OHIO DEPARTMENTOF NATURAL RESOURCES DIVISION of GEOLOGICAL SURVEY Reference No

Total Page:16

File Type:pdf, Size:1020Kb

OHIO DEPARTMENTOF NATURAL RESOURCES DIVISION of GEOLOGICAL SURVEY Reference No STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Reference No. 24 Lawrence H. Wickstrom, Chfef Valley Pike VOCs EPA ID No. OHN000510489 Open-File Report 2012-1 GEOLOGY OF THE DAYTON REGION IN CORE AND OUTCROP-A WORKSHOP AND FIELD TRIP FOR CITIZENS, ENVIRONMENTAL INVESTIGATORS, GEOLOGISTS, AND EDUCATORS By Gregory A. Schumacher. Michael P. Angle, Brian E. Matt, and Douglas J. Aden Prepared for the 2012 Geological Society of America North-Central Section meeting in Dayton, Ohio Columbus 2012 DISCLAIMER The information contained herein has not been reviewed for technical accuracy and conformity with current ODNR Division of Geological Survey standards for formally published materials. The ODNR Division of Geological Survey docs not guarantee this information to be free from errors, omissions, or inaccuracies and disclaims any responsibility or liability for interpretations or decisions based thereon. Cover photo: Steam Boat Rock- Large slump block of Cedarville Dolomite resting in the bed of the Little Miami River at Clifton Gorge State Nature Preserve. Recommended citation: Schumacher, G.A.,Angle, M.P., Matt, B. E., and Aden, D.J., 2012, Geology of the Dayton region in core and outcrop- A workshop and field trip for citizens, environmental investigators, geologists, and educators: Ohio Department of Natural Resources, Division of Geological Survey Open-File Report 2012·1, 58 p. AGENDA MORNING WORKSHOP 9:00-10:00 A.M. Welcome; Geology of the Dayton Region 10:00-11:00 A.M. Utility of ODNR Division of Geological Survey map products 11:00-12:00 l'.l\1. Geology of the Dayton Region in core (hands-on exercises) AFTERNOON FIELD TRIP 1:00 I'.M. Depart Dayton Convention Center 1:00-1:30 P.M. Drive to Oakes Quarry Park 1:30-2:50 l'.l\1. STOP 1: Oakes Quarry Park 2:50- 3:00 I'.M. Drive to Clifton Gorge State Nature Preserve 3:00-4:20 P.l\1. STOP 2: Clifton Gorge State Nature Preserve 4:20-5:00 P.M. Fill out evaluations; return to Dayton Convention Center WORKSHOP AND FIELD TRIP LEADERS Gregory A. Schumacher Ohio Department of Natural Resources Division of Geological Survey H. R. Collins Laboratory 33307 South Old State Road Delaware, OH 43015 (740) 548-7348, ext. 125 greg.schu [email protected] tc .oh. us Michael P. Angle Ohio Department of Natural Resources Division of Geological Survey 2045 Morse Road, Bldg. C-2 Columbus, OH 43229-6693 (614) 265-6602 [email protected] Brian E. Matt DLZOhio 6121 Huntley Road Columbus, OH 43229 (614) 848-4141 [email protected] Douglas J. Aden Ohio Department of Natural Resources Division of Geological Survey 2045 Morse Road, Bldg. C-2 Columbus, OH 43229-6693 (614) 265-6579 doug.aden@dnr. statc. oh .us iii CONTENTS Page Introduction .. +••·• · ··~~····~·-·~·-....9·· ·····•r• .. ·······························································,·••••·•··· ..· ··········· 1 Geology of the Dayton region .................... .............. ...... .. .. ............. .. ............................... ..... 1 What geologic maps should I usc to determine the geology bencnth my feot? .................. 5 What is rock coring?.............................................................................................................. 5 Fi{lld trip road log .. .. ... .............. ... .. .. .. .. ... .. .. .. .. .. ... .. .. ... .. ........... .. ....... .•.. ... .. ........ ........... ... .. .. 7 Stop 1. Oakes Quarry Park .................................................................................................. 8 Introduction ~ ......................................................... ~ ........... ~ .......... ............... ~~ · ······ · ... ········... ·····....................... 8 Geology of the Oakes Qunrry Park............................................................................... 8 Early Silurian ..............................................................................H.. ....................... 8 Ice· Age ........ ............................................ .................. ~ .................~ ........ ~ .................... ,. ..................... ~-· · ·~ · .... ... ~ . ...... 12 Stop 2. Clifton Gorge State Nature Pr,cscrve ...................................................................... 