Geology of the West-Central Part of the Southern Anthracite Field and Adjoining Areas, Pennsylvania
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A Summary of Petroleum Plays and Characteristics of the Michigan Basin
DEPARTMENT OF INTERIOR U.S. GEOLOGICAL SURVEY A summary of petroleum plays and characteristics of the Michigan basin by Ronald R. Charpentier Open-File Report 87-450R This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Denver, Colorado 80225 TABLE OF CONTENTS Page ABSTRACT.................................................. 3 INTRODUCTION.............................................. 3 REGIONAL GEOLOGY.......................................... 3 SOURCE ROCKS.............................................. 6 THERMAL MATURITY.......................................... 11 PETROLEUM PRODUCTION...................................... 11 PLAY DESCRIPTIONS......................................... 18 Mississippian-Pennsylvanian gas play................. 18 Antrim Shale play.................................... 18 Devonian anticlinal play............................. 21 Niagaran reef play................................... 21 Trenton-Black River play............................. 23 Prairie du Chien play................................ 25 Cambrian play........................................ 29 Precambrian rift play................................ 29 REFERENCES................................................ 32 LIST OF FIGURES Figure Page 1. Index map of Michigan basin province (modified from Ells, 1971, reprinted by permission of American Association of Petroleum Geologists)................. 4 2. Structure contour map on top of Precambrian basement, Lower Peninsula -
Cambrian Ordovician
Open File Report LXXVI the shale is also variously colored. Glauconite is generally abundant in the formation. The Eau Claire A Summary of the Stratigraphy of the increases in thickness southward in the Southern Peninsula of Michigan where it becomes much more Southern Peninsula of Michigan * dolomitic. by: The Dresbach sandstone is a fine to medium grained E. J. Baltrusaites, C. K. Clark, G. V. Cohee, R. P. Grant sandstone with well rounded and angular quartz grains. W. A. Kelly, K. K. Landes, G. D. Lindberg and R. B. Thin beds of argillaceous dolomite may occur locally in Newcombe of the Michigan Geological Society * the sandstone. It is about 100 feet thick in the Southern Peninsula of Michigan but is absent in Northern Indiana. The Franconia sandstone is a fine to medium grained Cambrian glauconitic and dolomitic sandstone. It is from 10 to 20 Cambrian rocks in the Southern Peninsula of Michigan feet thick where present in the Southern Peninsula. consist of sandstone, dolomite, and some shale. These * See last page rocks, Lake Superior sandstone, which are of Upper Cambrian age overlie pre-Cambrian rocks and are The Trempealeau is predominantly a buff to light brown divided into the Jacobsville sandstone overlain by the dolomite with a minor amount of sandy, glauconitic Munising. The Munising sandstone at the north is dolomite and dolomitic shale in the basal part. Zones of divided southward into the following formations in sandy dolomite are in the Trempealeau in addition to the ascending order: Mount Simon, Eau Claire, Dresbach basal part. A small amount of chert may be found in and Franconia sandstones overlain by the Trampealeau various places in the formation. -
Mapping Potential Geologic Hazards for Proposed Highway Construction Projects in Pennsylvania: Route 15 in Lycoming County
