@inbook {1398,
	title = {The deglaciation of eastern Maine: in Deglacial history and relative sea-level changes, northern New England and adjacent Canada},
	booktitle = {Deglacial history and relative sea-level changes, northern New England and adjacent Canada},
	series = {Special papers (Geological Society of America)},
	year = {2001},
	note = {id: 1310},
	month = {2001},
	publisher = {Geological Society of America},
	organization = {Geological Society of America},
	isbn = {0813723515},
	author = {Dorion, C. C. and Kaplan, M. R. and Kreutz, K. J. and Balco, G. and Wright, J. and Borns, H. W., Jr.},
	editor = {Weddle, T. K.}
}
@article {1488,
	title = {Stratigraphy, paleoceanography, chronology, and paleoenvironment during deglaciation of eastern Maine, Report},
	volume = {242},
	year = {2001},
	note = {id: 1333},
	month = {2001},
	pages = {215},
	institution = {Geological Society of America},
	address = {Boulder, CO},
	author = {Dorion, C. C. and Balco, G. and Kaplan, M. R. and Kreutz, K. J. and Wright, J. and Borns, H. W.}
}
@inbook {1425,
	title = {Late Pleistocene and Holocene geological evolution of the central Penobscot River Valley: Surficial geology, geoarchaeology, and water supply (Book Section)},
	booktitle = {Guidebook for Field Trips in Coastal and East-Central Maine: NEIGC 92nd Annual Meeting},
	year = {2000},
	note = {id: 152},
	month = {2000},
	address = {Orono, ME},
	author = {Kelly, A. R. and Dorion, C. C. and Balco, G. and Dieffenbacher-Krall, A. and Garrett, P. and Locke, D. and Tolman, A.},
	editor = {Yates, M. G.}
}
@article {872,
	title = {Glacioisostasy and lake-level change at Moosehead lake, Maine},
	journal = {Quaternary Research},
	volume = {49},
	year = {1998},
	note = {Zm315Times Cited:9Cited References Count:46},
	month = {Mar},
	pages = {157-170},
	abstract = {Reconstructions of glacioisostatic rebound based on relative sea level in Maine and adjacent Canada do not agree well with existing geophysical models. In order to understand these discrepancies better, we investigated the lake-level history of 40-km-long Moosehead Lake in northwestern Maine. Glacioisostasy has affected the level of Moosehead Lake since deglaciation ca. 12,500 C-14 yr B.P. Lowstand features at the southeastern end and an abandoned outlet at the northwestern end of the lake indicate that the lake basin was tilted down to the northwest, toward the retreating ice sheet, by 0.7 m/km at 10,000 C-14 yr B.P. Water level then rose rapidly in the southeastern end of the lake, and the northwestern outlet was abandoned, indicating rapid relaxation of landscape tilt. Lowstand features at the northwestern end of the lake suggest that the lake basin was tilted to the southeast at ca. 8750 C-14 yr B.P., possibly as the result of a migrating isostatic forebulge. After 8000 C-14 yr B.P., water level at the southeastern end was again below present lake level and rose gradually thereafter. We found no evidence suggesting that postglacial climate change significantly affected lake level. The rebound history inferred from lake-level data is consistent with previous interpretations of nearby relative sealevel data, which indicate a significantly steeper and faster-moving ice-proximal depression and ice-distal forebulge than geophysical models predict. (C) 1998 University of Washington.},
	issn = {0033-5894},
	doi = {10.1006/qres.1998.1962},
	author = {Balco, G. and Belknap, D. F. and Kelley, J. T.}
}
@article {877,
	title = {Paleoclimatic implications of Holocene lake-level fluctuations, Owasco Lake, New York: Comment},
	journal = {Geology},
	volume = {25},
	year = {1997},
	note = {Wu319Times Cited:0Cited References Count:7},
	month = {04/1997},
	pages = {383-383},
	issn = {0091-7613},
	author = {Balco, G. and Belknap, D. F. and Kelley, J. T.}
}
