THE PLUMMER FIELD, GREENE COUNTY, INDIAN~".Iy
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Modern Shale Gas Development in the United States: a Primer
U.S. Department of Energy • Office of Fossil Energy National Energy Technology Laboratory April 2009 DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe upon privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. Modern Shale Gas Development in the United States: A Primer Work Performed Under DE-FG26-04NT15455 Prepared for U.S. Department of Energy Office of Fossil Energy and National Energy Technology Laboratory Prepared by Ground Water Protection Council Oklahoma City, OK 73142 405-516-4972 www.gwpc.org and ALL Consulting Tulsa, OK 74119 918-382-7581 www.all-llc.com April 2009 MODERN SHALE GAS DEVELOPMENT IN THE UNITED STATES: A PRIMER ACKNOWLEDGMENTS This material is based upon work supported by the U.S. Department of Energy, Office of Fossil Energy, National Energy Technology Laboratory (NETL) under Award Number DE‐FG26‐ 04NT15455. Mr. Robert Vagnetti and Ms. Sandra McSurdy, NETL Project Managers, provided oversight and technical guidance. -
Harrodsburg Limestone in Kentucky
Harrodsburg Limestone In Kentucky By E. G. SABLE, R. C. KEPFERLE, and W. L. PETERSON CONTRIBUTIONS TO STRATIGRAPHY GEOLOGICAL SURVEY BULLETIN 1224-1 Prepared in cooperation with the Com monwealth of Kentucky, University of Kentucky, Kentucky Geological Survey UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director U.S. GOVERNMENT PRINTING OFFICE, WASHINGTON : 1966 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 10 cents (paper cover) CONTENTS Fag* Abstract.________________________________________________________ II Introduction.____________________________-_--____--____-__--_-_--_ 1 History of nomenclature_________________ ______________________ 1 Harrodsburg Limestone redefined in Kentucky._______________________ 6 Round Hollow section__-__-___-_---____._-___-_----__-._.__--_.__ 7 Correlations._____________________________________________________ 11 References cited.................__________________________________ 11 ILLUSTRATIONS Pag» FIGURE 1. Stratigraphic nomenclature of selected Mississippian units in 12 northwest-central Kentucky __________________________ 2. Map of central Kentucky showing counties and topographic quadrangles referred to in this re port..____.___.._.__.__.__ 4 ill 799-251 66 CONTRIBUTIONS TO STRATIGRAPHY HARRODSBURG LIMESTONE IN KENTUCKY By E. G. SABLE, R. C. KEPFERLE, and W. L. PETERSON ABSTRACT The Harrodsburg Limestone (Mississippian) in northwest-central Kentucky consists of 20 to 50 feet of light-gray coarse-grained fossil-fragmental limestone and minor silty limestone. It underlies the Salem Limestone, overlies the Borden Formation, and includes the Leesville and Guthrie Creek Members, of the Lower Harrodsburg of P. B. Stockdale and the Harrodsburg (restricted) as used by him. INTRODUCTION The name Harrodsburg Limestone was given (Hopkins and Sieben- tlial, 1897) to a unit of predominantly carbonate rocks of Mississippian age in Indiana and was subsequently used in Kentucky. -
Reflection Seismic Profiling of the Wabash Valley Fault System in the Illinois Basin
Reflection Seismic Profiling of the Wabash Valley Fault System in the Illinois Basin U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1538-0 MISSOURI ~"3t3fc: «tr- ^t-i. ARKANSAS Cover. Gray, shaded-relief map of magnetic anomaly data. Map area includes parts of Missouri, Illinois, Indiana, Kentucky, Tennessee, and Arkansas. Illumination is from the west. Figure is from Geophysical setting of the Reelfoot rift and relations between rift structures and the New Madrid seismic zone, by Thomas G. Hildenbrand and John D. Hendricks (chapter E in this series). Reflection Seismic Profiling of the Wabash Valley Fault System in the Illinois Basin By R.M. Rene and F.L. Stanonis INVESTIGATIONS OF THE NEW MADRID SEISMIC ZONE Edited by Kaye M. Shedlock and Arch C. Johnston U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1538-O This research was jointly supported by the U.S. Geological Survey and ARPEX (Industrial Associates' Research Program in Exploration Seismology—Indiana University, University of Southern Indiana, Indiana Geological Survey) UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1995 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director For sale by U.S. Geological Survey, Information Services Box 25286, Federal Center Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging-in-Publication Data Rene, R.M. Reflection seismic profiling of the Wabash Valley fault system in the Illinois Basin / by R.M. Rend and F.L. Stanonis. p. cm.—(U.S. -
