Sedimentology and geomorphic evolution of the South Shore of Lake Winnipeg / by Erik Nielsen and Glenn Conley.

By:

Nielsen, Erik, 1946-

Contributor(s):

Conley, Glenn, 1946

Material type: Text

TextSeries: Geological Report / Mineral Resources Division. 94-1 Publication details: Winnipeg, MB : Manitoba Energy and Mines, Geological Services, 1994.Description: viii, 58 p. : ill. ; 28 cmSubject(s):

LOC classification:

CA2 MB EN MN 1994

Online resources:

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Summary: The southern shoreline of Lake Winnipeg has transgressed landward, to the south, an estimated 60 to 100 metres since about 1650 AD. Radiometric dates on these deposits suggest that the lake level in the southern basin is rising 15 to 20 cm per 100 years due to isostatic tilting of the lake outlet and possibly climatic fluctuations over the past few centuries.

Holdings ( 1 )
Title notes ( 2 )

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Item type	Current library	Collection	Call number	Status	Date due	Barcode
Electronic Report	Electronic Library	Non-fiction	CA2 MB EN MN 1994 (Browse shelf(Opens below))	Available		16494

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Includes bibliographical references (p. 50-52).

The southern shoreline of Lake Winnipeg has transgressed landward, to the south, an estimated 60 to 100 metres since about 1650 AD. Radiometric dates on these deposits suggest that the lake level in the southern basin is rising 15 to 20 cm per 100 years due to isostatic tilting of the lake outlet and possibly climatic fluctuations over the past few centuries.

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