seen. slate The rhio green Lilerian Helms are like those seen at Beest Hill and else where to the north. Bill found one fossil that maybe a Chmets or an orthid. The strata throughout practically stand m end or at least at so degree. If there is a change in dip I did not notice it. The section is a descending one from Up. Criskey through to Bescroft at least and firstly into New Scotland. Then firstly a great time break (the contact seems to be a disemprontable one) with the Lileria slats at the base of the section. Fletcher measured the section as upwards of 1500 feet thick. Of this 1100 feet in Iron Diermian (top out seen), and on 400 feet in Lilerian (base nowhere near).