Changing Interpretations of Kentucky Geologv- Laver-Cake, Facies, Flexure, and Eustacy

Total Page:16

File Type:pdf, Size:1020Kb

Changing Interpretations of Kentucky Geologv- Laver-Cake, Facies, Flexure, and Eustacy MISCELLANEOUS REPORT NO. 5 CHANGING INTERPRETATIONS OF KENTUCKY GEOLOGV- LAVER-CAKE, FACIES, FLEXURE, AND EUSTACY edited by Frank R. Ettensohn .:·· •-- prepared for the 1992 Annual Meeting of the Geological Society of America DIVISION OF GEOLOGICAL SURVEY 4383 FOUNTAIN SQUARE DRIVE COLUMBUS, OHIO 43224-1362 (614) 265-6576 (Voice) llesrurces (614) 265-6994 (TDD) (614) 447-1918 (FAX) OHIO GEOLOGY ADVISORY COUNCIL Dr. E. Scott Bair, representing Hydrogeology Mr. Mark R. Rowland, representing Environmental Geology Dr. J. Barry Maynard, representing At-Large Citizens Dr. Lon C. Ruedisili, representing Higher Education Mr. Michael T. Puskarich, representing Coal Mr. Gary W. Sitler, representing Oil and Gas Mr. Robert A. Wilkinson, representing Industrial Minerals SCIENTIFIC AND TECHNICAL STAFF OF THE DIVISION OF GEOLOGICAL SURVEY ADMINISTRATION (614) 265-6576 Thomas M. Berg, MS, State Geologist and Division Chief Robert G. Van Hom, MS, Assistant State Geologist and Assistant Division Chief Michael C. Hansen, PhD, Senior Geologist, Ohio Geology Editor, and Geohazards Officer James M. Miller, BA, Fiscal Officer Sharon L. Stone, AD, Executive Secretary REGIONAL GEOLOGY SECTION (614) 265-6597 TECHNICAL PUBLICATIONS SECTION (614) 265-6593 Dennis N. Hull, MS, Geologist Manager and Section Head Merrianne Hackathorn, MS, Geologist and Editor Jean M. Lesher, Typesetting and Printing Technician Paleozoic Geology and Mapping Subsection (614) 265-6473 Edward V. Kuehnle, BA, Cartographer Edward Mac Swinford, MS, Geologist Supervisor Michael R. Lester, BS, Cartographer Glenn E. Larsen, MS, Geologist Robert L. Stewart, Cartographer Gregory A. Schumacher, MS, Geologist Lisa Van Doren, BA, Cartographer Douglas L. Shrake, MS, Geologist Ernie R. Slucher, MS, Geologist PUBLICATIONS CENTER (614) 265-6605 Quaternary Geology and Mapping Subsection (614) 265-6599 Garry E. Yates, NZCS, Public Information Officer and Acting Section Head Richard R. Pavey, MS, Geologist Supervisor Inaleigh E. Eisen, Public Inquiries Assistant C. Scott Brockman, MS, Geologist Donna M. Schrappe, Public Inquiries Assistant Billie Long, Account Clerk Core Drilling Subsection (614) 265-6594 Douglas L. Crowell, MS, Geologist Supervisor MINERAL RESOURCES AND GEOCHEMISTRY SECTION Roy T. Dawson, Driller (614) 265-6602 Michael J. Mitchell, Driller Mark E. Clary, Drilling Assistant David A. Stith, MS, Geologist Supervisor and Section Head William R. Dunfee, Drilling Assistant Allan G. Axon, PhD, Geologist Richard W. Carlton, PhD, Senior Geologist SUBSURFACE STRATIGRAPHY AND PETROLEUM GEOLOGY Norman F. Knapp, PhD, Chemical Laboratory Supervisor SECTION (614) 265-6585 Sherry L. Weisgarber, MS, Geologist and Mineral Statistician Kim E. Vorbau, BS, Geologist Ronald G. Rea, MS, Geologist Supervisor and Section Head Mark T. Baranoski, MS, Geologist LAKE ERIE GEOLOGY SECTION (419) 626-4296 James McDonald, MS, Geologist Ronald A. Riley, MS, Geologist Scudder D. Mackey, PhD, Geologist Supervisor and Section Head Lawrence H. Wickstrom, MS, Senior Geologist and Computer Coordinator Danielle A. Foye, BS, Geology Technician Angelena M. Bailey, Administrative Assistant Jonathan A. Fuller, MS, Geologist Donald