For the first two miles one walks almost along the strike and along the third mile the beds come to be more transverse to the road. These same red shales are seen across the river of the stream from the Lewis beds with the limestone. The thickness in the first two miles, nevertheless, thin one walks mostly along the strike, is great. There may be 2000 feet or more as there seems to be no repetition. The question now arises did layers go up or down the section. According to Annie dam into the cambrian = liller and shales. As I saw the Ordovician above Beebee, x Dilly village here Red Liller Lewis series. Lewis This appears to me as one can [illegible] Beesee Series Cittay coph Wianet Beebee and red shales downing into red shales liller zone may be 20 liller Black Shales This is not correct. There are faults that change all this See a later page