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Proglacial Lakes

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Part of the book series: Encyclopedia of Earth Sciences Series ((EESS))

Definition

Proglacial lake. Ice-contact lake occurring adjacent to the frontal margin of a glacier.

Introduction

A proglacial lake abuts and extends beyond the glacier terminus. Many proglacial lakes are moraine-dammed, whereas others form in basins created by isostatic depression near the ice margin. These latter lakes commonly are buttressed by the ice itself. Not all ice-dammed lakes, however, are proglacial, so these terms are not strictly synonymous. Some ice-dammed lakes, for instance, form laterally, such as when a glacier dams river flow in a side valley. Possibly the best-known ice-dammed lake was Glacial Lake Missoula, which occupied thousands of square kilometers of western Montana and Idaho before draining catastrophically (many times) to the Pacific.

Proglacial lakes can be ephemeral in nature or persist hundreds, if not thousands of years. The transient nature of some lakes results from several processes, including drainage (catastrophic or otherwise) caused by breaching...

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Bibliography

  • Allen, S., Schneider, D., and Ovens, I., 2009. First approaches towards modelling glacial hazards in the Mount Cook region of New Zealand’s Southern Alps. Natural Hazards and Earth System Sciences, 9, 481–499.

    Google Scholar 

  • Barber, D., Dyke, A., Hillaire-Marcel, C., Jennings, A., Andrews, J., Kerwin, M., Bilodeau, G., McNeely, R., Southon, J., Morehead, M., and Gagnon, J.-M., 1999. Forcing of the cold event of 8200 years ago by catastrophic drainage of Laurentide lakes. Nature, 400, 344–348.

    Google Scholar 

  • Hendy, C. H., Sadler, A. J., Denton, G. H., and Hall, B. L., 2000. Proglacial lake-ice conveyors: a new mechanism for deposition of drift in polar environments. Geografiska Annaler, 82A, 249–270.

    Google Scholar 

  • Leemann, A., and Niessen, F., 1994. Holocene glacial activity and climatic variations in the Swiss Alps – reconstructing a continuous record from proglacial lake sediments. The Holocene, 4, 259–268.

    Google Scholar 

  • Lliboutry, L., Morales Arnao, B., Pautre, A., and Schneider, B., 1977. Glaciological problems set by the control of dangerous lakes in Cordillera Blanca, Peru. I: historic failure of moraine dams, their causes and prevention. Journal of Glaciology, 18, 239–254.

    Google Scholar 

  • Lowell, T., Fisher, T., Comer, G., Hajdas, I., Waterson, N., Glover, K., Loope, H., Schaefer, J., Rinterknecht, V., Broecker, W., Denton, G., and Teller, J., 2005. Testing the Lake Agassiz meltwater trigger for the Younger Dryas. EOS. Transactions of the American Geophysical Union, 86(40), 365, 372.

    Google Scholar 

  • Nesje, A., Matthews, J., Dahl, S., Berrisford, M., and Andersson, C., 2001. Holocene glacier fluctuations of Flatebreen and winter-precipitation changes in the Jostedalsbreen region, western Norway, based on glaciolacustrine sediment records. The Holocene, 11, 267–280.

    Google Scholar 

  • Richardson, S., and Reynolds, J., 2000. An overview of glacial hazards in the Himalayas. Quaternary International, 65(66), 31–47.

    Google Scholar 

  • Shakesby, R. A., Smith, J. G., Matthews, J. A., Winkler, S., Dresser, P. Q., Bakke, J., Dahl, S. O., Lie, Y., and Nesje, A., 2007. Reconstruction of Holocene glacier history from distal sources: glaciofluvial stream-bank mires and a glaciolacustrine sediment core near Sota Søter, Breheimen, southern Norway. The Holocene, 17, 729–745.

    Google Scholar 

  • Teller, J. T., 2004. Controls, history, outbursts, and impact of large late-Quaternary proglacial lakes in North America. In Gillespie, A., Porter, S., and Atwater, B. (eds.), The Quaternary Period in the United States. Amsterdam: Elsevier, pp. 45–61.

    Google Scholar 

  • Teller, J. T., and Leverington, D. W., 2004. Glacial Lake Agassiz: a 5000-year history of change and its relationship to the δ18O record of Greenland. Geological Society of America Bulletin, 116, 729–742.

    Google Scholar 

  • Thomas, E., and Briner, J., 2009. Climate of the past millennium inferred from varved proglacial lake sediments on northeast Baffin Island, Arctic Canada. Journal of Paleolimnology, 41, 209–224.

    Google Scholar 

  • Warren, C., and Kirkbride, M., 2003. Calving speed and climatic sensitivity of New Zealand lake-calving glaciers. Annals of Glaciology, 36, 173–178.

    Google Scholar 

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Correspondence to Brenda L. Hall .

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© 2011 Springer Science+Business Media B.V.

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Hall, B.L. (2011). Proglacial Lakes. In: Singh, V.P., Singh, P., Haritashya, U.K. (eds) Encyclopedia of Snow, Ice and Glaciers. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-2642-2_420

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