Wednesday August 24, 1937 Wea. TUES. JULY 6, 1909 Ther. are oval qrs in the ridge by the Graniton qgl. On the High- gate is turning on its dips to dip. lastly. A full 1000' W of the first dome coming from the east at the forks of the same down the labythe Graniton qgl. The Dr. a fine expression of Highgate slate dipping SE 10°. One Highgate slate of to second house from E; 500' to E from the house to slate dips Wl at mr 15°. In the next 200 ft Dr. the whole pattern out to horizontal and then reverse and dips E 10° 100' W of the last house the Highgate dips E. Farther N. the land is low and flat and we see but few outcrops. To the Dr. of the third house are two other Highgate outcrops, and from no more. Near the end of the road to the mine pit is a little sharp sandy hump. It has the genuine Dolly Vigin outcropment of Horsey lenticuls and then fragmented pieces. Over the ones here occur large foots ones actually be lentils in the Miller River, off or the main heart of the Parker which is chiefly to the Dr. (estimate) About 300' E of N.S. oval occurs the Ruff brook dol. qgl with many joints to 12" and carry a piece up to 24". It is about 12-15' thick and dips 10° E. Over it lies the St. Alban slate with fossils, it is