. Bulletin - New York State Museum. Science. GEOLOGY AND PALEONTOLOGY OF THE SCHOHARIE VALLEY 135 The lower beds of the Coeymans formation are generally massive limestones, while the npper ones are more thin bedded and gener- ally show a transition to the overlying New Scotland formation. This relative character is maintained throughout the Helderberg region, and is also found in the outliers east of the Hudson, Mt Becraft and Mt Bob. Topographically this is expressed by a cliff wherever the massive. Please note that these images are extracted from scanned page images that may have been digita
. Bulletin - New York State Museum. Science. GEOLOGY AND PALEONTOLOGY OF THE SCHOHARIE VALLEY 135 The lower beds of the Coeymans formation are generally massive limestones, while the npper ones are more thin bedded and gener- ally show a transition to the overlying New Scotland formation. This relative character is maintained throughout the Helderberg region, and is also found in the outliers east of the Hudson, Mt Becraft and Mt Bob. Topographically this is expressed by a cliff wherever the massive. 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
