Alfred Huffman. We will lack of limerize, Black slate said to be faulted. [illegible] will. 18 ft sandy rock well stratified. 1ft very crinoidal and fossils. 110 ft Bedford clay bottom of valley, This would be a good place to get fossils from Lime Heldenberg, I must see. The Ostracods seen at McCle- downey occur here also. They occur in this shale (limestone?) lie boreled now to occur in Bedford clay or maybe sand, at least within 30 ft of top. The crinoidal limestones fowards by cut mine Limerica? B after single fault. tone erthed. section NE of Duncan house 11ft similar to below. 16'2 brown sandy, flat, rock massive 160 feet Bedford clay, bare not seen 57 lesg. S 5E 20' S 18 W 65' beyond, same ostracods S 5W 70 les. S 50 W 50 les, S 75 W 120. Gz. Bartley Harrison, Rad. S 75 W 7 At creek one 27 m of l. in thin beds dipping E. Is this 2ft bed massive? How the beds are thin. W 44 les. N 8E W 46 S 5E W 24 bridge. model, beyond S 58 W 15. W.H. Lawrence store, 2'2 mi to Odellton. Rilelt S 55 W 7 Cross Roads same girdage lesg. mule S 55 W 165 les. Micahund S 75 W 40 Parnis crop V 8E W 45 N 8E W 17 Chisty Cl. S 55 W 24 Hebertella S 55 W 29 bridge, creek occurrences 70 W 48 lesg. Chisty Cl. S 18 W 35 cabin S 38 W (5 simpson at S 26 W 25 springdale S 66 W 38 family farm yard S 66 W 50 S 88 W 136 N 8E W 35 S 8E W 120 S 8E W 45 church Bogdham N 75 W 66