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RI37 Stratigraphic Nomenclature Of
,--' ( UNIVERSITY OF DELAWARE DELAWARE GEOLOGICAL SURVEY REPORT OF INVESTIGATIONS NO.37 STRATIGRAPHIC NOMENCLATURE OF NONMARINE CRETACEOUS ROCKS OF INNER MARGIN OF COASTAL PLAIN IN DELAWARE AND ADJACENT STATES BY ROBERT R. JORDAN STATE OF DELAWARE.. NEWARK, DELAWARE JUNE 1983 STRATIGRAPHIC NOMENCLATURE OF NONMARINE CRETACEOUS ROCKS OF INNER MARGIN OF COASTAL PLAIN IN DELAWARE AND ADJACENT STATES By Robert R. Jordan Delaware Geological Survey June 1983 TABLE OF CONTENTS Page ABSTRACT. ....... 1 INTRODUCTION ..... 2 Purpose and Scope. 2 Acknowledgments.. 4 REGIONAL SETTING. 4 Regional Relationships . 4 Structural Features. 5 DESCRIPTIONS OF UNITS .. 8 Historical Summary 8 Potomac Formation. 13 Nomenclature. 13 Extent. 13 Lithology . 14 Patuxent Formation . 18 Nomenclature. 18 Extent.. 18 Lithology .... 18 Arundel Formation. 19 Nomenclature.. 19 Extent. .• 19 Lithology • 20 Page Patapsco Formation. .. 20 Nomenclature . 20 Extent .. 20 Lithology.. 20 Raritan Formation . 21 Nomenclature .. 21 Extent .. 22 Lithology.. 23 Magothy Formation .. 24 Nomenclature . 24 Extent .. 24 Lithology.. 25 ENVIRONMENTS OF DEPOSITION 28 AGES .... 29 SUBDIVISIONS AND CORRELATIONS .. 32 REFERENCES . 34 ILLUSTRATIONS Figure 1. Geologic map of nonmarine Cretaceous deposits .. ..•.• •.. 3 2. Structural features of the Coastal Plain. ............ 6 3. Schematic diagram of lateral and vertical relationships of nonmarine Cretaceous deposits•....•... 34 TABLES Page Table 1. Usage of group and formation names. 9 STRATIGRAPHIC NOMENCLATURE OF NONMARINE CRETACEOUS ROCKS OF INNER MARGIN OF COASTAL PLAIN IN DELAWARE AND ADJACENT STATES ABSTRACT Rocks of Cretaceous age deposited in continental and marginal environments, and now found along the inner edge of the northern Atlantic Coastal Plain, have historically been classified as the Potomac Group and the Potomac, Patuxent, Arundel, Patapsco, Raritan, and Magothy forma tions. -
Anne Arundel County
1 Anne I .\RUNDE1 County ilBII pi I • 'lill Mllvlli 'il I I I 1 ;■ ' 11 {[[•^1 I Dept. 6eo«ogy. 8B< Wj,w Johns Hopkins Univewity Baltimore, Maryland MARYLAND GEOLOGICAL SURVEY ANNE ARUNDEL COUNTY MARYLAND GEOLOGICAL SURVEY ANNE ARUNDEL COUNTY BALTIMORE THE JOHNS HOPKINS PRESS 1917 COMMISSION EMEESON C. HARRINGTON, .... Peesident. GOVERNOR OF MARYLAND JOHN M. DENNIS, COMPTROLLER OF MARYLAND FRANK J. GOODNOW, .... Executive Officer. PRESIDENT OF THE JOHNS HOPKINS UNIVERSITY H. J. PATTERSON, Secretary. PRESIDENT OF THE MARYLAND AGRICULTURAL COLLEGE ■ SCIENTIFIC STAFF Wm. Bullock Clark, State Geologist. SUPERINTENDENT OF THE SURVEY. Edward B. Matiiews, . Assistant State Geologist. C. K. Swartz, Geologist. E. W. Berry, Geologist. J. T. Singewald, Jr., Geologist. Also with the cooperation of several members of the scientific bureaus of the National Government. LETTER OF TRANSM1TTAL To His Excellency Emerson C. Harrington, Governor of Maryland and President of the Geological Survey Commission. Sir:—I have the honor to present herewith a report on The Physical Features of Anne Arundel County. This volume is the eighth of a series of reports on the county resources, and is accompanied by large scale topographical, geological, and agricultural soil maps. The information contained in this volume will prove of both economic and educational value to the residents of Anne Arundel County as well as to those who may desire information regarding this section of the State. I am, Very respectfully, Wm. Bullock Clark, State Geologist. Johns Hopkins University, Baltimore. March, 1916. ■ ■ CONTENTS page PREFACE 19 DEVELOPMENT OF KNOWLEDGE CONCERNING THE PHYSICAL FEATURES OF ANNE ARUNDEL COUNTY. By Homer P. Little 23 Introductory 23 HISTORICAL REVIEW 23 General Contributions 23 The Lower Cretaceous 26 The Upper Cretaceous 29 The Eocene 30 The Miocene 31 The Pliocene (?) and Pleistocene 32 Bibliography 34 THE PHYSIOGRAPHY OF ANNE ARUNDEL COUNTY. -
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). -
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.......................................................................................................... -
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. -
Stegosaurian Footprints from the Morrison Formation of Utah and Their Implications for Interpreting Other Ornithischian Tracks Gerard D
