The Eldon Formation is a stratigraphic unit that is present on the western edge of the Western Canada Sedimentary Basin in the southern Canadian Rockies of southwestern Alberta and southeastern British Columbia.[3] It is a thick sequence of massive, cliff-forming limestones and dolomites that was named for Eldon Switch on the Canadian Pacific Railway near Castle Mountain in Banff National Park by Charles Doolittle Walcott,[1][2] who discovered the Burgess Shale fossils. The Eldon Formation was deposited during Middle Cambrian time, and it includes fossil stromatolites.[1] The Eldon forms the scenic cliffs at the top of Castle Mountain, and can also be seen at Mount Yamnuska and other mountains in Banff and Yoho National Parks.[4]
| Eldon Formation | |
|---|---|
| Stratigraphic range: Middle Cambrian ~ | |
 The Eldon Formation forms the cliffs of Mount Yamnuska in Alberta | |
| Type | Formation |
| Underlies | Pika Formation |
| Overlies | Stephen Formation, Snake Indian Formation |
| Thickness | Up to 500 metres (1640 ft)[1] |
| Lithology | |
| Primary | Limestone, dolomite |
| Other | Mudstone |
| Location | |
| Coordinates | 51°18′8.5″N 115°55′45″W / 51.302361°N 115.92917°W |
| Region | Canadian Rockies |
| Country |  Canada |
| Type section | |
| Named for | Eldon Switch on the Canadian Pacific Railway in Banff National Park, Alberta |
| Named by | Charles Doolittle Walcott in 1908[2] |
Lithology and deposition
editThe Eldon Formation is a thick sequence of cliff-forming carbonate rocks that was deposited during the Middle Cambrian time. It originally formed as limestone and calcareous mudstone in the intertidal to supratidal zone along the western margin of the North American Craton.[3][5] It was subsequently altered to dolomite and dolomitic mudstone in some areas.[1]
Distribution and stratigraphic relationships
editThe Eldon Formation is present in the southern Rocky Mountains of southwestern Alberta and southeastern British Columbia. It reaches a maximum thickness of about 500 metres (1,640 feet) at Mount Bosworth on the Alberta-British Columbia border. The Eldon conformably overlies the Stephen Formation, which hosts the fossils of the Burgess shale, in the south, and the Snake Indian Formation in the north. It is conformably overlain by the Pika Formation. The Eldon grades into the Earlie Formation to the east, the Chancellor Formation to the west, and the Titkana Formation to the north. It is probably equivalent to the Windsor Mountain Formation to the south.[1][3][6]
References
edit- ^ a b c d e Glass, 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. ISBN 0-920230-23-7.
- ^ a b Walcott, C.D. 1908. Nomenclature of some Cambrian Cordilleran formations. Smithsonian Miscellaneous Collections, vol. 53, no. 1, 14 pp.
- ^ a b c Slind, O.L., Andrews, G.D., Murray, D.L., Norford, B.S., Paterson, D.F., Salas, C.J., and Tawadros, E.E., Canadian Society of Petroleum Geologists and Alberta Geological Survey (1994). "The Geological Atlas of the Western Canada Sedimentary Basin (Mossop, G.D. and Shetsen, I., compilers), Chapter 8: Middle Cambrian and Early Ordovician Strata of the Western Canada Sedimentary Basin". Retrieved 2018-07-13.
{{cite web}}: CS1 maint: multiple names: authors list (link) - ^ Leckie, D.A. 2017. Rocks, ridges and rivers – Geological wonders of Banff, Yoho, and Jasper National Parks. Brokenpoplars, Calgary, Alberta, 217 pp. ISBN 978-0-9959082-0-8.
- ^ Aitken, J.D. 1971. Control of lower Paleozoic sedimentary facies by the Kicking Horse Rim, southern Rocky Mountains, Canada. Bulletin of Canadian Petroleum Geology, vol. 19, no. 3, p. 557-569.
- ^ Alberta Geological Survey, 2019. "Alberta Table of Formations". Alberta Energy Regulator. Retrieved 2 July 2019.
{{cite web}}: CS1 maint: numeric names: authors list (link)