This section begins at mee north of the mayo road bridge. Between the ridge and the railroad me to the south all of the material is of the ipreous series marked by Stanley who's one as B. The large left "grees" came see from the mayo road ridge. It lies on the north side of the high. Another one in the opposite side is nearly 5 feet across. These haven't are not founders but rounded heads of the original ipreous floor. (under 75 feet once to be added). Lorn Cambic June 1-35 "2-0-25 "3-40 "4-4 In Smith's round 932 for I Z.E. are seen and at base visible, mostly shale with green modular lim. In Trinity Bay Dr gives it as fully 98s feet thick 104 feet thick Middle Cambic June 5-2 "6-270 "7-295 "8-400 There may be a far greater thickness lost in the sea between the Oranubs shore and their flue sides. 967 feet thick. In the paper of 1899 I see he makes green the base of the Middle Cambic. I did not know this at the time as in the depth of 1889 the first M.E. trilites occur at the top of June 6 or 270 feet higher. If Dean I will return to this place and note the character of the stratum.