Ohio Natural Gas Flaring and Venting Regulations

Total Page:16

File Type:pdf, Size:1020Kb

Ohio Natural Gas Flaring and Venting Regulations Fossil Ohio Natural Gas Flaring Energy OFFICE OF OIL & NATURAL GAS and Venting Regulations The U.S. Department of Energy’s Office of Fossil Energy (FE) supports research and development of technologies that can reduce the volume of natural gas (e.g., methane) flared or vented (released) into the atmosphere during crude oil and natural gas exploration, production, processing, transportation, and storage operations. This fact sheet was created by FE to inform stakeholders on state-level production and regulatory activity regarding natural gas flaring and venting. FE’s research portfolio includes efforts to reduce methane (and other hydrocarbon) flaring through the application of improved technologies to capture and utilize small volumes of natural gas at remote locations, as well as technologies to reduce (primarily) methane release during midstream gas processing and transportation. Intermittent flaring that occurs as a result of routine well testing, production facility process shutdowns, or facility and pipeline infrastructure maintenance, are normal aspects of safe oil and natural gas production. Increases in domestic oil and natural gas production have resulted in significant infrastructure buildouts, however, natural gas pipeline capacity constraints have led to regional increases in the flaring of associated gas in some unconventional plays (e.g., Permian Basin in Texas and New Mexico and Bakken Shale in North Dakota) in order to enable oil production. Ohio Producing Plays and primarily produces gas in northeast and Basins Pennsylvania but becomes more liquid rich in less thermally mature areas of According to the U.S. Energy Information southwestern Pennsylvania, West Virginia, Administration (EIA), Ohio’s proved and southeastern Ohio. According to the reserves are 189 million barrels of oil and U.S. Geological Survey (USGS), the 27 trillion cubic feet (Tcf) of natural gas Marcellus Shale play contains about 84 (2017). The “most likely” recoverable shale Tcf of natural gas and 3.4 billion barrels gas resource for the entire Appalachian of liquids (both undiscovered, technically Basin is understood to be 858.7 Tcf, recoverable). However, the Institute with 27.6 Tcf in non-shale gas resources. for Energy Research estimated that the These resources are contained within the play could hold as much as 500 Tcf of Marcellus Shale, the Utica Shale, and the Figure 1: Appalachian Basin and Pennsylvania major unconventional gas recoverable natural gas. Devonian (Ohio) Shale. plays outlined. Source: EIA The Utica Shale is a stacked play The Marcellus Shale play extends underlying the Marcellus Shale that from New York State in the north to The Marcellus currently produces in four includes both the Utica formation and southwestern West Virginia, and it is states: Pennsylvania, West Virginia, Ohio, the underlying Point Pleasant formation. the most productive natural gas play and New York. The Marcellus formation The most productive areas of the Point in the Appalachian Basin (Figure 1). ranges in depth from 100–9,900 feet Pleasant formation are located in eastern Ohio Oil and Natural Gas Statistics (EIA) 2013 2014 2015 2016 2017 2018 Crude Oil Production (Average Thousand Barrels/Day) 22 41 73 59 52 70 * Natural Gas Gross Withdrawals and Production 454 1,400 2,756 3,926 4,853 8,269 * (Average MMcf/Day) Natural Gas Gross Withdrawals and Production Ohio does not maintain a database of total annual gas vented or flared. (Vented and Flared) (MMcf/Day) Natural Gas Gross Withdrawals and Production 28.3 35.7 108.1 11.5 11.4 N/A (Oil Wells) (MMcf/Day) Natural Gas and Gas Producing Oil Wells (Thousands) 37.8 38.3 37.6 38.6 34.5 N/A MMcf – million cubic feet * Data from Ohio Department of Natural Resources, Division of Oil and Gas Resources 2017 ranking among 32 U.S. oil and natural