E. Guy, Jr., MS, Geologist Samples and Records Dale L. Liebenthal, Operations Officer & Research Vessel Operator Garry E. Yates, NZCS, Environmental Technology Supervisor Mary Lou McGurk, Office Assistant An Equal Opportunity Employer - M/F/H r STATE OF OHIO George V. Voinovich, Governor DEPARTMENT OF NATURAL RESOURCES Frances S. Buchholzer, Director DIVISION OF GEOLOGICAL SURVEY Thomas M. Berg, Chief MISCELLANEOUS REPORT NO. 5 CHANGING INTERPRETATIONS OF KENTUCKY GEOLOGY- LAYER-CAKE, -FACIES, FLEXURE, AND EUSTACY edited by_ Frank R. Ettensohn University of Kentucky with contributions by Stephen F. Barnett Stephen F. Greb Bryan College Kentucky Geological SuNey Dayton, Tennessee R. Thomas Lierman Donald R. Chesnut, Jr. Morehead State University Kentucky Geological SuNey Charles E. Mason Cortland F. Eble Morehead State University Kentucky Geological SuNey Frank R. Ettensohn Jack C. Pashin University of Kentucky Alabama Geological SuNey Peter T. Goodmann Gregory A. Schumacher University of Kentucky Ohio Geological SuNey Field Trip 15 for the Annual Meeting of the Geological Society of America Cincinnati, Ohio October 26-29, 1992 Centennial Field Trip of the University of Kentucky Department of Geological Sciences Columbus 1992 Cover illustration: Road cut on I-75 near Mt. Vernon, Kentucky, exposing 250 feet of Carboniferous section; Day 1, Stop 5. The lower 190 feet shows three unconformity- bound sequences of Mississippian carbonates in the Slade Formation. The upper 60 feet shows major slumping and deformation in the lower part of the Pennsylvanian Breathitt Formation, possibly related to movement on nearby structures. The Mississippian-Pennsylvanian unconformity is present on top of the third bench. TABLE OF CONTENTS INTRODUCTION ................................ , . -" . 1 PHYSIOGRAPHY ALONG FIELD-TRIP ROUTE . 2 STRUCTURAL FRAMEWORK OF KENTUCKY ........................................·. 6 IAPETAN RIFT . 6 UPLIFTS AND BASINS .... : . 9 APPALACHIAN BASINS....................................................... 9 BASIC FLEXURAL MODELS ............................... : . 9 SEDIMENTARY-STRATIGRAPHIC RESPONSE ...................................... 10 Unconformity Development . 1 O Foreland-Basin Subsidence . 10 Loading-Type Relaxation . 12 Unloading-Type Relaxation . 12 OVERVIEW .....................................- ........................... 12 PALEOZOIC SUBSIDENCE HISTORY OF APPALACHIAN BASIN IN KENTUCKY . 12 INTRODUCTION . 12 METHODS ................... ··............................................. 15 RESULTS AND DISCUSSION ................................................... 15 lapetan Extension . 15 Blountian-Taconian ..........· .............................................. 17 Salinic (?) ................................................................ 17 Acadian ................................................................ 17 Alleghanian . 19 CONCLUSIONS . .. 19 ORDOVICIAN PALEOGEOGRAPHIC AND TECTONIC FRAMEWORK FOR KENTUCKY ........... 19 DAY-ONE ROAD LOG AND STOP DESCRIPTIONS ...................................... 21 STOP 1. FAIRVIEW-KOPE CONTACT ................................................ 23 STOP 2A. CONTACT OF HIGH BRIDGE GROUP AND LEXINGTON LIMESTONE . 26 STOP 2B. CONTACTS BETWEEN THE CAMP NELSON, OREGON AND TYRONE FORMATIONS ... 28 STOP 2C. KENTUCKY RIVER FAULT SYSTEM AND THE CAMP NELSON LIMESTONE .......... 