DOCSLIB.ORG

GEOLOGY of the W M T E RANGLE POPE COUNTY, ILLINOI

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
GEOLOGY of the W M T E RANGLE POPE COUNTY, ILLINOI GEOLOGY OF THE WmTE RANGLE POPE COUNTY, ILLINOI C. Pius Weibel .W. John Nelson Lynne B. Oliver .Steven P. Esling Department of Energy and Natural Resources ILLINOIS STATE GEOLOGICAL SURVEY BULLETIN 98 1993 Southern Illinois University at Carbondale BULLETIN 98 1993 ILLINOIS STATE GEOLOGICAL SURVEY Morris W. Leighton, Chief 615 East Peabody Drive Champaign, IL 61820-6964 Cover photo Pounds Sandstone Member of the Caseyvllle Formation southwest of Rock in Pope County (photo by C. Pius Weibel) Printed by authority of the State of Illinois/1993/1200 ACKNOWLEDGMENTS ABSTRACT 1 INTRODUCTION Location Physiography Geologic Setting Previous Studies Method of Shrdy BEDROCK STRATIGRAPHY Mississippian System Undifferentiated Pope Group Golconda Formation Hardinsburg Sandstone Glen Dean Limestone Tar Springs Sandstone Vienna Limestone Waltersburg Formation Menard Limestone Palestine Sandstone Clore Forma tion Degonia Formation Kinkaid Limestone Mississippian-Pennsylvanian Unconformity Pennsylvanian System Caseyville Formation Wayside" Member Battery Rock Sandstone Member "Drury" Member Pounds Sandstone Member Tradewater Formation Lower shale and sandstone member Middle sandstone member Upper shaley member SURFICIAL GEOLOGY Introduction Methodology Field Methods Laboratory Methods Construction of the Stack-Unit Map Stratigraphy Lithostratigraphic Units: Upland Formations Oak formation Roxana Silt Peoria Silt Peyton Formation Lithostratigraphic Units: Valley Formations Equality Forma tion Cahokia Alluvium Pedostratigraphic Units Sangarnon Soil Farmdale Soil Buncombe Soil Resources Land Use Waste Disposal General Construction Seismic Risk STRUCTURAL GEOLOGY Lusk Creek Fault Zone Raum Fault Zone Hobbs Creek Fault Zone Flick Branch Fault Other Faults History and Origin of Faulting ECONOMIC GEOLOGY Fluorspar Limestone Sandstone Clay Petroleum Coal REFERENCES FIGURES Cooperative Geological Mapping Program (COGEOMAP), January 1993 Cultural features and drainages of the Waltersburg Quadrangle Map showing major structural features and the Illinois-Kentucky Fluorspar District in the vicinity of the Waltersburg Quadrangle Graphic column of Abner Field No. 1Well Graphic column of U.S. Government No. 1Well Graphic column of Truebger No. 3 Well Graphic column of COGEOMAP W-3 Well Basal chert bed of Degonia Forma tion Graphic column of Goreville Limestone Member of Kinkaid Limestone from an abandoned quarry Graphic column of U.S. Forest Service Eddyville guard station well Field sketch of deformed shale and thin bedded sandstone in "Wayside" member of Caseyville Formation Graphic column of COGEOMAP W-1 Well Graphic column of COGEOMAP W-2 Well Graphic column of "Drury" member of Caseyville Formation Pounds Sandstone Member of Caseyville Formation Graphic columns of measured sections in the Tradewater Formation within the Dixon Springs Graben Stratigraphic classification of the Quaternary deposits in the Waltersburg Quadrangle General locations of borings Vertical distribution of clay minerals and particle sizes for borhgs W2, W7, W3, W16, and W17 Cross section showing the distribution of the Quaternary ~tsin Flat Lick Valley Vertical distribution of clay minerals and particle sizes for borings W10, W12, and W9 Cross sections of Lusk Creek Fault Zone Cross sections of Raum Fault Zone Field sketch of deformed Tradewater strata in a stream bank Interpretive sketch of deformed Pounds Sandstone and Tradewater strata Origin of upthrown and downthrown slices in Lusk Creek Fault Zone Interpretive structural history of the Waltersburg Quadrangle 1 Location of wells used for bedrock study 7 2 Relation between modern soil series and Quaternary map units 23 3 Locations of borings 24 4 Chemical analyses of of channel sample of Tunnel Hill(?) Coal 38 The U.S. Geollogicd Survey (USGS), under the Cooperative Geological Mag- ping Program (COGEOMAP), provided significant