Articles liés à The Geology of the Syracuse Quadrangle (Classic Reprint)

The Geology of the Syracuse Quadrangle (Classic Reprint) - Couverture souple

Thomas Cramer Hopkins

 
9781331983897: The Geology of the Syracuse Quadrangle (Classic Reprint)

Synopsis

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Présentation de l'éditeur

University ol theS tate olN eiM-B tlletin Entered as second-class matter August 2, 1913, at the Post Office at A lbany, N. Y., under the act of August 24, 1912 Published fortnightly No. 571 ALBANY, N. Y. JULY 15, 1914 New York State Museum JOHN M. CLARKE, Director Museum Bulletin 171 THE GEOLOGY OF THE SYRACUSE QUADRANGLE BY THOMAS CRAMER HOPKINS INTRODUCTION The Syracuse topographic quadrangle, which is here specially under consideration, includes an area one-fourth of a degree square, in latitude 43 -43 15 N. and longitude 76 -76 15 W. Situated near the geographic center of theS tate of New York, including part of two of the great physiographic regions of theS tate, and the outcropping edges of many of the stratigraphic units of the paleozoic rock series, it has many features in common with, and hence may be taken as typical of, a rather broad belt extending east and west through the middle of theS tate. The city of Syracuse is on the line of theE rie canal; lies at the intersection of the east-west (N ew York Central and West Shore) and the north-south (D elaware, Lackawanna and Western) railways, and has besides several branch lines radiating from the city and several suburban electric lines. Central location and excellent transportation facilities make it an important commercial center. This quadrangle is located on the border line between the lake plains on the north and the Alleghany plateau on the south, two of the distinctive physiographic regions of theS tate. It has a varied physiography, which is somewhat intensified by glacial action.
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Présentation de l'éditeur

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