. Bulletin of the Geological Society of America. Geology. 148 KUMMET. AND WELLER IJMESTONES OP KITTATINNY VALLEY state line. On the northwest it is bounded by the Kittatinny mountain, the crest of which is composed of liard Oneida conglomerate and sand- stone. On the southeast lie the pre-Cambrian crystallines of the high- lands, while the rocks of the valle}^ are chiefly limestones and shales of. Scale Miles. Hudson Rtifr Shale Km a lin/iy lim n ton e â f're Cambrian Cryitultinfi Normal B»undari's Fault Boundaries Fkjluk 1.âMap of Northwestern New Jcrsri/. 1. Newton. 2. Hamburg. 3. Deckertow
. Bulletin of the Geological Society of America. Geology. 148 KUMMET. AND WELLER IJMESTONES OP KITTATINNY VALLEY state line. On the northwest it is bounded by the Kittatinny mountain, the crest of which is composed of liard Oneida conglomerate and sand- stone. On the southeast lie the pre-Cambrian crystallines of the high- lands, while the rocks of the valle}^ are chiefly limestones and shales of. Scale Miles. Hudson Rtifr Shale Km a lin/iy lim n ton e â f're Cambrian Cryitultinfi Normal B»undari's Fault Boundaries Fkjluk 1.âMap of Northwestern New Jcrsri/. 1. Newton. 2. Hamburg. 3. Deckertown. 4. Hardistonville. 5. Blairstown. G. Columbia. 7. Belvidere. 8. Phillipsburg. 9. Hackettstown. 11. Dover. 12. Washington. 13. Carpenters- ville. The Hardiston quartzite forms a narrow outcrop along the normal contact of the Kitta- tinnj'limestone and the crystallines. The Trenton limestone forms a narrow outcrop along the normal contact of the Kittatinny limestone and the Hudson River siiale. Cambrian and Ordovician age. In addition to this wide trough-like depression there are several long, narrow valleys within the highlands themselves, the rocks of which are of the same age as those of the Kitta- tinny valle3\ Small detached areas of the same formations occur along. 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 Geological Society of America. [New York : The Society]
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Keywords: ., bookcentury1800, bookdecade1890, booksubjectgeology, bookyear1890
