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Rapid Late Pleistocene Incision of Atlantic Passive-Margin River Gorges

2004; American Association for the Advancement of Science; Volume: 305; Issue: 5683 Linguagem: Inglês

10.1126/science.1097780

1095-9203

Luke J. Reusser, Paul R. Bierman, Milan J. Pavich, E‐an Zen, Jennifer Larsen, Robert C. Finkel,

Geological formations and processes

The direct and secondary effects of rapidly changing climate caused large rivers draining the Atlantic passive margin to incise quickly into bedrock beginning about 35,000 years ago. Measured in samples from bedrock fluvial terraces, 10-beryllium shows that both the Susquehanna and Potomac Rivers incised 10- to 20-meter-deep gorges along steep, convex lower reaches during the last glacial cycle. This short-lived pulse of unusually rapid down-cutting ended by 13,000 to 14,000 years ago. The timing and rate of downcutting are similar on the glaciated Susquehanna and unglaciated Potomac Rivers, indicating that regional changes, not simply glacial meltwater, initiated incision.