29 DEVONIAN PALEOGEOGRAPHIC AND TECTONIC FRAMEWORK FOR KENTUCKY ............. 32 MISSISSIPPIAN PALEOGEOGRAPHIC AND TECTONIC FRAMEWORK FOR KENTUCKY . 40 STOP 3. PORTWOOD MEMBER OF THE NEW ALBANY SHALE AND THE BOYLE DOLOSTONE . 42 REGIONAL STRUCTURE . 42 REGIONAL STRATIGRAPHY ...........................................•....... 42 LOCAL STRUCTURE ........................................... .': . 44 NORTH ROLLING FORK .............................. ; . 44 STOP 4. THE CARPENTER FORK GRABEN AND ITS IMPLICATIONS ....................... 44 DISCUSSION . 49 Previous Interpretations of Carpenter Fork Section ................................. 49 Origin of the Carpenter Fork Member . 49 Regional Implications ....................................' ..... : ............. 51 STOP 5. THE SLADE AND PARAGON FORMATIONS AND PENNSYLVANIAN SLUMPING ........ 56 DAY-TWO ROAD LOG AND STOP DESCRIPTIONS ............. -. 61 STOP 1. REGRESSIVE FACIES IN THE UPPER LEXINGTON LIMESTONE ...... .' ............. 62 STOP 2. KENTUCKY RIVER FAULT ZONE, THE LEXINGTON LIMESTONE AND CLAYS FERRY FORMATION NEAR THE SOUTHEASTERN MARGIN OF THE TANGLEWOOD BUILDUP ........ 66 OPTIONAL STOP. GRIER MEMBER AND VERTICAL GRIER-TANGLEWOOD TRANSITION ....... 69 OPTIONAL STOP. LATERAL GRIER-TANGLEWOOD TRANSITION AND IMPLICATIONS ......... 69 STOP 3. STRODE$ CREEK MEMBER, LEXINGTON LIMESTONE: PROBABLE SYNSEDIMENTARY STRUCTURAL INFLUENCE ............ , . , ...... ; ................ 71 STOP 4A. SILURIAN-DEVONIAN CONTACT AND TRANSGRESSIVE BLACK SHALES AT THE BASE OF THE OHIO SHALE ......................................... : ........... 74 STOP 4B. RE(;RESSIVE BLACK SHALES AND THE PROSTOSALV/NIA (FOERSTIA) ZONE . 76 STOP 5. CLEVELAND SHALE-THROUGH-LOWER BORDEN SEQUENCE ..............·. 77 OHIO SHALE (CLEVELAND SHALE MBR.) . 77 BEDFORD SHALE .................................. ; . 77 SUNBURY SHALE . 77 BORDEN FORMATION ....................................................... 80 Henley Bed .................................................. :· . 80 Farmers Member .......................................................... 80 Nancy Member ........................................................... 81 THE BEDFORD FAUNA ....................................................... 81 HISTORICAL AND REGIONAL FRAMEWORK ...................................... 82 STOP 6. PALEOSOLS AND RESTRICTED SLADE CARBONATES WEST OF THE WAVERLY ARCH APICAL ISLAND . 88 STRATIGRAPHY .......................................... : ................. 88 STRUCTURE .............................................................. 88 BARRIER-SHORELINE. MODEL ................................................. 92 TABULAR-EROSION MODEL . .. 97 PERRY BRANCH SECTION . 97 PENNSYLVANIAN PALEOGEOGRAPHIC, PALEOCLIMATIC AND TECTONIC FRAMEWORK FOR EASTERN KENTUCKY ........................................................ ; 100 PALEOGEOGRAPHIC POSITION AND CHANGING CLIMATES ..........................100 Tectonically Linked Basin Models ..............................................103 STRATIGRAPHIC
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
    [Show full text]
  • East and Central Farming and Forest Region and Atlantic Basin Diversified Farming Region: 12 Lrrs N and S
