The Alberta Group is a stratigraphical unit of Cenomanian to early Campanian age in the Lewis overthrust in the Western Canadian Sedimentary Basin.[2]
It takes the name from the province of Alberta, and was first described in outcrops along the Highwood River in southern Alberta by G.S. Hume in 1930.[3]
^Lexicon of Canadian Geologic Units. "Alberta Group". Archived from the original on 2013-02-21. Retrieved 2009-03-01.
^Sears, James W.; Harms, Tekla A.; Evenchick, Carol A., eds. (2007). Whence the Mountains?: Inquiries Into the Evolution of Orogenic Systems: a Volume in Honor of Raymond A. Price. United States: Geological Society of America. p. 171. ISBN 978-0-8137-2433-1 – via Google Books.
^Hume, G.S., 1930. The Highwood-Jumpingpound Anticline, with Notes on Turner Valley, New Black Diamond and Priddis Valley Structures, Alberta; Geological Survey of Canada, Summary Report 1929, Part B, pp. 1-24.
The AlbertaGroup is a stratigraphical unit of Cenomanian to early Campanian age in the Lewis overthrust in the Western Canadian Sedimentary Basin. It...
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disconformably overlain by the AlbertaGroup. It is equivalent to the Luscar Group north of the Clearwater River and to the Mannville Group in the plains to the...
Peoples Bank of Canada. It is a subsidiary of the Alberta-based holding company Triple Five Group and maintains offices in Vancouver, Montreal, Calgary...
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