Sunday August 21-1932 Wea. SUN. JUNE 20, 1909 Ther. Being on north it looks as if there maybe one to three a none of those rounded out sandy bits [quartzite] that got squished and moved together by the limestone falling around them, They are incomplete layers that have spun away due to the overriding Central Sequences. The contact level between the Drimrodi and the Phillipbury area is not a horizontal me. It undulates and may have dolins more than 60' and canting 45° at their drive rate on both sides of road near the hub an over six feet further south, the Drimrodi is down again to the level of the road. Further south it is between 40-70 above the road next a small dipley after Phillipbury with the knarled inter ducted ? quartzite. Around Tullers School the land is low and fairly flat but directly to E of School there are upswings Drimrodi up to 10' high. A few hundred feet to the north it is on the inside of the road, and in Stevens steadily Brook it makes a small fall to the east of the road. While the country is here undulating one sees no fine upswings of the Drimrodi. If Phillipbury is exposed it must be in the lower land 1/3 to 1/2 mile east. Being now on the S.E. across the Arantua road and is Champlain sands, but in the Stevens Brook