Changes in Stratigraphic Nomenclature by the U.S. Geological Survey, 1971
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Geologic Storage Formation Classification: Understanding Its Importance and Impacts on CCS Opportunities in the United States
BEST PRACTICES for: Geologic Storage Formation Classification: Understanding Its Importance and Impacts on CCS Opportunities in the United States First Edition Disclaimer This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference therein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed therein do not necessarily state or reflect those of the United States Government or any agency thereof. Cover Photos—Credits for images shown on the cover are noted with the corresponding figures within this document. Geologic Storage Formation Classification: Understanding Its Importance and Impacts on CCS Opportunities in the United States September 2010 National Energy Technology Laboratory www.netl.doe.gov DOE/NETL-2010/1420 Table of Contents Table of Contents 5 Table of Contents Executive Summary ____________________________________________________________________________ 10 1.0 Introduction and Background -
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. -
Contents List of Illustrations LETTER OF
STATE OF MICHIGAN Plate IV. A. Horizontal and oblique lamination, Sylvania MICHIGAN GEOLOGICAL AND BIOLOGICAL SURVEY Sandstone......................................................................27 Plate IV. B. Stratification and lamination, in sand dune, Dune Publication 2. Geological Series 1. Park, Ind.........................................................................28 THE MONROE FORMATION OF SOUTHERN Plate V. Sand grains, enlarged 14½ times ............................31 MICHIGAN AND ADJOINING REGIONS Plate VI. Desert sand grains, enlarged 14½ times ................31 by Plate VII. Sylvania and St. Peter sand grains, enlarged 14½ A. W. Grabau and W. H. Sherzer times. .............................................................................32 PUBLISHED AS PART OF THE ANNUAL REPORT OF THE BOARD OF GEOLOGICAL AND BIOLOGICAL SURVEY FOR Figures 1909. Figure 1. Map showing distribution of Sylvania Sandstone. 25 LANSING, MICHIGAN WYNKOOP HALLENBECK CRAWFORD CO., STATE Figure 2. Cross bedding in Sylvania sandstone ....................27 PRINTERS Figure 3. Cross bedding on east wall of Toll’s Pit quarry ......28 1910 Figure 4. Cross bedding shown on south wall of Toll’s Pit quarry.............................................................................28 Contents Figure 5. Cross bedding on south wall of Toll’s Pit quarry in Sylvania sandstone. .......................................................28 Letter of Transmittal. ......................................................... 1 Figure 6. Cross bedding shown on south wall -
Kope Formation Disturbed
Types and Examples of Slides Glossary – Clay-rich deposits prone to failure, – Fine-grained laminated deposits of Landslides and board Backwater deposits Lake bed clays they are best developed south of the Ohio River. They occur clay and silt laid down in lakes dammed by ice during fences tilted, monuments tilted pulled apart in terraces at the mouths of tributaries to a larger stream the Pleistocene Epoch (Ice Age). They are exceptionally Your Property colluvium - soil where glacial outwash caused a temporary lake to form. unstable, even on gentle slopes. OH tension Bedrock – Term used by engineers and geologists when Lamination – A texture in soil or rock that is made up of Study curved tree Area trunks cracks, tilted referring to the Ordovician limestones and shales that very thin (a few millimeters to a centimeter) parallel layers IN pavement underlie soil everywhere in the area. The bedrock itself (see fig. 21). The layers may reflect an annual pattern of seldom fails, and so determining the depth to bedrock is a sedimentation. KY Kope Formation tilted guard key part of any site investigation. rails and Ordovician System – The set of rock formations that utility poles Bridging – Large rock fragments that interfere with proper make up the local bedrock. It consists of limestone and trace of compaction of finer fill material. shale that was deposited in an ancient ocean between 444 scarp and 488 million years ago. Colluvium – A clay-rich deposit derived from weathering of bedrock that has moved downslope by gravity from its – Sand and gravel deposits left from the flowing CREEP Outwash place of origin. -
