Environmental Problems and the Construction Aggregate Industry

Total Page:16

File Type:pdf, Size:1020Kb

Environmental Problems and the Construction Aggregate Industry State of Michigan ENVIRONMENTAL PROBLEMS AND Department of Natural Resources THE CONSTRUCTION AGGREGATE Geological Survey Division INDUSTRY Miscellany 1 Papers presented at Sixth Forum on Geology by William E. Hole, Jr., President of Industrial Minerals American Aggregate Company, Greenville, Ohio Theme II: BUILDING AND CONSTRUCTION STONES AND MINERALS Abstract Edited by The theme of the 70’s will be the environment. The W. A. Kneller construction aggregates industry, already in difficulty with local zoning control, will be further affected by the Cosponsored by requirements of the "new thing". However, it may well Department of Geology and Mineralogy, University of be that proposed legislation could be the vehicle which Michigan Department of Geology, University of Toledo not only satisfies the wants of the environmentalist but Convened at Horace H. Rackham Building also recognizes the need for a viable construction University of Michigan aggregates industry. Ann Arbor At the beginning of each new decade, wise men attempt April 2 and 3, 1970 to forecast the highlights of the upcoming ten years. In the past, there has been a lack of consensus upon the part of this honored group. However, there seems to be a general agreement upon the part of the Contents prognosticating community this year that the "Theme of THEME II: BUILDING AND CONSTRUCTION STONES the 70’s" will be the environment. AND MINERALS The actions of the Federal government generally reflect ENVIRONMENTAL PROBLEMS AND THE the concerns of the public body. Seldom has our CONSTRUCTION AGGREGATE INDUSTRY, William government realigned itself so dramatically as it has with E. Hole, Jr......................................................................... 1 respect to this particular appeal. The "white hats" in Washington today are those who champion this cause. POTENTIAL USE OF OHIO LIMESTONES AND DOLOMITES FOR ARCHITECTURAL AGGREGATE, In the past two years the Federal government has David A. Stith................................................................... 4 entered the fields of water and air pollution. There is pending before the Congress at this time a "Surface TRANSPORTATION ADVANTAGE -- A UNIFYING Mining Reclamation Act". With the enactment of this FACTOR IN MINERAL AGGREGATE VALUATION, P. legislation, the Federal government will be involved in P. Hudec, J. R. Dunn, and S. T. Brown.......................... 9 the control of air, water and land -- and this is the EVALUATION OF THREE GRAVEL SAMPLING environment. METHODS, Thomas A. Herbert.................................... 12 The construction aggregate industry is involved in all A STUDY OF THE SAND AND GRAVEL DEPOSITS three of these environmental areas. With respect to air OF THE MAUMEE RIVER ESTUARY, Charles E. and water pollution, however, the solutions are finite Herdendorf and Lawrence L. Braidech ....................... 19 and, although burdensome, should not threaten our existence. In the area of land environmental problems, a SLAG - MICHIGAN'S ALL-PURPOSE totally different situation exists for the extraction process CONSTRUCTION AGGREGATE, R. Thomas Segall... 24 is in direct conflict with the basic precepts of the RELATIONSHIPS BETWEEN PHYSICAL AND environmentalist. It is in this area that I wish to direct my CHEMICAL PROPERTIES OF THE BRASSFIELD remarks. LIMESTONE (SILURIAN) IN INDIANA, OHIO, AND The management of American Aggregates Corporation KENTUCKY, Donald D. Carr, Robert R. French, and has no quarrel with the basic objectives of the Robert F. Blakely........................................................... 32 environmentalists. It is our belief that it is each man’s THE CHALLENGE FOR THE GEOLOGIST IN THE duty to make this world a better place in which to live. EXTRACTIVE INDUSTRY, H. Lyn Bourne ................... 38 For the past fifty years our company has been recognized as the leader in the sand and gravel industry MICHIGAN'S CLAY DEPOSITS AND INDUSTRY, on the reclamation of worked-out lands. I should add Harry O. Sorensen......................................................... 