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| 02158cam 2200361zi 4500 |
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| 001 | 9.870881 |
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| 003 | CaOODSP |
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| 005 | 20221107163236 |
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| 006 | m o d f |
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| 007 | cr ||||||||||| |
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| 008 | 190401s1999 onc #ot f000 0 eng d |
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| 040 | |aCaOODSP|beng|erda|cCaOODSP |
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| 043 | |an-cn-on |
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| 086 | 1 |aEn13-5/99-228E-PDF |
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| 100 | 1 |aCoakley, J. P. |eauthor.|q(John Phillip), |d1940- |
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| 245 | 10|aLevels in the Erie Basin : |b4000 BP to present / |cby: J.P. Coakley. |
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| 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] |
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| 300 | |a1 online resource (9 unnumbered pages) |
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| 336 | |atext|btxt|2rdacontent |
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| 337 | |acomputer|bc|2rdamedia |
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| 338 | |aonline resource|bcr|2rdacarrier |
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| 490 | 1 |aNWRI contribution ; |v99-228 |
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| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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| 500 | |a"Paleo Lake Levels - The Last Four-Thousand Years, Workshop at Great Lakes Environmental Research Laboratory, Ann Arbor MI, April 13-14, 1999." |
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| 504 | |aIncludes bibliographical references. |
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| 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]. |
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| 692 | 07|2gccst|aLakes |
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| 692 | 07|2gccst|aWater management |
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| 710 | 1 |aCanada. |bEnvironment Canada. |
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| 710 | 2 |aNational Water Research Institute (Canada) |
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| 830 | #0|aNWRI contribution ;|v99-228.|w(CaOODSP)9.844121 |
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| 856 | 40|qPDF|s721 KB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-99-228-eng.pdf |
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