Geological Investigations in Ohio
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Devoted to the Study and Appreciation of Ohio's Birdlife • Vol. 44, No. 1, Fall 2020
Devoted to the Study and Appreciation of Ohio’s Birdlife • Vol. 44, No. 1, Fall 2020 Debbie Parker enjoyed great looks at a Yellow-bellied Flycatcher on 16 Sept at Magee. On the cover: A very cooperative first state record Brown Booby was photographed by Josh Vardous on 26 Aug at Nimisila Reservoir. The bird was enjoyed by many birders across the state over the course of several weeks. Vol. 44 No. 1 Devoted to the Study and Appreciation of Ohio’s Birdlife EDITOR OHIO BIRD RECORDS Craig Caldwell COMMITTEE 1270 W. Melrose Dr. Westlake, OH 44145 Rob Harlan 440-356-0494 Vice-Secretary [email protected] [email protected] PHOTO EDITOR PAST PUBLISHERS Jamie Cunningham John Herman (1978–1980) [email protected] Edwin C. Pierce (1980–2008) LAYOUT PAST EDITORS Roger Lau John Herman (1978–1980) [email protected] Edwin C. Pierce (1980–1991) Thomas Kemp (1987–1991) Robert Harlan (1991–1996) Victor W. Fazio III (1996–1997) CONSULTANTS Bill Whan (1997–2008) Tim Colborn Andy Jones (2008–2010 Stephan Gleissberg Jill M. Russell (2010–2012) Rob Harlan Andy Jones Holly Latterman Kent Miller Su Snyder Brian Wulker And the 25+ eBird county reviewers ISSN 1534-1666 The Ohio Cardinal, Fall 2020 COMMENTS ON THE SEASON By Craig Caldwell system entered the state from the west. With the dryness came heat: Nov was the eighth hottest As this issue was in preparation, we received on record. Locally for me, stations in Akron and word of Bill Whan’s death. Bill passed on 14 Jan, Cleveland set several daily high records. -
Chapter 1. Natural History
CHAPTER 1. NATURAL HISTORY CHAPTER 1. NATURAL HISTORY —THE WILDERNESS THAT GREETED THE FIRST SETTLERS The land one sees today traveling through northern Ohio took gone. Thus, some 14,000 years ago as the last glacier receded millions of years to form. We can see evidence of tropical sea into the Lake Erie basin, the first Native Americans arrived and reefs on the Lake Erie Islands and deep ocean sediments here in began to utilize the natural resources that these natural processes the cliffs of the Black River. Ohio was just south of the equator had produced. at that time, some 350 million years ago, and over the millennia The natural history of Sheffield encompasses all those natural has migrated northward to its present position. Mountain features and processes of the environment that greeted the Native building to the east eventually raised the sea floor from under Americans, and later the pioneers, when they first arrived in the waves and erosion by streams, and later glacial ice, began Sheffield. To be sure, the landscape was a magnificent wilderness to sculpture the land. At the same time plants and animals were to the settlers, but it needed to be “tamed” in order to support evolving and began to populate the new land once the ice was the newcomers. Ice formation on the shale bluff of the Black River north of Garfield Bridge (2005). 1 BICENTENNIAL HISTORY OF SHEFFIELD TOPOGRAPHY Regional Physiography The topography of an area is the configuration of the land Physiography refers to the physical features or landforms of surface, including its relief [vertical differences in elevation of a region. -
U.S. Lake Erie Lighthouses
U.S. Lake Erie Lighthouses Gretchen S. Curtis Lakeside, Ohio July 2011 U.S. Lighthouse Organizations • Original Light House Service 1789 – 1851 • Quasi-military Light House Board 1851 – 1910 • Light House Service under the Department of Commerce 1910 – 1939 • Final incorporation of the service into the U.S. Coast Guard in 1939. In the beginning… Lighthouse Architects & Contractors • Starting in the 1790s, contractors bid on LH construction projects advertised in local newspapers. • Bids reviewed by regional Superintendent of Lighthouses, a political appointee, who informed U.S. Treasury Dept of his selection. • Superintendent approved final contract and supervised contractor during building process. Creation of Lighthouse Board • Effective in 1852, U.S. Lighthouse Board assumed all duties related to navigational