41 that our "Project Parklands", the name we use to describe our reclamation efforts, is not purely motivated by our desire to be good neighbors. For over this period of fifty years we have found out that the reclamation business can be a profitable business. Miscellany 1, Theme II – Page 1 of 47 In most of the construction aggregate industries, this fact It is often said that "necessity is the mother of invention". should be true. Due to the heavy nature of our product, How true this statement is - and sometimes, I feel - how it is essential that production facilities be located as unfortunate. Let me illustrate. close as possible to the consuming market. Our people initially felt that we had run into a stone wall Transportation costs double the cost of our product to when we first encountered the "time" argument. An the user every twenty miles that the commodity must be analysis of the factual situation showed that historically hauled. Therefore, most producing plants are located operators in our industry have selected plant sites within metropolitan areas. (hopefully removed from existing nearby homes) and Due to the rapid urbanization of our country which will be then conducted the operations outbound from this site to further accelerated by the current population explosion, the boundaries of the properties. There seemed to be there exists a ready market for the lands excavated and no reason to consider any other mode of operation. properly reclaimed by the construction aggregate On the other hand, consider the situation enjoyed by the industry. neighbors. Initially, the operations are distant and Furthermore, lakeside residential lots command twice therefore seem to be relatively innocuous. However, the selling price per acre as lots located elsewhere. We every year the mining operations get closer and closer -- have a commercial development overlooking a large the neighbors become more and more unhappy as time lake in North Columbus, Ohio, where an acre lot to passes. It isn't until the operator has reached the limits accommodate the district office of a major oil company of the property, if he is that lucky, that he finally reclaims was sold for a price of $150,000. This payment the area which enhances the value of the adjoining represented twice the original cost of the total tract which properties. encompassed 150 acres. It should have been evident years ago that, considering It would be foolhardy to think that every reclamation the cost of working the whole property, the total cost of project will generate such rewards. But at some date in working the property was essentially the same whether the future, all projects will have greater value than if our the operator started at the plant and worked outbound or operations had not taken place. Furthermore, to be started at the perimeter and worked plantward. economic, reclamation must be done as an integral part Furthermore, I have already pointed out how valuable of the excavation process. So when active operations these lands become after: reclamation. Through have ceased, the land is completely rehabilitated. experience our company has learned that when working One might think that with such a record our company outbound we could not dispose of any reclaimed lands would have no problems obtaining from zoning boards until the whole operation was completed. If we worked the right to excavate on gravel-bearing lands which we from the perimeter inward, we could release reclaimed may purchase. This is not the case. lands as fast as we desired, thereby permitting our company to realize the potential value much sooner. When the public hears the words "sand and gravel", it does not think of "Project Parklands". Instead, it thinks Psychologists tell us that the human body can stand of all the abandoned pits which dot the countryside. intense pain as long as the individual knows that relief is Generally, we can convince the neighbors that when our not far away. On the other hand, that same body will operations are completed, their property values will be tolerate a much lower level of pain if the individual feels enhanced. But the word "when" suggests a time factor, that it is going to get worse. I feel that this description