    East and Central Farming and Forest Region and Atlantic Basin Diversified Farming Region: 12 LRRs N and S Brad D. Lee and John M. Kabrick 12.1 Introduction snowfall occurs annually in the Ozark Highlands, the Springfield Plateau, and the St. Francois Knobs and Basins The central, unglaciated US east of the Great Plains to the MLRAs. In the southern half of the region, snowfall is Atlantic coast corresponds to the area covered by LRR N uncommon. (East and Central Farming and Forest Region) and S (Atlantic Basin Diversified Farming Region). These regions roughly correspond to the Interior Highlands, Interior Plains, 12.2.2 Physiography Appalachian Highlands, and the Northern Coastal Plains. The topography of this region ranges from broad, gently rolling plains to steep mountains. In the northern portion of 12.2 The Interior Highlands this region, much of the Springfield Plateau and the Ozark Highlands is a dissected plateau that includes gently rolling The Interior Highlands occur within the western portion of plains to steeply sloping hills with narrow valleys. Karst LRR N and includes seven MLRAs including the Ozark topography is common and the region has numerous sink- Highlands (116A), the Springfield Plateau (116B), the St. holes, caves, dry stream valleys, and springs. The region also Francois Knobs and Basins (116C), the Boston Mountains includes many scenic spring-fed rivers and streams con- (117), Arkansas Valley and Ridges (118A and 118B), and taining clear, cold water (Fig. 12.2). The elevation ranges the Ouachita Mountains (119). This region comprises from 90 m in the southeastern side of the region and rises to 176,000 km2 in southern Missouri, northern and western over 520 m on the Springfield Plateau in the western portion Arkansas, and eastern Oklahoma (Fig.
    [Show full text]
  • Geological Investigations in Ohio
    INFORMATION CIRCULAR NO. 21 GEOLOGICAL INVESTIGATIONS IN OHIO 1956 By Carolyn Farnsworth STATE OF OHIO C. William O'Neill, Governor DEPARTMENT OF NATURAL RESOURCES A. W. Marion, Director NATURAL RESOURCES COMMISSION Milton Ronsheim, Chairman John A. Slipher, Bryce Browning, Vice Chairman Secretary C. D. Blubaugh Dean L. L. Rummell Forrest G. Hall Dr. Myron T. Sturgeon A. W. Marion George Wenger DIVISION OF GEOLOGICAL SURVEY Ralph J. Bernhagen, Chief STATI OF OHIO DIPAlTMIMT 011 NATUlAL llSOUlCH DIVISION OF &EOLO&ICAL SURVEY INFORMATION CIRCULAR NO. 21 'GEOLOG·ICAL INVESTIGATIONS IN OHIO 1956 by CAROLYN FARNSWORTH COLUMBUS 1957 Blank Page CONTENTS Page Introduction 1 Project listing by author 2 Project listing by subject . 22 Economic geology 22 Aggregates . 22 Coal . • 22 Ground water 22 Iron .. 22 Oil and gas 22 Salt . 22 Sand and gravel 23 General .. 23 Geomorphology 23 Geophysics 23 Glacial geology 23 Mineralogy and petrology . 24 Clay .. 24 Coal . 24 Dolomite 24 Limestone. 24 Sandstone •• 24 Shale. 24 Till 25 Others 25 Paleontology. 25 Stratigraphy and sedimentation 26 Structural geology . 27 Miscellaneous . 27 Geographic distribution. 27 Statewide 27 Areal. \\ 28 County 29 Miscellaneous . 33 iii Blank Page I INTRODUCTION In September 1956, letters of inquiry and questionnaires were sent to all Ohio geologists on the mailing list of the Ohio Geological Survey, and to other persons who might be working on geological problems in Ohio. This publication has been compiled from the information contained on the returned forms. In most eases it is assumed that the projects listed herein will culminate in reports which will be available to the profession through scientific journals, government publications, or grad- uate school theses.
