View Original Image at Full SizeFigure 6: Cross-section B-B’, running west to east across the slackwater terrace. SVS-26 and 30 are sediment cores used to check against geophysical data collected in Resistivity Lines 1-4. Note how the slackwater materials thicken eastward, away from the Mississippi River. This indicates the original location of Rush Creek at the time the slackwater materials were deposited. (Johnson, 2009.)
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Sep22 11
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Beth A. Johnson, University of Wisconsin-Oshkosh
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