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View of Valley and Ridge Structures from ?:R Stop IX
GIJIDEBOOJ< TECTONICS AND. CAMBRIAN·ORDO'IICIAN STRATIGRAPHY CENTRAL APPALACHIANS OF PENNSYLVANIA. Pifftbutgh Geological Society with the Appalachian Geological Society Septembet, 1963 TECTONICS AND CAMBRIAN -ORDOVICIAN STRATIGRAPHY in the CENTRAL APPALACHIANS OF PENNSYLVANIA FIELD CONFERENCE SPONSORS Pittsburgh Geological Society Appalachian Geological Society September 19, 20, 21, 1963 CONTENTS Page Introduction 1 Acknowledgments 2 Cambro-Ordovician Stratigraphy of Central and South-Central 3 Pennsylvania by W. R. Wagner Fold Patterns and Continuous Deformation Mechanisms of the 13 Central Pennsylvania Folded Appalachians by R. P. Nickelsen Road Log 1st day: Bedford to State College 31 2nd day: State College to Hagerstown 65 3rd day: Hagerstown to Bedford 11.5 ILLUSTRATIONS Page Wagner paper: Figure 1. Stratigraphic cross-section of Upper-Cambrian 4 in central and south-central Pennsylvania Figure 2. Stratigraphic section of St.Paul-Beekmantown 6 rocks in central Pennsylvania and nearby Maryland Nickelsen paper: Figure 1. Geologic map of Pennsylvania 15 Figure 2. Structural lithic units and Size-Orders of folds 18 in central Pennsylvania Figure 3. Camera lucida sketches of cleavage and folds 23 Figure 4. Schematic drawing of rotational movements in 27 flexure folds Road Log: Figure 1. Route of Field Trip 30 Figure 2. Stratigraphic column for route of Field Trip 34 Figure 3. Cross-section of Martin, Miller and Rankey wells- 41 Stops I and II Figure 4. Map and cross-sections in sinking Valley area- 55 Stop III Figure 5. Panorama view of Valley and Ridge structures from ?:r Stop IX Figure 6. Camera lucida sketch of sedimentary features in ?6 contorted shale - Stop X Figure 7- Cleavage and bedding relationship at Stop XI ?9 Figure 8. -
Figure 3A. Major Geologic Formations in West Virginia. Allegheney And
82° 81° 80° 79° 78° EXPLANATION West Virginia county boundaries A West Virginia Geology by map unit Quaternary Modern Reservoirs Qal Alluvium Permian or Pennsylvanian Period LTP d Dunkard Group LTP c Conemaugh Group LTP m Monongahela Group 0 25 50 MILES LTP a Allegheny Formation PENNSYLVANIA LTP pv Pottsville Group 0 25 50 KILOMETERS LTP k Kanawha Formation 40° LTP nr New River Formation LTP p Pocahontas Formation Mississippian Period Mmc Mauch Chunk Group Mbp Bluestone and Princeton Formations Ce Obrr Omc Mh Hinton Formation Obps Dmn Bluefield Formation Dbh Otbr Mbf MARYLAND LTP pv Osp Mg Greenbrier Group Smc Axis of Obs Mmp Maccrady and Pocono, undivided Burning Springs LTP a Mmc St Ce Mmcc Maccrady Formation anticline LTP d Om Dh Cwy Mp Pocono Group Qal Dhs Ch Devonian Period Mp Dohl LTP c Dmu Middle and Upper Devonian, undivided Obps Cw Dhs Hampshire Formation LTP m Dmn OHIO Ct Dch Chemung Group Omc Obs Dch Dbh Dbh Brailler and Harrell, undivided Stw Cwy LTP pv Ca Db Brallier Formation Obrr Cc 39° CPCc Dh Harrell Shale St Dmb Millboro Shale Mmc Dhs Dmt Mahantango Formation Do LTP d Ojo Dm Marcellus Formation Dmn Onondaga Group Om Lower Devonian, undivided LTP k Dhl Dohl Do Oriskany Sandstone Dmt Ot Dhl Helderberg Group LTP m VIRGINIA Qal Obr Silurian Period Dch Smc Om Stw Tonoloway, Wills Creek, and Williamsport Formations LTP c Dmb Sct Lower Silurian, undivided LTP a Smc McKenzie Formation and Clinton Group Dhl Stw Ojo Mbf Db St Tuscarora Sandstone Ordovician Period Ojo Juniata and Oswego Formations Dohl Mg Om Martinsburg Formation LTP nr Otbr Ordovician--Trenton and Black River, undivided 38° Mmcc Ot Trenton Group LTP k WEST VIRGINIA Obr Black River Group Omc Ordovician, middle calcareous units Mp Db Osp St. -