support for the research reported in this publication. Annual grants from 1985 through 1991 provided partial funding for the project, Geologic Mapping Along the Southern Clo- sure of the Illinois Basin. The geologic mapping of sixteen 7.5-minute quad- rangles and the publication of quadrangle maps (1:24,OUO scale) and the accompanying reports were the objectives of this project. Joseph A. Devera (ISGS) mapped a part of the bedrock in the northwest comer of the quadrangle. Russel Peppers (ISGS) analyzed the palynology of the coals and provided biostratigraphic data. James W. Baxter (ISGS), Russell J. Jacobson OSGS), and Charles M. Rice (USGS) carefully critiqued the geo- logic map. Heinz H. Damberger, as project leader of COGEOMAP, provided continuous encouragement and advice. Finally, we are grateful to the private landowners who allowed us to enter their property to examine outcrops and especially to those who allowed us to drill the stratigraphic tests. Bedrock outcrops of the Waltersburg Four northeast-trending parallel the fault zones, occur between these 7.5-Minute Quadrangle in Pope fault zones transect the quadrangle. WOfault planes. County, southeastern Illinois, con- These post-Pennsylvanian faults are The principal mineral. resources sist mainly of upper Mississippian part of a regional northeast-trending in the quadrangle are sandstone for (Chesterian) and lower Pennsyl- fault system in the west part of the construction and limestone for con- vanian (Morrowan to early Atokan) Illinois-Kentucky Fluorspar District. struction and agriculture. Small strata. The Chesterian strata consist The Lusk Creek Fault Zone bounds shallow deposits of fluorspar and as- of fine grained clastic rocks and the northwest side of the Dixon sociated minerals have been mined limestones of the upper Pope Group Springs Graben, and the Hobbs locally, suggesting that unknown and include the Golconda Forma- Creek Fault Zone bounds the south- deeper resources may occur along tion up to the Kinkaid Limestone. east side. The Raum Fault Zone par- faults in the quadrangle. The The Pennsylvanian strata consist of allels the Lusk Creek and Hobbs amount of coal resources is small; the sandstonedominated Caseyville Creek Fault Zones and bisects the coal beds are too thin and discon- and Tradewater Formations. Upper Dixon Springs Graben. The Flick tinuous to exploit economically, al- Valmeyeran limestones occur within Branch Fault (new name) occurs though a few small coal mines have thin fault slices. A petroleum explo- southeast of the Hobbs Creek Fault operated in the past. Three explora- ration well reached the Devonian Zone. The geologic structure of the tion wells for oil and gas have been Lingle Limestone, the oldest known quadrangle is the result of several drilled and all were abandoned. Res- bedrock in the Waltersburg Quad- episodes of deformation. Rifting dur- ervoir characteristics of buried, pre- rangle. The well also drilled through ing the Cambrian Period resulted in upper Mississippian strata are the New Albany Shale, several normal faulting along the Lusk unknown within the quadrangle. lower (Kinderhookian) and middle Creek Fault. Additional normal fault- Laterally extensive aqtlifers and (Valmeyeran)Mississippian forma- ing may have occurred during the economic deposits of sand and tions, and the lowermost Pope Early Pennsylvanian. A post-at oh gravel aggregate are not present Group. compressional episode resulted in re- among the surficial materials. The Extensive Pleistocene (Illinoian verse faulting along the Lusk Creek geology of the area is unsuitable for and Wisconsinan) deposits cover and Raum Fault Zones (which landfills unless measures are taken much of the bedrock. The uplands merge at depth). Final deformation to prevent migration of leachate. are covered by bedrock residuum was an extensional episode, during Properly designed construction pro- (Oak formation) and loess (Roxana which normal faulting occurred jects can be sited throughout most of and Peoria Silts): the slopes by collu- along