The Arctomys Formation is present in the Rocky Mountains of Alberta and British Columbia. It thickens northward from White Man Mountain to a maximum of 336 metres (1,100 ft) at Mount Robson.[1] It is overlies the Pika Formation and is overlain by the Waterfowl Formation.[7] Both contacts are gradational.[1]
References
^ abcdGlass, D.J. (editor) 1997. Lexicon of Canadian Stratigraphy, vol. 4, Western Canada including eastern British Columbia, Alberta, Saskatchewan and southern Manitoba. Canadian Society of Petroleum Geologists, Calgary, 1423 p. on CD-ROM. ISBN0-920230-23-7.
^Walcott, C.D. 1920. Explorations and field work of the Smithsonian Institution in 1919. Smithsonian Institution Miscellaneous Collections, vol. 72, no. 1, p. 1-16.
^Leckie, D.A. 2017. Rocks, ridges and rivers – Geological wonders of Banff, Yoho, and Jasper National Parks. Brokenpoplars, Calgary, Alberta, 217 pp. ISBN978-0-9959082-0-8.
^Aitken, J.D. 1966. Middle Cambrian to Middle Ordovician cyclic sedimentation, southern Rocky Mountains of Alberta. Bulletin of Canadian Petroleum Geology, vol. 14, no. 6, p. 405-441.
^Spencer, R.J. and Demicco, R.V. 1993. Depositional environments of the Middle Cambrian Arctomys Formation, southern Canadian Rocky Mountains. Bulletin of Canadian Petroleum Geology, vol. 41, no. 4, p. 373-388.