GEOHYDROLOGY of the HOCKESSIN AREA with EMPHASIS on the COCKEYSVILLE AQUIFER By

Total Page:16

File Type:pdf, Size:1020Kb

GEOHYDROLOGY of the HOCKESSIN AREA with EMPHASIS on the COCKEYSVILLE AQUIFER By State of Delaware DELAWARE GEOLOGICAL SURVEY Robert R. Jordan, State Geologist BULLETIN NO. 19 John H. Talley, Editor GEOLOGY AND HYDROLOGY OF THE COCKEYSVILLE FORMATION NORTHERN NEW CASTLE COUNTY, DELAWARE GEOLOGY OF THE COCKEYSVILLE FORMATION by Kenneth D. Woodruff and Margaret 0. Plank GEOHYDROLOGY OF THE HOCKESSIN AREA WITH EMPHASIS ON THE COCKEYSVILLE AQUIFER by William H. Werkheiser University of Delaware Newark, Delaware 1995 State of Delaware DELAWARE GEOLOGICAL SURVEY Robert R. Jordan, State Geologist BULLETIN NO. 19 John H. Talley, Editor GEOLOGY AND HYDROLOGY OF THE COCKEYSVILLE FORMATION NORTHERN NEW CASTLE COUNTY, DELAWARE GEOLOGY OF THE COCKEYSVILLE FORMATION by Kenneth D. Woodruff and Margaret 0. Plank GEOHYDROLOGY OF THE HOCKESSIN AREA WITH EMPHASIS ON THE COCKEYSVILLE AQUIFER by William H. Werkheiser University of Delaware Newark, Delaware 1995 CONTENTS Page Page ABSTRACT . ..... ..... ........... .................. I Gravity and Magnetics .... ........................... 22 Structural Relations in the Mill Creek Dome .. ..... .... 22 INTRODUCTION by John H. Talley........ .......................... .. .. 2 SUMMARY AND CONCLUSIONS ...... ..... ......... ... 23 Purpose and Scope . 2 GEOHYDROLOGY OF THE HOCKESSIN AREA Locations of Study Areas . 2 WITH EMPHASIS ON THE COCKEYSYILLE AQUIFER Acknowledgments . 4 by William H. Werkheiser ........ ..................... 26 GEOLOGY OF THE COCKEYSYILLE FORMATION INTRODUCTION ..... .................. ... ... .. ... 26 by Kenneth D. Woodruff and Margaret 0. Plank . 4 GEOHYDROLOGY ....................................... 28 INTRODUCTION . 4 Geohydrologic Framework and Regional Setting . 4 Ground-Water Occurrence ................ ... .... 28 Previous Work . 6 Cockeysville Aquifer ................ ............ .... 32 Methods of In vesti gation . 6 Boundaries ............................................ 32 Field Mapping . 6 Recharge ..... ... ... ................... .. .. ....... 32 Test Drilling . 6 Discharge ... ..... ...... .......... ................. 35 Geophysical Logging . 6 Flow Directions and Water Levels .................... 35 Gravity Survey . 6 Water Quality . .. ... .. .... ....................... .... 39 Petrographic Analysis . 7 Occurrence of Chemical Constituents .... .... ....... 40 ROCK UNITS OF THE STUDY AREA . 8 Evidence for Ground-Water Flow Between Aquifers .. 42 Geologic Units Adjoining Cockeysville Formation . 8 Water Budgets ................ ......... .. ............. 43 Baltimore Gneiss . 8 Mill Creek Basin . .. ... ........ ......... .. ............ 43 Setters Formation . 9 Ground-Water Budget for the Stressed Part Wissahickon Formation . 9 of the Cockeysville Aquifer ......................... 46 Cockeysville Formation . 11 Effect of Reduced Recharge on the Ground-Water Field Description .................. ... ............... 11 Budget for the Cockeysville Aquifer ................ 47 Mapping ...... .. .................................... 11 SUMMARY AND CONCLUSIONS .. .. ................... 47 Lithology . 12 Petrography . 14 REFERENCES CITED . ..... .............. .... ... ...... 48 Fractures and Solution Cavities . ...... .... ........... 14 APPENDICES ... .... .... .... .... .. .. ...................... 5 1 Weathered Zone ...... ...... .. ..... ....... ... 15 I. Conversion factors, vertical datum. STRUCTURAL GEOLOGY ............. .... ........... 16 and abbreviated water-quality uni ts .. ........... ... 51 Hockessin-Yorklyn Area . 16 2. Map coordinates for rock samples Borehole Data . 17 used for modal analyses ...... ... .. ... ... .. ...... 51 Field Observations . 