History and drainage of large ice-dammed lakes along the Laurentide Ice Sheet
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Cited by (37)
Rise and fall of a small ice-dammed lake - Role of deglaciation processes and morphology
2017, GeomorphologyCitation Excerpt :Landscape and environmental changes of the glacial realm are commonly well recorded in the deposits of glacial lakes. Special attention has been devoted to the deposits of ice-dammed lakes because of catastrophic floods (Knight, 2003; Russell, 2007, 2009), effects of meltwater release on subglacial (Shaw, 2002) and proglacial environments (Magilligan et al., 2002), or spectacular ice-dam failures (Teller, 1995; Fisher et al., 2002). The presence and drainage of subglacial and proglacial lakes also have wider implications for terrestrial ice sheet stability, and marine processes including thermohaline circulation (Clark et al., 2001; Teller et al., 2002).
Glacial legacy effects on river landforms of the southern Laurentian Great Lakes
2015, Journal of Great Lakes ResearchCitation Excerpt :Rivers tend to respond to changes in baselevel (Schumm, 1993) which, in the context of this study, is the water surface elevation in the Lake Huron basin. The baselevel history for post-glacial fluvial systems draining to the Great Lakes is confounded by patterns of glacial isostatic rebound and changes in the major hydrological sources of water (Teller, 1995). The amount of glacial isostatic depression from the last glacial period generally varies with patterns of continental ice thickness over the late Pleistocene (Peltier, 2004), which in the Great Lakes region was greatest in the northeast, gradually decreasing to the southwest (Fig. 2B).
Introduction
2013, Encyclopedia of Quaternary Science: Second EditionGlaciolacustrine
2013, Encyclopedia of Quaternary Science: Second EditionLacustrine sediments in Porter Cave, Central Indiana, USA and possible relation to Laurentide ice sheet marginal positions in the middle and late Wisconsinan
2010, Palaeogeography, Palaeoclimatology, PalaeoecologyCitation Excerpt :This MIS 3 ice sheet is hypothesized to have advanced and retreated with variations in solar insolation and North Atlantic climate oscillations and to have a configuration at times closer to the MIS 2 extent than previously inferred (Clark et al., 1993; Dyke et al., 2002). The Laurentide ice sheet frequently pooled meltwater and diverted drainages forming proglacial lakes along the margin (cf. Teller, 1995). The focus of this study is the Mill Creek Valley of central Indiana (Fig. 1), which sits astride the mapped Late Wisconsinan margin and hosted proglacial lakes multiple times during the late Quaternary (Autio, 1990; Thornbury, 1940; Wood et al., 2010).
Provenance of freshwater pulses in the Gulf of Mexico during the last deglaciation
2010, Quaternary Research