Geohydrology of Southeastern Pennsylvania by Dennis J

Total Page:16

File Type:pdf, Size:1020Kb

Geohydrology of Southeastern Pennsylvania by Dennis J U.S. Department of the Interior U.S. Geological Survey Geohydrology of Southeastern Pennsylvania by Dennis J. Low, Daniel J. Hippe, and Dawna Yannacci Water-Resources Investigations Report 00-4166 In cooperation with the PENNSYLVANIA DEPARTMENT OF CONSERVATION AND NATURAL RESOURCES, BUREAU OF TOPOGRAPHIC AND GEOLOGIC SURVEY New Cumberland, Pennsylvania 2002 U.S. DEPARTMENT OF THE INTERIOR GALE A. NORTON, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director For additional information Copies of this report may be write to: purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Branch of Information Services 215 Limekiln Road Box 25286 New Cumberland, Pennsylvania 17070-2424 Denver, Colorado 80225-0286 Email: [email protected] Telephone: 1-888-ASK-USGS Internet address: http://pa.water.usgs.gov ii CONTENTS Page Abstract . 1 Introduction . 2 Purpose and scope . 2 Methods of investigation and analysis . 2 Water use . 3 Well depth and casing length . 3 Depth to water. 3 Well yield . 3 Specific capacity . 4 Storage coefficient . 4 Hydraulic conductivity and transmissivity . 4 Water-bearing zones and borehole flow . 5 Ground-water quality. 5 Statistical methods of analysis . 5 Description of study area. 6 Geohydrology of the Coastal Plain Physiographic Province. 8 Location and geographic setting . 8 Water-well density . 9 Previous work . 9 Geohydrologic setting . 10 Unconfined ground-water system . 12 Confined ground-water system . .13 Cretaceous sediments. 14 Lower sand and clay. 14 Middle sand and clay . 18 Upper sand and clay. 20 Post-Cretaceous sediments . 22 Bridgeton Formation. 23 Trenton Gravel . 23 Holocene deposits . 27 Summary characteristics of unconsolidated aquifers in the Coastal Plain Physiographic Province . 27 Geohydrology of the Piedmont Physiographic Province, Piedmont Upland Section . 33 Location and geographic setting . 33 Water-well density . 33 Previous work . 36 Geohydrologic setting . 36 Regolith . 40 Fractured bedrock . 40 Gneissic rocks . 41 iii CONTENTS—Continued Page Geohydrology of the Piedmont Physiographic Province, Piedmont Upland Section—Continued Plutonic rocks . 45 Serpentinite . 49 Setters Quartzite . 53 Cockeysville Marble. 57 Wissahickon Formation . 61 Wakefield Marble . 62 Metavolcanics . 62 Oligoclase-Mica Schist . 66 Albite-Chlorite Schist . 71 Marburg Schist. 77 Peters Creek Schist . 81 Peach Bottom Slate and Cardiff Conglomerate, undivided . 85 Chickies Formation. 90 Harpers Formation . ..
Recommended publications
  • Montgomery Township N.R.I. Appendix – Nitrate Dilution
    Nitrate Dilution Modeling of Montgomery Township, Somerset County, NJ Prepared for: Montgomery Township Environmental Commission Somerset County, NJ 2261 Route 206 Belle Mead, NJ 08502 Prepared by: The GIS Center Stony Brook-Millstone Watershed Association 31 Titus Mill Road Pennington, NJ 08534 April 8, 2004 Introduction Nitrate from natural sources generally only occurs in ground water at low levels but anthropogenic sources can lead to elevated concentrations. Sources include fertilizers, animal waste, and sewage effluent. Nitrate is considered a contaminant in ground water because of various impacts to human health and aquatic ecology. For instance, high levels of nitrate intake in infants can lead to methemoglobinemia, or blue baby syndrome (Hem, 1985; U.S. EPA, 1991). Because of its low natural occurrence and solubility and stability in groundwater, nitrate can also serve as an indicator for possible bacterial, viral, or chemical contaminants of anthropogenic origin. Nitrogen is present in septic system effluent and is converted to nitrate through biological processes active in the soil below the drain field. Once this nitrification process is complete, nitrate is a stable and mobile compound in ground water under normal conditions (Hoffman and Canace, 2001). Nitrate concentrations resulting from septic effluent are mitigated by dilution if the septic effluent is combined over time with water entering the ground through infiltration during and after storm events. The extent of this dilution effect is clearly dependent on long-term rates of both infiltration and nitrate loading from septic system sources. The density of septic systems relative to infiltration rates in a particular area is therefore a critical factor controlling the ultimate nitrate level in ground water.
