Evidence for Stagnation of the Harvard Sublobe (Lake Michigan Lobe) in Northeastern Illinois, U.S.A., from 24 000 to 17 600 BP and Subsequent Tundra-Like Ice-Marginal Paleoenvironments from 17 600 to 15 700 BP
Brandon B. Curry
Illinois State Geological Survey, 615 East Peabody Drive, Champaign, IL, 61820-6964, United States
Catherine H. Yansa
Department of Geography, Michigan State University, 125 Natural Sciences Building, East Lansing, MI, 48824‑1115, United States
Plan de l'article
The last glaciation in northeastern Illinois
Sediment succession of the last glaciation in northeastern Illinois
Hampshire Quadrangle ice-walled lake deposits
Fox River Stone Company site (FRSC)
Sleepy Hollow flood retention pond
Randall Road bridge over Tyler Creek
Nelson Lake and Crystal Lake, Brewster Creek, and Mastodon Lake
Paleohydrological interpretation
Paleoenvironments of northeastern Illinois
Comparison with other coeval fossil localities
Tundra localities outside the upper Midwest
| Auteurs : | Brandon B. Curry et Catherine H. Yansa |
|---|---|
| Titre : | Evidence for Stagnation of the Harvard Sublobe (Lake Michigan Lobe) in Northeastern Illinois, U.S.A., from 24 000 to 17 600 BP and Subsequent Tundra-Like Ice-Marginal Paleoenvironments from 17 600 to 15 700 BP |
| Revue : | Géographie physique et Quaternaire, Volume 58, numéro 2-3, 2004, p. 305-321 |
| URI : | http://id.erudit.org/iderudit/013145ar |
| DOI : | 10.7202/013145ar |
Tous droits réservés © Les Presses de l'Université de Montréal, 2006

