The Devon Island Formation is a geologic formation in the Canadian Arctic.[1] It preserves fossils dating back to the late Silurian and Devonian periods.[2]
| Devon Island Formation | |
|---|---|
| Stratigraphic range: Silurian - Devonian | |
| Type | Formation |
| Location | |
| Region | Nunavut |
| Country | Canada |
The formation was originally named by Raymond Thorsteinsson for a sequence of calcareous, graptolitic mudrocks on northern Devon Island situated between the Douro Formation below and the Sutherland River Formation above.[1] The latter formation is now considered synonymous with the Goose Fiord Formation.[2] The Devon Island Formation extends from the west coast of Devon Island through the Grinnell Peninsula, and well across the southern part of Ellesmere Island.[2]
See also
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References
edit- ^ a b Thorsteinsson, R. 1963. Prince Alfred Bay. In: Fortier, Y.O. et al. (eds.) Geology of the north-central part of the Arctic Archipelago, Northwest Territories (Operation Franklin). Geological Survey of Canada, Memoir 320. pp. 221-232 https://doi.org/10.4095/100547
- ^ a b c Mayr, U. and Packard, J.J. 1994. Chapter 5: Upper Ordovician to Lower Devonian Carbonate Platform. In: U. Mayr et al. (eds.) The Phanerozoic Geology of Southern Ellesmere and North Kent Islands, Canadian Arctic Archipelago. Geological Survey of Canada Bulletin 470. pp. 68-95 https://doi.org/10.4095/195161
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