    [Show full text]
  • Triassic- Jurassic Stratigraphy Of
    Triassic- Jurassic Stratigraphy of the <JF C7 JL / Culpfeper and B arbour sville Basins, VirginiaC7 and Maryland/ ll.S. PAPER Triassic-Jurassic Stratigraphy of the Culpeper and Barboursville Basins, Virginia and Maryland By K.Y. LEE and AJ. FROELICH U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1472 A clarification of the Triassic--Jurassic stratigraphic sequences, sedimentation, and depositional environments UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1989 DEPARTMENT OF THE INTERIOR MANUEL LUJAN, Jr., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging in Publication Data Lee, K.Y. Triassic-Jurassic stratigraphy of the Culpeper and Barboursville basins, Virginia and Maryland. (U.S. Geological Survey professional paper ; 1472) Bibliography: p. Supt. of Docs. no. : I 19.16:1472 1. Geology, Stratigraphic Triassic. 2. Geology, Stratigraphic Jurassic. 3. Geology Culpeper Basin (Va. and Md.) 4. Geology Virginia Barboursville Basin. I. Froelich, A.J. (Albert Joseph), 1929- II. Title. III. Series. QE676.L44 1989 551.7'62'09755 87-600318 For sale by the Books and Open-File Reports Section, U.S. Geological Survey, Federal Center, Box 25425, Denver, CO 80225 CONTENTS Page Page Abstract.......................................................................................................... 1 Stratigraphy Continued Introduction... ..........................................................................................
    [Show full text]
  • Hydrogeology and Ground-Water Quality of Northern Bucks County, Pennsylvania
    HYDROGEOLOGY AND GROUND-WATER QUALITY OF NORTHERN BUCKS COUNTY, PENNSYLVANIA by Ronald A. Sloto and Curtis L Schreftier ' U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 94-4109 Prepared in cooperation with NEW HOPE BOROUGH AND BRIDGETON, BUCKINGHAM, NOCKAMIXON, PLUMSTEAD, SOLEBURY, SPRINGFIELD, TINICUM, AND WRIGHTSTOWN TOWNSHIPS Lemoyne, Pennsylvania 1994 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director For additional information Copies of this report may be write to: purchased from: U.S. Geological Survey Earth Science Information Center District Chief Open-File Reports Section U.S. Geological Survey Box 25286, MS 517 840 Market Street Denver Federal Center Lemoyne, Pennsylvania 17043-1586 Denver, Colorado 80225 CONTENTS Page Abstract....................................................................................1 Introduction ................................................................................2 Purpose and scope ..................................................................... 2 Location and physiography ............................................................. 2 Climate...............................................................................3 Well-numbering system................................................................. 4 Borehole geophysical logging............................................................4 Previous investigations ................................................................. 6 Acknowledgments....................................................................