gas producing states — Oil: 13 Natural Gas: 8 OFFICE OF FOSSIL ENERGY OFFICE OF FOSSIL ENERGY Ohio and western Pennsylvania. The of the public or when the gas is lawfully burn between 10 and 32 MMBtu/hour. Utica Shale extends over 115,000 square produced and there is no economic market According to the Ohio EPA, once facilities miles and the Point Pleasant slightly less, at the well for escaping gas.” are permitted on a volume range, the actual of which about 75 percent is prospective. Additional relevant rules are included volumes are not collected and aggregated. The Utica play could hold technically as part of the Ohio Administrative Code recoverable volumes of 782 Tcf of natural within Chapter 1501:9-9, Division of Ohio State Points gas and nearly 2 billion barrels of oil. EIA Mineral Resources Management – Oil of Contact estimates proved reserves of 6.4 Tcf for and Gas; Safety Regulations. Chapter Ohio Department of Natural the Utica play (2017). 1501:9-9-05, Producing Operations, Resources: Division of Oil and The Devonian (Ohio) Shale is a shallower Section B mandates that “All gas vented Gas Resources formation that extends across the to the atmosphere must be flared, with the Contact the Division of Oil and Gas Appalachian Basin, including parts of exception of gas released by a properly Resources for information on oil and eastern Ohio, West Virginia, Kentucky, functioning relief device and gas released gas drilling operations, production, and and Pennsylvania. This low-pressure shale by controlled venting for testing, blowing restoration. formation has produced gas since the late down and cleaning out wells.” This section 1800s, and large numbers of stripper gas also outlines that flares must be 100 feet Website: http://oilandgas.ohiodnr.gov/ wells continue to produce at low rates. from the well, all surface equipment, and Email: [email protected] Western Pennsylvania, western Ohio, inhabited structures. Additionally, Chapter Phone: 614-265-6630 and northern West Virginia also produce 15.1:9-9-03, Drilling and Deepening limited amounts of crude oil from shallow Operations, Section K requires that local Ohio Environmental Protection formations. emergency response officials be notified Agency: Division of Air Pollution when flaring is expected to occur in urban Control Ohio Key Regulations areas. Contact the Division of Air Pollution Associated with Flaring In addition, the Ohio Environmental Control for information on permits for gas and Venting Protection Agency (EPA) is tasked with flaring. administering air quality permitting The Division of Oil and Gas Resources at Website: https://epa.ohio.gov/dapc/ programs in Ohio. All oil and gas the Ohio Department of Natural Resources production facilities are required to Email: brandon.schwendeman@epa. is charged with enforcing the rules related obtain an air permit before beginning ohio.gov to natural gas flaring and venting in the construction. After application, the Phone: 614-644-4840 state. The original regulation, recorded as approval process can take between 45–180 Ohio Revised Code Title 15, Conservation days. Facilities need to consider the flare of Natural Resources, Chapter 1509.20, Visit energy.gov/fe/state-natural-gas- size in order to apply for the appropriate Prevention of Waste – Gas Flaring, was flaring-and-venting-regulations for a permit. Flares expected to burn less than published in 1965 and amended in 2010. digital version of this fact sheet that 10 million British thermal units (MMBtu)/ This rule requires that well owners and includes hyperlinks to information hour should use the General Permit operators prevent wasting oil and gas sources. (GP) 12.1 air permit, while the GP 12.2 and allows for flaring gas “when it is should be used if the flare is expected to necessary to protect the health and safety For more information, visit: Information current as of May 2019. Fossil fossil.energy.gov Energy OFFICE OF OIL & NATURAL GAS.