14 Acknowledgments................................................................................................................. 17 References cited ......................... ....... .. ...... ..... ...... .. ....... ........................................................ 17 Fact Shoots........................................................................................................................... 18 Glacial till....................................................................................................................... 18 Glacial sand and gravel deposits .................................................................................. 20 Glocial sand deposits..................................................................................................... 23 Glocinl lacustrine d~posits ..................... ....................................................................... 26 Glacial silt deposits........................................................................................................ 29 Glocial clny deposits ............................................... -..................................................... 32 Orgnnic deposits....................................................................................... ..................... 35 Cedarville )){)lomite................................ ................................................ .. ..................... 38 Springfield Dolomite.................. ....... .. .................................................... .. .............. ....... 40 Euphemia Dolomite.......................... .. .................................................. .. ....... .... ............ 42 Mosaic Shale ... ... ... .. .. .. ......... ...... ......... ...... ...................... ....... ............. .... ..... .. .. ... .. .. .. ..... 44 Ost:<~od. Shale.......................................................................... ............................. .. .. ....... 46 Brassfield Formation ......... .......................................................... ,................................. 48 Drn.kcs Formation.......... ................................................................................................ 51 Whjtcwater Fonnation .................................................................................................. 53 Ljbcrty Formlltion.............. .. .. ... .. ..... ... ... ... .. ...... .. ... ........ .... ... .. .. .. .. .. .. .. .. .. .. .. .. .. 55 \Ynyncsville Formation............................................................. ............................... .... .. 57 FIGURES 1. Bedrock ncar-surface nnd subsurface stratigraphy of the Dayton region................. 2 2. Location of the Dayton region in Ordovician time...................................................... 3 3. Ohio karst areas............................................................................................................ 4 4. Typical drill bits ..............- ............................................................................................ 6 5. Bedrock geologic map of Oakes Quarry Pn rk.... ... .. ..... ............. ...... .. .. ..... .................... 9 6. The eastern high wall of Oakes Quarry Park displaying tbe chnractcristk limostonc of the Brnssficld Formation....................................................................................... 10 7. BclfastMemb~rofthe Brassfield Formation in Oakce Queny Park floor ................ 10 8. Ros<~ diagram illustrating the prominent joint orientations prca-crvcd within the Dclfn.st Member of the Brassfie]d Formation ........................, .................................. 11 9. Postulated position of the continents during tbc Late Ordovician!Enrly Silurien and Middle Pennsylvanian........................................................................................ 11 10. The polished upper surface of the Brassfield Formation............................................ 13 11. Rose diagram showing that the movement of glacial icc and meltwater was from the northwest to the southeast........................................................................................ 13 12. Bedrock geologic map of the Clifton Gorge State Nature Preserve ........................... 15 13. Stages of gorge formation of Little Miami River in the Clifton, Ohio, area .............. 