Barry Goldstein
University of Puget Sound, Tacoma, WA
Activity
2020
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THE TANWAX-OHOP VALLEY FLOOD AND DEBRIS FLOW, AN ICE AGE FLOOD FROM THE CASCADE RANGE INTO THE SOUTHERN PUGET LOWLAND AND LIKELY SOURCE OF SEDIMENTS FOR THE MIMA MOUNDS
T250 On the Edge—New Insights into Ice-Marginal Conditions IIFriday, 30 October 202010:00 AM - 2:00 PMMeeting Rooms
2016
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SEDIMENTOLOGICAL ANALYSIS OF THE BASAL MEMBER OF THE CHINLE FORMATION AND ITS PALEOGEOGRAPHIC AND PALEOHYDROLOGIC IMPLICATIONS
5 Sedimentology and Stratigraphy (Posters)Monday, 4 April 20168:30 AM - 5:30 PMBallroom C