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008190823s1993    oncbd  #ob   f000 0 eng d
040 |aCaOODSP|beng|erda|cCaOODSP
043 |an-cn-on
0861 |aEn13-5/93-36E-PDF
1001 |aCoakley, J. P. |q(John Phillip), |d1940- |eauthor.
24510|aReconstruction of post-Iroquois shoreline evolution in western Lake Ontario : |bprocedure and preliminary results / |cJohn P. Coakley and Paul F. Karrow.
264 1|aBurlington, Ontario : |bNational Water Research Institute, Lakes Research Branch ; |aWaterloo, Ontario : |bUniversity of Waterloo, Department of Earth Sciences, Quaternary Sciences Institute, |c[1993]
300 |a1 online resource (31 pages, 13 unnumbered pages) : |bmaps, graphs.
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |a[NWRI contribution] ; |v[93-36]
500 |aDigitized edition from print [produced by Environment and Climate Change Canada].
504 |aIncludes bibliographical references (pages 23-27).
5203 |a"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.
69207|2gccst|aLakes
69207|2gccst|aCoasts
69207|2gccst|aHistorical research
7001 |aKarrow, P. F., |d1930- |eauthor.
7101 |aCanada. |bEnvironment Canada.
7102 |aNational Water Research Institute (Canada). |bLakes Research Branch.
7102 |aUniversity of Waterloo. |bDept. of Earth Sciences.
7102 |aUniversity of Waterloo. |bQuaternary Sciences Institute.
830#0|aNWRI contribution ;|v93-36.|w(CaOODSP)9.844121
85640|qPDF|s3.19 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-93-36-eng.pdf