16 iv GEOLOGY OFTHE DAYTON REGION IN CORE AND OUTCROP-A WORKSHOP AND FIELD TRIP FOR CITIZENS, ENVIRONMENTAL INVESTIGATORS, GEOLOGISTS, AND EDUCATORS by Gregory A. Schumacher, Michael P. Angle. Brian E. Mott, and Douglas J. Aden INTRODUCTION distinguish one geologic unit from the underlying and overly­ ing units. For example, if you turn ahead to the Brassfield The goal of today's core workshop and field trip is to Formation fact sheet (p. 48), you will find an introductory learn about the geology of the Dayton, Ohio, region using paragraph describing: (1) the characteristic rock or rocks Ohio Department of Natural Resources (ODNR), Division found in the Brassfield, (2) the environment present in the of Geological Survey (Survey) mapping products and indi· Dayton region when the Brassfield was deposited, (3) how vidual fact sheets for a future field guide entitled: Ohio's the Brassfield was named, (4) the Brassfield's mapped
Recommended publications
  • Bedrock Stress Release Features on Manitoulin Island, Ontario Formes De Relâchement De Contrainte Dans La Roche En Place, À L’Île Manitoulin, En Ontario Paul F
    Document generated on 09/30/2021 7:02 a.m. Géographie physique et Quaternaire Bedrock Stress Release Features on Manitoulin Island, Ontario Formes de relâchement de contrainte dans la roche en place, à l’île Manitoulin, en Ontario Paul F. Karrow La néotectonique de la région des Grands Lacs Article abstract Neotectonics of the Great Lakes area Manitoulin Island has large exposed bedrock plains underlain by Ordovician Volume 47, Number 3, 1993 and Silurian carbonates. The generally flat-lying strata reveal evidence of rock stress reiased by faults at Little Current and by pop-ups elsewhere. Four URI: https://id.erudit.org/iderudit/032966ar pop-ups occur at widely separated localities on the island and several other DOI: https://doi.org/10.7202/032966ar small ridges may be pop-ups. Other bedrock stress-release features may be present but remain undiscovered in the extensively vegetated part of the island. See table of contents Publisher(s) Les Presses de l'Université de Montréal ISSN 0705-7199 (print) 1492-143X (digital) Explore this journal Cite this note Karrow, P. F. (1993). Bedrock Stress Release Features on Manitoulin Island, Ontario. Géographie physique et Quaternaire, 47(3), 389–393. https://doi.org/10.7202/032966ar Tous droits réservés © Les Presses de l'Université de Montréal, 1993 This document is protected by copyright law. Use of the services of Érudit (including reproduction) is subject to its terms and conditions, which can be viewed online. https://apropos.erudit.org/en/users/policy-on-use/ This article is disseminated and preserved by Érudit. Érudit is a non-profit inter-university consortium of the Université de Montréal, Université Laval, and the Université du Québec à Montréal.
    [Show full text]
  • Chapter 1. Natural History
    CHAPTER 1. NATURAL HISTORY CHAPTER 1. NATURAL HISTORY —THE WILDERNESS THAT GREETED THE FIRST SETTLERS The land one sees today traveling through northern Ohio took gone. Thus, some 14,000 years ago as the last glacier receded millions of years to form. We can see evidence of tropical sea into the Lake Erie basin, the first Native Americans arrived and reefs on the Lake Erie Islands and deep ocean sediments here in began to utilize the natural resources that these natural processes the cliffs of the Black River. Ohio was just south of the equator had produced. at that time, some 350 million years ago, and over the millennia The natural history of Sheffield encompasses all those natural has migrated northward to its present position. Mountain features and processes of the environment that greeted the Native building to the east eventually raised the sea floor from under Americans, and later the pioneers, when they first arrived in the waves and erosion by streams, and later glacial ice, began Sheffield. To be sure, the landscape was a magnificent wilderness to sculpture the land. At the same time plants and animals were to the settlers, but it needed to be “tamed” in order to support evolving and began to populate the new land once the ice was the newcomers. Ice formation on the shale bluff of the Black River north of Garfield Bridge (2005). 1 BICENTENNIAL HISTORY OF SHEFFIELD TOPOGRAPHY Regional Physiography The topography of an area is the configuration of the land Physiography refers to the physical features or landforms of surface, including its relief [vertical differences in elevation of a region.
