Page:Field Notes of Junius Henderson, Notebook 3.pdf/55

 sprinkling the slopes wherever we went, following up to the top of the mesa we found them alive under, but not elsewhere. The strata dip approximately S and the angle is 35¡ or 40¡. At top of mesa is a conglomerate composed of boulders up to 18 inches diameter of red sandstone well cemented. Then we followed along the limestone and calcareous shales resembling the Niobrara of region, and found  and. Proceeding up to the pond on above the U. S. G. S.  camp  and collected, , etc. and then found  ? under logs and. Then visited camp and met Beekley. He said the sandstone forming S face of hill N of town and NE face of hill W of town is base of Mesa Verde formation.