Research Article| December 01, 1985 Correlation of late Wisconsin glacial phases in the western Great Lakes area JOHN W. ATTIG; JOHN W. ATTIG 1Wisconsin Geological and Natural History Survey, 3817 Mineral Point Road, Madison, Wisconsin 53705 Search for other works by this author on: GSW Google Scholar LEE CLAYTON; LEE CLAYTON 1Wisconsin Geological and Natural History Survey, 3817 Mineral Point Road, Madison, Wisconsin 53705 Search for other works by this author on: GSW Google Scholar DAVID M. MICKELSON DAVID M. MICKELSON 2Department of Geology and Geophysics, University of Wisconsin, Madison, Wisconsin 53706 Search for other works by this author on: GSW Google Scholar Author and Article Information JOHN W. ATTIG 1Wisconsin Geological and Natural History Survey, 3817 Mineral Point Road, Madison, Wisconsin 53705 LEE CLAYTON 1Wisconsin Geological and Natural History Survey, 3817 Mineral Point Road, Madison, Wisconsin 53705 DAVID M. MICKELSON 2Department of Geology and Geophysics, University of Wisconsin, Madison, Wisconsin 53706 Publisher: Geological Society of America First Online: 01 Jun 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (1985) 96 (12): 1585–1593. https://doi.org/10.1130/0016-7606(1985)96<1585:COLWGP>2.0.CO;2 Article history First Online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation JOHN W. ATTIG, LEE CLAYTON, DAVID M. MICKELSON; Correlation of late Wisconsin glacial phases in the western Great Lakes area. GSA Bulletin 1985;; 96 (12): 1585–1593. doi: https://doi.org/10.1130/0016-7606(1985)96<1585:COLWGP>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract Late Wisconsin glacial phases of the Superior Lobe in Wisconsin and adjacent Minnesota are tentatively correlated across northern Wisconsin and adjacent Michigan to phases of the Green Bay and Lake Michigan Lobes. Spanning the period from about 26,000 yr B.P. to about 9500 yr B.P., 7 phases of the late Wisconsin Laurentide Ice Sheet are discussed, but only 2 of these are precisely dated.Ice advanced out of the basins of Lakes Superior and Michigan and stabilized during the St. Croix-Hancock phase, the most extensive late Wisconsin phase in most of the area, between about 18,000 and 15,000 yr ago. Following the St. Croix-Hancock phase, the general wasting of the ice was interrupted by stillstands or readvances of the ice margin during the intermediate and Mountain phases. The ice then wasted into the Superior basin before readvancing, over a landscape containing ice masses from earlier phases, during the Winegar-early Athelstane phase. This phase is believed to have occurred just prior to growth of the Two Creeks Forest in eastern Wisconsin. The ice then wasted back and advanced three more times during the Marenisco-late Athelstane, Porcupine (about 11,000 yr B.P.), and Marquette (about 9900 yr B.P.) phases. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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