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Geology and Engineering Geology of the New York Metropolitan Area New York Metropolitan Region July 20-25, 1989 Field Trip Guidebook T361 Leader: Charles A. Baskerville, Editor Associate Leaders: Nicholas K. Coch, Sidney Horenstein, Martin Prinz, John H. PuHer, Geneva R. Roberts-Dolgin and Dennis Weiss American Geophysical Union, Washington, D.C. Copyright 1989 American Geophysical Union 2000 Florida Ave., N.W., Washington, D.C. 20009 ISBN: 0-87590-601-X Printed in the United States of America COVER PHOTOGRAPH A low altitude oblique view ofa part of the New Yo'" Metropolitan area from over central Kings County (Brooklyn) looking a little north of west. The Island of Manhattan occupies the center of the scene with Governors Island just off its south end. Queens County is located in the south east corner of the photograph. The State of New Jersey occupies most of the remainder of the photograph. CREDn- NASA Aircraft 10 E-1704-99CT FRAME NUMBER 109 Provided by the U.S. Geological Survey CONTENTS Page INTRODUCTION 1 C.A. Baskerville BUILDING STONES OF THE NEW YORK CITY AREA......•............2 Sidney Horenstein Introduction ,..2 Excursion stops Part 1. Building stones 4 stop 1. Grand Central Terminal 4 stop 2~ 110 East 42 Street 6 stop 3. 51 East 42 Street 6 stop 4. 330 Madison Avenue 6 stop 5. The New York Public Library 7 stop 6. 530 Fifth Avenue 7 stop 7. Rockefeller Center 8 stop 7a. 30 Rockefeller Center 8 stop 7b. The Associated Press Building 8 stop 7c. British Building 9 stop 8. Sakis Fifth Avenue 10 stop 9. st. Patrick's Cathedral 10 stop 10. Villard Houses 10 stop 11. 477 Madison Avenue ll stop 12. 666 Fifth Avenue 11 Part 2. Stone Processing 12 stop 13. The Miller-Druck Company 12 Part 3. Original stone Samples for Grand Central Terminal ........•......................- 12 stop 14. Van Cortlandt Park 12 Part 4. Stone Quarry 13 stop 15. The DiRienzo stone Quarry 13 References cited 14 Suggested Readings 14 ENVIRONMENTAL GEOLOGY AND GEOLOGICAL DEVELOPMENT OF THE LOWER HUDSON ESTUARY AND NEW YORK HARBOR 15 N.K. Coch and Dennis Weiss Introduction 15 Drill core stratigraphy 16 Sea level curve 16 Foraminiferal zonation 17 Post-glacial geologic history - 18 Environmental geology of New York harbor 20 Stations to be occupied 20 Station 1. The Statue of Liberty 20 station 2. Entrance to the East River 21 Station 3. Entrance to the Gowanus Canal 22 station 4. Central part of the Upper New York Bay 22 Conclusion 23 References cited 23 GEOLOGY OF NORTHEASTERN NEW JERSEY 26 J.H. Puffer Introduction 26 Geologic setting of northeastern New Jersey, Proterozoic rocks of the New Jersey Highlands 26 Granites 26 Hornblende granites and alaskite (Byrum Intrusive Suite) 26 Pyroxene granite and pyroxene seyenite 27 Quartz-oligoclase gneiss 27 Amphiboli te 28 v contents Paqe Marble ......................•.....................28 Other Proterozoic rocks 29 Paleozoic rocks of northeastern New Jersey 29 Hardyston Formation 29 Allentown Dolomite 29 Martinsburg Formation 29 Shawangunk Formation and Green Pond Conglomerate 30 Alkalic intrusives 30 Triassic and Jurassic rocks of the Newark Basin 30 Mesozoic stratigraphy 30 Stocton Formation 30 Locatong Formation 30 Passic Formation .............................•....31 Orange Mountain Basalt 31 Feltville Formation 31 Preakness Basalt 31 Towaco Formation 32 Hook Mountain Basalt 32 The Boonton Formation 32 Palisades sill 32 GIaciaI geology 33 Field trip stops 33 stop 1. Ross Dock 33 stop 2. Great Falls, Paterson, New Jersey 34 The Ramapo Fault 34 stop 3. The Quartz-oligoclase gneiss 35 stop 4. Hook Mountain Basalt 35 Type sections of the Orange Mountain and Preakness Basalt flows 35 References cited .................•.....................36 NEW YORK CITY: JUXTAPOSITION OF CAMBRIAN AND ORDOVICIAN MIOGEOCLINAL AND EUGEOCLINAL ROCKS 39 C.A. Baskerville Introduction 39 Previous work 39 stratigraphy 41 Fordham Gneiss 41 Yonkers Gneiss 41 Lowerre Quartzite 41 Inwood Marble 41 The Manhattan Schist 42 Hartland Formation 42 Ravenswood Granodiorite 43 Structure 43 Field trip stops .................