is and, as Shakespeare stated, "Aye there’s the rub". analogous to the relative effects upon the neighbor of the inbound and outbound operating techniques. In order to generate low-cost material for the construction market, one important factor is sufficient life As a result of our difficulties in obtaining neighborhood over which to amortize developmental and plant costs. acceptance and thereby the right from a local zoning At a minimum a ten-year life is necessary and a twenty- board to operate, we have changed out pit operating year life is preferable. procedures in such a way that we complete operations along our boundaries first. Because we have made this Those neighbors who recognize the future benefits to change, we can realize the potential gains in reclaimed their own property are generally unwilling to wait the 10 properties much sooner. to 20 years until such gains could be realized. So through the expedient of local politics, zoning boards are I am convinced that there are other changes in operating induced to refuse to grant the right to excavate procedures which could make our industry more construction materials. acceptable to the urban areas in which we must exist. Despite this fact, I am also convinced that, even if
Recommended publications
  • Stratigraphic Succession in Lower Peninsula of Michigan
    STRATIGRAPHIC DOMINANT LITHOLOGY ERA PERIOD EPOCHNORTHSTAGES AMERICANBasin Margin Basin Center MEMBER FORMATIONGROUP SUCCESSION IN LOWER Quaternary Pleistocene Glacial Drift PENINSULA Cenozoic Pleistocene OF MICHIGAN Mesozoic Jurassic ?Kimmeridgian? Ionia Sandstone Late Michigan Dept. of Environmental Quality Conemaugh Grand River Formation Geological Survey Division Late Harold Fitch, State Geologist Pennsylvanian and Saginaw Formation ?Pottsville? Michigan Basin Geological Society Early GEOL IN OG S IC A A B L N Parma Sandstone S A O G C I I H E C T I Y Bayport Limestone M Meramecian Grand Rapids Group 1936 Late Michigan Formation Stratigraphic Nomenclature Project Committee: Mississippian Dr. Paul A. Catacosinos, Co-chairman Mark S. Wollensak, Co-chairman Osagian Marshall Sandstone Principal Authors: Dr. Paul A. Catacosinos Early Kinderhookian Coldwater Shale Dr. William Harrison III Robert Reynolds Sunbury Shale Dr. Dave B.Westjohn Mark S. Wollensak Berea Sandstone Chautauquan Bedford Shale 2000 Late Antrim Shale Senecan Traverse Formation Traverse Limestone Traverse Group Erian Devonian Bell Shale Dundee Limestone Middle Lucas Formation Detroit River Group Amherstburg Form. Ulsterian Sylvania Sandstone Bois Blanc Formation Garden Island Formation Early Bass Islands Dolomite Sand Salina G Unit Paleozoic Glacial Clay or Silt Late Cayugan Salina F Unit Till/Gravel Salina E Unit Salina D Unit Limestone Salina C Shale Salina Group Salina B Unit Sandy Limestone Salina A-2 Carbonate Silurian Salina A-2 Evaporite Shaley Limestone Ruff Formation
    [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]
  • Upper Ordovician and Silurian Stratigraphy in Sequatchie Valley and Parts of the Adjacent Valley and Ridge, Tennessee
    Upper Ordovician and Silurian Stratigraphy in Sequatchie Valley and Parts of the Adjacent Valley and Ridge, Tennessee GEOLOGICAL SURVEY PROFESSIONAL PAPER 996 Prepared in cooperation with the Tennessee Division of Geology Upper Ordovician and Silurian Stratigraphy in Sequatchie Valley and Parts of the Adjacent Valley and Ridge, Tennessee By ROBERT C. MILICI and HELMUTH WEDOW, JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 996 Prepared in cooperation with the Tennessee Division of Geology UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1977 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Milici, Robert C 1931- Upper Ordovician and Silurian stratigraphy in Sequatchie Valley and parts of the adjacent valley and ridge, Tennessee. (Geological Survey professional paper; 996) Bibliography: p. Supt. of Docs. no.: I 19.16:996 1. Geology, Stratigraphic--Ordovician. 2. Geology, Stratigraphic--Silurian. 3. Geology--Tennessee--Sequatchie Valley. 4. Geology--Tennessee--Chattanooga region. I. Wedow, Helmuth, 1917- joint author. II: Title. Upper Ordovician and Silurian stratigraphy in Sequatchie Valley .... III. Series: United States. Geological Survey. Professional paper; 996. QE660.M54 551.7'310976877 76-608170 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-03002·1 CONTENTS Page Abstract 1 Introduction -----------------------------------------------------------------------------
