1 an Investigation of Fertilizer-Derived Uranium in Ohio
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Carboniferous Formations and Faunas of Central Montana
Carboniferous Formations and Faunas of Central Montana GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 Carboniferous Formations and Faunas of Central Montana By W. H. EASTON GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 A study of the stratigraphic and ecologic associa tions and significance offossils from the Big Snowy group of Mississippian and Pennsylvanian rocks UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publication as follows : Eastern, William Heyden, 1916- Carboniferous formations and faunas of central Montana. Washington, U.S. Govt. Print. Off., 1961. iv, 126 p. illus., diagrs., tables. 29 cm. (U.S. Geological Survey. Professional paper 348) Part of illustrative matter folded in pocket. Bibliography: p. 101-108. 1. Paleontology Montana. 2. Paleontology Carboniferous. 3. Geology, Stratigraphic Carboniferous. I. Title. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, B.C. CONTENTS Page Page Abstract-__________________________________________ 1 Faunal analysis Continued Introduction _______________________________________ 1 Faunal relations ______________________________ 22 Purposes of the study_ __________________________ 1 Long-ranging elements...__________________ 22 Organization of present work___ __________________ 3 Elements of Mississippian affinity.._________ 22 Acknowledgments--.-------.- ___________________ -
Recent Information Maxville Lime.Stone
.·-~ . f GEOLOGICAL SURVEY OF OHIO WILBER STOUT, State Geologist Fourth Series Information Circular No. 3 RECENT INFORMATION ON THE MAXVILLE LIME.STONE by RAYMONDE. LAMBORN COLUMBUS 1945 Reprinted 1961 HOOK I\(..• OHIO GEOL. SURVEY. LAKE ERIE SECTION LIBRARY CARD NO. ·7 STATE CF OHIO Michael V. DiSalle Governor DEPARTMENT CF NATURAL RESOURCES Herbert B. Eagon Director NATURAL RESOURCES CCMMISSION C. D. Blubaugh Joseph E. Hunt Herbert B. Eagon Roy M. Kottman Byron Frederick DemClB L. Sean Forrest G. Hl1ll Myron T. Sturgeon Willian• Hoyne DIVISION OF GEQ.OGICAL SURVEY Ralph j. Bernhagen Chief COLUMBUS 1945 Reprinted 1961 Heer ptg. Co., Cols., O. INTRODUCTION The Maxville has been an important source of limestone for more than 100 years in southern and east central Ohio where it was first utilized for mortar and for furnace flux. Probably for this rea~on outcrops of a limestone later shown to be Maxville in age were described by Briggs in 1838 who noted occurrences near Maxville, Perry County; on Three Mile Run near Logan in Hocking County; near Reeds Mills near Wellston, Jackson County; and at the Canter Quarry in Hamilton Township, Jack- son County.1 Further obser.vations of this limestone were made by E. B. Andrews of the Second Geological Survey of Ohio and his report was published in the Report of Progress in 1869. Andrews named the lime- stone the Maxville for its occurrence near Maxville, Hocking County, noted its patchy distribution on the outcrop, described its stratigraphic position as immediately overlying the Logan sandstones ana shales, and declared the limestone to be of sub-Carboniferous (Mississippian) age. -
The Classic Upper Ordovician Stratigraphy and Paleontology of the Eastern Cincinnati Arch
International Geoscience Programme Project 653 Third Annual Meeting - Athens, Ohio, USA Field Trip Guidebook THE CLASSIC UPPER ORDOVICIAN STRATIGRAPHY AND PALEONTOLOGY OF THE EASTERN CINCINNATI ARCH Carlton E. Brett – Kyle R. Hartshorn – Allison L. Young – Cameron E. Schwalbach – Alycia L. Stigall International Geoscience Programme (IGCP) Project 653 Third Annual Meeting - 2018 - Athens, Ohio, USA Field Trip Guidebook THE CLASSIC UPPER ORDOVICIAN STRATIGRAPHY AND PALEONTOLOGY OF THE EASTERN CINCINNATI ARCH Carlton E. Brett Department of Geology, University of Cincinnati, 2624 Clifton Avenue, Cincinnati, Ohio 45221, USA ([email protected]) Kyle R. Hartshorn Dry Dredgers, 6473 Jayfield Drive, Hamilton, Ohio 45011, USA ([email protected]) Allison