18 3. Records of wells in the Gravity and Magnetics .... .......... ................. 18 Hockessin and Pleasant Hill areas ............ ..... 5 1 Pleasant Hill Area ..... ... .. .. .. ... ... ............ 18 4. Chemical analyses of ground and Borehole Data . 18 surface water in the Hockessin area ..... ..... ..... 56 ILLUSTRATIONS Plate I. Geologic map of the Pleasant Hill-Hockessin area ... ... .................... ............... .. ... ... .. ............... Pocket Page Figure I . Map showing locations of study areas . 3 2. Map showing location of study area for the geohydrology portion of the study . 5 3. Map showing location of wells and test holes drilled in support of this investigation . 7 4. Diagram showing Wi ssahickon-Cockeysville contact south of Hockessin . 11 5. Gamma-ray logs from well s in the Cockeysville Formation .. .. ................ ........................................... 12 6. Selected geophysical logs and lithology from test hole Bb35- I 6 . .. .. .. 13 7. Acoustic televiewer log of a portion of well Bb33-26 .. ............................................ ............. ......... 15 8. Acoustic televiewer log of a portion of well Bb34-35 . .......................... ............ ...... ... ............ .. 15 9. Acoustic televiewer log of a portion of well Bb44-22 ................. .. ............. ........ .. ... ...... ... ........ 16 10. Temperature logs in well Bb33-28 . ............ .. ................. ..................... ... ... ................. .. .. .. 16 11. Thickness of weathered zone in the Cockeysville Formation ................. .. ................... ......................... 17 12. Basic scheme for structural relations in the Delaware-Pennsylvani a Piedmont ..... ....................... ............... 18 13. Map showing locations of cross-sections . 19 14. Schematic cross-sections A-A'. B-B'. C-C', and D-D' in the Hockessin and Pleasant Hill areas ... .................... ..... 20 15. Descriptive and gamma-ray logs. composite for test holes Bb44-22 and Bb44-30 . ............... ......... ..... ...... .... 21 16. Bouguer gravity map of the Hockessin area .... .. ....... ... ................................ .......... .................. 22 17. Gravity model across the Hockessin-Yorklyn area .... ... ... ......... ...... ............... .......... ...... .... ..... .... 23 18. Aeromagnetic map of the study area ..................... ..................................... ... ........ ................. 24 19. Generalized geologic map of the Mill Creek dome .... .... ....... .. ....................... ...... .. ... ..... ...... 25 20. Graph showing precipitation at Wilmington, Delaware, 1961-90 ...... ......... .............. ... ......................... 26 21. Map showing well locations in the Hockessin area ............................. ... ...... .. .............. .... ...... 27 22. Graph showing ground-water withdrawals in the Hockessin area, 1975-90 . ... .. ......... ... ... .. .... .................. 28 23. Map showing data-collection sites in the Hockessin area ................. .... ..... ....... .. ................. ...... ..... 29 24. Graphs showing caliper logs for wells in the Cockeysville aquifer ..... ...... ..................... ... ... ... ..... ..... 30 25. Generalized hydrogeologic section of the Hockessin area .............. ... .. ............. ..... ............ ........... 3 1 26-30. Maps showing: 26. Stream discharge on June 27, 1990, and October 3, 1990 . ...... ... ... ............................. ....... .............. 33 27. Stream discharge on April 4, 1991 ........ .... .... ..... .. ....... ... ............................. ... .................. 34 28. Water-level altitudes in aquifers underlying White Briar ..... .......................................... .. ... ... ........ 36 29. Water-level altitudes in aquifers in the Hockessin area, November 14-16, 1990 ............................ .. .. ... ........ 37 30. Water-level altitudes in the Cockeysville aquifer, 1955 ....................................... .. ......................... 38 31-36. Graphs showing: 3 1. Water levels in observation wells .... ................. .............. .... ............... ... ..................... ... 39 (A) in the unstressed part of the Cockeysville aquifer . ... ..... ... ...... .......................... .......................... 39 (B) in the stressed part of the Cockeysville aquifer ....................................... .. ... ......................... 39 32. WaterlevelsinobservationwellBb43- 13, 1977-90 ...... .. ... .. ....... .................................... ................ 39 33. Water levels in observation well Bb34-40, 1979-90 ............................ ........................................ .. 39 34. Water levels in observation wells near pumped wells ... .................................. .............. .................. 40 35. Tri linear diagram for ground water from the Hockessin area ................................................................ 41 36. Box plots showing alkalinity, hardness. dissolved solids, and strontium concentrations in water from aquifers in the Hockessin area ................ ... ........... .. ............................................... 42 37-40. Graphs showing: 37. Relation of sum of cation concentrations to chloride concentrations ............ .................... .. .............. 42 38. Relation of sum of cation concentrations to strontium concentrati ons ...... ... ................................... .. ..... 43 39. Discharge of Mill C reek at Mill Creek Road at Hockessin, 1990 ................................................ ... .... .... 44 40. Annual recharge lO the Cockeysvi lie aquifer, 1978-90 ................................................................. .... 4 7 TABLES Page Table 1. Rocks of the Delaware Piedmont .. ............................................. ....... ............................... ...... 8 2. Modal analyses of the Baltimore Gneiss
Recommended publications
  • 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]
  • 2713^7 Contents
    MINERALS OF WASHINGTON, D.C. AND VICINITY by Lawrence R. Bernstein U. S. Geo^r^'ce.l Survey OPEN F-'::. r;.".r'0.?;r cer.-..: 2713^7 CONTENTS Introduction 1 Scope of report 4 Mineral collecting 5 Acknowledgments 6 Introduction 6a ITT3 Aclj.il1 -> ! T^______.___~^. -"» _«_____«..«_»«__.. " " .._.«__._.._*_.__._.,_.._.-. _>-.-- -_>-->.-..-. Q Triassic deposits 31 Mineral localities 38 District of Columbia : 38 IMavtrlWlCfci JT XClilUl a Tirl ~ __ ___« - - -_ -»-i-___ .__- _ __- - ________________ m~m~m~ m~ m~ «M » M* **A^J ^ Anne Arundel County 43 Baltimore County 45 Howard County - 74 Montgomery County 88 Prince Georges County 120 Virginia . 129 Arlington County 129 Fairfax County 131 Fauquier County 139 Loudoun County 143 Prince William County 149 Diabase quarries of northern Virginia 155 CAPTIONS Illustrations Plate 1. Mineral localities of Washington, B.C., and vicinity. Plate 2. Generalized geologic map of Washington. D.C. and vicinity, Plate 3. Mineral deposits and generalized geology of the Triassic rocks near Washington, D.C. List of Figures Figure 1. Index map showing region covered in this report. Stfaded area is covered in most detail. Figure 2. Block diagram of the Washington, D.C. region showing physiographic provinces and major geographic and geologic features. ITfgure -3. Coastal Plain deposits of Washington, D.C. and vicinity. Figure 4. Generalized cross section of a typical complex pegmatite of the Washington, D.C. area. Figure 5. Rhythmically.layered gabbro of the Baltimore Gabbro Com­ plex at Ilchester, Maryland. Figure 6. Triassic diabase dike forming a ridge north of Route 7 near Dranesville, Virginia.