    [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]
  • Middle Devonian Formations in the Subsurface of Northwestern Ohio
    STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Horace R. Collins, Chief Report of Investigations No. 78 MIDDLE DEVONIAN FORMATIONS IN THE SUBSURFACE OF NORTHWESTERN OHIO by A. Janssens Columbus 1970 SCIENTIFIC AND TECHNICAL STAFF OF THE OHIO DIVISION OF GEOLOGICAL SURVEY ADMINISTRATIVE SECTION Horace R. Collins, State Geologist and Di v ision Chief David K. Webb, Jr., Geologist and Assistant Chief Eleanor J. Hyle, Secretary Jean S. Brown, Geologist and Editor Pauline Smyth, Geologist Betty B. Baber, Geologist REGIONAL GEOLOGY SECTION SUBSURFACE GEOLOGY SECTION Richard A. Struble, Geologist and Section Head William J. Buschman, Jr., Geologist and Section Head Richard M. Delong, Geologist Michael J. Clifford, Geologist G. William Kalb, Geochemist Adriaan J anssens, Geologist Douglas L. Kohout, Geologis t Frederick B. Safford, Geologist David A. Stith, Geologist Jam es Wooten, Geologist Aide Joel D. Vormelker, Geologist Aide Barbara J. Adams, Clerk· Typist B. Margalene Crammer, Clerk PUBLICATIONS SECTION LAKE ERIE SECTION Harold J. Fl inc, Cartographer and Section Head Charles E. Herdendorf, Geologist and Sectwn Head James A. Brown, Cartographer Lawrence L. Braidech, Geologist Donald R. Camburn, Cartovapher Walter R. Lemke, Boat Captain Philip J. Celnar, Cartographer David B. Gruet, Geologist Aide Jean J. Miller, Photocopy Composer Jean R. Ludwig, Clerk- Typist STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Horace R. Collins, Chief Report of Investigations No. 78 MIDDLE DEVONIAN FORMATIONS IN THE SUBSURFACE OF NORTHWESTERN OHIO by A. Janssens Columbus 1970 GEOLOGY SERVES OHIO CONTENTS Page Introduction . 1 Previous investigations .. .. .. .. .. .. .. .. .. 1 Study methods . 4 Detroit River Group . .. .. .. ... .. ... .. .. .. .. .. .. .. ... .. 6 Sylvania Sandstone ..........................
    [Show full text]
  • Waddle Ditch Rattlesnake Creek
    Nine-Element Nonpoint Source Implementation Strategy (NPS-IS) for Waddle Ditch-Rattlesnake Creek HUC-12 (05060003 03 05) Prepared for: Fayette Soil and Water Conservation District Prepared by: Civil & Environmental Consultants, Inc. Toledo, Ohio Version 1.0 Approved: June 29, 2021 This page intentionally left blank. Acknowledgements Version 1.0 prepared and written by: Deanna Bobak Civil & Environmental Consultants, Inc. 4841 Monroe Street, Suite 103 Toledo, OH 43623 Brigitte Hisey Fayette Soil & Water Conservation District 1415 US 22 SW, Suite 500 Washington Court House, OH 43160 The Fayette Soil & Water Conservation District (SWCD) would like to acknowledge the collaboration of multiple partners in the preparation of this Nonpoint Source Implementation Strategy (NPS-IS) for the Waddle Ditch-Rattlesnake Creek HUC-12 (05060003 03 05). The Fayette SWCD appreciates those individuals and organizations that contributed background information, insight into objectives and projects for inclusion in this NPS-IS. Thank you to Rick Wilson, Ohio Environmental Protection Agency – Division of Surface Water, for guidance throughout the NPS-IS development process, as well as Jessica D’Ambrosio and the staff of The Nature Conservancy for providing modeling data generated by the Agricultural Conservation Planning Framework (ACPF). This product or publication was financed in part or totally through a grant from the United States Environmental Protection Agency through an assistance agreement with the Ohio Environmental Protection Agency. The contents and views, including any opinions, findings, conclusions or recommendations, contained in this product or publication are those of the authors and have not been subject to any Ohio Environmental Protection Agency or United States Environmental Protection Agency peer or administrative review and may not necessarily reflect the views of the Ohio Environmental Protection Agency or the United States Environmental Protection Agency and no official endorsement should be inferred.