U.S. Geological Survey Bulletin 1839-G, H
Stratigraphic Framework of Cambrian and Ordovician Rocks in the Central Appalachian Basin from Morrow County, Ohio, to Pendleton County, West Virginia Depositional Environment of the Fincastle Conglomerate near Roanoke, Virginia U.S. GEOLOGICAL SURVEY BULLETIN 1839-G, H i i i I ' i ' i ' X- »-v l^,:^ Stratigraphic Framework of Cambrian and Ordovician Rocks in the Central Appalachian Basin from Morrow County, Ohio, to Pendleton County, West Virginia By ROBERT T. RYDER Depositional Environment of the Fincastle Conglomerate near Roanoke, Virginia By CHRYSA M. CULLATHER Chapters G and H are issued as a single volume and are not available separately U.S. GEOLOGICAL SURVEY BULLETIN 1839-G, H 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 25425 Denver, CO 80225 Library of Congress Cataloging in Publication Data (revised for vol. G-H) Evoluation of sedimentary basins Appalachian basin. (U.S. Geological Survey bulletin ; 1839 A-D, G-H) Includes bibliographies. Supt. of Docs. no.:19.3:1839-G Contents: Horses in fensters of the Pulaski thrust sheet, southwestern Virginia / by Arthur P. Schultz [etc.] Stratigraphic framework of Cam brian and Ordovician rocks in central Appalachian basin from Morrow County, Ohio, to Pendleton County, West Virginia / by Robert T. -
Ordovician, in CH Shultz Ed, the Geology of Pennsylvania
SCALE :ii! o 10 20 30 40 50 MI I 'i I' "i' , o 20 40 60 80 KM 41 40 ' EXPLANATION ~ l1li Ordovician rocks in subsurface Autochthonous OrdOllician rocks at surface Hamburg klippe Figure 5-1. Distribution of Ordovician sedimentary rocks In Pennsylvania west of the Martie Line (modified from Berg and others, 1980, and Pennsylvania Geological Survey, 1990). Part II. Stratigraphy and Sedimentary Tectonics CHAPTERS ORDOVICIAN ALLAN M. THOMPSON INTRODUCTION Department of Geology University of Delaware This chapter contains a summary of lithologic, Newark, DE 19716 facies, and temporal relationships of sedimentary rocks of Ordovician age in Pennsylvania west and northwest of the Martie Line (Figure 5-1). Ordovician sedimentary rocks occur only in the subsurface of northern and western Pennsylvania (Fettke, 1961; Wagner, 1966b) and crop out in cen tral and southeastern Pennsylvania (Figure 5-1). In central and south-central Pennsylvania, the Ridge and Valley belt contains a nearly complete Ordovician section. The Great Valley contains predominantly Lower and Middle Ordovician strata. The east-central part of the Great Valley contains allochthonous Cam brian to Middle Ordovician rocks of the Hamburg klippe; these rocks have been compared to the Ta conian allochthons of eastern New York and western New England (Rodgers, 1970; Lash and others, 1984). The Piedmont Lowland contains carbonates and shale of Early and possibly Middle Ordovician age (Gobn, 1978). Possibly coeval rocks of the Glenarm Super group, which occur southeast of the Martic Line (Fig ure 5-1), are penetratively deformed and variably metamorphosed (see Chapters 3A and 4). Some were assigned Early Ordovician ages by Berg, McInerney, and others (1986), but the evidence is equivocal. -
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. -
Usgs Sir 2007-5066
