. Bulletin - New York State Museum. Science. GEOLOGY AND PALEONTOLOGY OP THE SCHOHARIE VALLEY 225 Ithaca beds in the Schoharie region, this replacement however not extending beyond central New York. In Blenheim township about 500 feet of this formation has been noted by Prosser, but northeast from this in Moheganter hill, the Ithaca is scarcely represented, the Oneonta beds follow- ing almost immediately on the Sherburne. This shows that the source of the nonmarine sediments was to the northeast. The Oneonta beds From the Chenango valley eastward the Ithaca is capped by the Oneonta formation w
. Bulletin - New York State Museum. Science. GEOLOGY AND PALEONTOLOGY OP THE SCHOHARIE VALLEY 225 Ithaca beds in the Schoharie region, this replacement however not extending beyond central New York. In Blenheim township about 500 feet of this formation has been noted by Prosser, but northeast from this in Moheganter hill, the Ithaca is scarcely represented, the Oneonta beds follow- ing almost immediately on the Sherburne. This shows that the source of the nonmarine sediments was to the northeast. The Oneonta beds From the Chenango valley eastward the Ithaca is capped by the Oneonta formation which is composed of red and green shales, reddish sandstones and coarse grained grajdsh to greenish gray sandstones. These rocks are nearly unfossiliferous, containing. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original New York State Museum; New York State Museum. Albany : New York State Education Dept
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Keywords: ., bookcentury1800, bookdecade1880, booksubjectscience, bookyear1887
