![Transcription Center logo](/themes/custom/tc_theme/assets/image/logo.png)
This transcription has been completed. Contact us with corrections.
Upper beds NW of ⤈ Str 40° E of N Dip 30 NW [[end page]] [[start page]] particular horizons more than others. There are also thin variable beds of conglomerate. About the middle of the series NW from the anchorage was a bed of conglomerate of small rounded pebbles in a limestone matrix which also contained fragments of organic remains, among which were Ammonites, Belemnites, Astrea, & another bivalve or two. At the outcrop of the first high bench of the same mountain mass dipping 30° NW. Purington found ammonites, a brachiopod like Rhynchonella, Belemnites and a bivalve or two. The dip of the strata became more steep near the valley of the stream. On the shaly streaks of the limestone