Glacial lake sedimentation and Holocene glacial history, Canadian Rocky Mountains

This project is aimed at understanding the relationship between glacial activity and sediment production, and at use of proglacial lake sediment sequences as indicators of upvalley glacial activity. Field work on the project has been undertaken in Banff and Jasper National Parks in Alberta and and Yoho National Park in British Columbia.

Vibra-coring at Hector Lake in Banff national Park, Alberta (courtesy of Christian Baxter)

Publications:
(* denotes Colorado College student co-author)

  • Leonard, E.M. and Reasoner, M.A., 1999, A continuous Holocene record inferred from proglacial lake sediments in Banff National Park, Alberta, Canada. Quaternary Research 51, 1-13.
  • Leonard, E.M., 1997, The relationship between glacial activity and sediment production: evidence from a 4450-year varve record of Neoglacial sedimentation in Hector Lake, Alberta, Canada: Journal of Paleolimnology 17, 319-330.
  • Leonard, E.M., 1995, A varve-based calibration of the Bridge River tephra fall: Canadian Journal of Earth Sciences 32, 2098-2102.
  • Leonard, E.M., 1990, An assessment of sediment loss and distortion at the top of short gravity cores: Sedimentary Geology 66, 57-63.
  • Leonard, E.M., 1986, Use of lacustrine sedimentary sequences as indicators of Holocene glacial history, Banff National Park, Alberta, Canada: Quaternary Researrch 26, 218-231.
  • Leonard, E.M., 1986, Varve studies at Hector Lake, Alberta, Canada, and the relationship between glacial activity and sedimentation: Quaternary Research 25, 199-214.
  • Leonard, E.M., 1985, Glaciological and climatic controls on lake sedimentation, Canadian Rocky Mountains: Zeitschrift für Gletscherkunde and Glazialgeologie 21, 35-42.
Abstracts:

  • Leonard, E.M., 1998, Is the type-Crowfoot Moraine, Alberta, really a Younger Dryas equivalent? Geological Society of America Abstracts with Programs, 30, 66.
  • *Dehn, G.A., Reasoner, M.A., and Leonard, E.M., 1998, Late Quaternary vegetation and climatic change in the Canadian Rocky Mountain Region: Evidence from the Dianna Lake pollen record. Geological Society of America Abstracts with Programs, 30, 284.
  • Leonard, E.M. and Reasoner, M.A., 1996, Altithermal of the Canadian Rockies – timing and internal structure: evidence from lake sediments: American Quaternary Association Program and Abstracts,14th biennial meeting, 173.
  • Leonard, E.M., 1995, Use of glaciolacustrine sediment records in reconstructing high-altitude glacial history and climatic change in the Canadian Rocky Mountains: Abstracts of Workshop on Climatic Change at High Altitude Sites, Wengen, Switzerland, 38.
  • Leonard, E.M. and Reasoner, M.A., 1995, High-resolution record of Neoglacial sedimentation in a 5000 year varved core from Hector Lake, Alberta: Canadian Quaternary Association Abstracts.
  • Leonard, E.M., 1987, New evidence on early to mid Holocene environmental changes and glacial activity, central Canadian Rocky Mountains: Programme with Abstracts, International Union for Quaternary Research, XIIth International Congress, 209.
  • Leonard, E.M., 1984, Glaciological and climatic controls on lake sedimentation, Canadian Rocky Mountains: Symposium on Climate and Paleoclimate of Lakes, Rivers, and Glaciers, Innsbruck, Austria, 11.
  • Leonard, E.M., 1982, Controls on sediment yield in a glacial environment: Geological Society of America Abstract with Programs 14, 545.
  • Leonard, E.M., 1982, Holocene glacial history, Central Canadian Rocky Mountains: evidence from lacustrine sedimentary records: American Quaternary Association Abstracts and Program, 7th biennial meeting, 120.
  • Leonard, E.M., 1980, Late Holocene glacial activity and sediment yield, Banff National Park, Alberta: American Quaternary Association Abstracts and Program, 6th biennial meeting, 127.

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