    [Show full text]
  • CONTROLS on DOLOMITIZATION of the UPPER ORDOVICIAN TRENTON LIMESTONE in SOUTH-CENTRAL KENTUCKY COLLIN JAMES GRAY Department Of
    CONTROLS ON DOLOMITIZATION OF THE UPPER ORDOVICIAN TRENTON LIMESTONE IN SOUTH-CENTRAL KENTUCKY COLLIN JAMES GRAY Department of Geological Sciences APPROVED: Dr. Katherine Giles, Ph.D., Chair Dr. Richard Langford, Ph.D. Dr. Matthew Johnston, Ph.D. Charles Ambler, Ph.D. Dean of the Graduate School Copyright © by Collin James Gray 2015 Dedication I dedicate my thesis work to my family. My dedicated and loving parents, Michael and Deborah Gray have always supported me and provided words of encouragement during the struggles of my research. The support provided was second to none and I could not imagine reaching this point in my education without them. I also dedicate this thesis to my two brothers, Michael and Nathan Gray and my sister Nicole Gray. Without these role models I cannot imagine where my education would have ended. I will always appreciate the support provided by all three of you and consider you to be role models that I can always look up to. CONTROLS ON DOLOMITIZATION OF THE UPPER ORDOVICIAN TRENTON LIMESTONE IN SOUTH-CENTRAL KENTUCKY by COLLIN JAMES GRAY, B.S. GEOLOGY THESIS Presented to the Faculty of the Graduate School of The University of Texas at El Paso in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE Department of Geological Sciences THE UNIVERSITY OF TEXAS AT EL PASO December 2015 Acknowledgements I wish to thank my committee whose time and expertise provided excellent input into my research. Dr. Katherine Giles, my M.S. supervisor provided guidance and provided endless suggestions and recommendations throughout my research while continuously motivating me to continue my education.
    [Show full text]
  • Geologic Cross Section
    Geologic Cross Section I–I′ Through the Appalachian Basin from the Eastern Margin of the Illinois Basin, Jefferson County, Kentucky, to the Valley and Ridge Province, Scott County, Virginia By Robert T. Ryder, Michael H. Trippi, and Christopher S. Swezey Pamphlet B to accompany Scientific Investigations Map 3343 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2015 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/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copy- righted items must be secured from the copyright owner. Suggested citation: Ryder, R.T., Trippi, M.H., and Swezey, C.S., 2015, Geologic cross section I–I′ through the Appalachian basin from the eastern margin of the Illinois basin, Jefferson County, Kentucky, to the Valley and Ridge province, Scott County, Virginia: U.S. Geological Survey Scientific Investigations Map 3343, 2 sheets and pamphlet A, 41 p.; pamphlet B, 102 p., http://dx.doi.org/10.3133/sim3343.
    [Show full text]
  • IGS 2015B-Maquoketa Group
    ,QGLDQD*HRORJLFDO6XUYH\ $ERXW8V_,*66WDII_6LWH0DS_6LJQ,Q ,*6:HEVLWHIGS Website Search ,1',$1$ *(2/2*,&$/6859(< +20( *HQHUDO*HRORJ\ (QHUJ\ 0LQHUDO5HVRXUFHV :DWHUDQG(QYLURQPHQW *HRORJLFDO+D]DUGV 0DSVDQG'DWD (GXFDWLRQDO5HVRXUFHV 5HVHDUFK ,QGLDQD*HRORJLF1DPHV,QIRUPDWLRQ6\VWHP'HWDLOV 9LHZ&DUW 7ZHHW *1,6 0$482.(7$*5283 $ERXWWKH,*1,6 $JH 6HDUFKIRUD7HUP 2UGRYLFLDQ 6WUDWLJUDSKLF&KDUW 7\SHGHVLJQDWLRQ 7\SHORFDOLW\7KH0DTXRNHWD6KDOHZDVQDPHGE\:KLWH S IRUH[SRVXUHVRIEOXHDQGEURZQVKDOH 025(,*65(6285&(6 WKDWDJJUHJDWHIW P LQWKLFNQHVVDORQJWKH/LWWOH0DTXRNHWD5LYHULQ'XEXTXH&RXQW\,RZD *UD\DQG6KDYHU 5HODWHG%RRNVWRUH,WHPV +LVWRU\RIXVDJH 6LQFHLWVILUVWXVHWKHWHUPKDVVSUHDGJUDGXDOO\HDVWZDUGLQWKHSURFHVVEHFRPLQJDJURXSWKDWHPEUDFHVVHYHUDO IRUPDWLRQV *UD\DQG6KDYHU ,WLVQRZXVHGWKURXJKRXW,OOLQRLV :LOOPDQDQG%XVFKEDFKS ZDV H[WHQGHGLQWRQRUWKZHVWHUQ,QGLDQDE\*XWVWDGW DQGZDVDGRSWHGIRUXVHLQDJURXSVHQVHWKURXJKRXW,QGLDQD 5(/$7('6,7(6 E\*UD\ *UD\DQG6KDYHU 86*6*(2/(; 'HVFULSWLRQ 1RUWK$PHULFDQ6WUDWLJUDSKLF $VGHVFULEHGE\*UD\ WKH0DTXRNHWD*URXSLQ,QGLDQDLVDZHVWZDUGWKLQQLQJZHGJHIW P WKLFNLQ &RGH VRXWKHDVWHUQ,QGLDQDDQGIW P WKLFNLQQRUWKZHVWHUQ,QGLDQD *UD\DQG6KDYHU ,WFRQVLVWVSULQFLSDOO\RI $$3*&2681$&KDUW VKDOH DERXWSHUFHQW OLPHVWRQHFRQWHQWLVPLQLPDOWKURXJKRXWPRVWRI,QGLDQDEXWLQFUHDVHVSURPLQHQWO\LQWKH VRXWKHDVWVRWKDWSDUWVRIWKHJURXSDUHLQSODFHVGRPLQDQWO\OLPHVWRQH *UD\DQG6KDYHU 7KHORZHUSDUWRIWKH JURXSLVHYHU\ZKHUHDOPRVWHQWLUHO\VKDOHDQGWKHORZHUSDUWRIWKHVKDOHLVGDUNEURZQWRQHDUO\EODFN *UD\DQG 6KDYHU $VDFRQVHTXHQFHRIWKLVSDWWHUQRIURFNGLVWULEXWLRQWZRVFKHPHVRIQRPHQFODWXUHDUHXVHGLQVXEGLYLVLRQRIWKH 0DTXRNHWD*URXSLQ,QGLDQD