Recommended publications
  • Late Devonian and Early Mississippian Distal Basin-Margin Sedimentation of Northern Ohio1
    Late Devonian and Early Mississippian Distal Basin-Margin Sedimentation of Northern Ohio1 THOMAS L. LEWIS, Department of Geological Sciences, Cleveland State University, Cleveland, OH 44115 ABSTRACT. Clastic sediments, derived from southeastern, eastern and northeastern sources, prograded west- ward into a shallow basin at the northwestern margin of the Appalachian Basin in Late Devonian and Early Mississippian time. The western and northwestern boundary of the basin was the submerged Cincinnati Arch. The marine clastic wedges provided a northwest paleoslope and a distal, gentle shelf-edge margin that controlled directional emplacement of coarse elastics. Rising sea levels coupled with differences in sedimen- tation rates and localized soft-sediment deformation within the basin help explain some features of the Bedford and Berea Formations. The presence of sand-filled mudcracks and flat-topped symmetrical ripple marks in the Berea Formation attest to very shallow water deposition and local subaerial exposure at the time of emplacement of part of the formation. Absence of thick, channel-form deposits eastward suggests loss of section during emergence. OHIO J. SCI. 88 (1): 23-39, 1988 INTRODUCTION The Bedford Formation (Newberry 1870) is the most The Ohio Shale, Bedford, and Berea Formations of lithologically varied formation of the group. It is com- northern Ohio are clastic units which record prograda- prised of gray and red mudshales, siltstone, and very tional and transgressional events during Late Devonian fine-grained sandstone. The Bedford Formation thins and Early Mississippian time. The sequence of sediments both to the east and west and reaches its maximum is characterized by (1) gray mudshale, clayshale, siltstone, thickness in the Cleveland area.
    [Show full text]
  • Assessing the Petroleum Geology and Future Development of the Clendenin Gas Field in Kanawha County, West Virginia
    Assessing the Petroleum Geology and Future Development of the Clendenin Gas Field in Kanawha County, West Virginia By: Jonathan Prevatte August 2020 Director of Thesis: Donald W. Neal Major Department: Geological Sciences Petroleum is one of the main sources for energy production in the US and is therefore important for the continuation of economic growth. Future development of petroleum resources in the US to meet supply demands is equally important. Understanding the controls on petroleum production will help in determining where and how to development these resources for maximum production. West Virginia is home to many gas fields and is underlain by one of the more prominent gas producing shales, the Marcellus Shale. The Clendenin Gas Field in Kanawha County is one of the historical gas producing areas found in West Virginia. This assessment is focused on the Devonian strata throughout the field including the Marcellus Shale. Using available geophysical logs, production data, and historic well records obtained from the West Virginia Geologic and Economic Survey (WVGES), cross-sections, isopach maps, and structure contour maps were created to give a visual representation of the subsurface geology across the field. Construction of the cross-sections and maps in conjunction with production and well record data aided in the identification of controls influencing production throughout the field. Applying the findings of this assessment to future production may reduce costs and improve yields of future petroleum wells. Results of this study indicate several options should be considered when planning for future production wells within the field. Target areas include the areas to the east of the field where formations tend to thicken.
    [Show full text]
  • Marcellus Shale,” Hamilton Group [email protected] 2045 Morse Rd., Bldg
    Matthew S. Erenpreiss Ohio Department of Natural Resources, Division of Geological Survey Mapping the Regional Organic Thickness of the “Marcellus Shale,” Hamilton Group [email protected] 2045 Morse Rd., Bldg. C-2, Columbus, OH 43229-6693 ABSTRACT • Regional and statewide isopach maps Shale” in each county and township, where available; this newly compiled data and observing the “Marcellus ASHTABULA REFERENCES WILLIAMS FULTON LUCAS OTTAWA LAKE GEAUGA WOOD Lash, G.G., and Engelder, Terry, 2011, Thickness HENRY TRUMBULL have been developed for the Middle Devonian “Marcellus this approach allowed for an even distribution of control Shale” upper and lower units, net organic thickness SANDUSKY CUYAHOGA DEFIANCE ERIE LORAIN trends and sequence stratigraphy of the Middle PORTAGE HURON SUMMIT Devonian Marcellus Formation, Appalachian Basin— PAULDING SENECA MEDINA Shale” for use in assessing Ohio’s shale gas potential. points and more consistent correlations. This correlation was calculated and contoured. Additional data was also PUTNAM HANCOCK MAHONING Implications for Acadian foreland basin evolution: VAN WERT WYANDOT CRAWFORD RICHLAND ASHLAND WAYNE AAPG Bulletin, v. 95, no. 1, p. 61–103. Existing stratigraphic analyses of Devonian shales in Ohio expansion of the Hamilton Group, “Marcellus Shale,” collected from the state geological surveys of New York, ALLEN STARK COLUMBIANA Ohio Division of Geological Survey, 1988, Analysis of HARDIN MERCER CARROLL stratigraphic and production relationships of Devonian MARION AUGLAIZE HOLMES MORROW TUSCARAWAS shale gas reservoirs in Ohio–Final report October were used as the starting dataset, which was expanded and Onondaga Limestone was based on U.S. Geological Pennsylvania, and West Virginia to create a new regional LOGAN KNOX SHELBY UNION JEFFERSON COSHOCTON HARRISON DELAWARE 1985–November 1988 (prepared for Gas Research DARKE A’ Institute): Ohio Department of Natural Resources, CHAMPAIGN LICKING with additional geophysical logs that span the “Marcellus Survey cross sections published in Bulletin 1909.