aids. • U.S. divided into 12 LH districts with inspector (naval officer) assigned to each district. • New LH construction supervised by district inspector with primary focus on quality over cost, resulting in greater LH longevity. • Soon, an engineer (army officer) was assigned to each district to oversee construction & maintenance of lights. Lighthouse Bd Responsibilities • Location of new / replacement lighthouses • Appointment of district inspectors, engineers and specific LH keepers • Oversight of light-vessels of Light-House Service • Establishment of detailed rules of operation for light-vessels and light-houses and creation of rules manual. “The Light-Houses of the United States” Harper’s New Monthly Magazine, Dec 1873 – May 1874 … “The Light-house Board carries on and provides for an infinite number of details, many of them petty, but none unimportant.” “The Light-Houses of the United States” Harper’s New Monthly Magazine, Dec 1873 – May 1874 “There is a printed book of 152 pages specially devoted to instructions and directions to light-keepers. -
Subsurface Facies Analysis of the Devonian Berea Sandstone in Southeastern Ohio
SUBSURFACE FACIES ANALYSIS OF THE DEVONIAN BEREA SANDSTONE IN SOUTHEASTERN OHIO William T. Garnes A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE December 2014 Committee: James Evans, Advisor Jeffrey Snyder Charles Onasch ii ABSTRACT James Evans, Advisor The Devonian Berea Sandstone is an internally complex, heterogeneous unit that appears prominently both in outcrop and subsurface in Ohio. While the unit is clearly deltaic in outcrops in northeastern Ohio, its depositional setting is more problematic in southeastern Ohio where it is only found in the subsurface. The goal of this project was to search for evidence of a barrier island/inlet channel depositional environment for the Berea Sandstone to assess whether the Berea Sandstone was deposited under conditions in southeastern Ohio unique from northeastern Ohio. This project involved looking at cores from 5 wells: 3426 (Athens Co.), 3425 (Meigs Co.), 3253 (Athens Co.), 3252 (Athens Co.), and 3251 (Athens Co.) In cores, the Berea Sandstone ranges from 2 to 10 m (8-32 ft) thick, with an average thickness of 6.3 m (20.7 ft). Core descriptions involved hand specimens, thin section descriptions, and core photography. In addition to these 5 wells, the gamma ray logs from 13 wells were used to interpret the architecture and lithologies of the Berea Sandstone in Athens Co. and Meigs Co. as well as surrounding Vinton, Washington, and Morgan counties. Analysis from this study shows evidence of deltaic lobe progradation, abandonment, and re-working. Evidence of interdistributary bays with shallow sub-tidal environments, as well as large sand bodies, is also present. -
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). -
Strophomenide and Orthotetide Silurian Brachiopods from the Baltic Region, with Particular Reference to Lithuanian Boreholes
Strophomenide and orthotetide Silurian brachiopods from the Baltic region, with particular reference to Lithuanian boreholes PETRAS MUSTEIKIS and L. ROBIN M. COCKS Musteikis, P. and Cocks, L.R.M. 2004. Strophomenide and orthotetide Silurian brachiopods from the Baltic region, with particular reference to Lithuanian boreholes. Acta Palaeontologica Polonica 49 (3): 455–482. Epeiric seas covered the east and west parts of the old craton of Baltica in the Silurian and brachiopods formed a major part of the benthic macrofauna throughout Silurian times (Llandovery to Pridoli). The orders Strophomenida and Orthotetida are conspicuous components of the brachiopod fauna, and thus the genera and species of the superfamilies Plec− tambonitoidea, Strophomenoidea, and Chilidiopsoidea, which occur in the Silurian of Baltica are reviewed and reidentified in turn, and their individual distributions are assessed within the numerous boreholes of the East Baltic, particularly Lithua− nia, and attributed to benthic assemblages. The commonest plectambonitoids are Eoplectodonta(Eoplectodonta)(6spe− cies), Leangella (2 species), and Jonesea (2 species); rarer forms include Aegiria and Eoplectodonta (Ygerodiscus), for