Development of Drinking Water and Ecological Unusually Sensitive Areas (Usas): Examples Using the Water and Biological Resources of Ohio
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Terran Cornoration Environmental Services
Page 11 Terran Cornoration Environmental Services Mr. James Yskamp, Esq. February 1, 2018 Fair Shake Environmental Legal Services 159 South Main Street, Suite 1030 Akron, Ohio 44308 RE: Technical Report Review: "Evaluation of Groundwater Impacts, Dewatering of Proposed Enon Quarry, Clark County, Ohio " Dear Mr. Y skamp, I, Brent E. Huntsman, CPG, President and Principal Hydrogeologist ofTerran Corporation (Terran) was retained by Fair Shake Environmental Legal Services to review and comment upon the hydrogeologic characterization and predicted dewatering effects to the water resources of Mad River Township, Clark County, OH as described in a groundwater model report prepared for a mining permit modification. This report review was to include an evaluation of the aquifer response and hydraulic performance predicted by the model simulations of the groundwater system; the magnitude and extent of a cone of depression resulting from dewatering various limestone quarry pits. The purpose of my review is to provide a letter report summarizing my expert opinions regarding the adequacy of the groundwater model to appropriately simulate dewatering effects upon the local groundwater regime. All opinions in this report are based upon my review of existing information (developed through the litigation process in this case or in the public record) together with my 43-years of experience in applied hydrogeology, specifically aquifer characterization and water resources development. My current curriculum vita is included with this letter report as Attachment 2. These opinions are expressed to a reasonable degree of scientific and professional certainty. I reserve the right to supplement this report and opinions as additional material becomes available through the litigation process or continued review of public literature. -
Guide to the Geology of Northeastern Ohio
SDMS US EPA REGION V -1 SOME IMAGES WITHIN THIS DOCUMENT MAY BE ILLEGIBLE DUE TO BAD SOURCE DOCUMENTS. GUIDE TO THE GEOLOGY of NORTHEASTERN OHIO Edited by P. O. BANKS & RODNEY M. FELDMANN 1970 Northern Ohio Geological Society ELYP.i.A PU&UC LIBRARt as, BEDROCK GEOLOGY OF NORTHEASTERN OHIO PENNSYLVANIAN SYSTEM MISSISSIPPIAN SYSTEM DEVONIAN SYSTEM \V&fe'£:i£:VS:#: CANTON viSlSWSSWM FIGURr I Geologic map of northeastern Ohio. Individual formations within each time unit are not dis- -guished, and glacial deposits have been omitted. Because the bedding planes are nearly ••.crizontal, the map patterns of the contacts closely resemble the topographic contours at those z evations. The older and deeper units are most extensively exposed where the major rivers rave cut into them, while the younger units are preserved in the intervening higher areas. CO «< in Dev. Mississippian r-c Penn. a> 3 CO CD BRADF. KINOERHOOK MERAMEC —1 OSAGE CHESTER POTTSVIUE ro to r-» c-> e-> e= e-i GO n « -n V) CO V* o ^_ ^ 0. = -^ eo CO 3 c= « ^> <C3 at ta B> ^ °» eu ra to a O9 eo ^ a* s 1= ca \ *** CO ^ CO to CM v» o' CO to CO 3 =3 13- *•» \ ¥\ A. FIGURE 1. Columnar section ol the major stratigraphic units in northeastern Ohio showing their relative positions in the standard geologic time scale. The Devonian-Mississippian boundary is not known with certainty to lie within the Cleveland Shale. The base of the Mississippian in the northern part of the state is transitional with the Bradford Series of the Devonian System and may lie within the Cleveland Shale (Weller er a/., 1948). -
GEOLOGIC SUMMARY of the APPALACHIAN BASIN, with REFERENCE to the SUBSURFACE DISPOSAL of RADIOACTIVE WASTE SOLUTIONS by George W
TEI-791 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY" GEOLOGIC SUMMARY OF THE APPALACHIAN BASIN, WITH;REFERENCE TO THE SUBSURFACE DISPOSAL OF RADIOACTIVE WASTE SOLUTIONS* By George W. Colton June 1961 Report TEI-791 This report is preliminary and ha^;not been edited for conformity with G^logical Survey format and nomenclature. ?1 ^Prepared on behalf of the U. S. Atomic Energy Commission. CONTENTS Abstract* .......................... 5 Introduction. ........................ 7 Purpose of report. ................... 7 Organization of report .................. 7 Location and extent of area. .............. Q Acknowledgments. .................... 10 Geologic framework. ..................... 10 Depositional framework ................. 10 Structural framework .................. llj. Stratigraphy. ........................ 17 Late Precambrian stratified sequence .......... 17 Early Cambrian clastic sequence. ............ 18 Thickness and depth ................ 22 Cambrian-Ordovician carbonate sequence ......... 23 Thickness and depth . , ........... 35 Late Ordovician clastic sequence ............ 35 Thickness and depth ................ Mi- Early Silurian clastic sequence. ............ kk Thickness and depth ................ 51 Silurian-Devonian carbonate sequence .......... 52 Thickness and depth ................ 62 Devonian classic sequence. ............... 63 Thickness and depth ................ 69 Mississippian sequence ................. 70 Thickness and depth ................ 79 Pennsylvanian sequence ................. 79 Waste -
