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The eastern [[?]] of the [[cay]] on the devide]] of the separation of the Cretaceous of the valley from the [[Tertary]]and[[Cretaceous W.W. uplifte in the western hills over to the Long  valley canon x. 
No evidence of a fault was observed in the Kanab Canon White Cliffs or in the canon east to the 2d opening in the Johnson cannon. To the west no observations were taken in the White Cliff or the Long Valley canon cuts off faults in that direction. 

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Note. From the base of the gray sandstone [[(sanetinis]]conglomerte)beneath the Pink Cliff limestone to the [[arenaceous?]] clays beneath the massive sandstone [[neat]]below the [[astrea]] appears to be a great natural grout characterized by the preponderance of sandstones + clays [[parting]] in great [[minimility]] as compared with the [[2d]]. 

The next division consisting of clays + [[marls]] [[arenaceous]] soft easily disintegrating strata extend down to the red bed of shale above the sandstones containing numerous fossils. This division forming low rounded hills [[usually]]extending southward  to the next [[bunch]] of hard [[2d]].