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Additional info for Subsurface geologic investigations of New York Finger Lakes: impliations for Late Quaternary deglaciation and environmental change (GSA Special Paper 311)
Hundreds to thousands of meters per year over periods of hundreds of years” (p. 20). In the case of its southern margin, the Laurentide ice sheet advanced 300 to 800 km between about 15 and 14 ka, correlative with Heinrich event H-1 (Clark, 1994). Most recently, Blanchon and Shaw (1995) have suggested that Laurentide ice sheet instability and collapse during H-1 was triggered by the storage and release of large volumes of glacial meltwaters, recorded as catastrophic sea-level rises in coral reef sequences.
King, J. , Banerjee, S. , 1983, Use of small scale–amplitude paleomagnetic fluctuations for correlation and dating of continental climatic changes: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 42, p. 167–183. King, L. , Fader, G. B. , 1991, Tilltongue stratigraphy: Geological Society of America Bulletin, v. 103, p. 637–659. Krall, D. , 1977, Late Wisconsin ice recession in east-central New York: Geological Society of America Bulletin, v. 88, p. 1697–1710. Lehman, J. , 1975, Reconstructing the rate of accumulation of lake sediment: The effect of sediment focusing: Quaternary Research, v.
And Wright, H. , North America and adjacent oceans during the last deglaciation: Boulder, Colorado, Geological Society of America, Geology of North America, v. K-3, p. 183–220. , 1992, Abrupt climate change related to unstable ice-sheet dynamics: Toward a new paradigm: Palaeogeography, Palaeoclimatology, Palaeoecology (Global and Planetary Change Section), v. 97, p. 203–234. Iverson, N. , Hooke, R. , 1995, Flow mechanism of glaciers on soft beds: Science, v. 267, p. 80–81. Karrow, P. , Warner, B.