•.....................44 stop 1. The Lake in Central Park 44 stop 2. Isham and Inwood Hill Parks 44 stop 3a. Johnson Avenue, Spuyten Duyvil section of Bronx County 45 stop 3b. Eastern side of Broadway north and south of Mosholu Avenue in Van Cortlandt Park ...45 stop 3c. Van Cortlandt Park East at East 235th Street •.........................................46 stop 4. Cross Bronx Expressway at Boro Hall Park .46 stop 5. East 233rd street in Seton Falls Park 46 stop 6. Madison Avenue and East 122nd street 46 References cited 47 vii contents paqe THE AMERICAN MUSEUM OF NATURAL HISTORY 49 Martin Prinz Suggested reading 50 S.C.H. Bailey collection 50 Clarence S. Bement collection 50 George F. Kunz collection 50 Mineral, gem, and meteorite collections 50 History of the Museum 50 THE GEOLOGY OF STATEN ISLAND AND WESTERN LONG ISLAND, KINGS COUNTY AND QUEENS COUNTIES, NEW YORK 51 G.R. Roberts-Dolgin Introduction 51 Geologic setting 51 staten Island 51 Basement rocks 51 Serpentini t e 52 Triassic-Jurassic Newark Basin 52 Cretaceous coastal plain deposits 53 Pleistocene geology 54 Pensauken Formation 54 Holocene tidal and upland marsh deposits 54 Western Long Island .............•......................54 Basement rocks 54 0 ••••••••••••••••• Cretaceous sediments 55 Pleistocene deposits 55 Holocene tidal marsh 55 Field trip stops 56 staten Island 56 stop 1. Bay and Canal streets 56 stop 2. Victory Boulevard on the east side of Silver Lake Reservoir 56 stop 3. Forest Avenue between Van Name and Coonley Avenues 56 stop 4. Veterans, Road and Arthur Kill Road 57 Western Long Island 57 stop 5. Highland Park 57 stop 6. Playground at 10th Street and 36th Avenue, Long Island City 57 References cited 57 ix Leader: Charles A. Baskerville U.S. Geological Survey 922 National Center Reston, VA 22092 Associate Leaders: Nicholas K. Coch Geology Department Queens College of CUNY Flushing, NY 11367 Sidney Horenstein Department of Invertebrates American Museum of Natural History 79th Street and Central Park West New York, NY 10024-5192 Martin Prinz Department of Mineral Sciences American Museum of Natural History 79th Street and Central Park West New York, NY 10024-5192 John H. Puffer, Chairman Department of Geology Rutgers, The State Univ. Newark, NJ 07102 Geneva R. Roberts-Dolgin New York City Department of General Services 1 Center Street New York, NY 10007 Dennis Weiss, Chairman Dept. of Earth and Planetary Sciences City College of CUNY 138th St. and Convent Avenue New York, NY 10031 xi INTRODUCTION Charles A. Baskerville This field trip enables delegates attending the Twenty-eighth International Geological Congress to spend several days in the largest city in the united states. Local geologists have designed day-long field trips to acquaint participants with the complex geology of the New York city metropolitan region. The papers included in this book will serve as guides to the planned trips but may not necessarily follow the order in which the trips will be scheduled. T~e City of New York lies at the junction of three physiographic provlnces-~theManhattan Prong of the New England Upland in the northeast, the Atlantlc Coastal Plain in the southeast, and the Newark Triassic Jurassi~ Basin (Triassic Lowland) in the west (Lyttle and Epstein, 1987; Baske~vllle, 1982; Thornbury, 1965). The juncture of these provinces also constltutes the eastern edge of the New York promontory (Williams, 1978), the narrowest east-west section of the Appalachian Piedmont-Coastal Plain rock units. The first day will include an orientation at The City College of the City University of New York and a visit to the American Museum of Natural History to look at the museum's fine collection of rocks and minerals from the New York City region. We will also get a glimpse into some of the laboratories not open to the pUblic. During the following four days we will cover the following areas: (1) most of the major Proterozoic to Ordovician rock units of the Manhattan Prong; (2) Cretaceous to Pleistocene and Holocene sediments of the Atlantic Coastal Plain; (3) the southernmost tip of the Manhattan Prong and easternmost edge of the Newark Triassic-Jurassic Basin on staten Island and Long Island; (4) the rocks of the Newark Basin,especially of northeastern New Jersey, and the Proterozoic to lower Paleozoic gneisses, granites, and sedimentary rocks of the New Jersey Highlands, in the Reading Prong (Thornbury, 1965; Lyttle and Epstein, 1987); and (5) the use of stone in New York city for construction purposes in some famous and not-so-famous buildings. We will visit a quarry where some of the building stone is obtained and a mill where stone finishing is done. We will also board an oceanographic research vessel to see how scientists perform estuarine studies of the waters surrounding the metropolitan area. To avoid confusion, please note that this city is composed of five counties, which are also called boroughs: New York County (Borough of Manhattan), Bronx County (Borough of the Bronx), Queens County (Borough of Queens), Kings County (Borough of Brooklyn), and Richmond County (Borough of staten Island). New York City covers a land and surface-water area of about 950 km2• REFERENCES CITED Baskerville, C.A., 1982, The foundation geology of New York City, in Legget, R.F., ed., Geology