Page:Field Notes of Junius Henderson, Notebook 2.pdf/24

 crinoidal limestone to the same point, but found no brachiopods in it after leaving the. Saw 2 {taxon|Buteo|buzzards}} and 1 at junction of.

Thursday

Dodds and I started on horseback NW from camp on, just S of , to examine the plain to the WNW and SW which appears to be approximately the ancient sea floor, from which most of the sedimentaries have been eroded. On the divide between and  creeks NW of, we measured dip of Fountain conglomerate and found it to be 6 deg. Bearing N. 30˚ E. The conglomerate covers a considerable portion of the plain. ¼ mi. further N dip is 6˚ S. 13˚ W., a valley occupying the syncline here, the sec. fence passing through the valley. It is probably the Syncline. 300 yds further N of last mentioned outcrop is an outcrop of thin bedded limestone resting on Fountain conglomerate and bearing