Cathedral Formation | |
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Stratigraphic range: Middle Cambrian ~ | |
Type | Formation |
Underlies | Stephen Formation |
Overlies | Mount Whyte Formation, Naiset Formation |
Thickness | Up to 610 metres (2000 ft)[1] |
Lithology | |
Primary | Limestone, Dolomite |
Other | Calcareous mudstone |
Location | |
Coordinates | 51°23′47″N 116°23′25″W / 51.39639°N 116.39028°W |
Region | Canadian Rockies |
Country | Canada |
Type section | |
Named for | Cathedral Mountain |
Named by | Charles Doolittle Walcott, 1908[2] |
Part of a series on |
The Burgess Shale |
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The Cathedral Formation is a stratigraphic unit in the southern Canadian Rockies of Alberta and British Columbia, on the western edge of the Western Canada Sedimentary Basin. It is a thick sequence of carbonate rocks of Middle Cambrian age. It was named for Cathedral Mountain in Yoho National Park by Charles Doolittle Walcott, the discoverer of the Burgess shale fossils.[1][3]
The Cathedral Formation includes fossil stromatolites, oncolites, and other algal remains, as well as a few shale beds with trilobites.[1] The Cathedral escarpment on its westernmost edge is thought to have played a major role in the deposition and preservation of the Burgess shale fossils.[4]
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