Toward the Phylogeny of a Fossil Species Flock, Semionotid Fishes from a Lake Deposit in the Early Jurassic Towaco Formation, Newark Basin (Classic Reprint)
Excerpt from Toward the Phylogeny of a Fossil Species Flock, Semionotid Fishes From a Lake Deposit in the Early Jurassic Towaco Formation, Newark Basin The Newark Basin. (fig. In central New jersey and eastern Pennsylvania, is the largest of the Newark Supergroup basins, covering an area of about km (manspeizer and Olsen The long axis of the basin runs from Rockland County, New York, southwest to Lancaster, Pennsylvania, a distance of about 220 km (olsen 1980b). At the southwestern tip of the basin, the terminal Robeson ...
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Excerpt from Toward the Phylogeny of a Fossil Species Flock, Semionotid Fishes From a Lake Deposit in the Early Jurassic Towaco Formation, Newark Basin The Newark Basin. (fig. In central New jersey and eastern Pennsylvania, is the largest of the Newark Supergroup basins, covering an area of about km (manspeizer and Olsen The long axis of the basin runs from Rockland County, New York, southwest to Lancaster, Pennsylvania, a distance of about 220 km (olsen 1980b). At the southwestern tip of the basin, the terminal Robeson Conglomerate pinches out into the New Oxford Formation and Gettysburg Shale of the neighboring Gettysburg Basin (mclaughlin The eastern border of the basin is defined by the Hudson River in the north, and the basin is overlapped by Cretaceous rocks in the south. Major northeast-southwest trending faults running from Stony Point, New York, to near Reading, Pennsylvania, delineate the northwestern lateral border of the basin and separate the neighboring Paleozoic strata from the Newark Mesozoic rocks. Six sedimentary formations and three basalt formations are exposed in the Newark Basin. In order of superposition, these formations are the Stockton, Lockatong, Passaic, Feltville, Orange Mountain Basalt, Towaco, Preakness Basalt, Boonton, and Hook Mountain Basalt (olsen l980a). Most of the exposed sediments in the basin are Late Triassic in age, including the Stockton arkose, the gray siltstones of the Lockatong Formation, and virtually all of the gray siltstones and red beds of the Passaic Formation. Early jurassic sediments, in cluding the Feltville, Towaco, and Boonton Formations (cornet and others are exposed primarily in the Watchung Syncline in the northwestern portion of the basin (fig. With minor exposures farther west in the New Germantown. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at ... This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.
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