Proceedings of the Indiana Academy of Science
Geologic Contrasts in Indiana State Parks Otis W. Freeman, Indiana University The state parks of Indiana, with sites selected largely for scenic and historic reasons but partly with the intent to secure wide geo- graphical distribution for recreational purposes, contain a fairly com- plete sequence of the geological formations outcropping in the state, besides providing examples for a large majority of the physiographic principles. Evidence of vulcanism is one of the chief things missing, since all of the exposed bedrock in Indiana is of sedimentary origin. Even so, many types of igneous and metamorphic rocks can be picked up among the glacial boulders in the northern part of the state. The oldest exposed rocks are those of the Ordovician period. Ex- cellent outcrops for the study of the Ordovician strata occur in south- eastern Indiana on the west flank of the Cincinnati Arch. The beds are highly fossiliferous and one of the famous collecting grounds for the life forms of this period is near Madison. Clifty Falls State Park includes strata classified in the upper Or- dovician, the Silurian and base of the Devonian periods. The Silurian rocks occupy the hill slopes above the falls and inner gorges in the park with the Devonian capping the higher hills. The Ordovician formations in the park area from the base up- ward, begin with 25 feet of the Bellevue, followed by 115 feet of the Arnheim, 55 feet of the Waynesville, 50 feet of the Liberty, about 32 feet of the Saluda and possibly 6 feet of Whitewater. Shale predominates from the Bellevue through the Liberty and is interbedded with thin layers and lenses of limestone, and in contrast the Saluda is a thick bedded limestone with reef corals occuring near its base. -
The Lower Carboniferous Area
THE GEOLOGY OF The Lower Carboniferous Area OF SOUTHERN INDIANA. BY GEORGE HALL ASHLEY, PH. D., Assisted by EDW ARD M. KINDLE, PH. D. -49- LETTER OF TRANSMITTAL . INDIANAPOLIS, IND., January 15, 1902. Hon. W. S. Blatchley, State Geologist of Indiana: Sir-I have the honor to hand you herewith my report on the ge ology of the area of the Lower Carboniferous rocks of Bouthern Indiana. This work was planned, in accordanc'e with your instruc tions, primarily as a continuation of the survey of the Bedford Oolitic Limestone made north of Orange County in 1896. Pursuant to your instructions, however, the other members of the Lower Carboniferous have been mapped, and examined, 'especially for any strata of economic value. The most valuable part ot the report is believed to be given on the accompanying maps, which attempt to show the distribution of the different formations with as much or greater accuracy than has hitherto been attempted in this State. They also show graphic'ally the character of the topography by pro files, and the structure of the strata as a whole. In addition a columnar section is added. In order to complete the work in the time allotted it wa.s necessary to omit much work that would have been necessary for the mapping of the quaternary and the forma tion herein called the "Ohio River Formation," believed to be of Tertia,ry age. The field work occupied the season of 190(). The writer was assisted by Dr. Edward M. Kindle. 'rhe writer is entirely responsible for the maps and reports of Washington and Harrison counties. -
105Th Annual Report of the State Geologist