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. -
Ordovician News 2005
ORDOVICIAN NEWS SUBCOMMISSION ON ORDOVICIAN STRATIGRAPHY INTERNATIONAL COMMISSION ON STRATIGRAPHY Nº 22 2005 ORDOVICIAN NEWS Nº 22 INTERNATIONAL UNION OF GEOLOGIAL SCIENCES President: ZHANG HONGREN (China) Vice-President: S. HALDORSEN (Norway) Secretary General: P. T. BOBROWSKI (Canada) Treasurer: A. BRAMBATI (Italy) Past-President: E.F.J. DE MULDER (The Netherlands) INTERNATIONAL COMMISSION ON STRATIGRAPHY Chairman: F. GRADSTEIN (Norway) Vice-Chairman: S. C. FINNEY (USA) Secretary General: J. OGG (USA) Past-Chairman: J. REMANE (Switzerland) INTERNATIONAL SUBCOMMISSION ON ORDOVICIAN STRATIGRAPHY Chairman: CHEN XU (China) Vice-Chairman: J. C. GUTIÉRREZ MARCO (Spain) Secretary: G. L. ALBANESI (Argentina) F. G. ACEÑOLAZA (Argentina) A. V. DRONOV (Russia) O. FATKA (Czech Republic) S. C. FINNEY (USA) R. A. FORTEY (UK) D. A. HARPER (Denmark) W. D. HUFF (USA) LI JUN (China) C. E. MITCHELL (USA) R. S. NICOLL (Australia) G. S. NOWLAN (Canada) A. W. OWEN (UK) F. PARIS (France) I. PERCIVAL (Australia) L. E. POPOV (Russia) M. R. SALTZMAN (USA) Copyright © IUGS 2005 i ORDOVICIAN NEWS Nº 22 CONTENTS Page NOTE FOR CONTRIBUTORS iii EDITOR'S NOTE iii CHAIRMAN´S AND SECRETARY´S ADDRESSES iii CHAIRMAN´S REPORT 1 SOS ANNUAL REPORT FOR 2001 1 INTERNATIONAL SYMPOSIA AND CONFERENCES 4 PROJECTS 7 SCIENTIFIC REPORTS 7 HONORARY NOTES 8 MISCELLANEA 9 CURRENT RESEARCH 9 RECENT ORDOVICIAN PUBLICATIONS 25 NAMES AND ADDRESS CHANGES 40 URL: http://www.ordovician.cn, http://seis.natsci.csulb.edu/ISOS Cover: The Wangjiawan GSSP for the base of the Hirnantian Stage, China. ii ORDOVICIAN NEWS Nº 22 NOTE FOR CONTRIBUTORS The continued health and survival of Ordovician News depends on YOU to send in items of Ordovician interest such as lists and reviews of recent publications, brief summaries of current research, notices of relevant local, national and international meetings, etc. -
Late Silurian Trilobite Palaeobiology And
LATE SILURIAN TRILOBITE PALAEOBIOLOGY AND BIODIVERSITY by ANDREW JAMES STOREY A thesis submitted to the University of Birmingham for the degree of DOCTOR OF PHILOSOPHY School of Geography, Earth and Environmental Sciences University of Birmingham February 2012 University of Birmingham Research Archive e-theses repository This unpublished thesis/dissertation is copyright of the author and/or third parties. The intellectual property rights of the author or third parties in respect of this work are as defined by The Copyright Designs and Patents Act 1988 or as modified by any successor legislation. Any use made of information contained in this thesis/dissertation must be in accordance with that legislation and must be properly acknowledged. Further distribution or reproduction in any format is prohibited without the permission of the copyright holder. ABSTRACT Trilobites from the Ludlow and Přídolí of England and Wales are described. A total of 15 families; 36 genera and 53 species are documented herein, including a new genus and seventeen new species; fourteen of which remain under open nomenclature. Most of the trilobites in the British late Silurian are restricted to the shelf, and predominantly occur in the Elton, Bringewood, Leintwardine, and Whitcliffe groups of Wales and the Welsh Borderland. The Elton to Whitcliffe groups represent a shallowing upwards sequence overall; each is characterised by a distinct lithofacies and fauna. The trilobites and brachiopods of the Coldwell Formation of the Lake District Basin are documented, and are comparable with faunas in the Swedish Colonus Shale and the Mottled Mudstones of North Wales. Ludlow trilobite associations, containing commonly co-occurring trilobite taxa, are defined for each palaeoenvironment. -
The Depositional History of the Point Pleasant Member of the Cynthiana Formation in Northern Kentucky
Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 12-1984 The Depositional History of the Point Pleasant Member of the Cynthiana Formation in Northern Kentucky Gary J. Stefaniak Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons Recommended Citation Stefaniak, Gary J., "The Depositional History of the Point Pleasant Member of the Cynthiana Formation in Northern Kentucky" (1984). Master's Theses. 1545. https://scholarworks.wmich.edu/masters_theses/1545 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. THE DEPOSITIONAL HISTORY OF THE POINT PLEASANT MEMBER OF THE CYNTHIANA FORMATION IN NORTHERN KENTUCKY by Gary J. Stefaniak A Thesis Submitted to the Faculty o f The Graduate College in partial fulfillm ent of the requirements for the Degree o f Master o f Science Department of Geology Western Michigan U niversity Kalamazoo, Michigan December 1984 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. THE DEPOSITIONAL HISTORY OF THE POINT PLEASANT MEMBER OF THE CYNTHIANA FORMATION IN NORTHERN KENTUCKY Gary J. Stefaniak, M.S. Western Michigan U nive rsity, 1984 Bioclastic limestones, siltstones, and shales of the Point Pleasant Member were deposited in a shallow marine environment immediately below normal e ffe c tiv e wave base. High-energy conditions produced by storms lowered the e ffe ctive wave base and s tirre d the bottom sediments and redistributed them into bedforms. -
Seismic Interpretation and Well Log Analysis of Jay County, Indiana, Focused on Lithologic Units Below the Mt
Wright State University CORE Scholar Browse all Theses and Dissertations Theses and Dissertations 2014 Seismic Interpretation and Well Log Analysis of Jay County, Indiana, Focused on Lithologic Units below the Mt. Simon Formation Jennifer Welder Wright State University Follow this and additional works at: https://corescholar.libraries.wright.edu/etd_all Part of the Earth Sciences Commons, and the Environmental Sciences Commons Repository Citation Welder, Jennifer, "Seismic Interpretation and Well Log Analysis of Jay County, Indiana, Focused on Lithologic Units below the Mt. Simon Formation" (2014). Browse all Theses and Dissertations. 1263. https://corescholar.libraries.wright.edu/etd_all/1263 This Thesis is brought to you for free and open access by the Theses and Dissertations at CORE Scholar. It has been accepted for inclusion in Browse all Theses and Dissertations by an authorized administrator of CORE Scholar. For more information, please contact [email protected]. Seismic Interpretation and Well Log Analysis of Jay County, Indiana, focused on lithologic units below the Mt. Simon Formation A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science By Jennifer Michelle Welder B.S., University of Cincinnati 2012 2014 Wright State University WRIGHT STATE UNIVERSITY GRADUATE SCHOOL Monday, January 5, 2015 I HEREBY RECOMMEND THAT THE THESIS PREPARED UNDER MY SUPERVISION BY Jennifer Michelle Welder ENTITLED Seismic Interpretation and Well Log Analysis of Jay County, Indiana, focused on lithologic units below the Mt. Simon Formation BE ACCEPTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF Master of Science. Ernest Hauser, Ph.D. Thesis Director David F. -
Silurian Rocks in the Subsurface of Northwestern Ohio
STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Horace R. Coli ins, Chief LIBRARJ BUREAU OF GEOLOGY TALLAHASSEE, FLORIDA Report of Investigations No. 100 SILURIAN ROCKS IN THE SUBSURFACE OF NORTHWESTERN OHIO by Adriaan Janssens Columbus 1977 SCIENTIFIC AND TECHNICAL STAFF 8DNRDEPARTMENT OF OF THE NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY ADMINISTRATION Horace R. Collins, MS, State Geologist and Division Chief Richard A. Struble, PhD, Geologist and Assistant Chief William J. Buschman, Jr., BS, Administrative Geologist Barbara J. Adams, Office Manager REGIONAL GEOLOGY SUBSURFACE GEOLOGY Robert G. Van Horn, MS, Geologist and Section Head Adriaan Janssens, PhD, Geologist and Section Head Richard W. Carlton, PhD, Geologist Charles R. Grapes II, BS, Geologist Michael L. Couchot, MS, Geologist Frank L. Majchszak, MS, Geologist Douglas L. Crowell, MS, Geologist James Wooten, Geology Technician Richard M. DeLong, MS, Geologist Garry E. Yates, Geology Technician Michael C. Hansen, MS, Geologist Linda C. Gearheart, Clerk Dennis N. Hull, MS, Geologist Brenda L. Rinderle, Office Machine Operator Michele L. Risser, BA , Geologist Joel D. Vormelker, MS, Geologist LAKE ERIE GEOCHEMISTRY LABORATORY Charles H. Carter, PhD, Geologist and Section Head D. Joe Benson, PhD, Geologist David A. Stith, MS, Geologist and Section Head Donald E. Guy, Jr., BA, Geologist George Botoman, MS, Geologist Dale L. Liebenthal, Boat Captain Norman F. Knapp, PhD, Chemist Thomas J. Feldkamp, BS, Geology Technician E. Lorraine Thomas, Laboratory Technician Marjorie L. VanVooren, Typist TECHNICAL PUBLICATIONS Jean Simmons Brown, MS, Geologist/Editor and Section Head Cartography Philip J. Celnar, BFA, Cartography Supervisor R. Anne Berry, BFA, Cartographer James A. Brown, Cartographer Donald R. -
Classification of the Koninckinacea
CLASSIFICATION OF THE KONINCKINACEA by ROBERT DENNIS STATON S.B., Massachusetts Institute of Technology (1960) SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE at the MASSACHUSETTS INSTITUTE OF TECHNOLOGY June, 1961 Signature of Author ...................... Department of Geology and Geophysics, May 20, 1961 Certified by .... ( Thesis Supervisor Accepted by . Chairman, Departmental Committee on Graduate Students -I ABSTRACT The brachiopod superfamily Athyracea Williams 1956 (=Rostrospiracea Schuchert & LeVene 1929) has been re- named Koninckinacea Davidson 1851-55 nom. trans. Boucot & Staton. Athyracea became void with the priority re- placement of the genus Athyris McCoy 1844 with a synonym, Cleiothyris Phillips 1841. According to Copenhagen nom- enclatural priority rules, the superfamily name should be elevated from the oldest group of suprageneric rank within the superfamily; that being, in this instance, the family Koninckinidae Davidson 1851-55. Correspondingly, the subfamily Athyrinae and family Athyridae have been renamed Cleiothyrinae and Cleiothyridae. Within the Cleiothyridae, a new sub- family, Tetractinellinae, has.been erected. The sub- family Diplospirellinae has been elevated to family rank, and within that family a new subfamily, Kayserinae, has been erected for the single Devonian genus Kayseria. The subfamily Camarophorellinae has been reassigned to the family Meristellidae. From with- in the latter, the subfamily Hindellinae has been reas- signed to the family Nucleospiridae. Fifty-two genera have been assigned to the super- family Koninckinacea and are described and classified within. A compilation of species assigned has been prepared for the lower paleozoic genera. Jugal pre- parations are diagrammatically figured for all genera for which this information is available. -
Iii Silurian Fauna
III SILURIAN FAUNA By AUGUST F. FOERSTE THE SILURIAN FAUNA OF KENTUCKY By AUGUST F. FOERSTE THE SOURCE AND AFFINITIES OF THE SILURIAN FAUNAS In prehistoric times the North American continent was invaded by oceanic faunas from various directions. The tilting of the continent toward the south permitted the invasion of oceanic faunas from the Gulf of Mexico, and tilting toward the east, permitted invasions from the North Atlantic. There have been invasions also from the Arctic and Pacific. Some of these invasions extended far inland. Some from the Gulf of Mexico spread northward along the Mississippi embayment as far as the southern part of Canada, and some from the North Atlantic reached Ohio and Kentucky. As far as known, none of the invasions from the Arctic or Pacific reached Kentucky. In most Silurian faunas, the brachiopod element predominates. Three of the southern invasions—the Brassfield, Osgood, and Waldron—are characterized by the abundance of bryozoans, in addition to the brachiopods. The Brassfield and Waldron contain also a considerable number of gastropods, pelecypods, cephalopods, and trilobites, all of which are relatively scarce in the Osgood and Louisville. In the Osgood, on the contrary, there are numerous cystids, though almost all of these were described originally under the single generic name Holocystites. The Waldron is characterized by the considerable variety of crinoids. In the Laurel and Louisville bryozoans are rare. The Laurel is now characterized by numerous species of crinoids, a considerable number of which show affinities with crinoids occurring in Gotland and England. Possibly these invaded the American continent from some North Atlantic source.