Scottslawn Road Widening Geotechnical Report
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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. -
Development of Drinking Water and Ecological Unusually Sensitive Areas (Usas): Examples Using the Water and Biological Resources of Ohio
Development of Drinking Water and Ecological Unusually Sensitive Areas (USAs): Examples Using the Water and Biological Resources of Ohio Colin Plank, Scott Zengel, Heidi Hinkeldey, Elaine Inouye, William Holton, Jeffery Dahlin, and Jacqueline Michel Research Planning, Inc., 1121 Park Street, Columbia, SC 29201, [email protected], 803-256-7322 (voice); 803-254-6445 (fax); and Christina Sames and Samuel Hall, Office of Pipeline Safety, Research and Special Programs Administration, U.S. Department of Transportation, Washington, D.C. 1.0 INTRODUCTION The U.S. Department of Transportation’s Research and Special Programs Administration (RSPA) is required to identify areas unusually sensitive to environmental damage in the event of a hazardous liquid pipeline accident. Pipeline operators that can affect "unusually sensitive areas" (USAs) must develop and follow an integrity management program to assess and evaluate the integrity of their pipelines. After extensive consultation with experts, government agencies, and other stakeholders, a process was developed to identify USAs for drinking water and ecological resources. In general the USA identification process involves selecting a subset of USA candidates from the larger group of Environmentally Sensitive Areas (ESAs), and then applying various filter criteria to the candidates to determine final USAs. For drinking water USAs this means identifying potentially sensitive public water systems (PWS), specifically surface water intakes and ground water wells, and subjecting them to filter -
Xerox University Microfilms
information t o u s e r s This material was produced from a microfilm copy of the original document. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the original submitted. The following explanation of techniques is provided to help you understand markings or patterns which may appear on this reproduction. 1.The sign or "target” for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting thru an image and duplicating adjacent pages to insure you complete continuity. 2. When an image on the film is obliterated with a large round black mark, it is an indication that the photographer suspected that the copy may have moved during exposure and thus cause a blurred image. You will find a good image of the page in the adjacent frame. 3. When a map, drawing or chart, etc., was part of the material being photographed the photographer followed a definite method in "sectioning" the material. It is customary to begin photoing at the upper left hand corner of a large sheet and to continue photoing from left to right in equal sections with a small overlap. If necessary, sectioning is continued again - beginning below the first row and continuing on until complete. 4. The majority of usefs indicate that the textual content is of greatest value, however, a somewhat higher quality reproduction could be made from "photographs" if essential to the understanding of the dissertation. -
Conodonts of the Estill Shale and Bisher Formation (Silurian, Southern Ohio): Biostratigraphy and Distribution1
