Dendroglaciological Evidence for a Neoglacial Advance of the Saskatchewan Glacier, Banff National Park, Canadian Rocky Mountains

Dendroglaciological Evidence for a Neoglacial Advance of the Saskatchewan Glacier, Banff National Park, Canadian Rocky Mountains

Seventeen glacially sheared stumps in growth position and abundant detrital wood fragments were exposed by stream avulsion at the terminus of the Saskatchewan Glacier in 1999. The stumps lay buried beneath the glacier and over 5 m of glacial sediment until historical recession and stream incision ex...

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Bibliographic Details
Main Authors: Wood, Chris, Smith, Dan
Other Authors: University of Victoria Tree-Ring Laboratory, Department of Geography, University of Victoria, Victoria, British Columbia V8W 3P5, Canada
Language:en_US
Published: Tree-Ring Society 2004
Subjects:
Dendrochronology
Tree Rings
Dendroglaciology
Floating Chronology
Saskatchewan Glacier
Peyto Advance
Canadian Rocky Mountains
Online Access:http://hdl.handle.net/10150/262633

Internet

http://hdl.handle.net/10150/262633

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