105TH ANNUAL REPORT OF THE STATE GEOLOGIST of INDIANA GEOLOGICAL SURVEY DEPARTMENT OF NATURAL RESOURCES for July 1, 1980 - June 30, 1981 1 GEOLOGICAL SURVEY ONE HUNDRED AND FIFTH ANNUAL REPORT OF THE STATE GEOLOGIST PERSONNEL Permanent Personnel Administration John B. Patton. • • . .•.•.State Geologist Maurice E. Biggs. .Assistant State Geologist Mary E. Fox • . • • • Mineral Statistician E. Coleen George. .Principal Secretary Coal and Industrial Minerals Section Dona ld D. Carr. • • • • . Geologist and Head Curtis H. Ault •• Geologist and Associate Head Pei-Yuan Chen • • • • .Geologist (To January 2, 1981) Donald L. Eggert. .Geologist Gordon S. Fraser. • .Geologist Denver Harper . • • • • . .Geologist Nancy R. Hasenmueller . Geologist (From February 2, 1981) Walter A. Hasenmueller•• • . •Geologist Nelson R. Shaffer • · . • . .Geologist Paul Irwin. • • Geological Assistant Janet Roller.. · .....Secretary Kathryn Shaffer . · . • • . Secretary Drafting and Photography Section William H. Moran. \I • • • . • . Chief Draftsman and Head Richard T. Hill • . .••Senior Geological Draftsman Roger L. Purcell. .Senior Geological Draftsman George R. Ringer. • • . • • • • Photographer Wilbur E. Stalions. .Geological Artist-Draftsman Educational Services Reevan Dee Rarick . • • • • . • . • • • • . .Geologist Geochemistry Section Richard K. Leininger. • .Geochemist and Head Margaret V. Golde · Instrument Analyst Joseph G. Hailer•.•. · . • . Geochemist 2 Jesse Hardin. · ••E1ectronic Technician (From September 29. 1980) Roger S. McCay .. .E1ectronic Technician -
2002 Ground-Water Resources in the White and West Fork White River Basin, Indiana
GROUND-WATER RESOURCES IN THE WHITE AND WEST FORK WHITE RIVER BASIN, INDIANA STATE OF INDIANA DEPARTMENT OF NATURAL RESOURCES DIVISION OF WATER 2002 GROUND-WATER RESOURCES IN THE WHITE AND WEST FORK WHITE RIVER BASIN, INDIANA STATE OF INDIANA DEPARTMENT OF NATURAL RESOURCES DIVISION OF WATER Water Resource Assessment 2002-6 Printed By Authority of the State of Indiana Indianapolis, Indiana: 2002 STATE OF INDIANA Frank O'Bannon, Governor DEPARTMENT OF NATURAL RESOURCES John Goss, Director DIVISION OF WATER Michael W. Neyer, Director Project Manager: Judith E. Beaty Editor: Judith E. Beaty This report was prepared by the Basin Studies Section Greg Schrader and Ralph Spaeth And The Ground Water Section Bill Herring, Glenn Grove, and Randy Meier For sale by Division of Water, Indianapolis, Indiana CONTENTS page INTRODUCTION . .1 Purpose and scope . .1 Previous investigations . .1 Acknowledgements . .3 GEOLOGY . .4 Sources of geologic data . .4 Regional physiography . .4 Overview of glacial history and deposits . .5 Summary of major Quaternary deposits . .9 Glacial terrains . .10 Bedrock geology . .12 Bedrock physiography . .13 Bedrock stratigraphy and lithology . .14 GROUND-WATER HYDROLOGY . .19 Ground-water resources . .19 Ground-water levels . .19 Potentiometric surface maps . .21 Aquifer systems . .21 Unconsolidated aquifer systems . .21 Tipton Till Plain Aquifer System . .24 Tipton Till Plain Aquifer Subsystem . .27 Dissected Till and Residuum Aquifer System . .29 White River and Tributaries Outwash Aquifer System . .29 White River and Tributaries Outwash Aquifer Subsystem . .29 Buried Valley Aquifer System . .30 Lacustrine and Backwater Deposits Aquifer System . .30 Bedrock aquifer systems . .30 Ordovician/Maquoketa Group . .31 Silurian and Devonian Carbonates . .32 Devonian and Mississippian/ New Albany Shale . -
Potentiometric Surface and Water Quality in the Principal Aquifer, Mississippian Plateaus Region, Kentucky
POTENTIOMETRIC SURFACE AND WATER QUALITY IN THE PRINCIPAL AQUIFER, MISSISSIPPIAN PLATEAUS REGION, KENTUCKY By P.O. Plebuch and Robert J. Faust, U.S. Geological Survey Margaret A. Townsend, Kentucky Geological Survey U.S. Geological Survey Water-Resources Investigations Report 84-4102 Prepared in cooperation with the KENTUCKY GEOLOGICAL SURVEY UNIVERSITY OF KENTUCKY Donald C. Haney, Director and State Geologist Louisville, Kentucky 1985 UNITED STATES DEPARTNENT OF THE INTERIOR WILLIAM P. CLARK, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director For additional information Copies of this report write to: can be purchased from: District Chief Open-File Services Section U.S. Geological Survey Western Distribution Branch Water Resources Division U.S. Geological Survey Room 572 Federal Building Box 25425 Federal Center 600 Federal Place Lakewood, CO 80225 Louisville, KY 40202 Telephone: (303) 234-5888 CONTENTS Page Abstract............................................................... 