Geologic Cross Section C–C' Through the Appalachian Basin from Erie
Geologic Cross Section C–C’ Through the Appalachian Basin From Erie County, North-Central Ohio, to the Valley and Ridge Province, Bedford County, South-Central Pennsylvania By Robert T. Ryder, Michael H. Trippi, Christopher S. Swezey, Robert D. Crangle, Jr., Rebecca S. Hope, Elisabeth L. Rowan, and Erika E. Lentz Scientific Investigations Map 3172 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 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 To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names 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: Ryder, R.T., Trippi, M.H., Swezey, C.S. Crangle, R.D., Jr., Hope, R.S., Rowan, E.L., and Lentz, E.E., 2012, Geologic cross section C–C’ through the Appalachian basin from Erie County, north-central Ohio, to the Valley and Ridge province, Bedford County, south-central Pennsylvania: U.S. Geological Survey Scientific Investigations Map 3172, 2 sheets, 70-p. -
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. -
Mississippian Stratigraphy of Northwestern Pennsylvania
Mississippian Stratigraphy of Northwestern Pennsylvania GEOLOGICAL SURVEY BULLETIN 1351-A Prepared in cooperation with the Pennsylvania Topographic and Geologic Survey r ' > 'I . t. I i 7 IT! i . * r * A »« ft - » '" * / 1 f V 4 1* / I 'i'- I 4 I Mississippian Stratigraphy of Northwestern Pennsylvania By GEORGE R. SCHINER and GRANT E. KIMMEL CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY BULLETIN 1331-A Prepared in cooperation with the Pennsylvania Topographic and Geologic Survey UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C B. MORTON, Secretary GEOLOGICAL SURVEY V, E. McKelvey, Director Library of Congress catalog-card No. 72-600086 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price $1.25 (paper cover) Stock Number 2401-2169 CONTENTS Page Abstract ____________________________ Al Introduction _______________________-__ 2 General geologic setting ____________ 3 Methods of investigation ________________ 3 Nomenclature ___________________________ _ 6 Stratigraphy ____________________________ _ 9 Cussewago Sandstone ______________ _ 9 Bedford Shale ____________________________ 11 Unnamed sandstone _____________________ 12 Berea Sandstone ___________________ _ 13 Corry Sandstone _________________________ 14 Shellhammer Hollow Formation _______________ 16 Cuyahoga Group (Orangeville Shale, Sharpsville Sandstone, Mead- ville Shale) ________________________________ 17 Orangeville Shale ___________________ _ 18 Bartholomew -
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. -
Guide to Thirty-First Annual Field Conference of the Section of Geology Combined with the Sections of Plant Science and Conservation of the Ohio Academy of Science
GUIDE TO THIRTY-FIRST ANNUAL FIELD CONFERENCE OF THE SECTION OF GEOLOGY COMBINED WITH THE SECTIONS OF PLANT SCIENCE AND CONSERVATION OF THE OHIO ACADEMY OF SCIENCE APRIL 213 1956 THE NATURAL ENVIRONMENT OF THE SPRINGFIELD AREA CHAIRMEN OF SECTIONS TOUR COMMITTEE Lee Walp, Plant Science Floyd Nave E. S. Thomas Robert Finlay, Conservation kenneth Hunt George Burns John Melvin, Geology John Lounsbury Daniel R. Atzenhoefer £. T. Bodenberg C. N. Savage K, * GEOLCGIC COLUMN The f-ilcwi:i£ chart sh ws that part ..if the gecl-gic column of Ohio that might be expected in Clark County and adjacent ;.:rtions of Greene and Champaign Counties. THICKNESS SYSTEM GROUP FORMATION DESCRIPTION fFe pt) Ground and end moraine, outwash, kames, Mid.die Wisconsin- drift 0 to 60 and valley-train deposit's PIe i stoce ne Quaternary Early Wisconsin drift Extensive gravel outwash and kames 5 to 200 series Mostly fine sand filling buried valleys. Pre-Wiscons in drift 0 to 400 Perhaps some till. Cedarville dolomite Massive, porous, dolomitic limestone 5 to 150? Springfield dolomite Thin-bedded and dense 10 to 15 Euphemia dolomite Massive and porous 6 to 8 S ilur ian Nia garan Massie shale Calcareous and dense 4 to 5 Laurel dolomite Thin-bedded and dense 5 Os go od shale Calcareous with limestone beds 20 to 25 Dayton. 1 inaestone Thin-bedded and dense 6 to 8 Beds of Cli nton Fossilif erous, massive to irregularly Brassfield limestone 30 a ge be dde d Shale, soft, calcareous, interbedded with Richmond, and O rdovi c ia n thin hard limestone layers; called the 1 yOCO-f M aysville Cincinnati shale in old reports GO S H EN :-7-\-~\\~i '5cge — OAYUGAN, -- - " "~ — ^. -
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