Wednesday, August 24 - 1932 Wea. Sun. July 4, 1909 Ther. Left in Bus for Georgia Center at 9:30 A.M. All appears like the Georgia slate for about one-half mile west of Georgia Center. Just before where the road forks there is facing to north a sharp rise of the land and it is all of the eastern plunging limit of the arch composed of Drantm cgl. It has much (about 2/3) of the hunchless Milltons and he is in the Hardy bluish white limestones and the immediate beneath, there can be no doubt it is the Drantm cgl. and east of it is the Georgia slate. The land underlying the Drantm cgl. rises about 180' and all of its fine at the surface Drantm cgl. It is highly ochriote, and here and there appears the underlying dol. The same seen with Long-well and Clentum in July 4th from this told that the dol blocks in the Drantm come from. To the W. Belmont land is Highgate banded slate. To the E it dips 25°-30°E and short farther west it dips 30° to NW. A little further W. (each of those mile road) overlying directly the Highgate in more Drantm cgl., dipping about 20° W. A little further W. (a stills south the house) in the dol, bed by 75° to W the dol is underlain by some regular Drantm cgl. Another 100' or so W is more Drantm cgl. Underlying it is some Highgate slate dip E about 25°. All highly ochriote. In same farm field but now we the slate dips W 20°-45°. All of fine slate