|Cordilleran Section - 103rd Annual Meeting (4–6 May 2007)|
|Paper No. 36-7|
|Presentation Time: 3:35 PM-3:55 PM|
LITTLE ICE AGE FLUCTUATIONS OF GLACIERS ON MT. BAKER, WASHINGTON
DAVIS, P. Thompson1, OSBORN, Gerald2, RYANE, Chanone2, MENOUNOS, Brian3, and CLAGUE, John4, (1) Natural Sciences, Bentley College, Waltham, MA 02452-4705, email@example.com, (2) Geology and Geophysics, Univ. of Calgary, Calgary, AB T2N 1N4, (3) Geography Program, Univ of Northern British Columbia, Prince George, BC V2N 4Z9, Canada, (4) Earth Sciences, Simon Fraser University, 8888 University Drive, Burnaby, BC V5A1S6, Canada|
Composite lateral moraines of Coleman and Easton glaciers provide evidence for an advance of glaciers on Mt. Baker, Washington, during the past millennium. An unconformity about 12 m below the crest of the southwest lateral moraine of Coleman Glacier is marked by a laterally continuous wood mat that was first identified and dated by Don Easterbrook. The wood mat dips into the proximal flank of the moraine and contains logs up to 0.4 m diameter. We obtained a radiocarbon age of 940 ± 50 14C yr BP (AD 1000-1210) on one of the logs. The mat records a forested surface that was overridden by Coleman Glacier during an early Little Ice Age advance. Two unconformities exist in the east lateral moraine of Easton Glacier. The lower unconformity, approximately 40 m below the crest of the moraine, is marked by a mat of wood and deformed peat that gave an age of 5260 ± 70 14C yr BP (5910-6270 cal yr BP). The upper unconformity, located 4 m below the moraine crest, contains a thin layer of wood fragments and small logs. A piece of wood from the layer returned an age of 410 ± 40 yr BP (AD1430-1630). An advance of Coleman Glacier early during the past millennium is consistent with evidence for advances of the same age in the Coast Mountains of the British Columbia and the Canadian Rocky Mountains. The advance of Easton Glacier sometime after AD 1430 appears to be broadly synchronous with mid Little Ice Age advances of glaciers in the Garibaldi Provincial Park and in the Mount Waddington area of the southern Coast Mountains, British Columbia. Taken together, the evidence suggests that Little Ice Age glacier fluctuations at Mount Baker mirrored those in the Canadian Cordillera.
Cordilleran Section - 103rd Annual Meeting (4–6 May 2007)
General Information for this Meeting
|Session No. 36|
The Little Ice Age in Western North America
WWU–Communications Facility: CF120
1:30 PM-6:00 PM, Sunday, 6 May 2007
© Copyright 2007 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.