All of this eroded matter should stand as it is in the Charlton series. The top is irregular due to the erosing interval. See Hartnagel's report for the same point. The Corniforms rest directly on the uppermost Marlites, although a definite contact was not seen. These Marlites li. are a large granular, coroidal limestone with scattered fossils. The flat Strophostomatia of this thin beds are here Rhyachotesta (two specimens), Lep-cells, Rhyechatina, huge namace logyra, Lepinhtmitalis, small Gonioteleids, Chipidocella Matha (me not occur), Thriellum down to 2 1/4 feet deep on a grassy slope probably not more than 2 or 3 feet. Marlites Below 30 inches of dark colored event bedded can aggregates Laminidae limestone almost without fossils. Rare small fucoida, and few red algae. Furcoids, a large variety come, Then 4 feet of the same kind of li. with an occasional other moderate size log and Lenticularae. That the upper Chretospongia bed here is less than 6 feet thick. Left Isgaense at 8.57 P.M for Albany, Arrived at Albany at 12/45 Spent one night at Kieler Hotel.