Mapping Potential Geologic Hazards for Proposed Highway Construction Projects in Pennsylvania: Route 15 in Lycoming County By Stuart O. Reese, P.G. Pennsylvania Geological Survey 3240 Schoolhouse Road Middletown, PA 17057 Telephone: (717) 702-2028 Fax: (717) 702-2065 email: [email protected] INTRODUCTION acidic drainage from uncovered Marcellus Shale (a black shale with approximately 3 percent sulfur) that had to be mitigated. The current project is situated in north-central Pennsyl- Recently, the Pennsylvania Geological Survey has vania in the Deep Valleys section of the Appalachian Plateaus worked on behalf of the Pennsylvania Department of Trans- portation (PennDOT) to develop maps for specific highway physiographic province in Lycoming County, Pennsylvania. construction projects. The purpose of these maps is to identify Section C41 of U.S. Route 15 is located from north of Trout potential geologic hazards such as landslides, sinkholes, min- Run to the Village of Buttonwood in the “Steam Valley” eralization, historic deep mines, acid drainage, and ground- area of Cogan House and Lewis Townships. The improved water conditions. Map layers have included aerial imagery, highway corridor will become part of Interstate 99, the Appa- digital elevation model (DEM) datasets, digital raster graphics lachian Thruway. This requires an upgrade of the 4 1/2 mile (DRGs), bedrock units and their contacts, surficial and struc- Steam Valley section (C41) to a four-lane limited access high- tural geology features, mapped landslides, glacial boundaries, way that meets current design standards comparable to adja- and water well locations. Possible issues are described in cent sections of U.S. 15. Construction is estimated to begin in the accompanying poster for the proposed construction zones fall 2007 (pending the availability of funds). -
(Medina, Clinton, and Lockport Groups) in the Type Area of Western New York
Revised Stratigraphy and Correlations of the Niagaran Provincial Series (Medina, Clinton, and Lockport Groups) in the Type Area of Western New York By Carlton E. Brett, Dorothy H. Tepper, William M. Goodman, Steven T. LoDuca, and Bea-Yeh Eckert U.S. GEOLOGICAL SURVEY BULLETIN 2086 Prepared in cooperation with the U.S. Environmental Protection Agency and the Department of Earth and Environmental Sciences of the University of Rochester UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1995 10 REVISED STRATIGRAPHY AND CORRELATIONS OF THE NIAGARAN PROVINCIAL SERIES been made in accordance with the NASC. Because the The history of nomenclature of what is now termed the NASC does not allow use of the "submember" category, Medina Group, beginning with Conrad ( 1837) and ending units that would be of this rank are treated as informal units with Bolton (1953), is presented in Fisher (1954); Bolton and have been given alphanumeric designations. Informal (1957, table 2) presents a detailed summary of this nomen- units are discussed under the appropriate "member" clature for 1910-53. A historical summary of nomenclature categories. of the Medina Group in the Niagara region is shown in fig- The use of quotes for stratigraphic nomenclature in this ure 7. Early investigators of the Medina include Conrad report is restricted to units that have been misidentified or (1837); Vanuxem (1840, first usage of Medina; 1842); Hall abandoned. If stratigraphic nomenclature for a unit has (1840, 1843); Gilbert (1899); Luther (1899); Fairchild changed over time, the term for the unit is shown, with cap- (1901); Grabau (1901, 1905, 1908, 1909, 1913); Kindle and italization, as given in whatever reference is cited rather Taylor (1913); Kindle (1914); Schuchert (1914); Chadwick than according to the most recent nomenclature. -
Geology of the Prater and Vansant Quadrangles, Virginia Commonwealth of Virgin Ia
VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 52 GEOLOGY OF THE PRATER AND VANSANT QUADRANGLES, VIRGINIA Jack E. Nolde and Martin L. Mitchell with sections on subsurface stratigraphy and gas resources by Joan K. Polzin COMMONWEALTH OF VIRGIN IA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Robert c. Milici, commissioner of Mineral Resources and state Geologist CHARLOTTESVI LLE, VI RGINIA 1984 VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 52 GEOLOGY OF THE PRATER AND VANSANT QUADRANGLES, VI RGINIA Jack E. Nolde and Martin L. Mitchell with sections on subsurface stratigraphy and gas resources by Joan K. Polzin COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Robert c. Milici, commissioner of Mineral Resources and state Geologist CHARLOTTESVILLE, VIRGI NIA 1984 COVER PHOTO: Jewell Coal and Coke Company coking operation on Dismal Creek in northeast Vansant quadrangle (photo by J.H. Grantham). VIRGINIA DIVISION OF MINERAL RESOURCES PUBLICATION 52 GEOLOGY OF THE PRATER AND VANSANT QUADRANGLES, VIRG I NIA Jack E. Nolde and Martin L. Mitchell with sections on subsurface stratigraphy and gas resources by Joan K. Polzin COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES Robert C. Milici, Commissioner of Mineral Resources and State Geologist CHARLOTTESVILLE, VIRGINIA 1984 DEPARTM ENT OF CONSERVATION AND ECONOMIC DEVELOPMENT Richmond, Virginia FRED W. WALKER, Director JERALD F. MOORE, Deputy Director BOARD HENRY T. N. GRAVES, Chairman, Luray ADOLF U. HONKALA, Vice Chairman, Midlothian FRANK ARMSTRONG. III. Winchester RICK E. BURNELL, Virginia Beach GWENDOLYN JO M. CARLBERG, Alexandria WILBUR S. DOYLE, Martinsville BRUCE B. GRAY, Waverly MILDRED LAYNE, Williamsburg JOHN E. -
Stratigraphic Succession in Lower Peninsula of Michigan
STRATIGRAPHIC DOMINANT LITHOLOGY ERA PERIOD EPOCHNORTHSTAGES AMERICANBasin Margin Basin Center MEMBER FORMATIONGROUP SUCCESSION IN LOWER Quaternary Pleistocene Glacial Drift PENINSULA Cenozoic Pleistocene OF MICHIGAN Mesozoic Jurassic ?Kimmeridgian? Ionia Sandstone Late Michigan Dept. of Environmental Quality Conemaugh Grand River Formation Geological Survey Division Late Harold Fitch, State Geologist Pennsylvanian and Saginaw Formation ?Pottsville? Michigan Basin Geological Society Early GEOL IN OG S IC A A B L N Parma Sandstone S A O G C I I H E C T I Y Bayport Limestone M Meramecian Grand Rapids Group 1936 Late Michigan Formation Stratigraphic Nomenclature Project Committee: Mississippian Dr. Paul A. Catacosinos, Co-chairman Mark S. Wollensak, Co-chairman Osagian Marshall Sandstone Principal Authors: Dr. Paul A. Catacosinos Early Kinderhookian Coldwater Shale Dr. William Harrison III Robert Reynolds Sunbury Shale Dr. Dave B.Westjohn Mark S. Wollensak Berea Sandstone Chautauquan Bedford Shale 2000 Late Antrim Shale Senecan Traverse Formation Traverse Limestone Traverse Group Erian Devonian Bell Shale Dundee Limestone Middle Lucas Formation Detroit River Group Amherstburg Form. Ulsterian Sylvania Sandstone Bois Blanc Formation Garden Island Formation Early Bass Islands Dolomite Sand Salina G Unit Paleozoic Glacial Clay or Silt Late Cayugan Salina F Unit Till/Gravel Salina E Unit Salina D Unit Limestone Salina C Shale Salina Group Salina B Unit Sandy Limestone Salina A-2 Carbonate Silurian Salina A-2 Evaporite Shaley Limestone Ruff Formation -
Subsurface Facies Analysis of the Devonian Berea Sandstone in Southeastern Ohio
SUBSURFACE FACIES ANALYSIS OF THE DEVONIAN BEREA SANDSTONE IN SOUTHEASTERN OHIO William T. Garnes A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE December 2014 Committee: James Evans, Advisor Jeffrey Snyder Charles Onasch ii ABSTRACT James Evans, Advisor The Devonian Berea Sandstone is an internally complex, heterogeneous unit that appears prominently both in outcrop and subsurface in Ohio. While the unit is clearly deltaic in outcrops in northeastern Ohio, its depositional setting is more problematic in southeastern Ohio where it is only found in the subsurface. The goal of this project was to search for evidence of a barrier island/inlet channel depositional environment for the Berea Sandstone to assess whether the Berea Sandstone was deposited under conditions in southeastern Ohio unique from northeastern Ohio. This project involved looking at cores from 5 wells: 3426 (Athens Co.), 3425 (Meigs Co.), 3253 (Athens Co.), 3252 (Athens