override the western beds and the lamination; how far no one knows. There is nothing in the Typography to call attention to the past overthrust. We then travelled farther south to Sturges- sawant are just south of the station back of the icehouse we sees 4x proms of the Bedlamerton. These are very light green shales and my thin bands of black shale (with graphites) lites) and goes of them (about 3/4 inch) white dinestones. In a very short vertical distance we gets graphite of two zones. On the upper Tetragraphite and lower down Byrographite with Phellographite. This again is confined as Lower Cambrian, but further on these beds do actually appear again. Left Sturgesant at 8:30 and SMatch to Albany at 9:15.