which the new species E. (Y.) bella is erected from the Lithuanian Wenlock. Eight strophomenoid families occur; the rare Leptaenoideidae only in Gotland (Leptaenoidea, Liljevallia). Strophomenidae are represented by Katastrophomena (4 spe− cies), and Pentlandina (2 species); Bellimurina (Cyphomenoidea) is only from Oslo and Gotland. Rafinesquinidae include widespread Leptaena (at least 11 species) and Lepidoleptaena (2 species) with Scamnomena and Crassitestella known only from Gotland and Oslo. In the Amphistrophiidae Amphistrophia is widespread, and Eoamphistrophia, Eocymostrophia, and Mesodouvillina are rare. In the Leptostrophiidae Mesoleptostrophia, Brachyprion,andProtomegastrophia are com− mon, but Eomegastrophia, Eostropheodonta, Erinostrophia,andPalaeoleptostrophia are only recorded from the west in the Baltica Silurian. -
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 .......................... -
Geologic Resources Inventory Ancillary Map Information Document for Little River Canyon National Preserve
U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Directorate Geologic Resources Division Little River Canyon National Preserve GRI Ancillary Map Information Document Produced to accompany the Geologic Resources Inventory (GRI) Digital Geologic Data for Little River Canyon National Preserve liri_geology.pdf Version: 6/30/2020 I Little River Canyon National Preserve Geologic Resources Inventory Ancillary Map Information Document for Little River Canyon National Preserve Table of Contents Geologic Reso..u..r..c..e..s.. .I.n..v..e..n..t.o...r.y.. .M...a..p.. .D...o..c..u..m...e...n..t............................................................................ 1 About the NPS.. .G...e..o..l.o..g..i.c... .R..e..s..o..u...r.c..e..s.. .I.n..v..e..n...t.o..r.y.. .P...r.o..g...r.a..m............................................................... 3 GRI Digital Ma.p..s.. .a..n...d.. .S..o..u...r.c..e.. .M...a..p.. .C...i.t.a..t..i.o..n..s.................................................................................. 5 Index Ma..p........................................................................................................................................................................ 6 Map Unit List ................................................................................................................................... 7 Map Unit Desc..r.i.p..t.i.o...n..s...................................................................................................................... 9 Qal - Allu..v..iu..m... .a..n..d.. .l.o..w... .t.e..r.r.a..c..e.. .d..e..p..o..s..i.t.s. .(..Q..u..a..t.e..r..n..a..r.y.)..................................................................................................... 9 Tal - Fluv..i.a..l. .d..e..p..o..s.i.t.s.. .(.T..e..r..t.ia..r..y.)........................................................................................................................................ 9 PNpv - P.o..t.t.s..v..i.l.le.. .F...o..r.m...a..t.i.o..n. -
Historical Development and Problems Within the Pennsylvanian Nomenclature of Ohio.1
Historical Development and Problems Within the Pennsylvanian Nomenclature of Ohio.1 GLENN E. LARSEN, OHIO Department of Natural Resources, Division of Geological Survey, Fountain Sq., Bldg. B, Columbus, OH 43224 ABSTRACT. An analysis of the historical development of the Pennsylvanian stratigraphic nomenclature, as used in Ohio, has helped define and clarify problems inherent in Ohio's stratigraphic nomenclature. Resolution of such problems facilitates further development of a useful stratigraphy and philosophy for mapping. Investigations of Pennsylvanian-age rocks in Ohio began as early as 1819- From 1858 to 1893, investigations by Newberry, I. C. White, and Orton established the stratigraphic framework upon which the present-day nomenclature is based. During the 1950s, the cyclothem concept was used to classify and correlate Pennsylvanian lithologic units. This classification led to a proliferation of stratigraphic terms, as almost every lithologic type was named and designated as a member of a cyclothem. By the early 1960s, cyclothems were considered