crinoidal limestone to the same point, but found no brachiopods in it after leaving the Box Elder . Saw 2 {taxon|Buteo|buzzards}} and 1 red tailed hawk at junction of N and S Box Elder .
Red Mt. Thursday June 13/07
Dodds and I started on horseback NW from camp on Ten Mile Creek , just S of Red Mt. , 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 Ten Mile and Lone Tree creeks NW of Red Mt. , 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 Red Mt. Syncline. 300 yds further N of last mentioned outcrop is an outcrop of thin bedded limestone resting on Fountain conglomerate and bearing