00000000nam 2200000zi 4500
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008190401s1999    onc    #ot   f000 0 eng d
040 |aCaOODSP|beng|erda|cCaOODSP
043 |an-cn-on
0861 |aEn13-5/99-228E-PDF
1001 |aCoakley, J. P. |eauthor.|q(John Phillip), |d1940-
24510|aLevels in the Erie Basin : |b4000 BP to present / |cby: J.P. Coakley.
264 1|a[Burlington, Ontario] : |bEnvironment Canada, Water Science and Technology Directorate = Environnement Canada, Direction générale des sciences et de la technologie, eau, |c[1999]
300 |a1 online resource (9 unnumbered pages)
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |aNWRI contribution ; |v99-228
500 |aDigitized edition from print [produced by Environment and Climate Change Canada].
500 |a"Paleo Lake Levels - The Last Four-Thousand Years, Workshop at Great Lakes Environmental Research Laboratory, Ann Arbor MI, April 13-14, 1999."
504 |aIncludes bibliographical references.
520 |a"Lake levels in the Erie basin are driven by three major factors: postglacial isostatic rebound of the outlets, regional hydrological and climatic changes, and to a lesser extent, by neotectonic movements of the outlet. Because of a combination of factors, Lake Erie has undergone a complex history of rises, declines, and stability since the close of the glacial period some 12 000 years ago. From a low-level stage more than 50 m below present levels, the lake has risen at its present level under the influence of these three factors primarily"--Introduction, page [3].
69207|2gccst|aLakes
69207|2gccst|aWater management
7101 |aCanada. |bEnvironment Canada.
7102 |aNational Water Research Institute (Canada)
830#0|aNWRI contribution ;|v99-228.|w(CaOODSP)9.844121
85640|qPDF|s721 KB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-99-228-eng.pdf