the same fault planes or along the quadrangle. The study area lies vium (Peyton Formation), and the adjacent fault planes. Narrow slices in a zone of high seismicity; struc- valleys by lacustrine (Equality For- of rock, which are older or younger tures built in valley bottoms are mation) and alluvial deposits (Ca- than the strata on adjacent sides of more at risk than structures having hokia Alluvium). foundations in bedrock. This study was conducted as part of larly of the Caseyville Formation. and E 1/2 SE, Section 11, T12S, R6E. the ongoing Cooperative Geologic Streams eroding the Pennsylvanian Upland exposures of Mississippian Mapping Program (COGEOMAP), and thick Mississippian sandstones strata are generally above 500 feet which is jointly supported by the have formed narrow valleys or can- rnsl; exposures of Pennsylvanian United States Geological Survey yons, whereas those eroding Missis- strata are generally above 600 feet (USGS) and the Illinois State Geo- sippian limestones, shales, and msl. Bottomlands are generally be- logical Survey (ISGS). This report is thin sandstones have formed broad, tween 350 and 400 feet msl. The low- a companion to the Waltersburg Geo- open valleys. Thicker Mississippian est elevation is less than 320 feet rnsl logic Quadrangle of Weibel et al. limestones are locally characterized in the southeast corner of the quad- (1992) and is one of a series of ISGS by a karst topography and drainage rangle along Eusk Creek. Total relief maps and reports on the geology of system. is 460 feet, although local relief is southern Illinois (fig. 1). This geo- The highest elevations in the typically
Load more

Recommended publications
  • Environmental Overview Data
    ENVIRONMENTAL OVERVIEW DATA for LYON and CALDWELL COUNTIES US 641 CORRIDOR FROM EDDYVILLE TO FREDONIA ITEM NUMBER: NOT ASSIGNED Prepared For KENTUCKY TRANSPORTATION CABINET DIVISION OF PLANNING Prepared By Palmer Engineering 400 Shoppers Drive Winchester, Kentucky 40392 859-744-1218 JUNE 2004 Revised July 2004 TABLE OF CONTENTS Introduction....................................................................................................................................1 General Characteristics of the Project and Project Area ..........................................................1 Project Description and Purpose......................................................................................1 Project Area Physiological and Soils Characteristics.....................................................4 Project Area Water Resources .........................................................................................7 Project Area Land Use ......................................................................................................7 Environmental Overview Considerations....................................................................................7 Land Use .........................................................................................................................................7 Air Quality Considerations ...............................................................................................8 Highway Noise Considerations .........................................................................................9
    [Show full text]
  • IC-29 Geology and Ground Water Resources of Walker County, Georgia
    IC 29 GEORGIA STATE DIVISION OF CONSERVATION DEPARTMENT OF MINES, MINING AND GEOLOGY GARLAND PEYTON, Director THE GEOLOGICAL SURVEY Information Circular 29 GEOLOGY AND GROUND-WATER RESOURCES OF WALKER COUNTY, GEORGIA By Charles W. Cressler U.S. Geological Survey Prepared in cooperation with the U.S. Geological Survey ATLANTA 1964 CONTENTS Page Abstract _______________________________________________ -··---------------------------- _____________________ ----------------·----- _____________ __________________________ __ 3 In trodu ction ------------------------------------------ ________________________________ --------------------------------------------------------------------------------- 