Friday Aug 19 - 1932 Wea. SAT. JUNE 12, 1909 Ther. Rained once last night and this morning all is over, but cold. At 12.30 P.M. Jam off north again on the bus for Fmda Junction. My still contact near Swantm = Fmda Junction I now do not believe in contact between the Central and Eastern Sequences. On the Brattleboro road there is some fresh outcrop in the Swantm to the south of the exposed contact and this does underlie the "Chazy granite." In other words all is here Drinorotic. Then walked N.W. along the Vermont Central R.R. to the little hill marked on map. All is here to my surprise Errin Drinorotic. There was to be a small quarry here that I understood we in town The whole dip goes S.E., but climbing the quarry, exposures shows much Steeply dips and in the opposite direction. How this can have been moved by the Pleistocene glaciers or has it been turned during time of Tertiary? This is a fine rep- resentation of the Drinorotic. On the west side there is a precipitous cliff 50' high all Drinorotic. What it lies in contact with seems to be W and N. I have applied to a flat of Chamythic late bottom both on north and south, going uphill in sight to the St. Bridge No. on the Brattleboro road of the Vt. Central R.R. at a