78 M. A. LAMB AND R. L. LOWE Vol. 87 Conodonts of the Estill Shale and Bisher Formation (Silurian, Southern Ohio): Biostratigraphy and Distribution1 MARK A. KLEFFNER, Department of Geology and Mineralogy, The Ohio State University, Columbus, OH 43210 ABSTRACT. Representatives of 20 species of conodonts have been isolated from samples of the Silurian Estill Shale and Bisher Formation at four localities in southern Ohio. The Estill belongs in the amorphognathoides Zone and is late Llandoverian to early Wenlockian. The Estill-Bisher contact is an unconformity. In Adams and southern Highland counties, the Bisher belongs in the middle and upper ranuliformis Zone and is late early to possibly early middle Wenlockian; in northern Highland County the Bisher belongs in the lower ranuliformis Zone and is middle early to late early Wenlockian. The Estill was deposited in a gradually shoaling sea that regressed from Adams and Highland counties in the early Wenlockian. The sea transgressed south- ward across the two counties later in the early Wenlockian and deposited the Bisher in a shallow, subtidal environment. OHIO J. SCI. 87 (3): 78-89, 1987 INTRODUCTION Highland County, Ohio. North of Fleming County, Kentucky, an unconformity separates the Noland and The Estill Shale and overlying Bisher Formation make Estill (Rexroad and Kleffner 1984). up most of the lower Niagaran sequence (Silurian) in The Estill Shale consists predominantly of blue-green, Adams and Highland counties in southern Ohio. The gray-green, green, and brown shale. Shale beds are com- first, and only detailed, published report on conodonts monly blocky or massive in the lower part of the for- from either the Estill or Bisher was by Rexroad and mation and silty and fissile in the upper part. -
The Silurian of Central Kentucky, U.S.A.: Stratigraphy, Palaeoenvironments and Palaeoecology
The Silurian of central Kentucky, U.S.A.: Stratigraphy, palaeoenvironments and palaeoecology FRANK R. ETTENSOHN, R. THOMAS LIERMAN, CHARLES E. MASON, WILLIAM M. ANDREWS, R. TODD HENDRICKS, DANIEL J. PHELPS & LAWRENCE A. GORDON ETTENSOHN, F.R., LIERMAN, R.T., MASON, C.E., ANDREWS, W.M., HENDRICKS, R.T., PHELPS, D.J. & GORDON, L.A., 2013:04:26. The Silurian of central Kentucky, U.S.A.: Stratigraphy, palaeoenvironments and palaeoecology. Memoirs of the Association of Australasian Palaeontologists 44, 159-189. ISSN 0810-8889. Silurian rocks in Kentucky are exposed on the eastern and western flanks of the Cincinnati Arch, a large-wavelength cratonic structure separating the Appalachian foreland basin from the intracratonic Illinois Basin. The Cincinnati Arch area experienced uplift during latest Ordovician-early Silurian time, so that the exposed Silurian section is relatively thin due to onlap and post- Silurian erosional truncation on the arch. On both flanks of the arch, dolomitic carbonates predominate, but the section on the eastern side reflects a more shale-rich ramp that faced eastern Appalachian source areas. In the Silurian section on the western side of the arch, which apparently developed across a platform-like isolation-accommodation zone, shales are rare except dur- ing some highstand episodes, and rocks in the area reflect deposition across a broad, low-gradient shelf area, interrupted by structurally controlled topographic breaks. Using the progression of interpreted depositional environments and nearshore faunal communities, a relative sea-level curve, which parallels those of previous workers, was generated for the section in Kentucky. While the curve clearly shows the influence of glacial eustasy, distinct indications of the far-field, flexural influence of Taconian and Salinic tectonism are also present. -
View of Pa Element, OSU 41751, X 28, Collection
INFORMATION TO USERS The most advanced technology has been used to photo graph and reproduce this manuscript from the microfilm master. UMI films the original text directly from the copy submitted. Thus, some dissertation copies are in typewriter face, while others may be from a computer printer. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyrighted material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are re produced by sectioning the original, beginning at the upper left-hand comer and continuing from left to right in equal sections with small overlaps. Each oversize page is available as one exposure on a standard 35 mm slide or as a 17" x 23" black and white photographic print for an additional charge. Photographs included in the original manuscript have been reproduced xerographically in this copy. 35 mm slides or 6" x 9" black and white photographic prints are available for any photographs or illustrations appearing in this copy for an additional charge. Contact UMI directly to order. Accessing theUMI World’s Information since 1938 300 North Zeeb Road, Ann Arbor, Ml 48106-1346 USA Order Number 8820S06 Taxonomy and biostratigraphic significance of Wenlockian and Ludlovian (Silurian) conodonts in the midcontinent outcrop area, North America Kleffner, Mark Alan, Ph.D. The Ohio State University, 1988 UMI 300 N. Zeeb Rd. Ann Arbor, MI 48106 PLEASE NOTE: In all cases this material has been filmed in the best possible way from the available copy. -
Synoptic Taxonomy of Major Fossil Groups
APPENDIX Synoptic Taxonomy of Major Fossil Groups Important fossil taxa are listed down to the lowest practical taxonomic level; in most cases, this will be the ordinal or subordinallevel. Abbreviated stratigraphic units in parentheses (e.g., UCamb-Ree) indicate maximum range known for the group; units followed by question marks are isolated occurrences followed generally by an interval with no known representatives. Taxa with ranges to "Ree" are extant. Data are extracted principally from Harland et al. (1967), Moore et al. (1956 et seq.), Sepkoski (1982), Romer (1966), Colbert (1980), Moy-Thomas and Miles (1971), Taylor (1981), and Brasier (1980). KINGDOM MONERA Class Ciliata (cont.) Order Spirotrichia (Tintinnida) (UOrd-Rec) DIVISION CYANOPHYTA ?Class [mertae sedis Order Chitinozoa (Proterozoic?, LOrd-UDev) Class Cyanophyceae Class Actinopoda Order Chroococcales (Archean-Rec) Subclass Radiolaria Order Nostocales (Archean-Ree) Order Polycystina Order Spongiostromales (Archean-Ree) Suborder Spumellaria (MCamb-Rec) Order Stigonematales (LDev-Rec) Suborder Nasselaria (Dev-Ree) Three minor orders KINGDOM ANIMALIA KINGDOM PROTISTA PHYLUM PORIFERA PHYLUM PROTOZOA Class Hexactinellida Order Amphidiscophora (Miss-Ree) Class Rhizopodea Order Hexactinosida (MTrias-Rec) Order Foraminiferida* Order Lyssacinosida (LCamb-Rec) Suborder Allogromiina (UCamb-Ree) Order Lychniscosida (UTrias-Rec) Suborder Textulariina (LCamb-Ree) Class Demospongia Suborder Fusulinina (Ord-Perm) Order Monaxonida (MCamb-Ree) Suborder Miliolina (Sil-Ree) Order Lithistida -
Stratigraphy, 1968
Stratigraphy, 1968 GEOLOGICAL SURVEY BULLETIN 1274 This volume was published as separate chapters A-Q UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director CONTENTS [Letters designate the separately published chapters] (A) Changes in stratigraphic nomenclature by the U.S. Geological Survey, 1967, by George V. Cohee, Robert G. Bates, and Wilna B. Wright. (B) Stratigraphy of the Albemarle Group of the Carolina slate belt in central North Carolina, by Arvid A. Stromquist and Harold W. Sundelius. (C) New and revised stratigraphic names in the Santa Rita Mountains of south- . eastern Arizona, by Harald Drewes. (D) The coal-bearing group in the Nenana coal field, Alaska, by Clyde Wahr- haftig, Jack A. Wolfe, Estella B. Leopold, and Marvin A. Lanphere. (E) Definition of Wisconsinan Stage, by John C. Frye, H. B. Willman, Meyer Rubin, and Robert F. Black. (F) The Reany Creek Formation, Marquette County, Michigan, by Willard P. Puffett. (G) The Aguada Limestone of northwestern Puerto Rico, by Watson H. Monroe. (H) Cretaceous Tertiary boundary in New Jersey, Delaware, and eastern Maryland, by James P. Minard, James P. Owens, Norman F. Sohl, Harold E. Gill, and James F. Mello. (I) Six new Paleozoic and Mesozoic formations in east-central Alaska, by Earl E. Brabb. (J) Four new members of the Upper Cretaceous Straight Cliffs Formation in the southeastern Kaiparowits region, Kane County, Utah, by Fred Peterson. (K) Summary of Cretaceous stratigraphy in part of the McCarthy quadrangle, Alaska., by D. L. Jones and E. M. MacKevett, Jr. (L) The Quimby and Greenvale Cove Formations in western Maine, by Robert H. -
