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7
August 21, 1888
This Limestone forms the bedrock for over a mile on the top of ridge. The road [[strikethrough]] crosses [[/strikethrough]] reaches the Limestone on the line between the [[insertion]] Wm [[/insertion]] Scheels and Ira Millard farms.
This morning, I have seen thousands of zaphren-toids, and two favosites.
Broken Crinoid Stems frequently constitute the main mass of this Limestone.
Afternoon.
I continue tracing this stone north to the south line of [[underlined]] Wm [[/underlined]] Jones' farm, where the road descends from the top of the limestone fully forty feet, to the Hamilton Shales, about 30 rods south of Mr Jones' house.