Environmental Overview Data
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
Jlogy of the Waltersburg Quadrangle Pope County, Illinois
JLOGY OF THE WALTERSBURG QUADRANGLE POPE COUNTY, ILLINOIS W Joh Ne ls on W ib l . C . Piu s e e n Oliv e r St v P . Eslin Lynne B . e en g Department of Energy and Natural Resources ILLINOISSTATEGEOLOGICAL SURVEY BULLETIN 98 1993 GEOLOGY OF THE WALTERSBURG QUADRANGLE POPE COUNTY , ILLINOIS i l W Joh N ls o C . Piu s We be . n e n Illinois Sta te Geological Survey liv r St v P . Eslin Lynne B . O e e en g Southern Illinois Univ ersity at Carbondale BULLETIN 98 1993 ILLINOIS STATE GEOLOGICAL SURVEY W i rris . L i Mo e ghton, Ch ef 615 East Peabody Drive a i 61820—69 Ch mpa gn, IL 64 Cover photo Pounds Sandstone Member of the Caseyville Formation southwest f R k P We b l o oc in Pope County (photo by C . ius i e ) Printed by authority of the State of Illinois/ 1993/ 1200 CONTENTS ACKNOWLEDGMENTS ABSTRACT INTRODUCTION Location Physiography Geologic Setting Previous Studies Method of Study BEDROCK STRATIGRAPHY Mississippian System Undifferentiated Pope Group Golconda Formation Ha rdinsburg Sandstone Glen Dean Limestone Tar Springs Sandstone Vi enna Limestone Waltersburg Formation Menard Limestone Palestine Sandstone Clore Formation De gonia 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-Uni t -
Bedrock Geology of Herod Quadrangle
BEDROCK GEOLOGY OF HEROD QUADRANGLE ILLINOIS STATE GEOLOGICAL SURVEY POPE, SALINE, AND HARDIN COUNTIES, ILLINOIS STATEMAP Herod-BG E. Donald McKay III, Interim Director F. Brett Denny, W. John Nelson, and Joseph A. Devera 2008 A ( o ( 15 o ( N J 10 ( Mk ª &cv Mdc EXPLANATION & o t ( Mm &t 18 o5 ( 25 ( Mp &t N J o ( 7 Igneous dikes, Permian P(i) Leonardian NJ ( o ( sills, and pipes Mk ? 4 ( 5 o Mk o ( Unconformity ( & J t N J N G ( H &cv &t Mu Mp o ( Mm &t Tradewater Formation Atokan NJ &t ( &cv 38 o e Mdc ( Mp Pennsylvanian NJ ( 10 ( S AB Land #1 ( ªÜ &cv Caseyville Formation 12 NJ 930 Morrowan o ( H King #1 o o 6 G 4 ( o 40 Unconformity Æ o 20 N J o 3 ( G 35 o &cv Ü 5 Mk Kinkaid Limestone ( ª 3172 o N J ANTICLINE Æ &t N J ( 8 ( o H Mdc Ä Degonia Sandstone N J ( G Mdc TON HILL and Clore Formation N J ? ( HOR Mp N Mk Jas Cox J 3 &cv o ( 25 Ü ª N o 476 J &cv JN ( Mk 2 Mp Palestine Formation N Mm J o ( 20 Ä o N J e 17 ( o Ä Æ &cv P(i) Mm Menard Limestone ? ( &cv H 8 ( Mp o Mdc N K G J RMIC o8 Waltersburg Fm, Vienna Ls, McCO ( Mwvt o Mk ANTICLINE T ZONE o and Tar Springs Ss UL ( 8 10 Mp N Unconformity Mdc Mk J o7 Mk Mm ( T ZONE UL Mdc Mgd Glen Dean Limestone ( Mp Mwvt WN FA N o J O ( 4 &t 10 Mgd ( OD FA o J N Mh Hardinsburg Sandstone Chesterian N WNEET J Mh J ( &t HER N o J Mm N SHA 4 5 Mwvt ( J Ä o N N Mwvt J o9 Mg Golconda Formation J N Mdc J &cv N J N Mm N J Mgd J N Mwvt Mh J Mp N o9 Mississippian Mcy Cypress Sandstone 3 Mg o N k J 142 Mk J Rose Creek Jacob Hamp N ½ N Unconformity J N J 14 k ½ o Mh k 1045 Mcy o Ridenhower Formation and &cv 22 Mrb J N J Hamp N Bethel Sandstone J N Mines½ Æ N J Williams ½ ½ Mk Mg Mrb ½ J ½ Mdc N Downeys Bluff Limestone, N J N J ½ N J J N J Mdc N 7 Mdyr ½ Mdyr Yankeetown Sandstone, 11 N J o J Mav N Mk 10 and Renault Limestone o o &cv N 10 J o N J Mh J J N J N Mp N Mk o N Mav J Aux Vases Sandstone N P(i) J J N ( N J J N J J 24N N J N N J ( Mgd Mk Mdc &cv Mdyr N Ste. -
Stratigraphy and Structure of the Western Kentucky Fluorspar District
Stratigraphy and Structure of the Western Kentucky Fluorspar District GEOLOGICAL SURVEY PROFESSIONAL PAPER Prepared tn cooperation with the Geological Surrey Stratigraphy and Structure of the Western Kentucky Fluorspar District 53? Robert D. Trace and Dewey H. Amos CONTRIBUTIONS TO THE GEOLOGY OF KENTUCKY GEOLOGICAL SURVEY PROFESSIONAL PAPER 1151-D Prepared in cooperation with the Kentucky Geological Survey Mississippian and Pennsylvanian limestone and clastic rocks are exposed in northeast- trending horsts and grab ens UNITED STATES GOVERNMENT PRINTING OFFICE, W ASH I NGT O N : 1984 UNITED STATES DEPARTMENT OF THE INTERIOR WILLIAM P. CLARK, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Trace, Robert Denny, 1917- Stratigraphy and structure of the western Kentucky fluorspar district. (Contributions to the geology of Kentucky) (Geological Survey professional paper ; 1151-D) Bibliography: p. Supt. of Docs, no.: I 19.16:1151-D 1. Geology, Stratigraphic Mississippian. 