Stegosaurian footprints from the Morrison Formation of Utah and their implications for interpreting other ornithischian tracks Gerard D. Gierliński and Karol Sabath Polish Geological Institute, Rakowiecka 4, 00-975 Warsaw, Poland. e-mail: [email protected] ABSTRACT - The supposed stegosaurian track Deltapodus Whyte & Romano, 1994 (Middle Jurassic of England) is sauro- pod-like, elongate and plantigrade, but many blunt-toed, digitigrade, large ornithopod-like footprints (including pedal print cast associated with the manus of Stegopodus Lockley & Hunt, 1998) from the Upper Jurassic of Utah, better fit the stego- saurian foot pattern. The Morrison Formation of Utah yielded other tracks fitting the dryomorph (camptosaur) foot pattern (Dinehichnus Lockley et al., 1998) much better than Stegopodus. If the Stegopodus pedal specimen (we propose to shift the emphasis from the manus to the pes in the revised diagnosis of this ichnotaxon) and similar ichnites are proper stegosaur foot- prints, Deltapodus must have been left by another thyreophoran trackmaker. Other Deltapodus-like (possibly ankylosaurian) tracks include Navahopus Baird,1980 and Apulosauripus Nicosia et al., 1999. Heel-dominated, short-toed forms within the Navahopus-Deltapodus-Apulosauripus plexus differ from the gracile, relatively long-toed Tetrapodosaurus Sternberg, 1932, traditionally regarded as an ankylosaurian track. Thus, the original interpretation of the latter as a ceratopsian track might be correct, supporting early (Aptian) appearance of ceratopsians in North America. Isolated pedal ichnites from the Morrison Formation (with a single tentatively associated manus print, and another one from Poland) and the only known trackways with similar footprints (Upper Jurassic of Asturias, Spain) imply bipedal gait of their trackmakers. Thus, problems with stegosaur tracks possibly stem from the expectation of their quadrupedality. -
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. -
HYDROGEOLOGIC FRAMEWORK of the COASTAL PLAIN of MARYLAND, DELAWARE, and the M
HYDROGEOLOGIC FRAMEWORK OF THE COASTAL PLAIN OF MARYLAND, DELAWARE, AND THE m. DISTRICT OF COLUMBIA U.S. GEOJ,0 HCM. Hydrogeologic Framework of the Coastal Plain of Maryland, Delaware, and the District of Columbia By DON A. VROBLESKY and WILLIAM B. FLECK REGIONAL AQUIFER-SYSTEM ANALYSIS-NORTHERN ATLANTIC COASTAL PLAIN U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1404-E UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1991 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 Library of Congress Cataloging in Publication Data Vroblesky, Don A. Hydrogeologic framework of the coastal plain in Maryland, Delaware, and the District of Columbia. (U.S. Geological Survey professional paper ; 1404-E) Bibliography: p. Supt. of Docs. no. : I 19.16 : 1404E 1. Water, Underground Maryland. 2. Water, Underground Delaware. 3. Water, Underground Washington (D.C.) I. Fleck, William B. II. Title. III. Series: U.S. Geological Survey professional paper ; 1404-E. GB1025.M3V76 1989 551.49'0975 87-600120 For sale by the Books and Open-File Reports Section, U.S. Geological Survey, Federal Center, Box 25425, Denver, CO 80225 FOREWORD THE REGIONAL AQUIFER-SYSTEM ANALYSIS PROGRAM The Regional Aquifer-System Analysis (RASA) Program was started in 1978 following a congressional mandate to develop quantitative appraisals of the major ground-water systems of the United States. The RASA Program represents a systematic effort to study a number of the Nation's most important aquifer systems, which in aggregate underlie much of the country and which represent important components of the Nation's total water supply. -
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. -
A Diverse Mammal-Dominated, Footprint Assemblage from Wetland Deposits in the Lower Cretaceous of Maryland Ray Stanford1, Martin G
A diverse mammal-dominated, footprint assemblage from wetland deposits in the Lower Cretaceous of Maryland Ray Stanford1, Martin G. Lockley2, Compton Tucker3, Stephen Godfrey4 & Sheila M. Stanford1 A newly discovered assemblage of predominantly small tracks from the Cretaceous Patuxent Formation at NASA’s Goddard Space Flight Center, Maryland, reveals one of the highest track densities and diversities ever reported (~70 tracks, representing at least eight morphotypes from an area of only ~2 m2). The assemblage is dominated by small mammal tracks including the new ichnotxon Sederipes goddardensis, indicating sitting postures. Small crow-sized theropod trackways, the first from this unit, indicate social trackmakers and suggest slow-paced foraging behavior. Tracks of pterosaurs, and other small vertebrates suggest activity on an organic-rich substrate. Large well-preserved sauropod and nodosaurs tracks indicate the presence of large dinosaurs. The Patuxent Formation together with the recently reported Angolan assemblage comprise the world’s two largest Mesozoic mammal footprint assemblages. The high density of footprint registration at the NASA site indicates special preservational and taphonomic conditions. These include early, penecontemporaneous deposition of siderite in organic rich, reducing wetland settings where even the flesh of body fossils can be mummified. Thus, the track-rich ironstone substrates of the Patuxent Formation, appear to preserve a unique vertebrate ichnofacies, with associated, exceptionally-preserved body fossil remains for which there are currently no other similar examples preserved in the fossil record. Reports of true Mammalia tracks, from the Mesozoic, as distinct from tracks of presumed synapsids (therapsids) from early Mesozoic (mostly Triassic and Jurassic) dune facies, are rare, and mostly involve very small samples of isolated tracks. -
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 -
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.