The Halgaito Formation is the basal Permian geologic member of the Cutler Group in southern Utah . The member consists of silty sandstone, siltstone and limestone. The Elephant Canyon may grade into the Halgaito and grades northward into the Cedar Mesa Formation .
1-766: There is no designated type locality for the Halgaito. The shale can be seen at the confluence of the Green River and Colorado Rivers and in Cataract Canyon . This article related to the Permian period is a stub . You can help Misplaced Pages by expanding it . This article about a specific stratigraphic formation in Utah is a stub . You can help Misplaced Pages by expanding it . Type locality (geology) Type locality , also called type area ,
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