About This Item

Share This Item

The AAPG/Datapages Combined Publications Database

CSPG Bulletin

Abstract


Journal of the Alberta Society of Petroleum Geologists
Vol. 6 (1958), No. 9. (October), Pages 218-226

Jasper Area Alberta, a Source of the Foothills Erratics Train1

E. W. Mountjoy2

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.


Pay-Per-View Purchase Options

The article is available through a document delivery service. Explain these Purchase Options.

Watermarked PDF Document: $14
Open PDF Document: $24