many parent of trilobite among them poor material of Agolitts, Olenellus in Orissacis, and half are in two other trilobites. This fluffy material is near shre deposits and is replete with mica. Before getting to these fluffy deposits are jamed one (Milton dolomite, Milton conglomerate up to 40 or more. Little faults makes the section repeat itself. In the afternoon went to Orange's Ledge south of St Albans to see what Keith interpreted as Cryptogorn. It looks or, Took along some samples. Associated are things that again look like Bryozoa. At the extreme south end of this ledge Keith got before Longjulella and trilobites. I took away several pieces that appear to have trilobites. To the north of the ledge one Mr josh Hoad Shales. Looked for fossils but got none. Long from Raymond thought he could find graptolites here. Maybe! Farther south and some to the east of Orange ledge is another similar conglomerate. It strikes