organisms in the certus. The Haell shales are replete with sporangia and when crushed give certain lagsms a slight amber tint, see the specimens. Also for two species of Lingula, and a Lepidodendron. See the specimens. We also saw short pieces of wood that had ten camotes to coal = a hydrocarbon or fatty, of Lepidodendron thus maybe 3 speed or more, the others had marks like this. These Williams has. Along the road large pieces of limestone with sand check are found among the crystalline cratics. These are of Hamilton age and have an abundance of Chonetes oricina (crasse but ferris striate). The other fossils are small Spirifer concinnatus, S. granulosa, Stephen denta papilana, S. intricata small, Cryptacus forthi and justly other fossils. At Otmy Point about 2 miles north of Kettle Point one sees the Hamilton limestone.