. Brachiopoda and Lamellibranchiata of the Raritan clays and greensand marls of New Jersey. Brachiopoda, Fossil; Bivalves, Fossil; Paleontology. :k-:^:i^^^.-'<^'y. Sooth Amboy Fireclay Bed 20ft. Kaolin Kimpaf" ]."»ft. Micaceous Sand Bed ?Ttr ft. Laminated Clay and Sand 30ft. Pipe Clay 15 ft. Woodbrid^e Fire CJay Bed 20 ft. Fire Sand Bed ^c^ f^^ Rarixan _ -. Fire Clay Bed 15 ft. Raritan Potters Clay Bed 244t Ked Shale 347 ft. CO OS eg o c (D O C3 © © o © © a o Q Sound, about four miles northeast of Woodbridge, through the northern part of that village, and then across the hills
. Brachiopoda and Lamellibranchiata of the Raritan clays and greensand marls of New Jersey. Brachiopoda, Fossil; Bivalves, Fossil; Paleontology. :k-:^:i^^^.-'<^'y. Sooth Amboy Fireclay Bed 20ft. Kaolin Kimpaf" ]."»ft. Micaceous Sand Bed ?Ttr ft. Laminated Clay and Sand 30ft. Pipe Clay 15 ft. Woodbrid^e Fire CJay Bed 20 ft. Fire Sand Bed ^c^ f^^ Rarixan _ -. Fire Clay Bed 15 ft. Raritan Potters Clay Bed 244t Ked Shale 347 ft. CO OS eg o c (D O C3 © © o © © a o Q Sound, about four miles northeast of Woodbridge, through the northern part of that village, and then across the hills to Metuchen, and onwards to the Raritan, which it crosses in the southern j^art of the city of New Bruns- wick, and thence onward to Ten Mile Run and Kingston, and thence along the valley in which the Delaware and Raritan Canal runs on the south of Princeton and Trenton to the Delaware River. The outcropping edge of these formations is thin, so that in many places the underlying red sandstone is exposed in the inequalities of the surface, or is easily reached in digging. This, of course, must leave the edge somewhat irregular, and in one place in Middlesex County, north of the Raritan, the red sandstone rises in a considerable hill south of this line, and is entirely surrounded by the white cla3^s of this later formation. The Raritan clav beds, with their intermediate beds of sand, which are the lowest in the series here described, are retained as a ]3art of the Cretaceous series. Stratigraphical relations war- rant The very few fossil shells which have been found in them are of estuary forms, and are thought by some paleontologists to bear a close resem- blance to those of the Wealden or Jurassic age. The greensand and in-. 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 Whitfield, Robert Parr,
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Keywords: ., bookcentury1800, bookdecade1880, booksubjectpaleontology, bookyea
