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Halgaito Formation
From Wikipedia, the free encyclopedia
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The Halgaito Formation is the basal Permian geologic member of the Cutler Group in southern Utah.[3] The member consists of silty sandstone, siltstone and limestone.[1] The Elephant Canyon may grade into the Halgaito and grades northward into the Cedar Mesa Formation.[4]
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Extent
There is no designated type locality for the Halgaito.[5] The shale can be seen at the confluence of the Green River and Colorado Rivers and in Cataract Canyon.[6]
References
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