3 Purpose and scope ------------------------------"--------------------------------------------------------------------------------------------------------- 3 Previous inv es tigati o ns ____ _____ ________ _______ __________ ------------------------------------------------------------------------------------------ 5 Geo Io gy _________________________________________________________________ --- ___________________ -- ___________ ------------- __________________ ---- _________________ ---- _______ 5 Ph ys i ogr a p hy ______________________________________________________ ---------------------------------------- __________________ -------------------------------- 5 Geo Io gi c his tory __________________________ _ __ ___ ___ _______ _____________________________________________ ------------------------------------------------- 5 Stratigraphy -·· __________________
    [Show full text]
  • 106Th Annual Report of the State Geologist
    106TH ANNUAL REPORT OF THE STATE GEOLOGIST of INDIANA GEOLOGICAL SURVEY DEPARTMENT OF NATURAL RESOURCES for July 1, 1981 - June 30, 1982 GEOLOGICAL SURVEY ONE HUNDRED AND SIXTH ANNUAL REPORT OF THE STATE GEOLOGIST PERSONNEL Permanent Personnel Administration John B. Patton •.•••• • .•.•••••••••.. State Geo 1og i st Maurice E. Biggs •. Assistant State Geologist Mary E. Fox • • • • • • • • . • . • . • • • • • • . •Mineral Statistician E. Co leen George. • . • . • . • • . • . • . • • • • • Principal Secretary Coal and Industrial Minerals Section Donald D. Carr .•• • •••.•••Geologist and Head Curtis H. Ault ••. .Geologist and Associate Head Donald L. Eggert. • Geologist Gordon S. Fraser •••••• • .•.• Geologist Denver Harper • • · .••• Geologist Nancy R. Hasenmueller .•...• • Geologist Wa 1ter A. Hasenmue 11 er. • • . .••••• Geologist Paul Irwin (Reclamation). • Geologist Nelson R. Shaffer ••• • Geologist Michele Wright (NRC) •. • • Geo log ist Janet Roller ••• · . • • • Secretary (To August 14, 1981) Susan E. Rumple . • • • . • Secretary (From August 12, 1981) Kathryn Shaffer • • . • • . • • Secretary Drafting and Photography Section William H. Moran. ••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 D. Rarick .•••. .•••.•.•. Geologist 1 Geochemistry Section Richard K. Leininger. Geochemist and Head Margaret V. Golde •.••. • .Instrument Analyst
    [Show full text]
  • Omaha Pool and Mica-Periodotite Intrusives, Gallatin County, Illinois
    lb 14.GS: RPI 130 c. 2 STATE OF ILLINOIS DWIGHT H. GREEN, Governor DEPARTMENT OF REGISTRATION AND EDUCATION FRANK G. THOMPSON, Director DIVISION OF THE STATE GEOLOGICAL SURVEY M. M. LEIGHTON, Chief URBANA REPORT OF INVESTIGATIONS—NO. 130 OMAHA POOL AND MICA-PERIDOTITE INTRUSIVES, GALLATIN COUNTY, ILLINOIS BY R. M. ENGLISH and R. M. GROGAN Reprinted from STRUCTURE OF TYPICAL AMERICAN OIL FIELDS, VOLUME III Amer. Assoc. Petrol. Geol. (April, 1948), pp, 189-212 PRINTED BY AUTHORITY OF THE STATE OF ILLINOIS URBANA, ILLINOIS 1948 ORGANIZATION STATE OF ILLINOIS HON. DWIGHT H. GREEN, Governor DEPARTMENT OF REGISTRATION AND EDUCATION HON. FRANK G. THOMPSON. Director BOARD OF NATURAL RESOURCES AND CONSERVATION HON. FRANK G. THOMPSON, Chairman W. H. NEWHOUSE, Ph.D., Geology ROGER ADAMS, Ph.D., D.Sc, Chettiistry LOUIS R. HOWSON, C.E., Engineering A. E. EMERSON, Ph.D., Biology LEWIS H. TIFFANY, Ph.D., Forestry GEORGE D. STODDARD, Ph.D., Litt.D.. LL.D., L.H.D. » President of the University of Illinois GEOLOGICAL SURVEY DIVISION M. M. LEIGHTON, Ph.D., Chief (53430-2M) SCIENTIFIC AND TECHNICAL STAFF OF THE STATE GEOLOGICAL SURVEY DIVISION 100 Natural Resources DuUding, Urbana M. M. LEIGHTON, Ph.D., Chief Enid Townley, M.S., Assistant to the Chief Helen E. McMorris, Secretary to the Chief Velda a. Millard, Junior Asst. to the Chief Elizabktii Stephens, B.S., Geological Assistant GEOLOGICAL RESOURCES GEOCHEMISTRY Arthur Bevan, Ph.D., D.Sc, Principal Geologist in Frank H. Reed, P H.D., Chief Chemist Charge Gkace C. Johnson, B.S., Research Assistant Coal Coal G. H. Cady, Ph.JJ., Senior Geologist and Head G.