1 Introduction........................................................... 2 Purpose and scope.................................................. 2 Location and description of area................................... 3 General geologic framework of the principal aquifer.................... 3 Water in the principal aquifer......................................... 6 Occurrence......................................................... 6 Hydrogeology....................................................... 9 Residual mantle or residuum................................... -
Division of Geology Crushed Stone in Indiana
STATE OF INDIANA HENRY F. SCHRICKER, GOVERNOR DEPARTMENT OF CONSERVATION KENNETH M. KUNKEL, DIRECTOR INDIANAPOLIS DIVISION OF GEOLOGY CHARLES F. DEISS, STATE GEOLOGIST BLOOMINGTON ______________________________________ REPORT OF PROGRESS NO. 3 ________________ CRUSHED STONE IN INDIANA BY JOHN B. PATTON PRINTED BY AUTHORITY OF THE STATE OF INDIANA __________ BLOOMINGTON, INDIANA APRIL 1949 STATE OF INDIANA HENRY F. SCHRICKER, GOVERNOR DEPARTMENT OF CONSERVATION KENNETH M. KUNKEL, DIRECTOR INDIANAPOLIS DIVISION OF GEOLOGY CHARLES F. DEISS, STATE GEOLOGIST BLOOMINGTON ____________________________________ REPORT OF PROGRESS NO. 3 ________________________________________________________________________ CRUSHED STONE IN INDIANA by JOHN B. PATTON PRINTED BY AUTHORITY OF THE STATE OF INDIANA _______________________ BLOOMINGTON, INDIANA APRIL 1949 ___________________________________ For sale by the Division of Geology, Indiana Department of Conservation Bloomington, Indiana Price $ .50 CONTENTS Page Introduction . 1 Limestones quarried in southern Indiana. 2 Saluda limestone . 2 Whitewater formation. 3 Elkhorn formation. 3 Brassfield limestone . 3 Osgood formation . 4 Laurel limestone . 4 Louisville limestone . 4 Geneva dolomite . 5 Jeffersonville limestone . 5 Speed limestone. 6 Silver Creek limestone . 6 Beechwood limestone . 6 Borden reef material . 6 Harrodsburg lim stone . 7 Salem limestone . 7 St. Louis limestone . 8 Ste. Genevieve limestone. 8 Aux Vases sandstone. 9 Paoli limestone . 9 Beaver Bend limestone . 9 Beech Creek limestone. 9 Glen Dean limestone . 10 “Minshall limestone” . 10 “Maria Creek limestone” . 10 i Page Limestones quarried in northern Indiana. 11 Middle Ordovician rocks . 11 Mississinewa shale . 11 Liston Creek formation . 12 Huntington dolomite. 12 Kokomo limestone. 13 Kenneth limestone . 13 Devonian limestone (undifferentiated) . 14 Indiana crushed stone quarries . 14 Analyses . 40 Bibliography. 46 ILLUSTRATIONS Plate 1. Quarries producing crushed stone in Indiana . -
North American Geology
DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Bulletin 684 BIBLIOGRAPHY OF NORTH AMERICAN GEOLOGY FOB 1917 WITH SUBJECT INDEX BY JOHN M. NICKLES i WASHINGTON.' GOVEENMENT PHINTING OFFICE 191 5 CONTENTS. Introduction................................................................. 3 Serials examined........................................................... 5 Bibliography............................................................... 9 Outline of subject headinga................................................. 89 Index.................................................................... 93 Lists..................................................................... 135 Chemical analyses...................................................... 135 Minerals described..................................................... 136 Rocks described.. '...................................................... 138 Geologic formations described........................................... 139 2 BIBLIOGRAPHY OF NORTH AMERICAN GEOLOGY FOR 1917, WITH SUBJECT INDEX. By JOHN M. NICKLES. INTRODUCTION. The bibliography of North American geology, including paleon tology, petrology, and mineralogy, for the year 1917 follows the plan and arrangement of its immediate predecessors. It includes publications bearing on the geology of the Continent of North America and adjoining islands; also Panama and the Hawaiian Islands. Papers by American writers on the geology of other parts of the world are not included. -