    [Show full text]
  • Geology, Geochemistry, and Age of Archean and Early Proterozoic
    Geology, Geochemistry, and Age of Archean and Early Proterozoic Rocks in the Marenisco-Watersmeet Area, Northern Michigan and Geologic Interpretation of Gravity Data, Marenisco-Watersmeet Area, Northern Michigan GEOLOGICAL SURVEY PROFESSIONAL PAPER 1292-A, B Geology, Geochemistry, and Age of Archean and Early Proterozoic Rocks in the Marenisco-Watersmeet Area, Northern Michigan By P. K. SIMS, Z. E. PETERMAN, W. C. PRINZ, and F. C. BENEDICT and Geologic Interpretation of Gravity Data, Marenisco-Watersmeet Area, Northern Michigan By J. S. KLASNER and P. K. SIMS CONTRIBUTIONS TO THE GEOLOGY OF THE LAKE SUPERIOR REGION GEOLOGICAL SURVEY PROFESSIONAL PAPER 1292-A,B UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1984 UNITED STATES DEPARTMENT OF THE INTERIOR WILLIAM P. CLARK, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Main entry under title: Geology, geochemistry, and age of Archean and early Proterozoic rocks in the Marenisco-Watersmeet area, Northern Michigan. (Contributions to the geology of the Lake Superior Region) (Geological Survey Professional Paper ; 1292A-B) Bibliography: P1292-A, 41 p.; P1292-B, 13 p. Supt. of Docs. No.: 119.16:1292-A & B 1. Geology, Stratigraphic Pre-Cambrian. 2. Geology Michigan Gogebic County. 3. Gravity Michi­ gan Gogebic County. I. Sims, P. K. (Paul Kibler), 1918- II. Klasner, J. S. Geologic interpretation of gravity data, Marenisco- Watersmeet area. 1983. III. Series. IV. Series: Geological Survey professional paper ; 1292A-B. QE653.G477 1983 551.7T09774983 83-600384 For sale by the Branch of Distribution U.S. Geological Survey 604 South Pickett Street Alexandria, VA 22304 Geology, Geochemistry, and Age of Archean and Early Proterozoic Rocks in the Marenisco-Watersmeet Area, Northern Michigan By P.
    [Show full text]
  • Northeastern Jones Falls Small Watershed Action Plan Volume 2: Appendices D & E
    Northeastern Jones Falls Small Watershed Action Plan Volume 2: Appendices D & E January 2013 December 2012 Final Prepared by: Baltimore County Department of Environmental Protection and Sustainability In Consultation with: Northeastern Jones Falls SWAP Steering Committee NORTHEASTERN JONES FALLS SMALL WATERSHED ACTION PLAN VOLUME II: APPENDICES D & E Appendix D Northeastern Jones Falls Characterization Report Appendix E Applicable Total Maximum Daily Loads APPENDIX D NORTHEASTERN JONES FALLS CHARACTERIZATION REPORT A-1 Northeastern Jones Falls Characterization Report Final December 2012 NORTHEASTERN JONES FALLS CHARACTERIZATION REPORT TABLE OF CONTENTS CHAPTER 1 INTRODUCTION 1.1 Purpose of the Characterization 1-1 1.2 Location and Scale of Analysis 1-1 1.3 Report Organization 1-5 CHAPTER 2 LANDSCAPE AND LAND USE 2.1 Introduction 2-1 2.2 The Natural Landscape 2-2 2.2.1 Climate 2-2 2.2.2 Physiographic Province and Topography 2-2 2.2.2.1 Location and Watershed Delineation 2-2 2.2.2.2 Topography 2-3 2.2.3 Geology 2-4 2.2.4 Soils 2-7 2.2.4.1 Hydrologic Soil Groups 2-7 2.2.4.2 Soil Erodibility 2-9 2.2.5 Forest 2-11 2.2.5.1 Forest Cover 2-11 2.2.6 Stream Systems 2-11 2.2.6.1 Stream System Characteristics 2-12 2.2.6.2 Stream Riparian Buffers 2-14 2.3 Human Modified Landscape 2-16 2.3.1 Land Use and Land Cover 2-16 2.3.2 Population 2-19 2.3.3 Impervious Surfaces 2-21 2.3.4 Drinking Water 2-24 2.3.4.1 Public Water Supply 2-24 2.3.5 Waste Water 2-24 2.3.5.1 Septic Systems 2-24 2.3.5.2 Public Sewer 2-24 2.3.5.3 Waste Water Treatment Facilities 2-26
    [Show full text]
  • Bulletin 19 of the Department of Geology, Mines and Water Resources
