Wea. THUR. MARCH 4, 1909 Ther. Sunday Sep. 23 - 1928 By morn it cleared up and we conclude to go to Canada with Clark, McShuffle and Griellmay. They had first to repair their car and it was nearly four oclock by the time we started. We go via Sweeny Corner to the northeast and finally near Richmond came on into Canada. Got to Lethian seven miles north of the Boundary, at 7 P.M. We traveled 35 miles and looked at some exposures of the Algonkian series, and two one with slate, and one Algonkian. It is getting cold The Pre-Cambrian is mainly gneiss rocks, buthere are zones of quartzite, schist, and dolom. ite. In Canada it has chlorite schist = metamorphed iron ore material - larnas and tufa. These silicomics do not seem in Mt.