As summarized in Rech and others, various studies have dated the buried logs and stumps from the Two Creeks forest using radiocarbon dating and analyzed their growth rings to determine a minimum lifespan for the forest.[3] Initial research into the age of this buried forest indicated an calibrated age range of ~13,840–13,620 cal BP and a minimum lifespan for the forest of ~230 to 250 yr.[4][5] Later research by Leavitt and others indicated a minimum lifespan of 329 yr for the Two Creeks and an age range of 13,760–13,530 cal BP.[6]
The lower layer of glacial till was deposited during the end of the Woodfordian substage of the Wisconsin glaciation. The remains in the park demonstrate that a warmer interval, called the Twocreekan substage, followed in which the glacier retreated and a forest of spruce, pine, and hemlock grew. Then the climate cooled again and the Greatlakean substage began.[7] A glacial tongue blocked Lake Michigan's drainage, causing the water level to rise and flood the forest, carrying in sediments which buried the forest floor. The glacier proceeded to flow over the forest, flattening it and ultimately depositing another layer of glacial till over it.[8]
Two Creeks Buried Forest State Natural Area is open to visitation. There is an historical marker at the location.[9] The site has no trails or displays, but visitors can park in the northwest corner of the site and wander freely across the grounds. Collection of any material is prohibited.[10]
^ abRech, J.A., Nekola, J.C. and Pigati, J.S., 2012. Radiocarbon ages of terrestrial gastropods extend duration of ice-free conditions at the Two Creeks forest bed, Wisconsin, USA.Quaternary Research, 77(2), pp.289-292.
^Broecker, W.S. and Farrand, W.R., 1963. Radiocarbon age of the Two Creeks forest bed, Wisconsin.Geological Society of America Bulletin, 74(6), pp.795-802.
^Kaiser, K.F., 1994. Two Creeks Interstade dated through dendrochronology and AMS. Quaternary Research, 42(3), pp.288-298.
^
Leavitt, S.W., Panyushkina, I.P., Lange, T., Cheng, L., Schneider, A.F. and Hughes, J., 2007. Radiocarbon “wiggles” in great lakes wood at about 10,000 to 12,000 BP.Radiocarbon, 49(2), pp.855-864.
^Evenson, E.B., Farrand, W.R., Eschman, D.F., Mickelson, D.M. and Maher, L.J., 1976. Greatlakean substage: a replacement for valderan substage in the lake Michigan basin.Quaternary Research, 6(3), pp.411-424.
^Mickelson, D.M., Hooyer, T.S., Socha, B.J., Winguth, C., 2007. Late-glacial ice advances and vegetation changes in east-central Wisconsin. In: Hooyer, T.S. (Ed.), Late-Glacial History of East-Central Wisconsin, Wisconsin Geological and Natural History Survey Open-File Report, 2007-01. pp. 72–87.
^"An Ancient Forest Bed". Wisconsin Historical Markers. August 31, 2013. Archived from the original on April 3, 2014. Retrieved September 6, 2013.
^Meyer, T., ed. Wisconsin, Naturally: A Guide to 150 Great State Natural Areas. Madison, Wisconsin, Wisconsin Department of Natural Resources, Bureau of Endangered Resources, State Natural Areas Program, 184 pp.
