In the ?Oriskany sarr. J. minchi[illegible], then brought from rather of the Lower Oriskany and Beecroft, Farther south on the same range of ? glance with yellowish iron stains comes out in a quarry quarry, a little farther south and the Beecroft is seen to lie above it. Then there comes the Ohio Salt Land, due to large petosiforms and flabella, to try to casts and crinoid stem fragments reminding of Maracrinus. Beecroft quarry the rock. silf. start 10° all on urford [illegible] slang quartzite latrubi shun dip. shot 25 + 30° Lime tree quarry In the above mentioned glance quartzite of the quarry seen crinoid segments reminding of Maracrinus as a petosiform bryozoan and stems of a flabella form, there are not found north of the Oriskany. From the river a little the same quartzite, even fluted appears on the east side bank of the Iron Furnace. There was made the above section. The limiture of this section is not the Beecroft since at a single specimen of Stenipor crininae was seen. On the other hand the limestone about in Maracrinus columnus, some Alcyon reticularis and Orthos pyr. O. Muta. Its same genus to are crystalline than the Beecroft. It must be the Ohio Saltland a Cosynans. Both quartzites look or smooth alike that at first I thought they were the same.