    [Show full text]
  • Geology and Resources of Fluorine in the United States
    Geology and Resources of Fluorine in the United States GEOLOGICAL SURVEY PROFESSIONAL PAPER 933 COVER PHOTOGRAPHS 1. Asbestos ore 8. Aluminum ore, bauxite, Georgia 1 2 3 4 2. Lead ore, Balmat mine, N . Y. 9. Native copper ore, Keweenawan 5 6 3. Chromite-chromium ore, Washington Peninsula, Mich. 4. Zinc ore, Friedensville, Pa. 10. Porphyry molybdenum ore, Colorado 7 8 5. Banded iron-formation, Palmer, 11. Zinc ore, Edwards, N. Y. Mich. 12. Manganese nodules, ocean floor 9 10 6. Ribbon asbestos ore, Quebec, Canada 13. Botryoidal fluorite ore, Poncha Springs, Colo. 11 12 13 14 7. Manganese ore, banded rhodochrosite 14. Tungsten ore, North Carolina Geology and Resources of Fluorine in the United States Edited by DANIEL R. SHAWE With sections by D. R. SHAWE, R. E. VAN ALSTINE, R. G. WORL, A. V. HEYL, R. D. TRACE, R. L. PARKER, W. R. GRIFFITTS, C. L. SAINSBURY, and J. B. CATHCART GEOLOGICAL SURVEY PROFESSIONAL PAPER 933 An evaluation of the geochemistry, geographic distribution, and geologic environments of fluorine, and descriptions of major United States fluorine mineral deposits UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1976 UNITED STATES DEPARTMENT OF THE INTERIOR THOMAS S. KLEPPE, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 76-600061 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02901-4 APPRAISAL OF MINERAL RESOURCES Continuing appraisal of the mineral resources of the United States is conducted by the U.S. Geological Survey in accordance with the provisions of the Mining and Minerals Policy Act of 1970 (Public Law 91-631, Dec.
    [Show full text]
  • Welge-Bg.Pdf (2.59
    BEDROCK GEOLOGY OF WELGE QUADRANGLE Illinois Department of Natural Resources Illinois Geologic Quadrangle Map ILLINOIS STATE GEOLOGICAL SURVEY RANDOLPH AND JACKSON COUNTIES, ILLINOIS IGQ Welge-BG William W. Shilts, Chief W. John Nelson 2007 Mk & e" 175 e" 84 sm o3 h &cv 164k" 170 k" k" 262 ^ ^ þ þüþü þ 2o o &c &s 250 h o 3 250 9 970 e" &cv -1 351e" Sª 00 136 k820 200 k" &t 62 k" 1 5 0 5 -5 N 0 J N 1 123 0 N J 757 0 e" J N N 0 J J N ª J N 0 350 J N oN J k" 87 k" Mc J S 377N 45 J k" 162 136 Mk NJ 165 N k 161 e" e" J 226 N J e" k" N S 677 J k Mk 161 145k" k"161 GS S 849 398 163 N 250 N 55 e" J k k J e" e" e" 142 k"164 172 S 395 143 k" Md S 411 i N k"142 J N N 130 k" ª J J NJ NJ NJ N N S J J N N 486 J J NJ N N J J NJ N 300 ª J N MASTER FAULT, J N &t k"46 COTTAGE GROVE FAULT SYSTEM J NJ N 205 Md 143 J 250 135 k" S k" k" N k" 41 k" k372 J 103 NJ 20 164 " 104 k k" N 0 15 J e" 248 0 EXPLANATION 150 e" e" 138 256 160 e" 5 k" 204k" k" 10 0 449 201 k" 0 350 k" 60 225 k" k"123 211 182 k" J N &cv sm Surface-mined area " k" 142 133 e k" 122 ª 150 k" 150 610 k" 150k" N e" J k" 200 &s Shelburn Formation 205 N k" J 136 k" 15 k" 0 146 142 Mk k" 282 h N k" S J 151e" ª k"153 k" &c Carbondale Formation 759 190 Desmoinesian J G 2165 N N Ü Mp J ª h, Herrin Coal Member N Mc 258 Pennsylvanian J k" N J k"123 N J J &t Tradewater Formation N &cv N J N J &cv N Md 205 J Unconformity k" N 25 J e"175 Md J N 0 J N N N J Morrowan J &cv Caseyville Formation Mps 30 Md N 730 k" J J o G N 152 N J k" N Unconformity N J J 110 " Sk e" k e" S 154 202 " k"164 S 724 e" k k" 129
    [Show full text]
  • Publications of the Illinois State Geological Survey
