Tuesday Sep. 11 1934. (2) The Dailor marine ls (40' thick) is fully eroded or Karsted, and in m places re- plete with Cryptogron. It has near the top various Cephalopods and among these is a closed coiled chief septeata form that which says oc: curs of wide high "Yppu Canadian" series. It has other forms, some Symbionic and fast. Because of this cephalopod which protrudes that the Dailor Ledge ls in front a fronte Lake Hill, and the reason why it seems delow the latter is because it was laid down m a cave that the mirady sea grown than the Lake Hills made and subsequently filled with the Dailor Ledge ls. The latter is known to extend 4 1/2 miles N to S, and about 1 1/2 miles fm E to W. This entire area according to which was laid down in m a sea made cave at least 40' high and then filled up by the Dailor Ls!! The filled siltuni holes are which "pillars" has supported the root. The very presence of Cryptogron alone forms hat this ls could not have been formed