"Note. At West Side Park in a shut-coring there is exposed the same soft yellowish-white soft limestone almost a chile having the same fresh as on the basal layer of the section of the previous page. Immediately above these beds at West Side Park occur the Chromet-form bed and although I don't remember seeing any of these fossils on Apple Hill yet I believe both take the same horizon. Beneath these soft limestones at West Side Park in the lowest adjacent field one can gather numerous P. incrusteens and small P. bipartite and rares an O. brachis. There are there the underlying Tanton beds while are above, which Sapping he called the Capitol Hill limestone, are