    [Show full text]
  • In the Supreme Court of Iowa ______
    IN THE SUPREME COURT OF IOWA _____________________________________________________________ Supreme Court No. 18-1199 _____________________________________________________________ ROY KARON, an individual, and, PEDDLER LLC, an Iowa Corporation, Plaintiffs-Appellants, v. JAMES MITCHELL, an individual, WYNN ELLIOTT, an individual, ELLIOTT AVIATION, a corporation, ELLIOTT AVIATION AIRCRAFT SALES, INC., a corporation, d/b/a ELLIOTTJETS, Defendants-Appellees. _____________________________________________________________ APPEAL FROM THE IOWA DISTRICT COURT FOR POLK COUNTY THE HONORABLE DAVID N. MAY _____________________________________________________________ APPELLANTS FINAL REPLY BRIEF _____________________________________________________________ Steven J. Crowley AT#0001845 Edward J. Prill AT#0012435 CROWLEY & PRILL 3012 Division Street Burlington, Iowa 52601 Phone: 319.753.1330 Fax: 319.752.3934 ELECTRONICALLY FILED FEB 13, 2019 CLERK OF SUPREME COURT Email: [email protected] [email protected] ATTORNEYS FOR PLAINTIFFS-APPELLANTS TABLE OF CONTENTS Table of Contents………………………………………………….... 2 Table of Authorities………………………………………………… 3 Statement of the Issues……………………………………………... 4 Argument …………………………………………………………... 11 I. The DISTRICT COURT ERRED BY APPLYING THE DACRES/PRIMA PAINT ANALYSIS BECAUSE IT IGNORED PRELIMINARY ISSUES ALLEGED IN THE PETITION…………………………………………………………... 11 A. The facts of this case make this dispute a tort issue rather than a contract issue………………………………….... 11 B. Due to the facts of this case, this dispute should
    [Show full text]
  • Songs of the Century
    Songs of the Century T. Austin Graham hat is the time, the season, the historical context of a popular song? When is it most present in the world, best able Wto reflect, participate in, or construct some larger social reality? This essay will consider a few possible answers, exploring the ways that a song can exist in something as brief as a passing moment and as broad as a century. It will also suggest that when we hear those songs whose times have been the longest, we might not be hearing “songs” at all. Most people are likely to have an intuitive sense for how a song can contract and swell in history, suited to a certain context but capable of finding any number of others. Consider, for example, the various uses to which Joan Didion is able to put music in her generation-defining essay “Slouching Towards Bethlehem,” a meditation on drifting youth and looming apocalypse in the days of the Haight-Ashbury counterculture. Songs create a powerful sense of time and place throughout the piece, with Didion nodding to the Grateful Dead, Jefferson Airplane, Quick- silver Messenger Service, and “No Milk Today” by Herman’s Hermits, “a song I heard every morning in the cold late spring of 1967 on KRFC, the Flower Power Station, San Francisco.”1 But the music that speaks most directly and reverberates most widely in the essay is “For What It’s Worth,” the Buffalo Springfield single whose chiming guitar fifths and famous chorus—“Stop, hey, what’s that sound / Everybody look what’s going down”—make it instantly recognizable nearly five decades later.2 To listen to “For What It’s Worth” on Didion’s pages is to hear a song that exists in many registers and seems able to suffuse everything, from a snatch of conversation, to a set of political convictions, to nothing less than “The ’60s” itself.
    [Show full text]
  • Bedrock and Surficial Geology in the Greater Belfast-Brooks Area, South-Central Maine
    Geological Society of Maine 2016 Summer Field Trip Bedrock and surficial geology in the greater Belfast-Brooks area, south-central Maine David P. West, Jr. Middlebury College Woodrow B. Thompson Maine Geological Survey Roger LeB. Hooke University of Maine Stephen Pollock University of Southern Maine Field Trip Objective On this field trip we will highlight prominent bedrock and surficial features in the general area between Belfast and Brooks, Maine. Many of the individual stops visited will allow for observations of features related to both the bedrock geologic history (hundreds of millions of years old), and the much more recent glacial history (tens of thousands of years old). The bedrock portion of the trip will provide opportunities to observe representative units within four major tectonic terranes that are juxtaposed in this region (St. Croix, Fredericton, Passagassawakeag, and Casco Bay belts). Additionally, aspects of the deformation, metamorphic, and plutonic history of the region will be examined. Finally, a spectacular traverse across the high strain portion of the regionally extensive Norumbega fault system will reveal a wide variety of fault rocks (e.g., mylonite, cataclasite, pseudotachylyte), and demonstrate a complex history of superimposed faulting. The glacial portion of the trip will include localities showing impressive glacial grooves revealing ice flow directions, erratic boulders eroded from till, a new glaciomarine delta exposure, and an esker pit. Additionally there will be stops that “ground-truth” the new stunning Lidar imagery in the area that has provided evidence of widespread removal of upland till by subglacial meltwater streams which, near the glacier margin, are associated with esker nets.