    [Show full text]
  • Lancaster County Geology
    LancasterLancaster CountyCounty GeologyGeology gfgh µ OverOver TopographicTopographic ReliefRelief Om Miles Í897 0 10 hg Lebanon County Adamstown ¦¨§76 ! Berks County Oha ! Oo Denver ab322 Ephrata Csc Í501 ! Í72 TRh 272 TRn Oco Lititz Í ! Akron Elizabethtown Manheim ! Dauphin County! ! TRhc Cr TRs c Os Rn ! T Terre Hill TRg Trd 322 772 ab 10 Í 222 625 Í ab Í897 Í Í283 Ohm Í230 Oan Í241 East New Holland Oe 722 Petersburg Í Cbs ! Mount Joy ! ! Czc Cch Í23 Cm gga fl R 743 T Í Csb gg pg ggd Í441 Ck Cl 772 72 Í 23 Í ! Í Ca Marietta Ch Lancaster Mountville ! 340 ! Í Columbia 30 ! ! ba Í462 Í462 ab30 Í999 Millersville Ccc Strasburg ! ! Cv Í741 Í741 Í272 41 Í County Chester 896 222 Í gn Christiana ba mg ! oct Cah Í372 S u sq u e h a n n a R iv e r Y o rk C o u n ty gqm LEGEND COUNTY BOUNDARIES Í324 Source: Lancaster County GIS, Copyright (c) 2019 MAJOR ROADS This map to be used for reference or illustrative purposes only. This map FAULT is not a legally recorded plan, survey, or engineering schematic Quarryville and it is not intended to be used as such. For complete disclaimer see: RIVERS AND STREAMS ! http://www.co.lancaster.pa.us/gisdisclaimer DIKE wc ORDOVICIAN Í472 Oan, ANNVILLE FORMATION LIMESTONE TRIASSIC 372 Oco, COCALICO FORMATION DARK GRAY SHALE TRfl, LIMESTONE FANGLOMERATE Í TRg, GETTYSBURG FORMATION SHALE-SANDSTONE Oe, EPLER FORMATION LIMESTONE TRh, HAMMER CREEK FORMATION SANDSTONE-SHALE Oha, ANNVILLE, HERSHEY, AND MYERSTOWN FORMATION TRhc, HAMMER CREEK QUARTZ-CONGLOMERATE Ohm, HERSHEY AND MYERSTOWN FORMATION LIMESTONE 272 TRn, NEW
    [Show full text]
  • Geospatial Analysis: Commuters Access to Transportation Options
    Advocacy Sustainability Partnerships Fort Washington Office Park Transportation Demand Management Plan Geospatial Analysis: Commuters Access to Transportation Options Prepared by GVF GVF July 2017 Contents Executive Summary and Key Findings ........................................................................................................... 2 Introduction .................................................................................................................................................. 6 Methodology ................................................................................................................................................. 6 Sources ...................................................................................................................................................... 6 ArcMap Geocoding and Data Analysis .................................................................................................. 6 Travel Times Analysis ............................................................................................................................ 7 Data Collection .......................................................................................................................................... 7 1. Employee Commuter Survey Results ................................................................................................ 7 2. Office Park Companies Outreach Results ......................................................................................... 7 3. Office Park
    [Show full text]
  • USNMP-76 2806 1929.Pdf
    NEW LOWER AND MIDDLE CAJ^IBRIAN CRUSTACEA By Charles E, Resser Associate Curator of Stratigraphic Paleontology INTRODUCTION Among the numerous Cambrian fossils that have been accumulating in the United States National Museum during the last 15 years, there are many undescribed species and some of the specimens are remarkable for the preservation of thin tests or of soft body parts. In order to stimulate further search for the rarer fossils, and par- ticularly for preservations of the softer parts of animals or of delicate plant tissues, it is planned to publish more or less related groups of these animals from time to time. Accordingly, in this paper I have assembled a group of species that centers mainly around the pre- viously described genus Tuzoia, but which also includes several unre- lated forms that were secured from the same localities as the others. This paper thus adds several new species preserving more than ordinarily thin tests of Crustacea and a few with the still softer fleshy parts. Some are from the well known Burgess shale that has already furnished so many interesting animals and plants, but other formations, some of which have not previously been known to yield such fossils, are also represented. This paper also contains information of interest aside from that naturally attaching to any description of the softer parts of such ancient animals, by presenting certain important stratigraphic facts in addition to further data regarding the geographic distribution and origin of the faunas to which these species belong. Acknowledgment.—In the preparation of this paper I was kindly assisted by Dr.
