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Reconstruction of post-Iroquois shoreline evolution in western Lake Ontario : procedure and preliminary results / John P. Coakley and Paul F. Karrow.En13-5/93-36E-PDF

"When Lake Iroquois drained between 11.7 - 11.4 ka BP, lake level in the Ontario basin fell from a high of more than 40 m above present lake level to a minimum close to the then-existing sea level, which was approximately 40 m below present sea level. Since that time, lake level has been rising at an exponentially-decreasing rate in the western portion of the basin as a result of postglacial and neotectonic uplift of the outlet near Kingston, at the eastern end"--Abstract, page 2.

Permanent link to this Catalogue record:
publications.gc.ca/pub?id=9.878458&sl=0

Publication information
Department/Agency
  • Canada. Environment Canada.
  • National Water Research Institute (Canada). Lakes Research Branch.
  • University of Waterloo. Dept. of Earth Sciences.
  • University of Waterloo. Quaternary Sciences Institute.
TitleReconstruction of post-Iroquois shoreline evolution in western Lake Ontario : procedure and preliminary results / John P. Coakley and Paul F. Karrow.
Series title
  • [NWRI contribution] ; [93-36]
Publication typeMonograph - View Master Record
Language[English]
FormatDigital text
Electronic document
Note(s)
  • Digitized edition from print [produced by Environment and Climate Change Canada].
  • Includes bibliographical references (pages 23-27).
Publishing information
  • Burlington, Ontario : National Water Research Institute, Lakes Research Branch ; Waterloo, Ontario : University of Waterloo, Department of Earth Sciences, Quaternary Sciences Institute, [1993]
Author / Contributor
  • Coakley, J. P. (John Phillip), 1940- author.
  • Karrow, P. F., 1930- author.
Description1 online resource (31 pages, 13 unnumbered pages) : maps, graphs.
Catalogue number
  • En13-5/93-36E-PDF
Subject terms
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