2/