    [Show full text]
  • Jjjn'iwi'li Jmliipii Ill ^ANGLER
    JJJn'IWi'li jMlIipii ill ^ANGLER/ Ran a Looks A Bulltrog SEPTEMBER 1936 7 OFFICIAL STATE September, 1936 PUBLICATION ^ANGLER Vol.5 No. 9 C'^IP-^ '" . : - ==«rs> PUBLISHED MONTHLY COMMONWEALTH OF PENNSYLVANIA by the BOARD OF FISH COMMISSIONERS PENNSYLVANIA BOARD OF FISH COMMISSIONERS HI Five cents a copy — 50 cents a year OLIVER M. DEIBLER Commissioner of Fisheries C. R. BULLER 1 1 f Chief Fish Culturist, Bellefonte ALEX P. SWEIGART, Editor 111 South Office Bldg., Harrisburg, Pa. MEMBERS OF BOARD OLIVER M. DEIBLER, Chairman Greensburg iii MILTON L. PEEK Devon NOTE CHARLES A. FRENCH Subscriptions to the PENNSYLVANIA ANGLER Elwood City should be addressed to the Editor. Submit fee either HARRY E. WEBER by check or money order payable to the Common­ Philipsburg wealth of Pennsylvania. Stamps not acceptable. SAMUEL J. TRUSCOTT Individuals sending cash do so at their own risk. Dalton DAN R. SCHNABEL 111 Johnstown EDGAR W. NICHOLSON PENNSYLVANIA ANGLER welcomes contribu­ Philadelphia tions and photos of catches from its readers. Pro­ KENNETH A. REID per credit will be given to contributors. Connellsville All contributors returned if accompanied by first H. R. STACKHOUSE class postage. Secretary to Board =*KT> IMPORTANT—The Editor should be notified immediately of change in subscriber's address Please give both old and new addresses Permission to reprint will be granted provided proper credit notice is given Vol. 5 No. 9 SEPTEMBER, 1936 *ANGLER7 WHAT IS BEING DONE ABOUT STREAM POLLUTION By GROVER C. LADNER Deputy Attorney General and President, Pennsylvania Federation of Sportsmen PORTSMEN need not be told that stream pollution is a long uphill fight.
    [Show full text]
  • Geologic Map of the Piedmont in the Savage and Relay Quadrangles, Howard, Baltimore, and Anne Arundel Counties, Maryland
    U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Geologic Map of the Piedmont in the Savage and Relay Quadrangles, Howard, Baltimore, and Anne Arundel Counties, Maryland By Avery Ala Drake, Jr.1 Open-File Report 98-757 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 'Reston, VA 1998 GEOLOGIC MAP OF THE PIEDMONT IN THE SAVAGE AND RELAY QUADRANGLES, HOWARD, BALTIMORE, AND ANNE ARUNDEL COUNTIES, MARYLAND by Avery Ala Drake, Jr. INTRODUCTION The Piedmont in the Savage and Relay quadrangles (fig. 1) is largely in Howard County, Maryland. The northeasternmost part is in Baltimore County, Maryland and about 0.03 square miles is in Anne Arundel County. Most of the area is suburban and almost all outcrops are restricted to the Patapsco, Middle Patuxent, Little Patuxent, and other stream valleys. Crystalline rocks of the central Appalachian Piedmont within these quadrangles are overlain in many places by Coastal Plain deposits of Cretaceous age. Alluvium occurs along most streams. The geology of adjacent quadrangles on the west and south has been mapped by Drake (in press, unpublished data, 1991-1997) and J.N. Roen and A.A. Drake, Jr. (in press), and that to the north and east by Crowley (1976). The tectonics of the area were interpreted by Crowley (1976) and Drake (1995). Aeromagnetic and gravity surveys of the area were interpreted by Bromery (1968).
    [Show full text]
  • Pre-Cambrian Rocks of the Western Piedmont of Maryland1
    BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA VOL. 33. PP. 335-364 JUNE 30. 1924 PRE-CAMBRIAN ROCKS OF THE WESTERN PIEDMONT OF MARYLAND1 BY ANNA I. JONAS (Presented before the Society December 28, 1923) CONTENTS Page Introduction...................................................................................................................... 355 General geology of the eastern Piedmont of Maryland................................... 356 General geology of the western Piedmont of Maryland................................. 357 Previous work in the western Piedmont of Maryland..................................... 357 Recent work in the western Piedmont of Maryland......................................... 358 General statement.................................................................................................. 358 Cockeysville marble.............................................................................................. 358 Extent................................................................................................................ 358 Lithology................................................................................ •......................... 358 Volcanic rocks......................................................................................................... 358 Extent................................................................................................................ 358 Lithology..........................................................................................................