    [Show full text]
  • Geology of Fairfield County, Ohio
    This dissertation has been 61—5134 microfilmed exactly as received WOLFE, Edward Winslow, 1936- GEOLOGY OF FAIRFIELD COUNTY, OHIO. The Ohio State University, Ph.D., 1961 Geology University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY OF FAIRFIELD COUNTY, OHIO DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of the Ohio State University By Edward Winslow Wolfe, B. A. The Ohio State University 1961 Approved by Department of Geology ! ACKNOWLEDGMENTS Thanks are due Mr. R. J. Bernhagen, State Geologist, who suggest­ ed the need for an investigation of the geology of Fairfield County. The writer is particularly indebted to Dr. Aurele La Rooque who di­ rected the investigation and guided the writer throughout the prepara­ tion of this report. Many others gave freely of their time in dis­ cussing with the writer the geology of Fairfield County. Among these, special thanks are due Dr. Jane L. Forsyth of the Ohio Division of Geological Survey, Mr. George J. Franklin, who is presently completing a report on the geology of Licking County, and the writer's colleagues in the Department of Geology at the College of Wooster. The writer thanks several members of the Ohio Division of Geological Survey, in­ cluding Miss Pauline Smyth, Mr. Karl V. Hoover, and Mr. Harold J. Flint, for their valuable assistance. Most helpful, too, was the as­ sistance of Mr. Jon S. Galehouse during the summer of i960. The field work was sponsored and financed by the Ohio Division of Geological Survey. Additional financial aid, in the form of a William H.
    [Show full text]
  • USEPA Hydraulic Fracturing SAB Example Photographs
    USEPA Hydraulic Fracturing SAB Example Photographs Target rocks, reservoir rocks, thin sections, SEM images of shales, joints in boreholes Copyrights held by E. Scott Bair Ohio Shale SEM Image of Venango Shale, Oil City, PA K = 10-7 ft/d SEM Image of Shale capping Mt. Simon Sandstone at People’s Energy Gas Storage Field, Champaign, IL K = 10-7 ft/d Vertical Joint in Shales in Residential Well, Bainbridge, OH Vertical joint in shale in a residential well, Bainbridge, OH Gas Migration Along Joints Gas Migration Along Bedding Planes St. Peter Sandstone (Ordovician), Dane County, Wisconsin outcrop sample St. Peter Sandstone (Ordovician), Dane County, Wisconsin outcrop sample n = 17.9 percent k = 2560 md, K = 6.98 ft/d @20oC • Quartz grains • No cement • Well sorted • Poorly graded Rose Run Sandstone (Ordovician), Scioto County, Ohio 4260 ft deep Rose