Sectional Meetings Details of Technical Meetings Follow
Sectional Meetings Details of technical meetings follow. See map for building locations. Bus- iness meetings are scheduled for each section. An important item of business is the election of officers. A. ZOOLOGY MORNING SESSION 1 KAUKE HALL F. LEE ST. JOHN, PRESIDING EFFECTS OF CALCIUM MODULATING DRUGS ON INSECT CENTRAL NERVOUS TISSUE. Kevin M. Hoffman & George F. Shambaugh, Department of Entomology, Ohio Agricultural Research & Development CEnter, Wooster, OHIO 44691 9:00 Drugs which modulate the movements of calcium ions into or within cells were perfused over the desheathed, last abdominal ganglion of the cockroach, Nauphoeta cinerea (Olivier). Synaptic transmission, endogenous spike activity, summed post-synaptic potentials and ganglionic polarization were measured. Sodium nitroprusside in low concentrations caused repetitive firing of giant interneurons after faradic stimulation. CONNECTIONS BETWEEN THE NUCLEUS BASALIS AND THE ARCHISTRIATUM IN THE MALLARD. Patrick Work, Department of Biological Sciences, Kent State University, Kent, Ohio 44242. 9:15 Research reported here is part of a study of the feeding mechanism of the mallard duck (Anas platyrhynchos) which is being conducted at the University of Leiden in the Netherlands. It was done through a Kent State University-Leiden University student exchange program in the summer of 1980. The research consisted of a neuroanatomical and histochemical investigation of the relationship between the forebrain nuclei basalis and archistriatum anterior. These are believed to be important elements in neural control of the feeding mecha- nism in the duck. Anatomical connections between these nuclei were studied with the aid of horseradish peroxidase injected into the archistriatum anterior nucleus, Peroxidase-labeled cells were found only in the most medial portions of the nucleus basalis from the level of the posterior commissure to the rostral border of the archistriatum anterior. -
Geotechnical Report
Geotechnical Exploration Report The Freese Center State Route 598 Galion, Ohio 44833 Prepared for Galion Port Authority P.O. Box 761 Galion, Ohio 44833 Daniel E Karch, E.I. Project Manager Prepared by Professional Service Industries, Inc. 4960 Vulcan Avenue Columbus, Ohio 43228 Paul S. Hundley, P.E. July 31, 2020 Geotechnical Dept. Manager/Principal Consultant PSI Project No. 01021746 PSI Project Number: 01021746 The Freese Center July 21, 2020 TABLE OF CONTENTS 1 PROJECT INFORMATION ....................................................................................................................... 1 1.1 PROJECT AUTHORIZATION ............................................................................................................... 1 1.2 PROJECT DESCRIPTION ..................................................................................................................... 1 1.3 PURPOSE AND SCOPE OF SERVICES ................................................................................................. 2 2 SITE AND SUBSURFACE CONDITIONS .................................................................................................... 4 2.1 SITE LOCATION AND DESCRIPTION .................................................................................................. 4 2.2 SITE GEOLOGY .................................................................................................................................. 4 2.3 SUBSURFACE CONDITIONS ............................................................................................................. -
