Palliser Formation

http://dbpedia.org/resource/Palliser_Formation an entity of type: SpatialThing

The Palliser Formation is a stratigraphic unit of Late Devonian (Famennian) age in the Western Canada Sedimentary Basin. It is a thick sequence of limestone and dolomitic limestone that is present in the Canadian Rockies and foothills of western Alberta. Tall cliffs formed of the Palliser Formation can be seen throughout Banff and Jasper National Parks. rdf:langString
rdf:langString Palliser Formation
rdf:langString Palliser Formation
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xsd:float -115.27490234375
xsd:integer 24726582
xsd:integer 976934825
rdf:langString Costigan Member
rdf:langString Morro Member
rdf:langString The type section of the cliff-forming Palliser Formation near Lake Minnewanka
rdf:langString Famennian
rdf:langString up to
xsd:string 51.26877 -115.2749
rdf:langString The Palliser Formation is a stratigraphic unit of Late Devonian (Famennian) age in the Western Canada Sedimentary Basin. It is a thick sequence of limestone and dolomitic limestone that is present in the Canadian Rockies and foothills of western Alberta. Tall cliffs formed of the Palliser Formation can be seen throughout Banff and Jasper National Parks. The formation was named for the Palliser Range in Banff National Park (which in turn took its name from John Palliser, the leader of the 1850s Palliser Expedition), by H.H. Beach in 1943. The type locality was defined in 1994 in the "Devil's Gap" section south of Mount Costigan of the Palliser Range, north of Lake Minnewanka.
rdf:langString H.H. Beach, 1943
xsd:nonNegativeInteger 6498
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