Run Sandstone (Devonian), Scioto County, Ohio 4260 ft deep n = 15.8 % k = 54.8 md, K = 0.149 ft/d @ 20oC • Quartz and calcite grains (stained orange) • Compaction, little cement Beekmantown Dolomite (Ordovician), Coshocton County, Ohio 6884 ft deep k = 0.03 md, n = 3.8 % Beekmantown Dolomite (Ordovician), Coshocton County, Ohio 6884 ft deep n = 3.8 percent k = 0.03 md, K = 0.0000818 ft/d @ 20oC • Calcite (micrite) grains • Large pore filled with secondary cement Castle Hayne Limestone (Eocene), Brunswick County, North Carolina U.S. Geological Survey well #6 at 300.5 ft depth Castle Hayne Limestone (Eocene), Brunswick County, North Carolina U.S. Geological Survey strat well#6 at 300.5 ft depth
    [Show full text]
  • Oil and Gas Fields Map of Ohio
    STA5&0'0)*0 t %&PARTMENT OF NA563"-3&4063$&4 t %*7*4*0/0'(&0LOGICAL SUR7EY OIL AND GAS FIELDS MAP OF OHIO ASHTABULA ERIE WILLIAMS FULTON LUCAS LAKE GEAUGA OTTAWA LAKE WOOD TRUMBULL HENRY CUYAHOGA SANDUSKY DEFIANCE ERIE LORAIN PORTAGE HURON MEDINA SUMMIT PAULDING SENECA PUTNAM HANCOCK MAHONING VAN WERT WYANDOT CRAWFORD RICHLAND ASHLAND WAYNE ALLEN STARK COLUMBIANA HARDIN MERCER CARROLL MARION AUGLAIZE HOLMES MORROW TUSCARAWAS KNOX LOGAN JEFFERSON SHELBY UNION COSHOCTON HARRISON DELAWARE DARKE LICKING CHAMPAIGN MIAMI GUERNSEY MUSKINGUM BELMONT FRANKLIN MADISON CLARK PREBLE FAIRFIELD PERRY NOBLE MONTGOMERY MONROE GREENE PICKAWAY MORGAN FAYETTE BUTLER WARREN HOCKING WASHINGTON CLINTON ROSS ATHENS HIGHLAND VINTON HAMILTON CLERMONT PIKE MEIGS JACKSON N BROWN ADAMS GALLIA 0 10 20 30 40 miles SCIOTO 0 10 20 30 40 50 kilometers LAWRENCE EXPLANATION OIL FIELD GAS FIELD COALBED METHANE PRODUCING HORIZON(S) GROUPED BY STRATIGRAPHIC INTERVAL Pennsylvanian undifferentiated sandstones and coals Mississippian undifferentiated sandstones and Maxville Limestone Devonian Berea Sandstone and Cussewago Sandstone Devonian Ohio Shale and siltstones Silurian-Devonian “Big Lime” interval Silurian “Clinton/Medina” sandstone and “Packer Shell” Ordovician fractured shale, Trenton Limestone, Black River Group, and Wells Creek Formation Cambrian-Ordovician Knox Dolomite Recommended citation: Ohio Division of Geological Survey, 2004, Oil and gas fields map of Ohio: Ohio Department of Natural Resources, Division of Geological Survey Map PG-1, generalized page-size version with text, 2 p., scale 1:2,000,000. [Updated 2014.] OIL AND GAS FIELDS MAP OF OHIO Ohio has a rich history of oil-and-gas production that began as a natural seep. It is the trapped occurrences of hydrocarbons nearly 150 years ago.
