- Clinton fossils are of the Rochester type. I think here as at Pinto a whole series with thousands of limestone. Which makes it 58 feet. There are less of the Rochester limestone bands here than at Pinto. In other words more shale passing more quickly into the Clinton phase, which begins the Rochester here here at the heavy bedded ferruginous arenaceous lying about above a thickness of about 6 feet followed by a ten inch band of [only locally surviving] Politic high frondiferae and etc. It occurs abundantly Philodimella circularis the Clinton guilds, Amphistea hemithelyza occurs below here but not above the heavy bedded ferruginous also limestone arenaceous (At Pinto are seen three fossils in the Rochester series) and says nearly here (a little to the east of the Lakeport end) he sit Palaeoveselus rotuloides 20 feet below the heavy beds or limestones lie. Created well above, which says it also occurs in N.Y. high near the In other 8 feet below the heavy bedded arenaceous lie, occurs the upper Clinton fossil iron ore. Thickness about 4 feet intwined with mud shale. Locally all of it is fossil iron ore. This bedded frondiferae lie occur still below for at least one foot more. Then nothing but Clinton shales, to the Lake- and Park lode at the base of the massive lime near the base of the "Middle series" in red shale or we have seen about first Caeapm.. This goes of oolite occur about 100 two feet above here beside the railroad track Almost due west of Bald Hills may be seen