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- W2081566757 abstract "The scarcity of lake basins in Alberta dating earlier than 11,000 BP has been interpreted as indicating the continued presence of active glacial ice. Because of the related implication that the presence of ice precludes the existence of an ice-free corridor, it is useful to examine this issue more closely. Due to the effects of deglaciation, many areas of Alberta were dominated by chaotic ice-stagnation conditions, with continual reversal of topography and rapid transformation of the surface. The dynamic nature of the environment affects arguments regarding the existence of an ice-free corridor as well as having implications for archeological site formation, preservation and discovery. Deglaciation models utilizing paradigms of active ice retreat may result in dichotomous depictions of the land surface as either ice covered or deglaciated. Due to the insulating properties of supraglacial debris, stagnant ice results in a situation that is simultaneously neither and both of the above conditions. While the landscape is ice covered and thus not ‘ice-free’, an accessible landscape characterized by glacial karst topography exists on top of the stagnating ice surface. General reconstructions of the impact of stagnant ice and glacial karst topography on the paleogeography of Alberta are presented for discussion." @default.
- W2081566757 created "2016-06-24" @default.
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- W2081566757 date "1996-01-01" @default.
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- W2081566757 title "Late Wisconsinan deglaciation of Alberta: Processes and paleogeography" @default.
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- W2081566757 doi "https://doi.org/10.1016/1040-6182(95)00054-2" @default.
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