Hydrogeologic Setting and Ground-Water Flow in the Leetown Area, West Virginia Scientific Investigations Report 2007–5066 U.S. Department of the Interior U.S. Geological Survey Hydrogeologic Setting and Ground-Water Flow in the Leetown Area, West Virginia By Mark D. Kozar, David J. Weary, Katherine S. Paybins, and Herbert A. Pierce Scientific Investigations Report 2007–5066 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia: 2007 For sale by U.S. Geological Survey, Information Services Box 25286, Denver Federal Center Denver, CO 80225 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS 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 material contained within this report. Suggested citation: Kozar, M.D., Paybins, K.S., Weary, D.J., and Pierce, H.A., 2007, Hydrogeologic Setting and Ground-Water Flow in the Leetown Area, West Virginia: U.S. Geological Survey Scientific Investigations Report 2007-5066. iii Contents Abstract . 1 Introduction . 2 Purpose and Scope . 2 Methods of Study . -
Fracture Analysis and Dye Trace Report Fracture Analysis and Dye Trace Report
ATLANTIC COAST PIPELINE, LLC ATLANTIC COAST PIPELINE and DOMINION ENERGY TRANSMISSION, INC. SUPPLY HEADER PROJECT Implementation Plan EC26 Attachment 1 Fracture Analysis and Dye Trace Report Fracture Analysis and Dye Trace Report Dominion ACP Augusta, Bath and Highland Counties, Virginia & Pocahontas and Randolph Counties, West Virginia August 30, 2017 19955 Highland Vista Drive, Suite 170 Ashburn, Virginia 20147 703-726-8030 19955 Highland Vista Dr., Suite 170 Ashburn, Virginia 20147 (703) 726-8030 www.geoconcepts-eng.com August 30, 2017 Colin Olness, PE Contractor Atlantic Coast Pipeline - Construction 99 Edmiston Way Buckhannon, WV 26201 Subject: Fracture Analysis and Dye Trace Report Dominion ACP, Augusta, Bath and Highland Counties, Virginia & Pocahontas and Randolph Counties, West Virginia (GeoConcepts Project No. 11002.04) Dear Mr. Olness: GeoConcepts Engineering, Inc. (GeoConcepts) is pleased to present this fracture analysis and existing dye trace report for the proposed Atlantic Coast Pipeline. Sincerely, GEOCONCEPTS ENGINEERING, INC. Joshua D. Valentino, PhD Robert K. Denton Jr., CPG, LPSS Senior Staff Geologist Senior Geologist [email protected] [email protected] Table of Contents Executive Summary ............................................................................................................................. 1 Introduction........................................................................................................................................ 1 Scope of Services ............................................................................................................................... -
Article Full Text
THE OHIO JOURNAL OF SCIENCE Volume 86 April Program Abstracts No. 2 CONTENTS 95th Annual Meeting The Ohio Academy of Science Hosted by The University of Toledo April 25-27, 1986 Theme: Ohio's Research Community: LINKS WITH THE WORLD Registration Form Last page Campus Map 64 Academy Officers 61 Meeting Planning Form 62 General Schedule and All-Academy Lecture ii Parking and Registration ..... ii Meals & Housing ii, iii & vi General Area Map vi Special Events and Field Trips iii Summary of Symposia iv Local Arrangements iv Our Host v Schedule of Technical Section Meetings and Poster Sessions A. Zoology 1 K. Genetics & Cell Biology 33 B. Plant Sciences.... 2 L. Mathematics & Computer Science 35 C. Geology.... 6 M. Psychology 36 D. Medical Sciences .12 N. Junior Academy..... 38 E. Physics & Astronomy ..18 0. Engineering 46 F. Geography 19 Q. Economics 49 G. Chemistry 21 R. Ecology 50 H. Science Education 25 S. Information & Library Sciences 57 I. Anthropology & Sociology....29 J. Conservation. 31 Index to Senior Authors of Abstracts . 63 GENERAL SCHEDULE REGISTRATION & PARKING Except as otherwise Indicated, all sessions and events are on the campus of the University of Toledo. REGISTRATION Is required for all meeting participants. See registration form Inside back cover. FRIDAY, APRIL 25 1986 +++ Access to meeting rooms by name tag only +++ 8:30 A.M. Registration for Section S. Library and Information Science and symposium In the Ward Pick up name tag at registration desk M. Canaday Center, William S. Carlson Library BEFORE attending sessions. See page 57. Meal reservations and payments must be postmarked by Registration for Section Q. -