L. Young Department of Geology, University of Cincinnati, 2624 Clifton Avenue, Cincinnati, Ohio 45221, USA ([email protected]) Cameron E. Schwalbach 1099 Clough Pike, Batavia, OH 45103, USA ([email protected]) Alycia L. Stigall Department of Geological Sciences and OHIO Center for Ecology and Evolutionary Studies, Ohio University, 316 Clippinger Lab, Athens, Ohio 45701, USA ([email protected]) ACKNOWLEDGMENTS We extend our thanks to the many colleagues and students who have aided us in our field work, discussions, and publications, including Chris Aucoin, Ben Dattilo, Brad Deline, Rebecca Freeman, Steve Holland, T.J. Malgieri, Pat McLaughlin, Charles Mitchell, Tim Paton, Alex Ries, Tom Schramm, and James Thomka. No less gratitude goes to the many local collectors, amateurs in name only: Jack Kallmeyer, Tom Bantel, Don Bissett, Dan Cooper, Stephen Felton, Ron Fine, Rich Fuchs, Bill Heimbrock, Jerry Rush, and dozens of other Dry Dredgers. We are also grateful to David Meyer and Arnie Miller for insightful discussions of the Cincinnatian, and to Richard A. -
Changes in Stratigraphic Nomenclature by the U.S. Geological Survey
Changes in Stratigraphic Nomenclature by the U.S. Geological Survey, By GEORGE V. COHEE, ROBERT G. BATES, and WILNA B. WRIGHT CONTRIBUTIONS TO STRATIGRAPHY GEOLOGICAL SURVEY BULLETIN 1294-A UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1970 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 35 cents (paper cover) CONTENTS Listing of nomenclatural changes- --- ----- - - ---- -- -- -- ------ --- Ortega Quartzite and the Big Rock and Jawbone Conglomerate Members of the Kiawa Mountain Formation, Tusas Mountains, New Mexico, by Fred Barker---------------------------------------------------- Reasons for abandonment of the Portage Group, by Wallace de Witt, Jr-- Tlevak Basalt, west coast of Prince of Wales Island, southeastern Alaska, by G. Donald Eberlein and Michael Churkin, Jr Formations of the Bisbee Group, Empire Mountains quadrangle, Pima County, Arizona, by Tommy L. Finnell---------------------------- Glance Conglomerate- - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - Willow Canyon Formation ....................................... Apache Canyon Formation-- ................................... Shellenberger Canyon Formation- - --__----- ---- -- -- -- ----------- Turney Ranch Formation---- ------- ------ -- -- -- ---- ------ ----- Age--_------------------------------------------------------- Pantano Formation, by Tommy L. Finnell----------_----------------- -
Development of Drinking Water and Ecological Unusually Sensitive Areas (Usas): Examples Using the Water and Biological Resources of Ohio
Development of Drinking Water and Ecological Unusually Sensitive Areas (USAs): Examples Using the Water and Biological Resources of Ohio Colin Plank, Scott Zengel, Heidi Hinkeldey, Elaine Inouye, William Holton, Jeffery Dahlin, and Jacqueline Michel Research Planning, Inc., 1121 Park Street, Columbia, SC 29201, [email protected], 803-256-7322 (voice); 803-254-6445 (fax); and Christina Sames and Samuel Hall, Office of Pipeline Safety, Research and Special Programs Administration, U.S. Department of Transportation, Washington, D.C. 1.0 INTRODUCTION The U.S. Department of Transportation’s Research and Special Programs Administration (RSPA) is required to identify areas unusually sensitive to environmental damage in the event of a hazardous liquid pipeline accident. Pipeline operators that can affect "unusually sensitive areas" (USAs) must develop and follow an integrity management program to assess and evaluate the integrity of their pipelines. After extensive consultation with experts, government agencies, and other stakeholders, a process was developed to identify USAs for drinking water and ecological resources. In general the USA identification process involves selecting a subset of USA candidates from the larger group of Environmentally Sensitive Areas (ESAs), and then applying various filter criteria to the candidates to determine final USAs. For drinking water USAs this means identifying potentially sensitive public water systems (PWS), specifically surface water intakes and ground water wells, and subjecting them to filter -
