000	00000nam 2200000zi 4500
001	9.870955
003	CaOODSP
005	20241203113647
006	m     o  d f
007	cr |||||||||||
008	190402s1999    onc    #ot   f000 0 eng d
040	|aCaOODSP|beng|erda|cCaOODSP
043	|an-cn-on
086	1 |aEn13-5/99-217E-PDF
100	1 |aCoakley, J. P. |eauthor.|q(John Phillip), |d1940-
245	10|aLake levels in the Erie basin : |bdriving factor and recent trends / |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 (7 pages).
336	|atext|btxt|2rdacontent
337	|acomputer|bc|2rdamedia
338	|aonline resource|bcr|2rdacarrier
490	1 |aNWRI contribution ; |v99-217
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 crust at their outlets, regional hydrological and climatic changes, and to a less dramatic extent, by long-term neotectonic movements of a continental nature. Under the influence of the above factors, Lake Erie 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 to its present stage"--Introduction, page 1.
692	07|2gccst|aLakes
710	1 |aCanada. |bEnvironment Canada.
710	2 |aNational Water Research Institute (Canada)
830	#0|aNWRI contribution ;|v99-217.|w(CaOODSP)9.844121
856	40|qPDF|s828 KB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-99-217-eng.pdf