St. Albans, Vermont, Tuesday Sep. 3 1924 It was 8:30 AM when we left Philipstburgh and paid $50 by toll to Clarke and Orc Leagle. Two miles south we refuted out as "Burling Canada", and Orantin it ore answered the cus- toms question and orkorn south to be skinned is quary, Then on S to be road totates us north to our cnp, at the base of the eastern Beedmantown. The first place had be logathered oreaf surrounded by ls cnyl, but Corpus said it was a residual resting on the High gate of, and that the Bed mountain sea had caten into State and finally placing the cnpl. in little over into the under cut areas. The man is "trad-stuff" like while the cnpl, in the international character, To ore the residual is covered by a regular's cnyl. made up dominantly of High gate ls pieces. The Rockland great man is layer residual of the High gate, covered with by Beedmantown shale, or by the regula- tion ls cnyl. of many Highgate pice. Next we visited the Oriniqui page at Hyffpate Falls. How to their redded Oriniquari has much international cnpl. derminated by the great ls cnyl at the base of the Hyffgate. This cnyl, is dominantly of its descent from the upper Oriniquaric. Then we examined the sequence from near Champlain shae to St Albans - the southern sheet in the Beedmantown sle- encasing of Primovoli, some Mallet, Crickhartn, St Albans the trend ls Cnyl, at he base of the Highgate, and finally the Highgate slate - our Highgate ls is mostly laminated.