    [Show full text]
  • Palisades Trolley Trail & Foundry Trestle Bridge Feasibility
    Appendix 5b December 2019 Palisades Trolley Trail & Foundry Trestle Bridge Feasibility Study Public Meeting Summary Report: Public Meeting #2 Contract No. DCKA-2017-T-0059 Category: L – Bicycle and Pedestrian Studies, Planning & Design Prepared for: District Department of Transportation 55 M Street, SE Suite 400 Washington, DC 20003 Prepared by: Commun-ET, LLC and Kittelson & Associates, Inc. Palisades Trolley Trail& Foundry Trestle Bridge P u b l i c M e e t i n g R e p o r t : Public Meeting #2 P a g e 1 | DRAFT 10/30/19 Table of Contents 1.0 Project Background ..................................................................................................... 3 2.0 Purpose of Public Meeting #2 ...................................................................................... 4 3.0 Public Meeting Location & Notifications ...................................................................... 4 3.1. Public Input Outreach Format & Comment Period… ……………………………………………………………5 4.0 Public Meeting Format & Summary ............................................................................. 6 4.1. Meeting Attendance & Survey Data Obtained………………………………………………………………………7 4.2. Information Station Meeting Process in Detail………………………………………………..……………………9 4.3. Exhibits & Presentations…………………………………………………………………………………………………….11 4.4. Written Comments Received at Public Meeting…………………………………………..…………………….12 4.4.1. Public Comments Captured at the Information Stations……………………………………..13 4.4.2. Title VI Comments Received from Public Meeting #2………………………………………….24
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Geological Controls on Stratigraphy and Sedimentation of the Mississippian Marshall Formation, Michigan Basin, U.S.A
    Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 8-2015 Geological Controls on Stratigraphy and Sedimentation of the Mississippian Marshall Formation, Michigan Basin, U.S.A. Joseph G. Adducci Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons, Geomorphology Commons, and the Sedimentology Commons Recommended Citation Adducci, Joseph G., "Geological Controls on Stratigraphy and Sedimentation of the Mississippian Marshall Formation, Michigan Basin, U.S.A." (2015). Master's Theses. 617. https://scholarworks.wmich.edu/masters_theses/617 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]. GEOLOGICAL CONTROLS ON STRATIGRAPHY AND SEDIMENTATION OF THE MISSISSIPPIAN MARSHALL FORMATION, MICHIGAN BASIN, U.S.A by Joseph G. Adducci A thesis Submitted to the Graduate College in partial fulfillment of the requirements for the degree of Master of Science Geosciences Western Michigan University August 2015 Thesis Committee: David A. Barnes, Ph.D. (Chair) William B. Harrison, III, Ph.D. Peter J. Voice, Ph.D. GEOLOGICAL CONTROLS ON STRATIGRAPHY AND SEDIMENTATION OF THE MISSISSIPPIAN MARSHALL FORMATION, MICHIGAN BASIN, U.S.A. Joseph G. Adducci, M.S. Western Michigan University, 2015 An understanding of regional orogenic, climatic, and eustatic processes is critical to the interbasinal correlation of Paleozoic strata in eastern North America. Tectonic activity associated with the culmination of Appalachian Orogenic events has been shown to have regional influence on paleostructure and sediment dispersal in the Appalachian foreland basin and adjacent intracratonic Illinois and Michigan basins.
