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Adapted from published geologic quadrangle maps ROCK UNITS TIME UNITS GEOLOGIC TIME SCALE Gravel Geologic Time Scale adapted from American Association of Petroleum Geologists, Stratigraphic Correlation Charts for Northern Appalachian and FORMATION, Crossbedded Midwestern Basin and Arches MEMBER, or BED sandstone Regions. PERIOD 3 million years Sandstone or sand Sandstone and shale Alluvium interbedded Interbedded shale and sandstone QUATERNARY Glacial deposits Shale and minor sandstone 3 million years Drift The following geologic units are absent because of either nondepos- tion or erosion: Tertiary, Cretaceous, Jurassic, Triassic, Permian, and part Silty shale of the Pennsylvanian. 320 million years Flint clay Carbonaceous shale Formations Lee and Breaathitt Clay shale PENNSYLVANIAN Olive Hill Clay Bed 330 million years Dolomitic shale Newman Limestone Interbedded shale and Nada Member limestone; shale dominant Interbedded limestone Cowbell Member and shale Interbedded limestone Nancy Member and shale; limestone dominant Borden Formation Farmers Member Nodular-bedded MISSISSIPPIAN limestone, minor shale Henley Shale Bed Cherty limestone Sunbury Shale Dolomitic limestone ? Berea Sandstone Silty to sandy dolomite Bedford Shale Soft-sediment deformation 365 million years DEVONIAN Unconformity Ohio Shale 415 million years Bisher Dolomite 420 million years Crab Orchard Formation SILURIAN Brassfield Formation 425 million years Drakes Formation Bull Fork Formation Grant Lake Limestone Fairview Formation ORDOVICIAN Upper Part of Ordovician Kope Formation Point Pleasant Tongue of Clays Ferry Formation Figure 3. Stratigraphy of rock units along the AA Highway and U.S. 23. 9.

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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 -----------------------------------------------------------------------------
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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.
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Changes in Stratigraphic Nomenclature by the U.S. Geological Survey
Changes in Stratigraphic Nomenclature by the U.S. Geological Survey, By GEORGE V. COHEE, ROBERT G. BATES, and WILNA B. WRIGHT CONTRIBUTIONS TO STRATIGRAPHY GEOLOGICAL SURVEY BULLETIN 1294-A UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1970 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 35 cents (paper cover) CONTENTS Listing of nomenclatural changes- --- ----- - - ---- -- -- -- ------ --- Ortega Quartzite and the Big Rock and Jawbone Conglomerate Members of the Kiawa Mountain Formation, Tusas Mountains, New Mexico, by Fred Barker---------------------------------------------------- Reasons for abandonment of the Portage Group, by Wallace de Witt, Jr-- Tlevak Basalt, west coast of Prince of Wales Island, southeastern Alaska, by G. Donald Eberlein and Michael Churkin, Jr Formations of the Bisbee Group, Empire Mountains quadrangle, Pima County, Arizona, by Tommy L. Finnell---------------------------- Glance Conglomerate- - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - Willow Canyon Formation ....................................... Apache Canyon Formation-- ................................... Shellenberger Canyon Formation- - --__----- ---- -- -- -- ----------- Turney Ranch Formation---- ------- ------ -- -- -- ---- ------ ----- Age--_------------------------------------------------------- Pantano Formation, by Tommy L. Finnell----------_-----------------
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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.
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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.
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The Geology of Ohio—The Ordovician
A Quarterly Publication of the Division of Geological Survey Fall 1997 THE GEOLOGY OF OHIO—THE ORDOVICIAN by Michael C. Hansen o geologists, the Ordovician System of Ohio bulge), accompanying development of a foreland is probably the most famous of the state’s basin to the east at the edge of the orogenic belt. As Paleozoic rock systems. The alternating shales the Taconic Orogeny reached its zenith in the Late Tand limestones of the upper part of this system crop Ordovician, sediments eroded from the rising out in southwestern Ohio in the Cincinnati region mountains were carried westward, forming a com- and yield an incredible abundance and diversity of plex delta system that discharged mud into the well-preserved fossils. Representatives of this fauna shallow seas that covered Ohio and adjacent areas. reside in museums and private collections through- The development of this delta, the Queenston Delta, out the world. Indeed, fossils from Ohio’s Ordovi- is recorded by the many beds of shale in Upper cian rocks define life of this geologic period, and the Ordovician rocks exposed in southwestern Ohio. rocks of this region, the Cincinnatian Series, serve The island arcs associated with continental as the North American Upper Ordovician Standard. collision were the sites of active volcanoes, as docu- Furthermore, in the late 1800’s, Ordovician rocks in mented by the widespread beds of volcanic ash the subsurface in northwestern Ohio were the source preserved in Ohio’s Ordovician rocks (see Ohio of the first giant oil and gas field in the country. Geology, Summer/Fall 1991).
