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Radiocarbon Age Constraints on Rates of Advance and Retreat of the Puget Lobe of the Cordilleran Ice Sheet during the Last Glaciation

Published online by Cambridge University Press:  20 January 2017

Stephen C. Porter  and
Terry W. Swanson
Stephen C. Porter
Affiliation:
Quaternary Research Center and Department of Geological Sciences, University of Washington, Seattle, Washington, 98195-1360
Terry W. Swanson
Affiliation:
Quaternary Research Center and Department of Geological Sciences, University of Washington, Seattle, Washington, 98195-1360
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Abstract

Calibrated radiocarbon dates of organic matter below and above till of the last (Fraser) glaciation provide limiting ages that constrain the chronology and duration of the last advance–retreat cycle of the Puget Lobe in the central and southeastern Puget Lowland. Seven dates for wood near the top of a thick proglacial delta have a weighted mean age of 17,420 ± 90 cal yr B.P., which is the closest limiting age for arrival of the glacier near the latitude of Seattle. A time–distance curve constructed along a flowline extending south from southwestern British Columbia to the central Puget Lowland implies an average glacier advance rate of ca. 135 m/yr. The glacier terminus reached its southernmost limit ca. 16,950 yr ago and likely remained there for ca. 100 yr. In the vicinity of Seattle, where the glacier reached a maximum thickness of 1000 m, ice covered the landscape for ca. 1020 yr. Postglacial dates constraining the timing of ice retreat in the central lowland are as old as 16,420 cal yr B.P. and show that the terminus had retreated to the northern limit of the lowland within three to four centuries after the glacial maximum. The average rate of retreat was about twice the rate of advance and was enhanced by rapid calving recession along flowline sectors where the glacier front crossed deep proglacial lakes.

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Type
Original Articles
Information
Quaternary Research , Volume 50 , Issue 3 , November 1998 , pp. 205 - 213
Copyright
University of Washington

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