    [Show full text]
  • The 'Great Unconformity' and Associated Geochemical Evidence
    JOURNAL OF CREATION 30(1) 2016 || PERSPECTIVES The ‘Great Unconformity’ and associated geochemical evidence for Noahic Flood erosion Harry Dickens he Bible’s Flood account describes Tthe greatest rain event ever recorded. Forty days and nights of rain falling on the earth (Genesis 7:12) would have caused immense denud­ ation of landmasses around the globe. Evi dence for this is provided by a key stratigraphic surface and by associated geochemical signatures. Nature and extent of the ‘Great Unconformity’ The term ‘Great Unconformity’ was originally used to describe the prominent stratigraphic surface exposed in the Grand Canyon that separates the Lower Cambrian Tapeats Sandstone (of the Sauk cratonic sequence) from the underlying Precambrian strata (Granite Gorge Metamorphic Suite and tilted sedimentary rocks of the Grand Canyon Supergroup).1 The Great Unconformity can be traced across North America and globally, including most of today’s southern hemisphere landmasses, along with Western Europe and Siberia—this makes it the “most widely recognised and distinctive stratigraphic surface in the rock record”.2 This surface in most regions separates continental crystalline base­ ment rock from overlying undeformed Cambrian marine fossil­bearing sedimentary rock. It thus records the onset of the denudation of continental 8 PERSPECTIVES || JOURNAL OF CREATION 30(1) 2016 Geochemical signatures consistent with continental denudation Numerous geochemical signatures indicative of continental denudation have been described from Upper Proterozoic strata.2,17
    [Show full text]
  • Description of the Hollidaysburg and Huntingdon Quadrangles
    DESCRIPTION OF THE HOLLIDAYSBURG AND HUNTINGDON QUADRANGLES By Charles Butts INTRODUCTION 1 BLUE RIDGE PROVINCE topography are therefore prominent ridges separated by deep SITUATION The Blue Ridge province, narrow at its north end in valleys, all trending northeastward. The Hollidaysburg and Huntingdon quadrangles are adjoin­ Virginia and Pennsylvania, is over 60 miles wide in North RELIEF ing areas in the south-central part of Pennsylvania, in Blair, Carolina. It is a rugged region of hills and ridges and deep, The lowest point in the quadrangles is at Huntingdon, Bedford, and Huntingdon Counties. (See fig. 1.) Taken as narrow valleys. The altitude of the higher summits in Vir­ where the altitude of the river bed is about 610 feet above sea ginia is 3,000 to 5,700 feet, and in western North Carolina 79 level, and the highest point is the southern extremity of Brush Mount Mitchell, 6,711 feet high, is the highest point east of Mountain, north of Hollidaysburg, which is 2,520 feet above the Mississippi River. Throughout its extent this province sea level. The extreme relief is thus 1,910 feet. The Alle­ stands up conspicuously above the bordering provinces, from gheny Front and Dunning, Short, Loop, Lock, Tussey, Ter­ each of which it is separated by a steep, broken, rugged front race, and Broadtop Mountains rise boldly 800 to 1,500 feet from 1,000 to 3,000 feet high. In Pennsylvania, however, above the valley bottoms in a distance of 1 to 2 miles and are South Mountain, the northeast end of the Blue Ridge, is less the dominating features of the landscape.
    [Show full text]