A model for the demise of large, glacial Lake Ojibway, Ontario and Quebec

Journal of Paleolimnology

Volumn 50, Issue 1, 2013, Pages 105-121

  Stroup, Justin S ^a,c   Lowell, Thomas V ^a   Breckenridge, Andy ^b  

^a UNIVERSITY OF CINCINNATI   (United States)

^b UNIVERSITY OF WISCONSIN SUPERIOR   (United States)

^c DARTMOUTH COLLEGE   (United States)

Author keywords

8,200 cal yr BP event; Glacial lake drainage; Ice rafted debris; Lake Ojibway; Laurentide ice sheet

Indexed keywords

CLIMATE CHANGE; CONGLOMERATE; CORE ANALYSIS; DEGLACIATION; DRAINAGE BASIN; FINE GRAINED SEDIMENT; GLACIAL LAKE; GLACIAL SEDIMENTATION; GRAIN SIZE; ICE FLOW; ICE-RAFTED DEBRIS; LAURENTIDE ICE SHEET; MAGNETIC SUSCEPTIBILITY; MELTWATER; PEBBLE; RHYTHMITE; TILL; VARVE; X-RAY DIFFRACTION; X-RAY FLUORESCENCE;

CANADA; LAKE OJIBWAY; ONTARIO [CANADA]; QUEBEC [CANADA];

EID: 84877802121     PISSN: 09212728     EISSN: None     Source Type: Journal    
DOI: 10.1007/s10933-013-9707-9     Document Type: Article

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