New York State Agricultural College. Charter, Ordinances, Regulations, And Course of Studies, 1859

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Brewer, indicates the varieties of its soil and its adaptation to the purposes for which it is designed.
The farm is about two and a half miles long, and extends east from the shore of Seneca Lake, the eastern end lying on the ridge between the Lakes, and has an elevation of about 550 feet greater than the western, the slope being gradual and the exposure to the 9 west. A small stream, having its sources mostly beyond the farm, runs through it to the Lake. It is bordered in some places by dry g
...rain land, in others by a narrow swale, while nearer the Lake it sinks into a deep rocky ravine. The immediate banks of the Seneca Lake form low bluffs, from, the top of which the land rises gradually to the extreme eastern end of the farm at Ovid village.
The rock underlying the soil at the western end of the farm, and which crops out at the Lake shore and in the ravine, is a soft shale, the '■^Moscow shales'''' (of Prof. Hall, in his reports on the Geology of New York), belonging to the upper part of the Hamilton group.'''' On this lies the " Tully limesione,'''' an impure limestone, having a thickness on the farm of about eleven feet, half of which is suffici- ently compact for building purposes, and is burned for lime, which is being used in the construction of the College buildings.


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