    COMMISSION OF MARYLAND GEOLOGICAL SURVEY S. JAMES CAMPBELL Towson RICHARD W. COOPER Salisbury JOHN C. GEYER Baltimore ROBERT C. HARVEY Frostburg M. GORDON WOLMAN Baltimore PREFACE In 1906 the Maryland Geological Survey published a report on "The Physical Features of Maryland", which was mainly an account of the geology and min- eral resources of the State. It included a brief outline of the geography, a more extended description of the physiography, and chapters on the soils, climate, hydrography, terrestrial magnetism and forestry. In 1918 the Survey published a report on "The Geography of Maryland", which covered the same fields as the earlier report, but gave only a brief outline of the geology and added chap- ters on the economic geography of the State. Both of these reports are now out of print. Because of the close relationship of geography and geology and the overlap in subject matter, the two reports were revised and combined into a single volume and published in 1957 as Bulletin 19 of the Department of Geology, Mines and Water Resources. The Bulletin has been subsequently reprinted in 1961 and 1966. Some revisions in statistical data were made in the 1961 and 1968 reprints. Certain sections of the Bulletin were extensively revised by Dr. Jona- than Edwards in this 1974 reprint. The Introduction, Mineral Resources, Soils and Agriculture, Seafood Industries, Commerce and Transportation and Manu- facturing chapters of the book have received the most revision and updating. The chapter on Geology and Physiography was not revised. This report has been used extensively in the schools of the State, and the combination of Geology and Geography in one volume allows greater latitude in adapting it to use as a reference or textbook at various school levels.
    [Show full text]
  • Geologic Formations DISCLAIMER: Howard County, Maryland Assumes No Responsibility for the Accuracy of This Map Or the Information Contained Herein Derived There From
    MarriottsvilleMarriottsvilleMarriottsville Rd RdRd MarriottsvilleMarriottsvilleMarriottsville Rd RdRd OOl OOllllddd FFFrrreeededederri derrriiiiccckkk RRddd RogersRogersRogers Ave AveAve RogersRogersRogers Ave AveAve OOlllldldd FFrrreeedddeeerrriiiicicckkk RRddd ick RRdd OOlllldldd FFrrreeedddeeerrriiiiccckkk RRdd n n n n n n n n n L L L L L L L L L n n n n n y n y n y n y n y y y y y L L L L L L n n L n L L n n n n n n a a s a s a s a s a s a s a s a s s h h n h n h n h n h n h n h n h n n t t t F t Fre t Fred t Freder t M Frederick t Ma FFrredeerriiick Rd t MMaiin S Frederick Rd h Main St Fred rick Rd h Main St rederick Rd h Main St derick Rd h Main St rick Rd h Main St ck Rd h ain St Rd h in St d h St h t e e e e e e e e e o o o o o o o o o B B B B J B J B J B J B J B J J J J t t t t t t t t t n n k Rd n rick Rd n rederick Rd n Frederic k Rd n Frede rick Rd n F de i d n re r ck R i F de i d n Freder c k Rd i Fre derick Rd i Frederiick R i Freder c i Fre i i Fr de i FFrrreeedddeeerrriiiicicckkk RRddd i a a a a a a a a deerrriiiccckkk RRddd a ed er ic S rederic S rederi S Fr ed er S Frede S Frede S Fr ed S Fre S FFrre S ddd RRR rrrr eeer nnneee nnnn rrrrnnn eennn ddd ooor PPee RR ooo ddd ddd PP pp R CCC oopp C RRR RRR hhoo ggg R SShh nngg aaa e SS nnn iiiiiaiaa eee ooo hhh ggg LLoo hhh ggg LLL lplpp ddd ddd llllpl d iiiiiiidiid eee RRR eee RRR RRR ddd rrr RRR aaad rrr iiiaiiaa tetee rrrrri rrtttt TTT rrrr TTT aaa uua u n u n u n u n u n u n u n n n L Q L Q L Q L Q L Q L Q L Q L Q L Q l l l l l l l y l y l llllylylyy lll a ll a l a l
    [Show full text]
  • Origin of Tourmaline in the Setters Formation, Maryland: Evidence from Major and Trace Element, Boron Isotope, and Rare Earth Element Characteristics