    [Show full text]
  • Building Stones of the National Mall
    The Geological Society of America Field Guide 40 2015 Building stones of the National Mall Richard A. Livingston Materials Science and Engineering Department, University of Maryland, College Park, Maryland 20742, USA Carol A. Grissom Smithsonian Museum Conservation Institute, 4210 Silver Hill Road, Suitland, Maryland 20746, USA Emily M. Aloiz John Milner Associates Preservation, 3200 Lee Highway, Arlington, Virginia 22207, USA ABSTRACT This guide accompanies a walking tour of sites where masonry was employed on or near the National Mall in Washington, D.C. It begins with an overview of the geological setting of the city and development of the Mall. Each federal monument or building on the tour is briefly described, followed by information about its exterior stonework. The focus is on masonry buildings of the Smithsonian Institution, which date from 1847 with the inception of construction for the Smithsonian Castle and continue up to completion of the National Museum of the American Indian in 2004. The building stones on the tour are representative of the development of the Ameri­ can dimension stone industry with respect to geology, quarrying techniques, and style over more than two centuries. Details are provided for locally quarried stones used for the earliest buildings in the capital, including A quia Creek sandstone (U.S. Capitol and Patent Office Building), Seneca Red sandstone (Smithsonian Castle), Cockeysville Marble (Washington Monument), and Piedmont bedrock (lockkeeper's house). Fol­ lowing improvement in the transportation system, buildings and monuments were constructed with stones from other regions, including Shelburne Marble from Ver­ mont, Salem Limestone from Indiana, Holston Limestone from Tennessee, Kasota stone from Minnesota, and a variety of granites from several states.
    [Show full text]
  • Geologic Cross Section C–C' Through the Appalachian Basin from Erie
    Geologic Cross Section C–C’ Through the Appalachian Basin From Erie County, North-Central Ohio, to the Valley and Ridge Province, Bedford County, South-Central Pennsylvania By Robert T. Ryder, Michael H. Trippi, Christopher S. Swezey, Robert D. Crangle, Jr., Rebecca S. Hope, Elisabeth L. Rowan, and Erika E. Lentz Scientific Investigations Map 3172 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Ryder, R.T., Trippi, M.H., Swezey, C.S. Crangle, R.D., Jr., Hope, R.S., Rowan, E.L., and Lentz, E.E., 2012, Geologic cross section C–C’ through the Appalachian basin from Erie County, north-central Ohio, to the Valley and Ridge province, Bedford County, south-central Pennsylvania: U.S. Geological Survey Scientific Investigations Map 3172, 2 sheets, 70-p.
    [Show full text]
  • Stratigraphic Framework of Cambrian and Ordovician Rocks in The
    Stratigraphic Framework of Cambrian and Ordovician Rocks in the Central Appalachian Basin from Medina County, Ohio, through Southwestern and South-Central Pennsylvania to Hampshire County, West Virginia U.S. GEOLOGICAL SURVEY BULLETIN 1839-K Chapter K Stratigraphic Framework of Cambrian and Ordovician Rocks in the Central Appalachian Basin from Medina County, Ohio, through Southwestern and South-Central Pennsylvania to Hampshire County, West Virginia By ROBERT T. RYDER, ANITA G. HARRIS, and JOHN E. REPETSKI Stratigraphic framework of the Cambrian and Ordovician sequence in part of the central Appalachian basin and the structure of underlying block-faulted basement rocks U.S. GEOLOGICAL SURVEY BULLETIN 1839 EVOLUTION OF SEDIMENTARY BASINS-APPALACHIAN BASIN U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, Jr., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government UNITED STATES GOVERNMENT PRINTING OFFICE: 1992 For sale by Book and Open-File Report Sales U.S. Geological Survey Federal Center, Box 25286 Denver, CO 80225 Library of Congress Cataloging in Publication Data Ryder, Robert T. Stratigraphic framework of Cambrian and Ordovician rocks in the central Appalachian Basin from Medina County, Ohio, through southwestern and south-central Pennsylvania to Hampshire County, West Virginia / by Robert T. Ryder, Anita C. Harris, and John E. Repetski. p. cm. (Evolution of sedimentary basins Appalachian Basin ; ch. K) (U.S. Geological Survey bulletin ; 1839-K) Includes bibliographical references. Supt. of Docs, no.: I 19.3:1839-K 1. Geology, Stratigraphic Cambrian.
    [Show full text]