    [Show full text]
  • Detroit River Group in the Michigan Basin
    GEOLOGICAL SURVEY CIRCULAR 133 September 1951 DETROIT RIVER GROUP IN THE MICHIGAN BASIN By Kenneth K. Landes UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director Washington, D. C. Free on application to the Geological Survey, Washington 25, D. C. CONTENTS Page Page Introduction............................ ^ Amherstburg formation................. 7 Nomenclature of the Detroit River Structural geology...................... 14 group................................ i Geologic history ....................... ^4 Detroit River group..................... 3 Economic geology...................... 19 Lucas formation....................... 3 Reference cited........................ 21 ILLUSTRATIONS Figure 1. Location of wells and cross sections used in the study .......................... ii 2. Correlation chart . ..................................... 2 3. Cross sections A-«kf to 3-G1 inclusive . ......................;.............. 4 4. Facies map of basal part of Dundee formation. ................................. 5 5. Aggregate thickness of salt beds in the Lucas formation. ........................ 8 6. Thickness map of Lucas formation. ........................................... 10 7. Thickness map of Amherstburg formation (including Sylvania sandstone member. 11 8. Lime stone/dolomite facies map of Amherstburg formation ...................... 13 9. Thickness of Sylvania sandstone member of Amherstburg formation.............. 15 10. Boundary of the Bois Blanc formation in southwestern Michigan.
    [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]
  • XRF Workshop Book
    Workshop Materials (1 of 2) Table of Contents Workshop Materials (book 1 of 2) Page Agenda 1 Welcome Presentation (Steve Kaczmarek) 3 Lectures Introduction to the Chemistry of Rocks and Minerals (Peter Voice) 7 Geology of Michigan (Bill Harrison) 22 XRF Theory (Steve Kaczmarek) 44 Student Research Posters Silurian A-1 Carbonate (Matt Hemenway) 56 Silurian Burnt Bluff Group (Mohamed Al Musawi) 58 Classroom Activities Powder Problem 60 Fossil Free For All 69 Bridge to Nowhere 76 Get to Know Your Pet Rock 90 Forensic XRF 92 Alien Agua 96 Appendices (book 2 of 2) Appendix A: MGRRE Factsheet 105 Appendix B: Michigan Natural Resources Statistics 107 Appendix C: CoreKids Outreach Program 126 Appendix D: Graphing & Statistical Analysis Activity 138 Appendix E: K-12 Science Performance Expectations 144 Appendix F: Workshop Evaluation Form 179 Workshop Facilitators Bridging the Gap between Geology & Chemistry Sponsored by the Western Michigan University, the Michigan Geological Repository for Research and Education, and the U.S. National Science Foundation This workshop is for educators interested in learning more about the chemistry of geologic materials. Wednesday, August 9, 2017 (8 am - 5 pm) Tentative Agenda 8:00-8:20: Welcome (Steve Kaczmarek) Agenda, Safety, & Introductions 8:20-8:50: Introduction to Geological Materials (Peter Voice) An introduction to rocks, minerals, and their elemental chemistry 8:50-9:00: Questions/Discussion 9:00-9:30: Introduction to MI Basin Geology (Bill Harrison) An introduction to the common rock types and economic
    [Show full text]
  • Summary of Hydrogelogic Conditions by County for the State of Michigan. Apple, B.A., and H.W. Reeves 2007. U.S. Geological Surve