    [Show full text]
  • Waste Transfer Stations: a Manual for Decision-Making Acknowledgments
    Waste Transfer Stations: A Manual for Decision-Making Acknowledgments he Office of Solid Waste (OSW) would like to acknowledge and thank the members of the Solid Waste Association of North America Focus Group and the National Environmental Justice Advisory Council Waste Transfer Station Working Group for reviewing and providing comments on this draft document. We would also like to thank Keith Gordon of Weaver Boos & Gordon, Inc., for providing a technical Treview and donating several of the photographs included in this document. Acknowledgements i Contents Acknowledgments. i Introduction . 1 What Are Waste Transfer Stations?. 1 Why Are Waste Transfer Stations Needed?. 2 Why Use Waste Transfer Stations? . 3 Is a Transfer Station Right for Your Community? . 4 Planning and Siting a Transfer Station. 7 Types of Waste Accepted . 7 Unacceptable Wastes . 7 Public Versus Commercial Use . 8 Determining Transfer Station Size and Capacity . 8 Number and Sizing of Transfer Stations . 10 Future Expansion . 11 Site Selection . 11 Environmental Justice Considerations . 11 The Siting Process and Public Involvement . 11 Siting Criteria. 14 Exclusionary Siting Criteria . 14 Technical Siting Criteria. 15 Developing Community-Specific Criteria . 17 Applying the Committee’s Criteria . 18 Host Community Agreements. 18 Transfer Station Design and Operation . 21 Transfer Station Design . 21 How Will the Transfer Station Be Used? . 21 Site Design Plan . 21 Main Transfer Area Design. 22 Types of Vehicles That Use a Transfer Station . 23 Transfer Technology . 25 Transfer Station Operations. 27 Operations and Maintenance Plans. 27 Facility Operating Hours . 32 Interacting With the Public . 33 Waste Screening . 33 Emergency Situations . 34 Recordkeeping. 35 Environmental Issues.
    [Show full text]
  • The Geology of Ohio—The Precambrian
    No. 13 OHIOGeoFacts DEPARTMENT OF NATURAL RESOURCES • DIVISION OF GEOLOGICAL SURVEY THE GEOLOGY OF OHIO—THE PRECAMBRIAN Precambrian time (all of geologic time before the Cambrian Pe- million years ago a continent to the east collided with North America, riod) began when the Earth became a solid entity about 4.5 billion resulting in extensive crustal compression and development of a years ago and ended when the Cambrian Period began, about 570 mountain range that geologists call the Grenville Mountains. What million years ago. “Precambrian” is actually an informal term used is thought to be the zone of continental collision, known as a suture by geologists. This long period of time is divided formally into two zone, is located in eastern Ohio and is called the Coshocton Zone. eons—the Archeozoic (greater than 2.5 billion years ago) and the As these continents collided along a 3,000-mile-long line, stretch- Proterozoic (2.5 billion to 570 million years ago). Despite the immense ing perhaps from Sweden to Mexico, rocks were folded, twisted, span of time it represents, the Precambrian is the most poorly known metamorphosed, and thrust westward across part of the rift zone of the geologic subdivisions in Ohio, in part because Precambrian in western Ohio. This north-south-oriented, 30-mile-wide zone of rocks are nowhere exposed in the state. These primarily crystalline east-dipping, imbricated thrust slices is called the Grenville Front igneous and metamorphic rocks are deeply buried beneath younger Tectonic Zone and marks the westward limit of the Grenville Moun- Paleozoic sedimentary rocks at depths ranging from about 2,500 feet tains.