    [Show full text]
  • 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)
    [Show full text]
  • 2001, No. 2 Newsletter
    A Quarterly Publication of the Ohio Department of Natural Resources, Division of Geological Survey 2001, No. 2 THE GEOLOGY OF OHIO—THE MISSISSIPPIAN by Michael C. Hansen cursory glance at Mississippian-age rocks in Ohio suggests a monotonous sequence of Apoorly fossiliferous shales and sandstones. Siberia But these rocks have been and continue to be of China economic importance to the state. They also form some of Ohio’s most spectacular geological scen- Laurentia ery, including cliffs, gorges, waterfalls, natural (North America) bridges, and rock-shelter caves. Mississippian rocks Baltica record a quiescent phase in Late Paleozoic conti- Australia nental collision and mountain building during most Ohio of the period, but provide a signal of the great South America revolution that occurred at the end of the Paleo- Africa India zoic Era: the rise of the Appalachian Mountains. During the Mississippian Period, which began about 360 million years ago and ended about 325 million years ago, Ohio was in equatorial latitudes and had a warm, tropical climate. Although the Continental configuration during Mississippian time. Modified from W. S. McKerrow and preserved fossil record of the Mississippian in C. R. Scotese, 1990, Revised World maps and introduction, in Palaeozoic Palaeogeography and Biogeography, Geological Society Memoir 12, fig. 17. Ohio is relatively poor, life flourished in the seas and, more importantly, gained a strong foothold on the land. of the state, primarily in Williams and Fulton Coun- As geologists began to study the sequence of ties; however, they are deeply buried beneath Paleozoic rocks in Europe, especially in Great thick glacial sediments and are not exposed at the Britain, they recognized a coal-bearing sequence of surface.
    [Show full text]
  • Black River Watershed Action Plan December 30, 2011
    Black River Watershed Action Plan December 30, 2011 Written By: Christina Znidarsic Former Black River Watershed Coordinator Lorain County Community Development Department (Sections I through- IV) And Coldwater Consulting, LLC With input from Chagrin River Watershed Partners, Inc. and the Lorain County Community Development Department (Sections V through IX) With technical assistance from: Christopher Alvarado, CCPC Marty Rowe, Lorain County Auditor’s Office Jim Boddy, LCGHD Nancy Funni, Lorain SWCD Ryan Kemper, NRCS Karl Schneider, NRCS Tom Holmes, ODNR Matt Adkins, ODNR OCM Brian George, ODNR OCM Steve Lewis, ODNR OCM Ted Conlin, Ohio EPA Bill Zawiski, Ohio EPA Liz Mather, WRLC Special Thanks to: Joe Reitz, Avon Lake Engineering Dept. Mike McNutt, Columbus Board of Health Betty Blair, Lorain County Commissioner Col. Matthew Nahorn, New Indian Ridge Museum Cheryl Wolfe, Oberlin College Greg Nageotte, ODNR Rosa Garcia-Gee, Sheffield Lake SUAB 1 Black River Watershed Action Plan Community Endorsement We support and agree to pursue implementation of this plan and agree to seek the necessary resources to improve and protect the water quality of the Black River. Amherst Township, Lorain County LaGrange Township, Lorain County Brighton Township, Lorain County Litchfield Township, Medina County Camden Township, Lorain County Liverpool Township, Medina County Carlisle Township, Lorain County New London Township, Huron County Chatham Township, Medina County New Russia Township, Lorain County City of Avon, Lorain County Olmsted Township, Cuyahoga
    [Show full text]
  • Data on the Thickness and Character of Certain Sedimentary Series in Ohio
    THE OHIO JOURNAL OF SCIENCE VOL. XXXIV NOVEMBER, 1934 No. 6 DATA ON THE THICKNESS AND CHARACTER OF CERTAIN SEDIMENTARY SERIES IN OHIO R. E. LAMBORN, Geological Survey of Ohio INTRODUCTION The total thickness of the sedimentary rocks in Ohio as measured on the outcrop is a little more than 5,000 feet. As the various series pass under cover away from the outcrop changes in thickness occur which can be determined by a study of data derived from well borings. Based on rather limited data of this type, various estimates have been made from time to time of the thickening of certain sedimentary series to the eastward in Ohio along designated lines.2 However, as deep well drilling has continued the quantity of available data has increased and a comparative study of some 8,500 well records now on file in the office of the Geological Survey of Ohio has yielded the results set forth in the following pages. Such data lack much that is to be desired in the way of scientific accuracy and detail, but nevertheless the close correspondence in essential fact of data derived from many sources argues for considerable accuracy in its major features. It is believed that the results of such a study will be of interest to geologists and to all who are engaged in the search for oil and gas. CLASSIFICATION OF THE SEDIMENTARY ROCKS OF OHIO The following table gives a brief classification of the sedi- mentary strata in Ohio and includes the name and character Published by permission of Mr.