    In cooperation with the State of Michigan, Department of Environmental Quality Summary of Hydrogeologic Conditions by County for the State of Michigan Open-File Report 2007-1236 U.S. Department of the Interior U.S. Geological Survey Summary of Hydrogeologic Conditions by County for the State of Michigan By Beth A. Apple and Howard W. Reeves In cooperation with the State of Michigan, Department of Environmental Quality Open-File Report 2007-1236 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia: 2007 For more information about the USGS and its products: Telephone: 1-888-ASK-USGS World Wide Web: http://www.usgs.gov/ Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation Beth, A. Apple and Howard W. Reeves, 2007, Summary of Hydrogeologic Conditions by County for the State of Michi- gan. U.S. Geological Survey Open-File Report 2007-1236, 78 p. Cover photographs Clockwise from upper left: Photograph of Pretty Lake by Gary Huffman. Photograph of a river in winter by Dan Wydra. Photographs of Lake Michigan and the Looking Glass River by Sharon Baltusis. iii Contents Abstract ...........................................................................................................................................................1
    [Show full text]
  • ENVIRONMENT of DEPOSITION of the BRASSFIELD FORMATION Asenior Thesis Submitted in Partial Fulfillment for the Degree of Bachelor
    - ENVIRONMENT OF DEPOSITION OF THE BRASSFIELD FORMATION Asenior thesis submitted in partial fulfillment for the degree of Bachelor of Science at IDhe Ohio State University Department of Geology and Mineralogy by William Allan Clapper, Jr. } advisors Kenneth Stanley TABLE OF CONTENTS ,.;;: Page INTRODUCTION 1 Previous Work 1 Definition J INVES'f ItiA'f I6N 4 CONCLUSIONS .jO BIBLIOGRAPHY "ft_- Jl APPENDIX 32 MAPS Map of Ohio 2 Map of Highland Cou~ty Map of Highland Plant ~uarry g Areal extent of Brassfield 9 l!.IST OF ILLUSTRATIONS East Wall of Quarry 10 Stratigraphic Column of Upper Section 11 Stratigraphic Golumn of Lower Section 12 1 INTRODUCTION This study is an examination of the Brassfield limestone at the Hihgland Stone Plant Quarry near Hillsboro in Highland County, Ohio.The purpose was a petrographic examination of a typical section of the Brassfield Formation in order to determine the environment of deposition and ultimatly to det­ ermine the depositional history of the formation. Previous Work The Brassfield Formation has been studied at least since before 1838 by Owen in Indiana. It was originally correlated with the Clinton of New York by Orton {1871), based on strat­ igraphy and lithology rather than on faunal evidence. Due to differences in fauna, Foerst (1896) proposed a land barrier between the two and proposed the name Montgomery limestone for the typical development in Montgomery County, Ohio. The name lapsed, and in 1906 he renamed the Clinton beds in Ken­ tucky the Brassfield, and three years later he did the same for the Clinton age beds in Ohio.
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • Geology of Michigan and the Great Lakes
    35133_Geo_Michigan_Cover.qxd 11/13/07 10:26 AM Page 1 “The Geology of Michigan and the Great Lakes” is written to augment any introductory earth science, environmental geology, geologic, or geographic course offering, and is designed to introduce students in Michigan and the Great Lakes to important regional geologic concepts and events. Although Michigan’s geologic past spans the Precambrian through the Holocene, much of the rock record, Pennsylvanian through Pliocene, is miss- ing. Glacial events during the Pleistocene removed these rocks. However, these same glacial events left behind a rich legacy of surficial deposits, various landscape features, lakes, and rivers. Michigan is one of the most scenic states in the nation, providing numerous recre- ational opportunities to inhabitants and visitors alike. Geology of the region has also played an important, and often controlling, role in the pattern of settlement and ongoing economic development of the state. Vital resources such as iron ore, copper, gypsum, salt, oil, and gas have greatly contributed to Michigan’s growth and industrial might. Ample supplies of high-quality water support a vibrant population and strong industrial base throughout the Great Lakes region. These water supplies are now becoming increasingly important in light of modern economic growth and population demands. This text introduces the student to the geology of Michigan and the Great Lakes region. It begins with the Precambrian basement terrains as they relate to plate tectonic events. It describes Paleozoic clastic and carbonate rocks, restricted basin salts, and Niagaran pinnacle reefs. Quaternary glacial events and the development of today’s modern landscapes are also discussed.
    [Show full text]