Xerox University Microfilms
information t o u s e r s This material was produced from a microfilm copy of the original document. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the original submitted. The following explanation of techniques is provided to help you understand markings or patterns which may appear on this reproduction. 1.The sign or "target” for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting thru an image and duplicating adjacent pages to insure you complete continuity. 2. When an image on the film is obliterated with a large round black mark, it is an indication that the photographer suspected that the copy may have moved during exposure and thus cause a blurred image. You will find a good image of the page in the adjacent frame. 3. When a map, drawing or chart, etc., was part of the material being photographed the photographer followed a definite method in "sectioning" the material. It is customary to begin photoing at the upper left hand corner of a large sheet and to continue photoing from left to right in equal sections with a small overlap. If necessary, sectioning is continued again - beginning below the first row and continuing on until complete. 4. The majority of usefs indicate that the textual content is of greatest value, however, a somewhat higher quality reproduction could be made from "photographs" if essential to the understanding of the dissertation. -
Conodonts of the Estill Shale and Bisher Formation (Silurian, Southern Ohio): Biostratigraphy and Distribution1
78 M. A. LAMB AND R. L. LOWE Vol. 87 Conodonts of the Estill Shale and Bisher Formation (Silurian, Southern Ohio): Biostratigraphy and Distribution1 MARK A. KLEFFNER, Department of Geology and Mineralogy, The Ohio State University, Columbus, OH 43210 ABSTRACT. Representatives of 20 species of conodonts have been isolated from samples of the Silurian Estill Shale and Bisher Formation at four localities in southern Ohio. The Estill belongs in the amorphognathoides Zone and is late Llandoverian to early Wenlockian. The Estill-Bisher contact is an unconformity. In Adams and southern Highland counties, the Bisher belongs in the middle and upper ranuliformis Zone and is late early to possibly early middle Wenlockian; in northern Highland County the Bisher belongs in the lower ranuliformis Zone and is middle early to late early Wenlockian. The Estill was deposited in a gradually shoaling sea that regressed from Adams and Highland counties in the early Wenlockian. The sea transgressed south- ward across the two counties later in the early Wenlockian and deposited the Bisher in a shallow, subtidal environment. OHIO J. SCI. 87 (3): 78-89, 1987 INTRODUCTION Highland County, Ohio. North of Fleming County, Kentucky, an unconformity separates the Noland and The Estill Shale and overlying Bisher Formation make Estill (Rexroad and Kleffner 1984). up most of the lower Niagaran sequence (Silurian) in The Estill Shale consists predominantly of blue-green, Adams and Highland counties in southern Ohio. The gray-green, green, and brown shale. Shale beds are com- first, and only detailed, published report on conodonts monly blocky or massive in the lower part of the for- from either the Estill or Bisher was by Rexroad and mation and silty and fissile in the upper part. -
The Silurian of Central Kentucky, U.S.A.: Stratigraphy, Palaeoenvironments and Palaeoecology
