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Ch. 3: Brooklyn and Queens

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156             GEOLOGY OF NEW YORK CITY
Long Island to New Jersey, and the Long Island beds gen­erally are related to the older (Raritan, Amboy) beds of New Jersey, but the lignite-bearing sands on the south merge into the formation next above, vis., the Matawan. This Cretaceous zone is a narrow strip, striking northeast and southwest, crossed from New Jersey to Long Island.
Outcrops that have become famous and have yielded plant remains are at Glen Cove, Cold Spring, Great Neck, Lloyd Neck, and Sea Cliff. Cretaceous fossils have been found in the drift in Brooklyn, at Flushing (Cemetery), but their origin is, of course, problematical. The Cretaceous beds have been folded and disturbed, and this vitiates conclusions, so far as they are guided by depths. It would seem that if the marine marls and greensands of Monmouth County, New Jersey, are Upper Cretaceous, Long Island Cretaceous, in which they are absent, is Lower Cretaceous, and did not ex­perience during its Cretaceous history as deep a submergence as the southern areas now included in New Jersey.
Succeeding the Cretaceous the Tertiary deposits should be expected, but on Long Island, however naturally it might be regarded as an areal prolongation of New Jersey, and geo­logically assimilable to New Jersey, these deposits are not represented very unmistakably. Of course, they may have largely been removed by erosion, or Long Island may have been withdrawn, through elevation, northward from the arena of Tertiary sedimentation.
At this stage of his study of the development of Long Island topography, Mr. Veatch unfolds a scheme of recon­struction by which, through erosion, at higher levels than at present, a hill and valley system was wrought out. This had a continental significance. It was represented in Long Island, in New Jersey, in Delaware, in Maryland, and had, it is as­sumed, something to do with the final and recent courses of the Connecticut, Delaware, and Potomac Rivers. The suc­cession of events, as pictured, was like this: The early Plio­cene (Tertiary) was an erosion interval; the softer Cretaceous
Ch. 3: Brooklyn and Queens Page of 281 Ch. 3: Brooklyn and Queens
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