Age of marginal Wisconsin drift at Corry, northwestern Pennsylvania

J.B. Droste; M. Rubin; G. W. White

doi:10.1126/science.130.3391.1760.a

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Age of marginal Wisconsin drift at Corry, northwestern Pennsylvania

J.B. Droste·M. Rubin·G. W. White

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Abstract

Marl began to accumulate about 14,000 years ago, as determined by radiocarbon dating, in a pond in a kettle hole in Kent drift at Corry, Pa., 9 miles inside the Wisconsin drift margin. This radiocarbon age represents the minimum time since the disappearance of the ice from Corry and confirms an assignment of Cary age to the drift.

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Source-reported bounding extent: 41.904127695039165° to 41.947621733403906° latitude; -79.68200482460028° to -79.60218635375541° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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BibTeX RIS

J.B. Droste, M. Rubin, G. W. White. 1959. Age of marginal Wisconsin drift at Corry, northwestern Pennsylvania. https://doi.org/10.1126/science.130.3391.1760.a

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