New insights on Illinoian deglaciation from deposits of Glacial Lake Quincy, central Indiana

The deposits of Glacial Lake Quincy overlie a diamicton associated with the classically defined Illinoian limit in central Indiana. This lake covered at least 180 km2 with a depth of > 20 m and developed when the Illinoian ice sheet retreated 15 km from the maximum limit, causing lake impoundment...

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Veröffentlicht in:	Quaternary research 2010-03, Vol.73 (2), p.374-384
Hauptverfasser:	Wood, J.R., Forman, S.L., Pierson, J., Gomez, J.
Format:	Artikel
Sprache:	eng
Schlagworte:	Age Deglaciation Deposition Freshwater Glacial lacustrine sediments Illinoian limit Lakes Marine Optical dating Original Articles Regenerative Ridges Sediments Sunlight
Online-Zugang:	Volltext
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