. Annual report of the Regents. New York State Museum; Science. 11 N* X tI U ,frT! n l r(| ,y "tt\o. i »i ? v.' Fig. 7 Contact of the trap and sandstone south of the entrance to the tunnel of the "West Shore railroad near Haverstraw. The sandstones dip away from the observer westward. ledge of highly altered slate (hornfels) outcrops a few feet from the trap along the road leading south from Long Clove. West of Short Clove no cases of metamorphism were noted, though the sedimentary beds were often exposed close to the trap, and in one locality, figure 8, the actual contact was seen.
. Annual report of the Regents. New York State Museum; Science. 11 N* X tI U ,frT! n l r(| ,y "tt\o. i »i ? v.' Fig. 7 Contact of the trap and sandstone south of the entrance to the tunnel of the "West Shore railroad near Haverstraw. The sandstones dip away from the observer westward. ledge of highly altered slate (hornfels) outcrops a few feet from the trap along the road leading south from Long Clove. West of Short Clove no cases of metamorphism were noted, though the sedimentary beds were often exposed close to the trap, and in one locality, figure 8, the actual contact was seen. Other effects than metamorphism. In general the trap has no effect on the sedimentary beds other than specified above. The latter were not disturbed beyond the movement necessary to pro- vide room for the intruded mass. The overlying beds were gently raised, apparently without any great distortion. Where the trap. 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; University of the State of New York. Board of Regents. Albany : J. B. Lyon, State Printer
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Keywords: ., bookauthorne, bookcentury1800, bookdecade1880, booksubjectscience