    Origin of Tourmaline in the Setters Formation, Maryland: Evidence from Major and Trace Element, Boron Isotope, and Rare Earth Element Characteristics Joseph Browning Advisors: Dr. Philip Piccoli & Dr. Richard Ash April 26, 2017 GEOL 394 ABSTRACT The occurrence of tourmaline within the Setters Formation of the Glenarm Series in the Maryland Piedmont is poorly understood. Very little research has been conducted to elucidate the origins of the tourmaline. The focus of this study has been to provide geochemical and petrologic evidence to gain a more thorough understanding of the conditions under which the tourmaline of the Setters Formation developed. Tourmaline can form in a wide variety of geologic settings. Natural tourmaline has a δ 11B range from -30‰ to +40‰, and individual samples fall within sub-ranges that may be indicative of the boron source reservoir. Studies of tourmaline are growing in popularity as petrological tools due to several unique chemical and physical characteristics that have implications for its use as a single-crystal indicator of numerous geologic processes and conditions. Major element chemistry of tourmaline collected as part of this study from the Setters formation along the margin of the Woodstock Dome is consistent with the dravite-schorl solid-solution series. This solid-solution is expected of tourmaline developed during prograde metamorphism within a metapelitic host rock. Single collector LA-ICP-MS analysis was performed in situ to acquire boron isotopic measurements for tourmaline concentrates. Tourmaline from the Setters Formation is isotopically heavy with a δ 11B range of -21.13 to +9.58‰ (with an accuracy of <±10.72‰).
    [Show full text]
  • Bedrock Geology of the West Grove Quadrangle, Pennsylvania-Delaware Piedmont
    Geological Society of America Digital Map and Chart Series DMCH002 2005 Bedrock geology of the West Grove Quadrangle, Pennsylvania-Delaware piedmont J. Alcock Department of Environmental Sciences, Pennsylvania State University, Abington, Pennsylvania 19001, USA ABSTRACT Three lithotectonic units are exposed across the West Grove Quadrangle in the Pennsylvania-Delaware piedmont. These are mid-Proterozoic gneisses that core the Landenberg, Avondale, and Woodville Massifs, latest Proterozoic to Early Paleozoic metasediments of the Glenarm Series (Setters Formation and Cockeysville Marble) that form the margins of the massifs, and the allocthonous latest Proterozoic to early Paleozoic metasediments of the Wissahickon Formation. Metamorphic and structural discontinuities can be used to establish that each unit has experienced a distinct meta- morphic and tectonic history. Keywords: Pennsylvania-Delaware piedmont, Glenarm Series, Wissahickon Forma- tion, metamorphic discontinuity, structural discontinuity. INTRODUCTION tify key locations and relationships among the different map units and supports the interpretation that the Wissahickon Formation Multiple deformational and metamorphic events affecting in this area is allocthonous, having been thrust across the lower the Pennsylvania-Delaware piedmont during early Paleozoic units during Paleozoic plate collision. plate collision produced a complex regional structure that con- Mapping by the author was initiated in an effort to bet- tinues to cause debate amongst geologists working in the area. ter defi ne metamorphic and structural relationships among the A key issue of contention is the relationship of metapelites and various lithotectonic units exposed in the Pennsylvania-Delaware metapsammites of the Wissahickon Formation to the Cock- Piedmont as part of a doctoral thesis (Alcock, 1989) with addi- eysville Marble and Setters Formation, which were originally tional work continuing until 1996.