The Silurian of central Kentucky, U.S.A.: Stratigraphy, palaeoenvironments and palaeoecology FRANK R. ETTENSOHN, R. THOMAS LIERMAN, CHARLES E. MASON, WILLIAM M. ANDREWS, R. TODD HENDRICKS, DANIEL J. PHELPS & LAWRENCE A. GORDON ETTENSOHN, F.R., LIERMAN, R.T., MASON, C.E., ANDREWS, W.M., HENDRICKS, R.T., PHELPS, D.J. & GORDON, L.A., 2013:04:26. The Silurian of central Kentucky, U.S.A.: Stratigraphy, palaeoenvironments and palaeoecology. Memoirs of the Association of Australasian Palaeontologists 44, 159-189. ISSN 0810-8889. Silurian rocks in Kentucky are exposed on the eastern and western flanks of the Cincinnati Arch, a large-wavelength cratonic structure separating the Appalachian foreland basin from the intracratonic Illinois Basin. The Cincinnati Arch area experienced uplift during latest Ordovician-early Silurian time, so that the exposed Silurian section is relatively thin due to onlap and post- Silurian erosional truncation on the arch. On both flanks of the arch, dolomitic carbonates predominate, but the section on the eastern side reflects a more shale-rich ramp that faced eastern Appalachian source areas. In the Silurian section on the western side of the arch, which apparently developed across a platform-like isolation-accommodation zone, shales are rare except dur- ing some highstand episodes, and rocks in the area reflect deposition across a broad, low-gradient shelf area, interrupted by structurally controlled topographic breaks. Using the progression of interpreted depositional environments and nearshore faunal communities, a relative sea-level curve, which parallels those of previous workers, was generated for the section in Kentucky. While the curve clearly shows the influence of glacial eustasy, distinct indications of the far-field, flexural influence of Taconian and Salinic tectonism are also present. -
Geology of Fairfield County, Ohio
This dissertation has been 61—5134 microfilmed exactly as received WOLFE, Edward Winslow, 1936- GEOLOGY OF FAIRFIELD COUNTY, OHIO. The Ohio State University, Ph.D., 1961 Geology University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY OF FAIRFIELD COUNTY, OHIO DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of the Ohio State University By Edward Winslow Wolfe, B. A. The Ohio State University 1961 Approved by Department of Geology ! ACKNOWLEDGMENTS Thanks are due Mr. R. J. Bernhagen, State Geologist, who suggest ed the need for an investigation of the geology of Fairfield County. The writer is particularly indebted to Dr. Aurele La Rooque who di rected the investigation and guided the writer throughout the prepara tion of this report. Many others gave freely of their time in dis cussing with the writer the geology of Fairfield County. Among these, special thanks are due Dr. Jane L. Forsyth of the Ohio Division of Geological Survey, Mr. George J. Franklin, who is presently completing a report on the geology of Licking County, and the writer's colleagues in the Department of Geology at the College of Wooster. The writer thanks several members of the Ohio Division of Geological Survey, in cluding Miss Pauline Smyth, Mr. Karl V. Hoover, and Mr. Harold J. Flint, for their valuable assistance. Most helpful, too, was the as sistance of Mr. Jon S. Galehouse during the summer of i960. The field work was sponsored and financed by the Ohio Division of Geological Survey. Additional financial aid, in the form of a William H. -
The Geology of Ohio—The Ordovician
A Quarterly Publication of the Division of Geological Survey Fall 1997 THE GEOLOGY OF OHIO—THE ORDOVICIAN by Michael C. Hansen o geologists, the Ordovician System of Ohio bulge), accompanying development of a foreland is probably the most famous of the state’s basin to the east at the edge of the orogenic belt. As Paleozoic rock systems. The alternating shales the Taconic Orogeny reached its zenith in the Late Tand limestones of the upper part of this system crop Ordovician, sediments eroded from the rising out in southwestern Ohio in the Cincinnati region mountains were carried westward, forming a com- and yield an incredible abundance and diversity of plex delta system that discharged mud into the well-preserved fossils. Representatives of this fauna shallow seas that covered Ohio and adjacent areas. reside in museums and private collections through- The development of this delta, the Queenston Delta, out the world. Indeed, fossils from Ohio’s Ordovi- is recorded by the many beds of shale in Upper cian rocks define life of this geologic period, and the Ordovician rocks exposed in southwestern Ohio. rocks of this region, the Cincinnatian Series, serve The island arcs associated with continental as the North American Upper Ordovician Standard. collision were the sites of active volcanoes, as docu- Furthermore, in the late 1800’s, Ordovician rocks in mented by the widespread beds of volcanic ash the subsurface in northwestern Ohio were the source preserved in Ohio’s Ordovician rocks (see Ohio of the first giant oil and gas field in the country. Geology, Summer/Fall 1991). -