Co.), and 3251 (Athens Co.) In cores, the Berea Sandstone ranges from 2 to 10 m (8-32 ft) thick, with an average thickness of 6.3 m (20.7 ft). Core descriptions involved hand specimens, thin section descriptions, and core photography. In addition to these 5 wells, the gamma ray logs from 13 wells were used to interpret the architecture and lithologies of the Berea Sandstone in Athens Co. and Meigs Co. as well as surrounding Vinton, Washington, and Morgan counties. Analysis from this study shows evidence of deltaic lobe progradation, abandonment, and re-working. Evidence of interdistributary bays with shallow sub-tidal environments, as well as large sand bodies, is also present. -
Birds of Mount Greylock Mount Greylock State Reservation INFORMATION GUIDE & SIGHTING LIST
Birds of Mount Greylock Mount Greylock State Reservation INFORMATION GUIDE & SIGHTING LIST Birds of Mount Greylock is a two-part document. Part 1 is a basic overview of the variety of bird species found in and around Mount Greylock, where you might encounter them in the Reservation. Part 2 is a birding checklist for your records. Part 1 Managed by the Department of Conservation & Recreation (DCR), Mount Greylock State Reservation covers over 12,500 acres of upland habitat. The summit at 3,491 feet above sea level is the highest point in Massachusetts and supports the only sub-alpine ecosystem in the state; one of the southernmost extensions of the boreal or spruce-fir forest, normally associated with Canada. Why go birding? If you want a challenge, camaraderie, fun, passion, beauty, insight, travel, and discovery, go birding. All this aside, humans have certainly altered face of the landscape, sometimes negatively impacting bird habitats. Bird populations, over time, have responded by shifting to more suitable habitats or disappearing altogether from certain areas. Still other species have been either hunted to extinction, their distinctive habitats completely destroyed, affected by pesticides or pollution, or even displaced by competing bird species. There is a widely held belief within the bird watching community is that an interest in birds is often the first step toward building a sound conservation ethic. Birds are sensitive indicators of the health of the environment. It is likely that a popular widespread commitment to their well- being will lead to a greater concern for the quality of the environment on which humans and birds are mutually dependent. -
Further Paleomagnetic Evidence for Oroclinal Rotation in the Central Folded Appalachians from the Bloomsburg and the Mauch Chunk Formations
TECTONICS, VOL. 7, NO. 4, PAGES 749-759, AUGUST 1988 FURTHER PALEOMAGNETIC EVIDENCE FOR OROCLINAL ROTATION IN THE CENTRAL FOLDED APPALACHIANS FROM THE BLOOMSBURG AND THE MAUCH CHUNK FORMATIONS Dennis V. Kent Lamont-DohertyGeological Observatory and Departmentof GeologicalSciences ColumbiaUniversity, Palisades, New York Abstract.Renewed paleomagnetic investigations of red fromthe Bloomsburg, Mauch Chunk, and revised results bedsof theUpper Silurian Bloomsburg and the Lower recentlyreported for theUpper Devonian Catskill Formation Carboniferous Mauch Chunk Formations were undertaken togetherindicate 22.8•>+_11.9 oof relativerotation, accounting with theobjective of obtainingevidence regarding the for approximatelyhalf thepresent change in structuraltrend possibilityof oroclinalbending as contributing to thearcuate aroundthe Pennsylvania salient. The oroclinalrotation can be structuraltrend of thePennsylvania salient. These formations regardedas a tightenS.*'.3 o/'a lessarcuate depositional package cropout on both limbs of thesalient and earlier, but less thatdeveloped across a basementreentrant, to achievea definitivepaleomagnetic studies on these units indicate that curvaturecloser to that of the earlierzigzag continental margin earlyacquired magnetizations can be recovered. Oriented outline. sampleswere obtained from nine sites on the southern limb of thesalient and eight sites from the northern limb in the INTRODUCTION Bloomsburg.The naturalremanent magnetizations are multivectorial,dominated by a component(B) with a A testof the oroclinehypothesis -
