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This is a polygon coverage of isopachs of the combined thickness of the Calico and A-sequences in the Kaiparowits Plateau study area. The outside polygon defines the base of the John Henry Member of the Straight Cliffs Formation east of 112 degrees of longitude. The polygon includes areas where the Calico and A-sequences have been partially eroded. The northern boundary is delineated by the Paunsaugunt fault and volcanic rocks of Tertiary age.


map background search result map search result map The outcrop and area underlain by the Upper Cretaceous Drip Tank Mb. of the Straight Cliffs Fm. in the Kaiparowits Plateau study area, southern Utah (kaikdtg) Tertiary dikes in the Southern Piceance Basin, Colorado (psintrg) Isopachs of the combined thickness of the Calico and A-sequences of the Straight Cliffs Formation in the Kaiparowits Plateau study area, southern Utah (kjhthk*g) The outcrop and area underlain by the Upper Cretaceous Drip Tank Mb. of the Straight Cliffs Fm. in the Kaiparowits Plateau study area, southern Utah (kaikdtg) Tertiary dikes in the Southern Piceance Basin, Colorado (psintrg) Isopachs of the combined thickness of the Calico and A-sequences of the Straight Cliffs Formation in the Kaiparowits Plateau study area, southern Utah (kjhthk*g)