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Upper beds NW of ⤈
Str 40° E of N
Dip 30 NW
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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