Corner of the Beach. Tuesday, August 16-1938. Another foggy morning with light rain. I remain at the hotel, but Cloud goes gathering and collecting. After lunch walked south to the Corner and then along the mountain road to a quarry for road metal just S.E. of a Protestant church. Saw no fossils in site, but in the brook laid aside about ten pieces with Whitchell fossils. These come down the brook from beds of fine sand further up the stream. Just N.W. of the Protestant Church some red oys stand on end and these according to Allcock and Kindle are of the Cannes de Roche form. Below an coarse coy, 40' thick; then middle ss and sl 80'; and above in the Upper Coy: 40' = 200. Has plants suggestive rather of the early Penn. than Miss. See Allcock's map for distribution. Regards it as a part of the Bunaventine defined in different rocks. The red rock on the top of Reed Peak is Barke- sandstone. This is what Corder and Hornblunt.