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159571755.Pdf
·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-· STATE at OHIO MICH.Ul. V. DISALLE. C:O- DEPAll'IMENT at NATUkAL RESOUllCES HERBERT I. EAGON, D1rec11or DIVISION OF GEOLOGICAL SURVEY RALl'H J. IERNHAGDf1 Chief Information Circular No. 26 THE AMERICAN UPPER ORDOVICIAN STANDARD Development of I II. STRATIGRAPHIC CLASSIFICATION OF ORDOVICIAN ROCKS ,in the I Cincinnati 'Region By Malcolm P. Weiss I and Carl E. Norman COLUMIUS 1960 ~--·~·~·-·-·-·-·-·-·~·-·-·-·-·-·-·-·~·-·-·-·-·-·-·~ STATE OF OHIO Michael V. DiSalle Governor DEPARTMENT OF NATURAL RESOURCES Herbert B. Eagon Director NATUR.AL RESOURCES C~ISSic;>N c. D. Blubaugh Joseph E. Hurst Herbert B. Eagon L. L. Rummell Byron Frederick Demas L. Sears Forrest G. Hall Myron T. Stllrgeon William Hoyne DMSION OF GEOLOGICAL SURVEY Ralph J. Bernhagen Chief ·~ The F. J. Heer Printing Company Columbus 16, Ohio 1960 Bound by the State of Ohio THE AMERICAN UPPER ORDOVICIAN STANDARD II. DEVELOPMENT OF STRATIGRAPHIC CLASSIFICATION OF ORDOVICIAN ROCKS IN THE CINCINNATI REGION Malcolm P. Weiss 1 and Carl E. Norman2 ABSTRACT The development of the classification of the rocks in the region about Cincinnati, Ohio is shown in tabular form. The successive columns of stratigraphic names that make up the chart have been correlated in order that the history of the nomenclature of even the smallest stratigraphic units may be traced. The text accompanying the table supplements it in certain respects and includes an historical analysis of the stratigraphic unit called Madison or Saluda. INTRODUCTION A number of authors, particularly of theses and dissertations, have found it help- ful to trace the complicated development of the classification and nomenclature of the beds in the Cincinnati region.
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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.
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Enhanced Resolution of the Paleoenvironmental and Diagenetic Features of the Silurian Brassfield Formation
Wright State University CORE Scholar Browse all Theses and Dissertations Theses and Dissertations 2013 Enhanced Resolution of the Paleoenvironmental and Diagenetic Features of the Silurian Brassfield ormationF Lisa Marie Oakley Wright State University Follow this and additional works at: https://corescholar.libraries.wright.edu/etd_all Part of the Earth Sciences Commons, and the Environmental Sciences Commons Repository Citation Oakley, Lisa Marie, "Enhanced Resolution of the Paleoenvironmental and Diagenetic Features of the Silurian Brassfield ormationF " (2013). Browse all Theses and Dissertations. 787. https://corescholar.libraries.wright.edu/etd_all/787 This Thesis is brought to you for free and open access by the Theses and Dissertations at CORE Scholar. It has been accepted for inclusion in Browse all Theses and Dissertations by an authorized administrator of CORE Scholar. For more information, please contact [email protected]. ENHANCED RESOLUTION OF THE PALEOENVIRONMENTAL AND DIAGENETIC FEATURES OF THE SILURIAN BRASSFIELD FORMATION A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science By LISA MARIE OAKLEY B.S., Wright State University, 2009 2013 Wright State University WRIGHT STATE UNIVERSITY GRADUATE SCHOOL I HEREBY RECOMMEND THAT THE THESIS PREPARED UNDER MY SUPERVISION BY Lisa Marie Oakley ENTITILED Enhanced Resolution Of The Paleoenvironmental And Diagenetic Features Of The Silurian Brassfield Formation BE ACCEPTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF Master of Science. ______________________________ David Schmidt, Ph.D. Thesis Co-Director ______________________________ David Dominic, Ph.D. Thesis Co-Director Department Chair Committee on Final Examination ___________________________________ David Schmidt, Ph.D., Co-director ___________________________________ David Dominic, PhD., Co-director ___________________________________ Chuck Ciampiaglio, PhD., Committee member ______________________________________ R.
