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The ^ [[insertion]] 5 to [[/insertion]] 700 feet of strata crossing the intervals between the headwaters of Kanab creek (springs below White Cliffs) is c. b. sd. red, brownish red, vermilion with an occasional fillet of white. The upper portion merges into the white cliff sd by an irregular line of contact & union. The change is in the color.
The upper 400 feet is mostly of a vermilian hue & is a soft
easily disintegralia sd. [[?]] low, foothills below the cliffs.
The [[insertion]] white [[/insertion]] cliffs all present a normal surface to the south and large masses are separated as buttes.  Above the vermilion bed, which is a somewhat fluctuating horizon the true light gray or white cliff towers of
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[[crossed out]]massive light colored divided into five principal beds each consisting of five crossbeds 575 feet. 

Capping sandstone of a redish hue. 100 feet. upon this rests a limestone containing fossils. Notes of white cliff sandstones.
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