    LINv -~ ... t·,.;l.' iGtC.Ai. s SURVEY. LI JlAA'( 14.GS: CIR 340 OH A c. 1 STATE OF ILLINOIS DEPARTMENT OF REGISTRATION AND EDUCATION LATE MISSISSIPPIAN SANDSTONES OF ILLINO.IS Paul Edwin Potter ILLINOIS STATE GEOLOGICAL SURVEY URBANA CIRCULAR 340 1962 LATE MISSISSIPPIAN SANDSTONES . OF ILLINOIS Paul Edwin Potter ABSTRACT Sandstones, one of the distincti ve lithologies of the late Mississippian sediments ofthe Illinois Basin, constitute approx­ imately one-fourth of the section. The sandstones consist chiefly of well sorted and moderately well rounded, mineralogically stable detrital grains and their chief sedimentary structures are cross-bedding and ripple marks. The sandstones occur as sheets and as four types of elon­ gate sand bodies: pods, ribbons, dendroids, and belts. Detailed local maps showing the thicknes s of sand of the Degonia, Waltersburg, and Cypres s Formations and regional maps for the Degonia, Palestine, Waltersburg, and Hardinsburg For­ mationsdisplay the recurring types of sand bodies and emphasize the·essential similarity of all the late Mississippian sandstones. This similarity is a basis for better understanding and improved prediction of sandstone trends. Data gained from the study of the sandstones integrates well with other known features relative to paleogeography of late Mississippian time. INTRODUCTION Sandstones are an important constituent in the late Mississippian rocks of the Illinois Basin. They occur not only "in the Chesterian (Upper Mississippian) Series but also in the upper part of the Valmeyerian (Middle Mississippian) Series. The sandstone-bearing sediments in both series have been placed in the Pope Megagroup by Swann and Willman (1961), but are generally referred to in this paper as late Misslssippian.
    [Show full text]
  • Airphoto Interpretation of Engineering Soils of Interstate Route I-64
    AIRPHOTO INTERPRETATION OF ENGINEERING SOILS OF INTERSTATE HIGHWAY ROUTE 64 BETWEEN SCALESVILLE AND NEW ALBANY IN WARRICK, SPENCER, DUBOIS, PERRY, CRAWFORD, HARRISON AND FLOYD COUNTIES, INDIANA SEPTEMBER 1965 NO. 24 Digitized by the Internet Archive in 2011 with funding from LYRASIS members and Sloan Foundation; Indiana Department of Transportation http://www.archive.org/details/airphotointerpre6524yehp Progress Report AIRPHOTO INTERPRETATION OF EKGIMEERIKG SOILS INTERSTATE ROUTE 1-64? BETWEEN SCALESVILLE AND NEW ALBANY IN WARRICK, SPENCER, DUBOIS, PERSY, CRAWFORD, HARRISON AND FLOYD COUNTIES, INDIANA Tos G. A. Leonards, Director Joint Highway Research Project September 24, 1965 Frooj H. L Michael, Associate Director Files 1-5-5 Joint Highway Research Project Project: C-36-51E The steadied report entitled "Airphoto Interpretation of Engineering Soils of Interstate Route 1-64 between Scalesville and New Albany in Warrick, Spencer, Dubois, Perry, Crawford, Harrison and Floyd Counties, Indiana," completes the project concerned with engineering soils napping of the Interstate system from aerial photographs This project was prepared as a part of an investigation conducted by Joint Highway Research Project in cooperation with the Indiana State Highway Coaaisslon, the Bureau of Public Roadn and the Soil Conservation Service. The report was prepared by P. T. Yeh Research Engineer, Joint Highway Research Project The soil mapping of 1-64 between Scslesville and flew Albany was done entirely by airphoto interpretation technique To Increase the value, the soil strip nap was prepared on a photographic base with annotation to show soil areas The generalized soil profiles were .prepared from the available literature. Respectfully submitted. ?/? 7*~A~S H. L.
