Abstract
Oxygen isotopic data were used to assess how far waters from the Savannah River, a major river in the Southeastern United States, backed up and inundated the wetlands along a small Coastal Plain tributary during a flood. This approach worked because the water of this tributary, Unper Three Runs, had an oxygen isotopic composition (δ18O = −4.9 ‰) distinct from Savannah River water (δ18O = −3.2 ‰).
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