OZARK UPLIFT PROVINCE (057) by Joseph R
OZARK UPLIFT PROVINCE (057) By Joseph R. Hatch INTRODUCTION The Ozark Uplift Province covers approximately 53,000 sq mi in eastern and southern Missouri (76 counties) and northern Arkansas (10 counties). The province is bounded on the north by the Iowa Shelf Province (052), on the east by the Illinois Basin Province (064), on the south by the Arkoma Basin Province (058), and on the west by the Cherokee Platform (060) and Forest City Basin (056) Provinces. The major structural element in the province is the domal Ozark Uplift, from which sedimentary rocks have been eroded, leaving approximately 350 sq mi of Precambrian granite exposed in the core area. The sedimentary cover in the Ozark Uplift Province averages less than 2000 ft and primarily consists of dolomites and sandstones of Cambrian and lower Ordovician age. A generalized stratigraphic column for the province is shown in figure 2. In the western part of the Ozark area, Mississippian rocks overlap lower Ordovician rocks, and Middle Ordovician, Silurian, and Devonian rocks are absent. Middle Ordovician, Middle Devonian, Mississippian, and Pennsylvanian rocks are generally present in the counties north of the Missouri River (Adler and others, 1971). One conventional hypothetical play has been defined for this province, Middle Ordovician (Champlainian) Play (5701). ACKNOWLEDGMENTS Scientists affiliated with the American Association of Petroleum Geologists and from various State geological surveys contributed significantly to play concepts and definitions. Their contributions are gratefully acknowledged. CONVENTIONAL PLAYS 5701. MIDDLE ORDOVICIAN (CHAMPLAINIAN) PLAY (HYPOTHETICAL) The hypothetical Middle Ordovician (Champlainian) Play in the Ozark Uplift Province is based on (1) current hydrocarbon production from age-equivalent rocks in the adjacent Illinois Basin and Forest City Basin Provinces (064 and 056); (2) the presence of potentially good to excellent hydrocarbon source rocks in the Middle Ordovician section; and (3) the presence of potential sandstone and porous dolomite and limestone reservoirs. -
W. John Nelson
TUR R W. John Nelson Department of Natural Resources ILLINOIS STATE GEOLOGICAL SURVEY BULLETIN 100 1995 BULLETIN 100 1995 ILLINOIS STATE GEOLOGICAL SURVEY illiam W. Shilts, Chief Natural Resources Building 615 East Peabody Drive Champaign, Illinois 61820-6964 Cover Photo Steeply tilted lower Pennsylvanian sandstone on the southeast side of the L,usk Creek Fault Zone near Manson Ford, about 5 miles northeast of Dixon Springs, Pope County. Photo by W. John Nelson. Graphic Artist - Sandra Stecyk Plates - Michael Knapp Printed by authority of the State of Illinois/l995/3000 @ printed with soybean ink on recycled paper Acknowledgments STRUCTURAL FEATURES IN ILLINOIS Abstract Introduction Guidelines for Naming Structures Removal of Names New Names Major Structural Features Basins, Arches, and Domes Folds and Faults Northern Illinois Western Illinois Eastern Illinois Southern Illinois Structural History Precambrian Cambrian Period Ordovician Period Silurian Period Devonian Period Mississippian Period Pennsylvanian Period Late Paleozoic (?) Compressional Events Mesozoic (?) Extensional Events Cretaceous to Recent Events STRUCTURAL FEATURES - CATALOG BIBLIOGRAPHY TABLES 1 Wells that reach Precambrian rocks in Illinois 2 167 structures recommended for removal from stratigraphic records 3 33 renamed structures shown as follows: (new name) 4 33 newly named structural features shown as follows: (new) 5 In situ stress measurements in Illinois 6 Silurian reefs in Illinois FIGURES 1 Regional structural setting of Illinois 2 Major structural features in Illinois and neighboring states 3 Oil fields and structure of the Beech Creek ("Barlow") Limestone in part of Clinton County 4 Wells that reach Precambrian rocks in Illinois 5 Generalized Precambrian geology of eastern and central United States 6 An interpretive cross section of Rough Creek Graben 7 Stratigraphiccolumn showing the units mentioned in the text 8 Paleogeography of Illinois during deposition of Mt.