    [Show full text]
  • Geology Field Trip Guide: an Upper Devonian-Lower Mississippian Sequence in Central Ohio, with Emphasis on the Bedford and Berea Formations
    104th Annual Meeting The Ohio Academy of Science Hosted by Otterbein College and Ross Products Division of Abbott Laboratories, Columbus Held at Otterbein College, Westerville APRIL 28,29,30,1995 GEOLOGY FIELD TRIP GUIDE: AN UPPER DEVONIAN-LOWER MISSISSIPPIAN SEQUENCE IN CENTRAL OHIO, WITH EMPHASIS ON THE BEDFORD AND BEREA FORMATIONS 8:00 AM, Sunday, April 30,1995 Arranged by: LAWRENCE A. KRISSEK and KENNETH P. COATS, The Ohio State University Transportation will be in private vehicles leaving from Roush Hall at Otterbein College at 8:00 AM to visit sites in Franklin and Delaware Counties. Lunch is on your own following the field trip. The Devonian and Lower Mississippian stratigraphic sequence exposed in central and east- central Ohio consists of the Columbus Limestone, the Delaware Limestone, the Olentangy Shale, the Ohio Shale, the Bedford Shale, the Berea Sandstone, and the Sunbury Shale. On this field trip we will examine portions of the above units at three localities: Camp Lazarus, Galena, and Rocky Fork. The Camp Lazarus locality contains exposures of the uppermost Columbus Limestone (low river level permitting), Delaware Limestone, Olentangy Shale, and lower Ohio Shale. The Galena locality contains exposures of the Ohio Shale-Bedford Shale contact and the lower Bedford Shale. The Rocky Fork locality contains exposures of the "Red Bedford", upper Bedford Shale, Berea Sandstone, and Sunbury Shale. During the Late Devonian and Early Mississippian, Ohio was located at approximately 10-15 degrees south latitude, and was covered by the shallow epeiric seas of the Appalachian Basin. The composite section we will observe on this trip represents a major transgressive-regressive sequence deposited in the western part of the basin, and is capped by the subsequent transgressive deposit of the Sunbury Shale.
    [Show full text]
  • Subsurface and Petroleum Geology Of
    SUBSURFACE AND PETROLEUM GEOLOGY OF ASHTABULA COUNTY, OHIO A Thesis Presented in Partial Fulfillment of the Requirements For the Degree Bachelor of Science by James W. Shoots The Ohio State University 1985 Approved by : A visor Department of Geology and Mineralogy CONTENTS ~ Introduction 1 The Precambrian Surface 3 The Cambrian Period 8 Ordovician and the Tippecanoe Sequence 12 The Lower Silurian and the Grimsqy Sandstone 14 Middle and Upper Silurian 19 Devonian Carbonates and Shales 22 Lower Mississippian Outcrop 26 Summary and Conclusions 28 Bibliography 29 INTRODUCTION Ashtabula County, Ohio is located in the very northeastern corner of the state (fig. 1). Its geographical boundaries include: Lake Erie to the north; Crawford and Erie Counties, Pennsylvania to the east; Trumbull County, Ohio to the south; and Geauga and Lake Counties to the west. All these surrounding areas were helpful in correlating well data to make inferences to trends that underlie Ashtabula County. The study area is located on the northwestern flank of the Appala­ chian Basin. This basin is an elongate structural trough trending northeast-southwest. It stretches from New York to Alabama. Cambrian seas deposited large sections of carbonates in a depression that developed on the Precambrian surface (ref. 9, p. 17). The Taconic orogeny of Late Ordovician time filled the basin with large quantities of clastic mater­ ial from the east and southeast. Again, in Middle Devonian time, new uplift, accompanying the Acadian Orogeny, deposited masses of marine and terrestrial materials in the same subsiding basin. A continuing orogeny, throughout the late Paleozoic, culminated in the Appalachian orogeny which occurred near the close of the Paleozoic (ref.
    [Show full text]