    [Show full text]
  • Ohio Division of Geological Survey Great Lakes Geologic Mapping Coalition Publications Updated March 2020
    Link to ODGS Publications Ohio Division of Geological Survey Great Lakes Geologic Mapping Coalition Publications Updated March 2020 2019 Aden, Douglas, 2019, Karst in the Lilley Formation, Peebles 7.5-minute quadrangle, Ohio, in Thorleifson, L. H., ed., Geologic Mapping Forum 2019 Abstracts: Minnesota Geological Survey Open-File Report 19-1, p. 4–5. Aden, D. J., 2019, Surficial geology of the Gnadenhutten quadrangle, Ohio: Columbus, Ohio Department of Natural Resources, Division of Geological Survey, Digital Map Series SG-4A, scale 1:24,000. Aden, D. J., 2019, Surficial geology of the New Philadelphia quadrangle, Ohio: Columbus, Ohio Department of Natural Resources, Division of Geological Survey, Digital Map Series SG-4A, scale 1:24,000. Aden, D. J., 2019, Surficial geology of the Tippecanoe quadrangle, Ohio: Columbus, Ohio Department of Natural Resources, Division of Geological Survey, Digital Map Series SG-4A, scale 1:24,000. Aden, D. J., 2019, Surficial geology of the Uhrichsville quadrangle, Ohio: Columbus, Ohio Department of Natural Resources, Division of Geological Survey, Digital Map Series SG-4A, scale 1:24,000. Aden, D. J., and Parrick, B. D., 2018, Karst of northern portions of the Peebles and Jaybird 7.5-minute quadrangles, Ohio: Columbus, Ohio Department of Natural Resources, Division of Geological Survey Open-File Report 2018-3, 40 p., 44 map tiles. Nash, T. A., 2019, Surficial geology of the Antrim quadrangle, Ohio: Columbus, Ohio Department of Natural Resources, Division of Geological Survey, Digital Map Series SG-4A, scale 1:24,000. Nash, T. A., 2019, Surficial geology of the Birmingham quadrangle, Ohio: Columbus, Ohio Department of Natural Resources, Division of Geological Survey, Digital Map Series SG-4A, scale 1:24,000.
    [Show full text]
  • Ethical Bedrock Under a Changing Negotiation Landscape Kevin Gibson Marquette University, [email protected]
    Marquette University e-Publications@Marquette Philosophy Faculty Research and Publications Philosophy, Department of 1-1-2017 Ethical Bedrock Under a Changing Negotiation Landscape Kevin Gibson Marquette University, [email protected] Published version. "Ethical Bedrock Under a Changing Negotiation Landscape," in The Negotiator's Desk Reference / Christopher Honeyman, Andrea Kupfer Schneider, editors Saint Paul, Minn. : DRI Press, [2017]: 493-502. Publisher link. © 2017 DRI Press. Used with permission. -----~------------- ------------------~----.--~~--~~~-~ 03 36 ro The Ethical Bedrock under the Negotiation Landscape Kevin Gibson Editors')\~ " ~vote· }'j d' what's Pas 'bl o~r zlemmas as a negotiator fall into two basic sets, ch~Pters in~. e? and "what's right?" The first is treated by many UJ~ztes about t~ b?ok. Here,from his philosopher's background, Gibson thznk more e zrif[uence ofmorality on negotiations, and how we can should bere cJe?rly ~bout what's the right thing to do. This chapter The .Moralitya .~n coTl)unction with Carrie M enkel-Meadow's chapter on 0 J Compromise. Ethics in N Negot· . egotiation b Iabona ~ckdrop th PProaches and personal attitudes vary widely and against a tnight think ~ promo~es bargaining as optimizing personal gains some 0nlybYth t~ at anythmg goes. However, individuals are constrained not shape oure reshold requirements oflaw but also by personal values that . l'he d. co.nd.uct at the negotiating table. It ProVid Isciphne of philosophy can help negotiators in two ways. First, frarnewo e~ a set of time-tested principles that give us the conceptual benchrna \ and language to assess our actions. Secondly, it gives us or difficu~ s of acceptable behavior, which are particularly useful in novel are a numbcases when the law may give little or no guidance.
    [Show full text]