Rock formations in North America
| Colorado Group |
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| Type | Geological formation |
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| Sub-units | Colorado (type) and Kansas:
Graneros, Greenhorn, Carlile, Niobrara
Canada:
Phillips Sandstone, Second White Speckled Shale, Bowdoin Sandstone, Cardium Sandstone, Martin Sandy Zone, Medicine Hat Sandstone, First White Speckled Shale |
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| Underlies | Montana Group, Belly River Group, Lea Park Formation, Milk River Formation |
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| Overlies | Dakota Group, Blairmore Group, Mannville Group, Swan River Group |
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| Thickness | more than 1,000 metres (3,280 ft)[1] |
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|
| Primary | Shale, Chalk, Sandstone |
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| Other | Siltstone, Conglomerate, Limestone, concretionary beds |
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|
| Region |  Alberta,  Saskatchewan,  Montana,  Wyoming,  Colorado |
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| Country |  US,  Canada |
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| Named for | Colorado, specifically for the hogbacks and plains facing the Front Range of that state[2][1] |
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| Named by | F.V. Hayden[2][3] |
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Colorado is a geologic name applied to certain rocks of Cretaceous age in the North America, particularly in the western Great Plains. This name was originally applied to classify a group of specific marine formations of shale and chalk known for their importance in Eastern Colorado. The surface outcrop of this group produces distinctive landforms bordering the Great Plains and it is a significant feature of the subsurface of the Denver Basin and the Western Canadian Sedimentary Basin. These formations record important sequences of the Western Interior Seaway. As the geology of this seaway was studied, this name came to be used in states beyond Colorado but later was replaced in several of these states with more localized names.
The USGS convention has been to use Colorado Group where the rocks are further divided into formations, Colorado Formation where no beds are developed enough to be mapped as formations, and Colorado Shale where the unit is composed of little more than shale with no distinctive structures (such as in north-central Montana).[4]
Lithology
The Colorado Group consists primarily of chalky and non-chalky shale, and incorporates conglomerate, sandstone and siltstone, rhythmite beds of chalk, chalky limestone, coquinas, phosphorite, and concretionary beds including calcite, siderite, and pyrite.[17]
The Canadian distribution presents with more sandstone. The lower part includes the following sandstone members: Phillips Sandstone (below the Second White Speckled Shale), Bowdoin Sandstone and Cardium Sandstone in the non-calcareous shale unit. The upper part includes the Martin Sandy Zone and Medicine Hat Sandstone.[1]
Oil/gas production
Gas is produced from the sandstone members in southern Alberta, southern Saskatchewan and in Montana, such as in the Bowdoin gas field.
Distribution
Shales of middle Albian to Santonian age are distributed throughout much of the former extent of the Western Interior Seaway, including broadly from Arizona, to Iowa and Alberta. The Greenhorn-Carlile contact represents the maximum extent of the seaway of that sequence, perhaps of the entire time of the seaway; and, so, coupled with the Graneros Shale, the "old Benton" shales are the widest durable remnant of the Western Interior Seaway.[18] Older literature may use the term Colorado Group in this extent, but several states outside of Colorado no longer use the term in current publications; nevertheless, the evidence of correlated seaway sequences and fossil patterns remains, regardless of current names.
From Iowa to Arizona, the lithology is remarkably consistent and the bentonites and rhythmic chalk beds of the upper Greenhorn especially are geologic events that can be traced over that distance.[19] Beyond the historic western extent of the Colorado Group usage into the Mancos Shale, the chalky beds of the group can be identified and are named accordingly, e.g, Smoky Hill, Fort Hays, Bridge Creek, Greenhorn.[20] However, northwest of the Transcontinental Arch where western sediment sources are more dominant, altering the lithology, these names have less current use.
The Canadian Colorado Group occurs in the sub-surface throughout southern and central Alberta, western and central Saskatchewan. It is found in outcrops along the south-western edge of the Canadian Shield. The sediments of the Colorado group exceed 1,000 metres (3,280 ft) in thickness in central Alberta. In central Saskatchewan, it thins to 150 metres (490 ft).[1]
Relationship to other units
The rocks of Colorado Group age are overlain by the Montana Group and underlain by the Dakota Group in the Denver Basin, Powder River Basin, and Williston Basin of the western Great Plains. In Western Canada, they are unconformably overlain by the Lea Park Formation shale and unconformably underlain by the Blairmore, Mannville or Swan River Group.
The lower part is equivalent with the Ashville Formation in eastern Saskatchewan and southern Manitoba, with the upper part corresponding to the Vermillion River Formation and Favel Formation. It is equivalent to the sum of Crowsnest Formation, Blackstone Formation, Cardium Formation, and the lower Wapiabi Formation of the Alberta Group in the Canadian Rockies foothills. It correlates with the upper Smoky Group, Dunvegan Formation, Shaftesbury Formation, Paddy Member and Labiche Formation in northern Alberta. The Canadian Colorado Group was previously named Lloydminster Shale in the Lloydminster region, but the term is now obsolete.
Sub-units
United States sub-unit classifications have generally derived from the related Colorado and Kansas classifications, from top to bottom:
The Colorado Group in Canada, which retains the Santonian-time Pierre Shale correlations, is divided into an upper part which is calcareous, and a lower part, which is non-calcareous. The sub-units are defined at the base of two regional markers, called First and Second White Speckled Shale characterized by coccolithic debris.
The Canadian Geological Survey classification of the Colorado Group includes the following sub-units, from top to bottom:
