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The AAPG/Datapages Combined Publications Database
CSPG Bulletin
Abstract
Jasper Area Alberta, a Source of the Foothills Erratics Train1
ABSTRACT
Glacial features and bedrock geology in the Jasper area suggest that the latter was the source and an Athabasca Valley glacier was the transporting agent for the Foothills Erratics Train. It is believed that the former Athabasca glacier extended from its present fronts northwest to Jasper, and then flowed northeast through the Front Ranges via the present Athabasca Valley to the Plains where it was deflected southeast by the Keewatin ice-sheet.
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