16 Undergraduate Research (Posters)

Monday, 18 May 2020
8:30 AM - 5:30 PM
Lake Superior Ballroom KJ

INTERPRETATIONS OF QUATERNARY LANDSCAPE DEVELOPMENT IN THE BUFFALO RIVER VALLEY USING SEDIMENTOLOGIC AND STRATIGRAPHIC ANALYSIS: MSUM REGIONAL SCIENCE CENTER IN WEST-CENTRAL MINNESOTA

Paper number: 16-4
Program: Theme Sessions
Time: 8:30 AM – 5:30 PM

Authors

Abstract

Being able to understand the evolution of a landscape is critical for geologic and archaeologic research. Understanding paleotopography in relation to geomorphic history has the potential to enhance predictive models for locating archaeological sites. This study focuses on the collaborative efforts of Archaeologists at MSUM, Geomorphologists at Wisconsin Eau Claire, and Geologists at North Dakota State University focuses on landscape evolution in the area now occupied by the MSUM Regional Science Center (“RSC”). Analysis thus far has included sedimentological analyses of pit excavations, description of river cuts, examination of sediment cores, and sieve analysis of bulk sediment samples.

Study sites occur primarily in the incised valley margin of a glacio/deltaic complex developed on the eastern margin of glacial Lake Agassiz. Modern soils developed on aeolian sheet sands directly overlying fluvial gravels, which are underlain by sediments interpreted as offshore bar forms. These deposits lie west of a major shoreline of glacial Lake Agassiz.

Buried and partially developed soil horizons have been identified by field examination of excavated profiles, and these may be important for the recovery of artifacts that date back to the Early Archaic. Proximity of fluvial gravels appear to act as an erosional barrier allowing for the preservation of paleo-topographic highs (offshore bars). Thicker aeolian sands accumulate in close proximity to these preserved bar forms and appear to favor the development of buried horizons. Both OSL and 14C dates are being analyzed to build a chronology for correlation of buried soil horizons. Four OSL dates (in years) have been obtained at the base of the aeolian sheet sand at three localities and are; 8340, 8300, 8500, and 12,520. The offshore bars are a key factor in predicting the location of archaeological sites and understanding how the landscape has changed over time.

Geological Society of America Abstracts with Programs. Vol. 52, No. 5

doi: 10.1130/abs/2020NC-348302

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