Silurian Rocks in the Subsurface of Northwestern Ohio
STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Horace R. Coli ins, Chief LIBRARJ BUREAU OF GEOLOGY TALLAHASSEE, FLORIDA Report of Investigations No. 100 SILURIAN ROCKS IN THE SUBSURFACE OF NORTHWESTERN OHIO by Adriaan Janssens Columbus 1977 SCIENTIFIC AND TECHNICAL STAFF 8DNRDEPARTMENT OF OF THE NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY ADMINISTRATION Horace R. Collins, MS, State Geologist and Division Chief Richard A. Struble, PhD, Geologist and Assistant Chief William J. Buschman, Jr., BS, Administrative Geologist Barbara J. Adams, Office Manager REGIONAL GEOLOGY SUBSURFACE GEOLOGY Robert G. Van Horn, MS, Geologist and Section Head Adriaan Janssens, PhD, Geologist and Section Head Richard W. Carlton, PhD, Geologist Charles R. Grapes II, BS, Geologist Michael L. Couchot, MS, Geologist Frank L. Majchszak, MS, Geologist Douglas L. Crowell, MS, Geologist James Wooten, Geology Technician Richard M. DeLong, MS, Geologist Garry E. Yates, Geology Technician Michael C. Hansen, MS, Geologist Linda C. Gearheart, Clerk Dennis N. Hull, MS, Geologist Brenda L. Rinderle, Office Machine Operator Michele L. Risser, BA , Geologist Joel D. Vormelker, MS, Geologist LAKE ERIE GEOCHEMISTRY LABORATORY Charles H. Carter, PhD, Geologist and Section Head D. Joe Benson, PhD, Geologist David A. Stith, MS, Geologist and Section Head Donald E. Guy, Jr., BA, Geologist George Botoman, MS, Geologist Dale L. Liebenthal, Boat Captain Norman F. Knapp, PhD, Chemist Thomas J. Feldkamp, BS, Geology Technician E. Lorraine Thomas, Laboratory Technician Marjorie L. VanVooren, Typist TECHNICAL PUBLICATIONS Jean Simmons Brown, MS, Geologist/Editor and Section Head Cartography Philip J. Celnar, BFA, Cartography Supervisor R. Anne Berry, BFA, Cartographer James A. Brown, Cartographer Donald R. -
Generalized Correlation Chart of Bedrock Units In
STATE OF OHIO THIS PUBLICATION WAS FINANCED IN PART THROUGH A GRANT George V. Voinovich, Governor GENERALIZED CORRELATION CHART OF BEDROCK UNITS IN OHIO FROM THE OHIO ENVIRONMENTAL PROTECTION AGENCY DEPARTMENT OF NATURAL RESOURCES UNDER PROVISIONS OF SECTION 319 (h) OF THE CLEAN WATER ACT AS AMENDED IN 1987. Donald C. Anderson, Director OPEN-FILE REPORT 98-2 DIVISION OF GEOLOGICAL SURVEY Compiled by Glenn E. Larsen, September 1998 Thomas M. Berg, Chief EXPLANATION This correlation chart is a product of the Ohio Department of Natural Resources, Division of Root, S. I., Rodriguez, Joaquin, and Forsyth, J. L., 1961, Geology of Knox County: Ohio Division of Kleffner, M. A., 1990, Wenlockian (Silurian) conodont biostratigraphy, depositional environments, and CHRONOSTRATIGRAPHIC UNITS Geological Survey and was prepared as part of a grant (project no. 95 (h) EPA-15) from the Ohio Geological Survey Bulletin 59, 232 p. depositional history along the eastern flank of the Cincinnati Arch in southern Ohio: Journal of Environmental Protection Agency under provisions of Section 319 (h) of the Clean Water Act as Scatterday, J. W., 1963, Stratigraphy and conodont faunas of the Maxville Group (Middle and Upper Paleontology, v. 64, no. 2, p. 319-328. amended in 1987. Funding for the geologic mapping that is the basis for the mapped units shown Mississippian) of Ohio: Ohio State University Ph.D. dissertation (unpub.), The Ohio State Kleffner, M. A., 1994, Conodont biostratigraphy and depositional history of strata comprising the on the chart was provided by the U.S. Geological Survey (National Cooperative Geologic Mapping University, 162 p. Niagaran sequence (Silurian) in the northern part of the Cincinnati Arch region, west-central Ohio, and M NORTH M GLOBAL E AMERICAN AREA 1 AREA 2 AREA 3 AREA 4 AREA 5 AREA 6 AREA 7 AREA 8 AREA 9 AREA 10 AREA 11 AREA 12 AREA 13 AREA 14 Program, STATEMAP component), the Ohio Department of Transportation, and the Ohio Shaver, R.