invalid as a lithostratigraphic classification. Currently, Pennsylvanian nomenclature of Ohio, as used by the Ohio Division of Geological Survey, consists of four groups containing 123 named beds, with no formal formations or members. In accordance with the 1983 North American Stratigraphic code, the Ohio Division of Geological Survey considers all nomenclature below group rank as informal. OHIO J. SCI. 91 (1): 69-76, 1991 INTRODUCTION DISCUSSION Understanding the historical development of Pennsyl- The Early 1800s vanian stratigraphy in Ohio is important to the Ohio The earliest known references to Pennsylvanian-age Division of Geological Survey (OGS). Such an under- rocks in Ohio are found in Atwater's (1819) report on standing of Pennsylvanian stratigraphy helps define Belmont County, and an article by Granger (1821) on plant stratigraphic nomenclatural problems in order to make fossils collected near Zanesville, Muskingum County. -
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. -
Where to See Ohio's Geology
PLEASE NOTE: Some of the information provided, such as phone numbers and Web addresses, may have changed since release of this publication. No. 21 OHIOGeoFacts DEPARTMENT OF NATURAL RESOURCES • DIVISION OF GEOLOG I CAL SURVEY WHERE TO SEE OHIO’S GEOLOGY Listed below are places where you can hike through scenic areas, collect fossils, or visit archaeological or historical sites that have a geological focus.The facilities of the Ohio Geological Survey (Delaware County__Horace R. Collins Laboratory, 740-548-7348; Erie County__Lake Erie Geology Group, 419-626-4296; Franklin County__main offi ce, 614-265-6576) have displays and information on geology. For ad di tion al in for ma tion on the sites listed below, please contact the ap pro pri ate agency, not the Ohio Geolog i cal Survey. KEY: Franklin County: Co lum bus and Franklin Coun ty Metropolitan Park District (614-508-8000, <http://www.metroparks.net>): Blendon Woods A archaeology site (S, MP), Highbanks (S, H, A, MP, RR7); Friendship Park (S, CP); Glen CP city or county park Echo Park (S, CP); Griggs Reser voir and Dam (S, CP); Hayden Run Falls F fossil collecting, by permission only (S, CP); Indian Village Camp (S, H, CP); Whetstone Park (S, CP); Ohio GSA# Ohio Division of Geological Survey GSA reprint (see Refer- Historical Center ($, 614-297-2300, <http://www.ohiohistory.org>); Ohio ences) State Uni ver si ty Orton Muse um (614-292-6896) H historical site Gallia County: Tycoon Lake State Wildlife Area (S); Bob Evans MP metropark Farm (S, H) PR permit required Geauga County: Aquilla -
Summerfield and Woodsfield Quadrangles, Ohio
DEPARTMENT OF THE INTERIOR ALBERT B. FALL, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Bulletin 720 ECONOMIC GEOLOGY OF THE SUMMERFIELD AND WOODSFIELD QUADRANGLES, OHIO WITH DESCRIPTIONS OF COAL AND OTHER MINERAL RESOURCES EXCEPT OIL AND GAS BY D. DALE CONDIT WASHINGTON GOVERNMENT PRINTING OFFICE 1923 ADDITIONAL COPIES OF THIS PUBLICATION MAY BE PROCURED FROM THE SUPERINTENDENT OF DOCUMENTS GOVERNMENT PRINTING OFFICE WASHINGTON, D. C. AT 30 CENTS PER COPY CONTENTS. Bibliography............................................................. 6 Introduction. ^........................................................... 7 i Abstract of report.............................................:....... 7 Field and office work................................................. 7 Acknowledgments.................................................... 8 Geography .................../...................................... ..... 8 Location............................................................ 8 Topographic features................................................... 9 Drainage........................................................ 9 Relief and land forms...............:........... '. ................. 10 Agricultural and commercial conditions................................ 11 Transportation facilities........................................... 11 Railroads.................................................... 11 New railroad routes........................................... 11 Highways...................................................