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Figure 2 (Pdf)
South North West East West East West East West East Eastern Kentucky Central West Virginia Eastern and Central Ohio Western and Central Pennsylvania Western and Central New York Age Stratigraphy from: Repetski and others (2008) Stratigraphy from: Ryder and others (2008, 2009) Stratigraphy from: Ryder and others (2008, 2009, 2010) Stratigraphy from: Berg and others (1983); Ryder and others (2010) Stratigraphy from: Repetski and others (2008) Era System Series (Ma) Valley Valley Rome Trough Rome Trough Rome Trough and Ridge Bedford Shale and Ridge Cleveland Member Venango Group Catskill Formation 359.2 Upper Devonian strata, undivided Ohio Shale Ohio Three Lick Bed Chagrin Shale equivalent rocks Chagrin Shale Bradford Group Foreknobs Formation Perrysburg Formation Shale Dunkirk Shale Member Huron Member of Ohio Shale Huron Member Elk Group Scherr Formation Upper Dunkirk Shale Java Formation Angola Shale Member Olentangy Shale (upper) Java Formation Java Formation Angola Shale Member West Falls West Falls Brallier Formation West Falls Angola Shale Member Formation Rhinestreet Shale Member Rhinestreet Shale Member of the Formation Rhinestreet Shale Member Formation Rhinestreet Shale Member Upper Devonian strata, undivided West Falls Formation 385.3 Sonyea and Genesee Formations, undivided Sonyea and Genesee Formations, undivided Sonyea and Genesee Formations, undivided Tully Limestone Tully Limestone Tully Limestone Mahantango Formation Mahantango Formation Moscow, Ludlowville, and Skaneateles Shales, undivided Hamilton Olentangy Shale (lower)
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Iii Silurian Fauna
III SILURIAN FAUNA By AUGUST F. FOERSTE THE SILURIAN FAUNA OF KENTUCKY By AUGUST F. FOERSTE THE SOURCE AND AFFINITIES OF THE SILURIAN FAUNAS In prehistoric times the North American continent was invaded by oceanic faunas from various directions. The tilting of the continent toward the south permitted the invasion of oceanic faunas from the Gulf of Mexico, and tilting toward the east, permitted invasions from the North Atlantic. There have been invasions also from the Arctic and Pacific. Some of these invasions extended far inland. Some from the Gulf of Mexico spread northward along the Mississippi embayment as far as the southern part of Canada, and some from the North Atlantic reached Ohio and Kentucky. As far as known, none of the invasions from the Arctic or Pacific reached Kentucky. In most Silurian faunas, the brachiopod element predominates. Three of the southern invasions—the Brassfield, Osgood, and Waldron—are characterized by the abundance of bryozoans, in addition to the brachiopods. The Brassfield and Waldron contain also a considerable number of gastropods, pelecypods, cephalopods, and trilobites, all of which are relatively scarce in the Osgood and Louisville. In the Osgood, on the contrary, there are numerous cystids, though almost all of these were described originally under the single generic name Holocystites. The Waldron is characterized by the considerable variety of crinoids. In the Laurel and Louisville bryozoans are rare. The Laurel is now characterized by numerous species of crinoids, a considerable number of which show affinities with crinoids occurring in Gotland and England. Possibly these invaded the American continent from some North Atlantic source.
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Marion County Geology O
Marion County Geological Formation Marion County is at the extreme southwest corner of 11 11 East Tennessee and bordered on the south by the 11 Alabama and Georgia State lines. Although the county is part of the Cumberland Plateau, it also µ encompasses a large part of Sequatchie Valley and part of the north side of the valley of Tennessee 03 River. Throughout the county, relatively level rock 07 strata form the plateau and crop out in the valleys cut into its surface. Pennsylvanian- age sandstones, shales, and conglomerates, along with several minable coal seams, cap the Cumberland Plateau 38 tableland, Walden Ridge, the regional name of the 03 37 07 plateau east of Sequatchie Valley, and the crest of 07 Raccoon Mountain. Ordovician- and Mississippian -age limestones underlie the valley floors of 03 03 Tennessee and Sequatchie Rivers. The walls of the valleys and their tributaries are composed of 03 03 Mississippian-age limestones, sandstones, and 03 07 03 03 19 shales. Sequatchie Valley, the most prominent 14 15 39 topographic feature in Marion County, runs 19 03 03 03 northeast to southwest through its center. Linear 20 in appearance as a result of the geologic processes that formed it, the valley covers a little over 07 37 one-fourth of the county's total area. 17 40 27 07 03 03 "Tennessee Topology" by David D. Starnes 03 26 TN Div of Geology, Bulletin 86 15 19 03 33 39 15 03 19 03 17 03 23 07 03 03 14 03 03 14 38 1419 15 37 19 03 03 23 07 17 14 03 19 n 19 Cumberland Trail 23 Brassfield Formation 03 d 03 a n 20 14 i d a o r i i Marion
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