149 [illegible] [illegible] [illegible] occurs at a lo [illegible] [illegible] [illegible] this collection of the same or like [illegible] [illegible] [illegible] [illegible] [illegible] [illegible] [illegible] [illegible] [illegible] 16/47. [illegible] [illegible] [illegible] [illegible] [illegible] [illegible] [illegible] [illegible] [illegible] 150 [illegible] though of the same type (probably the same species). [illegible] Some of the fossils seen Coll. 8/3/58/4 which have been may be from the tenacre alluvium, but certainly not all of them. The relation still probably indicates that these folded rocks lie low way you see. The trend of the "high" would pass somewhat the Widgeon centre and a lot so it's possible that either the Widgeon are 1) in place in the "Widgeon" 2) they are folded over plants on the top, the Gajeta or 3) a time folded with the Gajeta-beds both to the whole preserve is an overturned anticline and the slip E slipping coal on the west. [illegible] I do not favor explanation B. made at the moment. The collector for small end of Pigeon hills is in a limestone similar in color to the Deigha, of the same Fucalina beds as I