Lexington Quadrangle Virginia
COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES GEOLOGY OF THE LEXINGTON QUADRANGLE VIRGINIA KENNETH F. BICK REPORT OF INVESTIGATIONS I VIRGINIA DIVISION OF MINERAL RESOURCES Jomes L. Colver Commissioner of Minerol Resources ond Stote Geologist CHARLOTTESVI LLE, VI RGI N IA 1960 COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES GEOLOGY OF THE LEXINGTON QUADRANGLE VIRGINIA KENNETH F. BICK REPORT OF INVESTIGATIONS I VIRGINIA DIVISION OF MINERAL RESOURCES Jomes L. Colver Commissioner of Minerol Resources ond Stote Geologist CHARLOTTESVI LLE, VI RGI N IA 1960 Couuowwoer,rn op Vtncrwre DopenrupNr op Puncnesrs exo Supptv Rrculroxn 1960 DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT Richmond. Virginia MenvrN M. SurHnnr,eNn, Director BOARD Vrcron W. Stnwenr, Petersburg, Chairtnan G. Ar,vrn MessnNnunc, Hampton, Viee'Chairman A. Pr,urvrnr BmnNn, Orange C. S. Cenrnn, Bristol ANpnpw A. Fenr,pv, Danville WonrnrrvcroN FauLKNEn, Glasgow SvoNpv F. Slter,r,, Roanoke EnwrN H. Wrr,r,, Richmond Wrr,r,renr P. Wooor,nv. Norfolk CONTENTS Pece Abstract. '"*i"#:;;;;: . : ::: , : ::.:::::::::..::::::. :.::.::::::: ::,r Z Geography 8 Purpose. 4 Previous Work. Present Work and Acknowledgements. 5 Geologic Formations. 6 Introduction. 6 Precambrian System. 6 Pedlar formation 6 Precambrian and Cambrian Systems. 6 Discussion. 6 Swift Run formation 8 Catoctin greenstone. I Unieoiformation...... ......... I Hampton(Harpers)formation. .......... I Erwin (Antietam) quartzite. Cambrian System . I0 Shady (Tomstown) dolomite 10 Rome (Waynesboro) formation.... ll Elbrook formation. 12 Conococheague limestone. l3 Ordovician System. ......., 14 Chepultepeclimestone. .......... 14 Beekmantown formatron. 14 New Market limestone. 15 Lincolnshire limestone. 16 Edinburg formation. 16 Martinsburg shale... 17 SilurianSystem. ......... 18 Clinchsandstone..... .......... 18 Clinton formation. -
A New Eurypterid from the Saaremaa- (Oesel-) Beds in Estonia
TARTU ÜLIKOOLI GEOLOOGIA-INSTITUUDI TOIMETUSED .M 37 PUBLIGA TIONS OF THE GEOLOGICAL INSTITUTION .M 37 OF THE UNIVERSITY OF TARTU A NEW EURYPTERID FROM THE SAAREMAA- (OESEL-) BEDS IN ESTONIA BY LEIF STÖRMER TARTU 1934 K. Mattieseni trükikoda o-ü., Tartu 1934. A new Eurypterid from the Saaremaa- (Oesal-) bads in Estonia. B y L ei f Stör m er. The famous Eurypterus fi�cheri-faunaof Rootsiküla (Rootziküll), Saaremaa, became known to science through the monographs of N iesz kow sk i (1858), Sc hmidt (1.883), and Ho lm (1898). The unique preservation of the eurypterid shells has made it possible to study in detail the finest morphv logical structures of these old arthropods. By means of a special metbod, Ho lm succeeded in separating the chitinaus tests from the matrix. The Saaremaa beds have also furnished a considerable supply of vertebrates and crustaceans. In later years Professor dr. W. Patten from Dartmouth College, Hanover, N. H., U. S. A. made extensive collections in tbe Saaremaa beds. He was specially interested in the remains of the primitive vertebra tes, but also collected a considerable mate rial of merostomes. The sad death of Professor Pat.ten in the fall of 1932 prevented him frorn finishing bis interesting studies on the valuable material of prim itive >ertebrates. In May 1932 I had the fortunate opportunity to visit Professor Patten in Dartmouth Col lege. He very kindly showed me bis fine collections of eurypterids from Saaremaa. Looking through the material I became aware of an eurypterid specimen , belanging to a genus not known, from tbe Eurypterus fischeri-fauna of Saaremaa. -
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.