    [Show full text]
  • Paleozoic Geology of the New Madrid Area
    NUREG/CR-2909 I ..Paleozoic Geology of the New Madrid Area Prepared by H. R. Schwalb Illinois State Geological Survey Prepared for U.S. Nuclear Regulatory Commission NOTICE 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, or any of their employees, makes any warranty, expressed or implied, or assumes any legal liability of re- sponsibility for any third party's use, or the results of such use, of any information, apparatus, product or protess disclosed in this report, or represents that its use by such third party would not infringe privately owned rights. Availability of Reference Materials Cited in NRC Publications Most documents cited in NRC publications will be available from one of the following sources: 1. The NRC Public Document Room, 1717 H Street, N.W. Washington,'DC 20555 2. The NRC/GPO Sales Program, U.S. Nuclear Regulatory Commission, Washington, DC 20555 3. The National Technical Information Service, Springfield, VA 22161 Although the listing that follows represents the majority of documents cited in NRC publications, it is not intended to be exhaustive. Referenced documents available for inspection and copying for a fee from the NRC Public Docu- ment Room include NRC correspondence and internal NRC memoranda; NRC Office of Inspection and Enforcement bulletins, circulars, information notices, inspection and investigation notices; Licensee Event Reports; vendor reports and correspondence; Commission papers; and applicant and licensee documents and correspondence. The following documents in the NUREG series are available for purchase from the NRC/GPO Sales Program: formal NRC staff and contractor reports, NRC-sponsored conference proceedings, and NRC booklets and brochures.
    [Show full text]
  • 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 .
    [Show full text]
  • Description of the Bessemer and Vandiver
    DESCRIPTION OF THE BESSEMER AND VANDIVER INTRODUCTION the west of the Appalachian Plateaus are the Interior Low mentary, including limestone, dolomite, conglomerate, sand­ LOCATION AND EXTENT OF THE AREA Plateaus, which are included in the Interior Plains by the stone, and shale, which have been greatly disturbed by folding United States Geological Survey but which in the opinion of and faulting, as hereinafter described. The Bessemer and Vandiver quadrangles, which are called some, including the writer, should be included in the Appala­ in this folio the Bessemer-Vandiver area, are in Jefferson and chian Highlands. SUBDIVISIONS IN ALABAMA Shelby counties in the north-central part of Alabama. (See The boundary between the Piedmont and Blue Ridge Gahaba Ridges. Although the province is in general a fig. 1.) The area is bounded by parallels 33° 15' and 33° provinces is the east foot of the Blue Ridge and the foot of valley, there are within it many high ridges that extend the high but irregular eastern scarp of the mountains of west­ parallel to its general direction, of which Red Mountain is a ern North Carolina and northern Georgia which form the good example. These ridges are generally grouped along the southern extension of the Blue Ridge. The boundary between west side of the valley from New York to Alabama. In Ala­ the Blue Ridge and Appalachian Valley provinces is the west bama the ridge section includes all the valley west of the east foot of the Blue Ridge of Virginia and of the high mountains margin of the Coosa coal field and of a line in continuation of of eastern Tennessee.
    [Show full text]
  • Areal Geology of the Illinois Fluorspar District
    STATE OF ILLINOIS DEPARTMENT OF REGISTRATION AND EDUCATION AREAL GEOLOGY OF THE ILLINOIS FLUORSPAR DISTRICT Part 3 - Herod and Shetlerville Quadrangles James W. Baxter George A. Desborough Chester W. Shaw ILLINOIS STATE GEOLOGICAL SURVEY John C. Frye, Chief URBANA CIRCULAR 413 1967 AREAL GEOLOGY OF THE ILLINOIS FLUORSPAR DISTRICT Part 3 - Herod and Shetlerville Quadrangles James W. Baxter, George A. Desborough, and Chester W. Shaw ABSTRACT This report and map of the Herod and the Illinois part of the Shetlerville 7;-minute Quadrangles complete the geologic remapping of the Illinois fluorspar district. These quadrangles include portions of eastern Pope, westernHar- din, and southern Saline Counties and comprise the west- ern part of the mineralized district. Twenty-nine sedimentary rock units ranging from Lower Devonian to middle Pennsylvanian in age, and two units of Pleistocene age, are differentiated on the geologic map. In addition, the top and bottom of major sandstone members within formations of Pennsylvanian age are delin- eated wherever possible. The Herod and Shetlerville Quadrangles occupy a position on the north and west flanks of a large domal anti- cline that extends southeastward from the Shawneetown- Rough Creek Fault Zone in northern Pope, southern Saline, and southernGallatin Counties into Kentucky. Hicks Dome, subsidiary to the domal anticline, but located on its axis, forms a structural apex on the eastern margin of the Herod Quadrangle. North and west of Hicks Dome, the strata dip into the Moorman-Eagle Valley Syncline. Hicks Dome lies between two major northeast-trend- ing grabens that transect the domal anticline-the Rock Creek Graben on the east and the Dixon Springs Graben on the west.
    [Show full text]