is but a few hundred feet wide. Germanic comes its way, red granite on both sides. To the north rise mountains up to 1150 feet above the lake, as one stream turns Little Carrick over an island like the mouth only I which is rugged pre-Cambrian, while the south side is flat Ireland and of Trenton age. The strata here appear little deformed and to lie in domes with considerably faster dips than farther south- ward. Left for Manitoulin at 3 P.M. Stopping at Queens Hotel. Spend the rest of the afternoon looking over the limestone Richmond in the Manitoulins about one- half mile to the north of the hotel, About 50 feet of limestone with almost no shale goes are to be seen. All of them are crowded by many less for abundance of Stretfulusma or Rectum Paristella stellata, Calocrecia canadensis Orthis insculpta, Q, sinuata and Refinosquilia alternata, Saw or O. subquadrate, Stylomera or Atychostrea, Menticuli fra are abundant and as well Jygrozin Kentuckyensis. There is our trace here of the red and