At Cornell

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And the records of these varying levels of Cayuga remain today in the shape of deltas which the tributary streams, such as Fall creek and Coy Glen Stream, formed in these higher level lakes with the sediment load they car- ried. Thus Cornell Heights are built on the succes- sive delta terraces of Fall creek, while opposite, on the western side of the Cayuga valley, one can count, at Coy Glen, four distinct flat-topped, delta terraces of that stream, each marking a different level of the glacial... lake. These deltas contain the coarse mater- ial which the streams brought down, the fine clay was distributed widely over the whole lake bottom, and is now found spread over all the slopes. Ice- bergs broke off from the glacier front and floated out into the lake, carrying angular, glacially- The Waters of Cayuga JTljp "^toitp (Slants" aa Jjltrturrft btj an Jroqitnia Artist scratched boulders, which melted out and were dropped far from shore in the midst of the fine clay deposits forming on the bottom.

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