under cities: Geological society of America Reviews in Engineering Geology, v. 5, p. 95-117. Lyttle, P.T., and Epstein, J.B., 1987, Geologic map of the Newark 1° x 2° quadrangle. New Jersey. Pennsylvania. and New York: Miscellaneous Investigations Series 1-1715, 2 sheets, scale 1:250,000. Thornbury, W.O., 1965, Regional geomorphology of the united states: John Wiley & Sons, Inc., New York, 609 p. Williams, Harold, compiler, 1978, Tectonic lithofacies map of the Appalachian orogen: Memorial University of Newfoundland, Map No.1, scale 1:1,000,000. T361: 1 BUILDING STONES OF THE NEW YORK CITY AREA Sidney Horenstein Department of Invertebrates American Museum of Natural History, New York INTRODUCTION setting; and (4) that they serve as an excellent way to popularize New York city, especially the geology. island of Manhattan, is a treasure Trip participants will observe a trove of building stones, a small sample of the variety of the repository of materials that are construction materials used in New imported from many regions of the York City and address the points world. It is also a library of mentioned above. The study of dimension stone no longer being dimension stone in buildings is quarried. Many factors contribute to instructive to architects and others the variety of stone including in the building industry who need to competition among architects, price, make decisions about future choices. and quality. The choice of a In this context we will examine particular stone for a building several locations where problems project is a complex series of associated with design as well as decisions based on the architect's poor choice of material are apparent design, availability of material, (fig. 1). Many "problems" are appropriate physical properties, such esthetic, such as discoloration and as compressive strength, absorptive (or) loss of polish. Although not capacity, appropriate mineralogy for necessarily detrimental to the the particular climate, and cost. strength of the stone, discoloration Decorative stones for interior use- may indicate other problems in the lobbies, offices and rest rooms--need building or the site. to meet minimum requirements for The excursion is divided into four strength and resistance to parts: (l)a walking tour from Grand weathering; therefore, they include a Central Terminal at 42nd Street and much broader array of materials than Park Avenue to Fifth Avenue and 52nd dimension stone used for exterior street; (2) a visit to a small stone facades and monuments. Choice of shop in the South Bronx where materials for exterior use in New dimension stone is cut, shaped and York City take into account the polished; (3) a walk in Van Cortlandt amount of rainfall, the maritime Park, Bronx to view original stone climate, and the freeze-thaw cycle. samples for Grand Central Terminal; Another important factor is the and (4) a visit to the last remaining susceptibility of a stone to dimension stone quarry in westchester disruption by the crystallization of County (fig. 1). salt used to melt ice during the One point that should be addressed winter. at this time is the naming of The study and documentation of building stones. Quarriers and stone building stones are important because dealers have coined their own we see: (1) how building stones descriptive names for stones for respond to the processes of marketing identification. This weathering, and thus provide insights practice leads to much confusion for future use; (2) how these stones because the commercial names usually are a record of changing contain geological terms, but the architectural styles and thus an names may not match the scientific important historical record; (3) how meaning of these terms. "Granite," they are an important resource for for instance, is used by dealers for students, an outdoor classroom of almost any coarse grained igneous worldwide stratigraphy and rock, including "Canadian Black paleontology, including strata no Granite" which is an anorthosite. longer exposed in their original For clarity, wherever the commercial T361: 2 NOTTOSCALE FIGURE 1 BronxandManhattan location map. The numbersreferto thesites discussedin the textandto be visitedin the field. 1. GrandCentralTerminal 7c. BritishBuilding 2. BowerySavings Bank 8. Sak'sFifthAvenue 3. East42Sf. office building 9. Sf.Patrick'sCathedral 4. Madison Ave. ottice building 10. VillardHouses 5. N. Y. Public Library 11. Madison Ave. ottice building 6. Bankandottice building 12. Tishman Building 7. RockefellerCenter 13. Miller-DruckCompany 7a. 30RockefellerCenter 14. Van CortlandtPark 7b. AssociatedPress 15. DiRienzoStone Quarry T361: 3

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