    [Show full text]
  • Maryland Geological Survey Volume One Baltimore The
    MARYLAND GEOLOGICAL SURVEY VOLUME ONE BALTIMORE THE JOHNS HOPKINS PRESS 1897 ILLUSTRATIONS. PLATE FACING PAGE I. View of Model of the State of Maryland 23 II. The Potomae River Valley at Williamsport, on the Western Maryland Railroad 64 III. View of the Great Valley from Blue Mountain, on the Western Mary- land Railroad ; 104 IV. Map showing Atlas Sheets and Charts in Maryland 114 V. Map showing leading Triangnlation in Maryland 123 VI. Hypsometric Map of Maryland 142 VII. View showing Estuary of the Chesapeake Bay near Queenstown 146 VIII. The Falls of the Potomac 148 IX. View of the Youghiogheny Valley In the Alleghany Mountains, on the Baltimore and Ohio Railroad 152 X. The Gorge of the Potomac, at Harper's Ferry looking east, on the Bal- timore and Ohio Railroad 176 XI. Folded Strata of Lewistown Formation at Hancock, on the Baltimore and Ohio Railroad 182 XII. View of "Devil's Backbone" in Lewistown Formation north of Cum- berland, on the Baltimore and Ohio Railroad 186 XIII. Geological Map of Maryland 204 XIV. Isogonic Map of Maryland 404 XV. Instruments used in Magnetic Observations 450 XVI. Map showing the Preliminary Lines of Equal Magnetic Inclination and the Preliminary Lines of Equal Horizontal Force for Mary- land on January 1, 1897 4j93 XVII. Map showing the Lines of Equal Magnetic Declination for Maryland in the years 1700 and 1800 494 MARYLAND GEOLOGICAL SURVEY VOLUME TWO BALTIMORE THE JOHNS HOPKINS PRESS 1898 ILLUSTRATIONS PLATE facing page I, The Potomac River near Cherry Run, at the Junction of the Balti- more and Ohio and Western Maryland Railroads 37 II.
    [Show full text]
  • RI59 Bedrock Geology of the Piedmont of Delaware And
    State of Delaware DELAWARE GEOLOGICAL SURVEY Robert R. Jordan, State Geologist REPORT OF INVESTIGATIONS NO. 59 BEDROCK GEOLOGY OF THE PIEDMONT OF DELAWARE AND ADJACENT PENNSYLVANIA by Margaret O. Plank1, William S. Schenck1, LeeAnn Srogi2 University of Delaware Newark, Delaware 2000 1Delaware Geological Survey 2West Chester University State of Delaware DELAWARE GEOLOGICAL SURVEY Robert R. Jordan, State Geologist REPORT OF INVESTIGATIONS NO. 59 BEDROCK GEOLOGY OF THE PIEDMONT OF DELAWARE AND ADJACENT PENNSYLVANIA by Margaret O. Plank1 William S. Schenck1 LeeAnn Srogi2 University of Delaware Newark, Delaware 2000 1Delaware Geological Survey 2West Chester University CONTENTS Page Page ABSTRACT . 1 Montchanin Metagabbro. 15 Mill Creek Metagabbro . 16 INTRODUCTION. 1 Rockford Park Gneiss . 16 Purpose and Scope. 1 Brandywine Blue Gneiss. 17 Regional Geologic Setting . 2 Arden Plutonic Supersuite . 18 Acknowledgments. 2 Ardentown Granitic Suite. 19 GEOLOGIC UNITS. 2 Perkins Run Gabbronorite Suite. 20 Baltimore Gneiss . 2 Biotite Tonalite. 21 Setters Formation. 4 Bringhurst Gabbro. 21 Cockeysville Marble. 6 Iron Hill Gabbro. 22 Wissahickon Formation. 7 Diabase Dike . 23 Ultramafic Lens . 10 GEOCHEMISTRY OF THE MAFIC ROCKS . 23 Wilmington Complex. 10 Windy Hills Gneiss . 11 DISCUSSION . 23 Faulkland Gneiss . 12 CONCLUSIONS . 25 Christianstead Gneiss. 13 Barley Mill Gneiss. 14 REFERENCES CITED . 26 APPENDIX Page TYPE AND REFERENCE SECTION LOCATION MAPS AND LITHOLOGIES . 31 Baltimore Gneiss in Delaware . 32 Setters Formation in Pennsylvania. 33 Setters Formation in Delaware. 34 Cockeysville Marble in Delaware. 35 Wissahickon Formation at Brandywine Springs Park, Delaware. 36 Wissahickon Formation at Mt. Cuba, Delaware . 37 Ultramafic Lens . 38 Windy Hills Gneiss. 39 Faulkland Gneiss. 40 Christianstead Gneiss . 41 Barley Mill Gneiss .
    [Show full text]