A Geology Field Trip
Readings and Notes An Introduction to Earth Science 2016 A Geology Field Trip John J. Renton Thomas Repine Follow this and additional works at: https://researchrepository.wvu.edu/earthscience_readings Part of the Geology Commons A GEOLOGY FIELD TRIP by Dr. John J. Renton Dept. of Geology and Geography West Virginia University _,-....~-?IJ~'I Introduction to Field Trip I .I I had several objectives in mind when I prepared this field trip. I want to develop I in you an interest, an understanding, and an appreciation of geology of the region. I ~ ~ I want to show you differences between three of the basic physiographic provinces !3' /f,... within Appalachia, the Low Plateau, the High Plateau, and the Appalachian l'«(t/1 Mountain Section of the Valley and Ridge Province. I also want to show you the role ,}J, I ,~...., " that the kinds and structures of the underlying rocks plays in the formation of the I topography of a region in order to have you better understand why the appearance of the land changes as you travel about FIGURE 2 the country. During the trip, you will also see excellent examples of the process of weathering as well as the erosive I .I power of streams. The trip will visit .I several tourist areas and, in addition to 0. I " ~ r.::: I their scenic beauty, you will learn that ,J they represent excellent examples of g> I 'S~ I important geologic features. C , - --,J~ ~' ,, I '~, G> I ROAD LOG ~ I Cl> I ch .Ct Introduction: As you begin the trip, 0 I there are two figures you will want to s: 1 •~~ ... -
Bedrock Geology of Pennsylvania"
POLYGON ATTRIBUTES FOR "BEDROCK GEOLOGY OF PENNSYLVANIA" UNITNO: A unique number assigned to each map unit in the data sets for geologic units and dikes. The number, which is not derived from the 1980 map, places the units approximately, but not completely, in a sequence ranging from those having the youngest ages (lower numbers) to those having the oldest ages (higher numbers). In the data set for geologic units, there are 193 unique unit numbers ranging from 1 to 195 (unit number 6, kimberlite, and unit number 15, Quarryville Diabase, occur only in the data set for dikes). Units 8 (diabase), 163 (pegmatite), and 183 (metadiabase) occur in both the data set for geologic units and the data set for dikes. MAP_SYMBOL: The symbol used to label the unit on the 1980 state geologic map, except where modified as indicated in "changes.pdf." Please note that the "double-bar P" shown on the 1980 map to indicate units of Pennsylvanian age has been changed to "P," the special character for Triassic units (capital "T" joined to small capital "R") has been changed to "Tr,"and the special character for units of Cambrian age ("C" with horizontal bar) has been changed to "C" in the attribute table. NAME: The name of the geologic unit in the explanation of the 1980 state geologic map (Berg and others, 1980), except where modified as indicated in "changes.pdf." AGE: The age of the geologic unit as shown on the 1980 state geologic map (Berg and others, 1980). Ages are at the level of a geologic period. -
COMMONWEALTH of VIRGIN IA DEPARTMENT of CONSERVATION and ECONOMIC DEVELOPMENT DIVISION of MINERAL RESOURCES Jomes L
VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 7 CONTRIBUTIONS TO VIRGIN IA GEOTOGY-II I COMMONWEALTH OF VIRGIN IA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Jomes L. Colver, Commissioner of Minerol Resources ond Stofe Geologist CHARLOTTESVILLE, VIRGINIA 1978 VIRGlNIA DIVISION OF MINERAL RESOURCES PUBLICATION 7 CONTRIBUTIONS TO VIRGIN IA GEOTOGY-III COMMONWEALTH OF VIRGIN IA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Jomes L. Colver, Commissioner of Minerol Resources ond Stote Geologist CHARLOTTESVILLE, VIRGINIA r978 FRONT COVER: Offices of the Virginia Division of Mineral Resources in the west wing of the Natural Resources Building, McCormick Road, Charlottesville, Virginia. VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 7 CONTRIBUTIONS TO VIRGIN IA GEOLOGY-III COMMONWEALTH OF VIRGIN IA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Jomes L. Colver, Commissioner of Minerol Resources qnd Stote Geologist CHARLOTTESVILLE, VIRGINIA 1978 COMMONWEALTH OF VIRGINIA DEPARTMENT OF PURCHASES AND SUPPLY RICHMOND 1978 Portions of this publication may be quoted if credit is given to the Virginia Division of Mineral Resources. It is recommended that reference to the entire putrlication be made in the following lbrm: Virginia Division of Mineral Resources, 1978, Contributions to Virginia geology-III: Virginia Division of Mineral Resources Publication 7, 154 p. '.f he recommended form for individual citations is noted in each contribution. DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT Richmond, Virginia Fnno W. WRlxnn, Director JnRell F. Moonn,Deputg Director BOARD J.H. JoitNsoN, West Point, Chairman D. HnNnv AlvloNo, Richmond, Vice Chairman A.R. DuNNtNG,Millwood MvRoN P. EnKrLsrIeN, Alexandria ARrnun P. Fltppo, Doswell Aooln U. -
8. Terrain and the Battle of Fredericksburg, December 13, 1862
3. The Paleozoic Record of Changes in Global Climate and Sea Level: Central Appalachian Basin By C. Blaine Cecil,1 David K. Brezinski,2 and Frank Dulong1 With stop contributions by Bascombe Blake,3 Cortland Eble,4 Nick Fedorko,3 William Grady,3 John Repetski,1 Viktoras Skema,5 and Robert Stamm1 Introduction to the Field Trip ally attributed to trapping of sediment in estuaries in response to sea-level rise. More specifically, basal sandstone units of the Cambrian, Silurian, Mississippian, and Pennsylvanian in By C. Blaine Cecil the Appalachian basin are generally attributed to influx induced by tectonic uplift, whereas laterally extensive shale This field trip provides an update of an earlier trip that deposits, such as the Ordovician Martinsburg Formation and was conducted in conjunction with the 1998 Annual Meeting Devonian black shale units, are inferred to result from sedi- of The Geological Society of America (Cecil and others, ment trapping or autocyclic deposition of prodelta muds. 1998). The present trip emphasizes global climate change and Although tectonics clearly plays a role in uplift and subsi- eustatic sea-level change (allocyclic processes of Beerbower, dence, and eustasy also governs the amount of accommoda- 1964) (in a global paleogeographic context) as the predomi- tion space, variation in climate, particularly long- to short- nant controls on Paleozoic sedimentation and stratigraphy in term variation in rainfall in tropical conditions, is of greater the Appalachian foreland basin. The trip stops illustrate long- importance as a control on sediment supply and sedimenta- to short-term paleoclimate change (table 1) as the predomi- tion (for example, Ziegler and others, 1987; Cecil, 1990 and nant control on sediment supply, both chemical and siliciclas- references therein; Cecil and others 1993; Cecil and others, tic (fig.