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light colored sandstone. partially conglomerate in places with silicified wood 50 feet.
This is overlaid by a [[red?]] sandstone similar to the red band of sands[[?]] beneath. Thickness - 20 feet to summit of hill. [[strikethrough]] [[?]] [[/strikethrough]] (section continued on pg 6)

From the summit of the [[?]] of conglomerate, capped with brown sandstone, [[?]] out from the east side of the Kanab valley 4 miles below the town.  The strata of the Vermillion Cliffs - rise one above the other to the east + west of the canon.  [[image - pencil drawing of the cliffs]]
The Shinarump cong rises slowly towards the east + is entirely (nearly) [[strikethrough]] [[?]] [[/strikethrough]] lost in the hills a few miles back from its valley to the west it passes beneath the [[brown?]]
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[[underlined]] sandstone. [[/underlined]] (3) The Conglomerate consists largely of a course sand, unevenly bedded with small quartz pebbles scattered through it irregularly, with an occasional thin stratum of ^[[small]] pebbles, from [[2 in?]] to 1 foot in thickness. The silicified wood appears to have been silicified and broken before being imbedded in the sand. Some fragments are rolled [[?]]  ( while others evidently [[?]] [[broken?]] + [[?]] imbedded) Found one mass of sandstone 6 x 5 ft [[?]] which there was a pile of silicified wood [[embedded?]] in the sand + Conglomerate fragments 15th in diamet + 2 feet long + other small + broken all water worn + rolled.

Dip of Conglomerate [[leds?]] N. 175[[degrees sign]]
"   of Vermilion Clifs        "   "