Huron River Basin, 2016
Appendices to the Biological and Water Quality Study of the Huron River Basin, 2016 Erie, Seneca, Huron, Crawford and Richland Counties Huron River at Milan Wildlife Area Ohio EPA Technical Report AMS/2016-HURON-2 Division of Surface Water Assessment and Modeling Section January 2020 Draft Appendices to the Biological and Water Quality Study of the Huron River Basin, 2016 Erie, Seneca, Huron, Crawford and Richland Counties January 2020 Ohio EPA Technical Report AMS/2016-HURON-2 Prepared by: Ohio Environmental Protection Agency Division of Surface Water Lazarus Government Center 50 W. Town Street, Suite 700 Columbus, Ohio 43215 Ohio Environmental Protection Agency Division of Surface Water Groveport Field Office 4675 Homer Ohio Lane Groveport, Ohio 43125 and Ohio Environmental Protection Agency Northwest District Office 347 N. Dunbridge Road Bowling Green, Ohio 43402 Mail to: P.O. Box 1049 Columbus, Ohio 43216-1049 Mike DeWine, Governor, State of Ohio Laurie A. Stevenson, Director, Ohio Environmental Protection Agency Appendices • Appendix A – NPDES Descriptions • Appendix B – Macroinvertebrate Collection Results • Appendix C – Macroinvertebrate ICI Scores and Metrics • Appendix D – Fish Species and Abundance for Each Sampling Location • Appendix E – Fish IBI Scores and Metrics • Appendix F – Qualitative Habitat Evaluation Index Scores and Attributes • Appendix G – Surface Water Inorganic Chemistry Results • Appendix H – Surface Water Organic Chemistry Results • Appendix I – Sediment Chemistry Results • Appendix J – Water Quality Sonde Results • Appendix K – Surface Water Bacteriological Results • Appendix L – Lake Sampling Results Appendix A NPDES‐Permitted Facilities A total of 43 National Pollutant Discharge Elimination System (NPDES)-permitted facilities discharge sanitary wastewater, industrial process water or industrial storm water into the study area. -
Geological Survey of Michigan Lower Peninsula 1896-1900 Vol. Vii Part Ii
GEOLOGICAL SURVEY OF MICHIGAN § 2. Level of Lake Huron.............................................17 ALFRED C. LANE, STATE GEOLOGIST § 3. Types of shore line...............................................19 (a) Mud flat ............................................................ 19 GEOLOGICAL SURVEY OF MICHIGAN (b) sand beach....................................................... 20 LOWER PENINSULA (c) cliff and shingle................................................. 20 1896-1900 § 4. Explanation of contour map. ................................21 § 5. Tables of altitudes. ...............................................21 VOL. VII (a) Lake survey bench marks ................................ 21 PART II (b 1) Port Austin Division....................................... 22 GEOLOGICAL REPORT ON HURON COUNTY (b 2) Harbor Beach Division, Pere Marquette R.R.22 MICHIGAN (b 3) Pontiac, Oxford & Northern R.R.................... 22 (c 1) Preliminary line of Saginaw, Tuscola & Huron BY R.R......................................................................... 23 ALFRED C. LANE (c 2) Goodman Logging Road: .............................. 23 (c 3) Main line Saginaw, Tuscola and Huron R.R..23 ACCOMPANIED BY ELEVEN PLATES AND TWELVE (c 4) Survey from Sebewaing to limestone FIGURES INCLUDING TWO COLORED MAPS quarries.................................................................. 23 PUBLISHED BY AUTHORITY OF THE LAWS OF (c 5) Survey from Sebewaing to Kilmanagh, and MICHIGAN Caseville. ..............................................................