2. Geology, Stratigraphic Pennsylvanian. 3. Geology Kentucky. I. Amos, Dewey Harold, 1925- joint author. II. Kentucky. Geological Survey. III. Title. IV. Series. V. Series: United States. Geological Survey. Professional paper ; 1151-D. QE672.T7 551.7'009769 80-607000 For sale by the Distribution Branch, U.S. Geological Survey, 604 South Pickett Street, Alexandria, VA 22304 CONTENTS Page Page Abstract ————————————— Dl Stratigraphy—Continued Introduction ——————————— 2 Pennsylvanian System—Continued Production ——————————— 3 Morrowan Provincial Series—Continued History of previous geologic work • 4 Caseyville Formation—Continued Stratigraphy — 5 Caseyville Formation, undivided, along eastern Mississippian System —— 5 margin of district ——————— ———— D22 Osagean Provincial Series——————— 5 Sequence between the Pounds Sandstone Fort Payne Formation——————— 5 Member of the Caseyville Formation and Meramecian Provincial Series ———— 7 the Grindstaff Sandstone Member of the Trade- Warsaw-Salem-St. -
(Pennsylvanian) Sedimentation in the Illinois Basin
s 14. QS: STATE OF ILLINOIS CIR 5^ REGISTRATION C-3 DEPARTMENT OF AND EDUCATION PRE-PENNSYLVANIAN EVANSVILLE VALLEY AND CASEYVILLE (PENNSYLVANIAN) SEDIMENTATION IN THE ILLINOIS BASIN Paul Edwin Potter George A. Desborough ILLINOIS STATE GEOLOGICAL SURVEY John C. Frye, Chief URBANA CIRCULAR 384 1965 ILLINOIS STATE GEOLOGICAL Sj»YK[|||| 3 3051 00004 5405 . PRE-PENNSYLVANIAN EVANSVILLE VALLEY AND CASEYVILLE (PENNSYLVANIAN) SEDIMENTATION IN THE ILLINOIS BASIN Paul Edwin Potter and George A. Desborough ABSTRACT In southeastern Illinois and adjacent parts of Kentucky and Indiana, the Evans ville and other valleys existing in the pre-Pennsylvanian topography strongly affected the distribu- tion, thickness, lateral continuity, and transport direction of the sediments composing the basal members of the Caseyville Formation of early Pennsylvanian age. Regionally, the Casey- ville sandstones and shales are thickest and most continuous along the south-central edge of the Illinois Basin where basin subsidence was greatest. Up the paleoslopeto the northwest, north, and northeast, these sediments become thinner, are pro- gressively confined to erosional valleys of the unconformity, and finally pinch out. INTRODUCTION The Pennsylvanian sediments of the Illinois Basin were deposited on an erosional topography cut into Mississippian and older rocks. By detailed subsur- face and outcrop mapping, this study explores the relationships between the un- conformity and the overlying sediments of the Caseyville Formation along a portion of the south side of the basin (fig. 1) The magnitude of the sub-Pennsylvanian unconformity was early recognized in outcrop in the Illinois Basin. Rocks of the Pennsylvanian System lie on sediments as old as Ordovician and Devonian along the northern edge of the basin and princi- pally on Chesterian (Mississippian) sediments along the southern edge. -
Bedrock Geology of Williamson County, Illinois
STATEMAP Williamson County-BG Bedrock Geology of Williamson County, Illinois W. John Nelson 2020 615 East Peabody Drive Champaign, Illinois 61820-6918 (217) 244-2414 http://www.isgs.illinois.edu © 2020 University of Illinois Board of Trustees. All rights reserved. For permission information, contact the Illinois State Geological Survey. R. 4 E. R. 1 E. R. 2 E. R. 3 E. Pond Crk Freeman Pond ver k Spur Cree Creek Pond Bush 148 57 Big M Hurst Big Muddy Ri ud dy Rive r Lake Cree 149 k Johnston T. 8 S. Wade City Pond Creek Madison Prairie Lake Colp ek B r H re ushy u C Creek r Herrin r Johnston e i L ak c Bear Cree a City Lake n e C 37 r e k White Pittsburg Cambria e k Energy Ash Spillertown Buckley Carterville Herrin Reservoir Rock Cree Cree Crainville k k P 13 ig e Li o ttl ab Orcha ek n e Cr rd re Marion C C k Rock Creek r T. 9 S. e e k Cana Cr 13 Crab Crab Bankston For Or char d Orchard k Lake k 1 Caplinger Cree rd Pond rcha Brier Crab O C r e e k W k olf For S k ali e Marion h n k Cree Sou t e h ee re nc r a C C Reservoir 37 r k r B st y a k 166 o s g L s R a u iv r k e e S r G e r 57 L 148 k itt C h l e c k e Cana Cree n Cree e r r a e v sy r C e R i s B n a i r y l T. -
Proceedings of the Indiana Academy of Science (1988) Volume 98 P
Proceedings of the Indiana Academy of Science (1988) Volume 98 p. 281-295. SUBSURFACE BELT SANDSTONES IN THE HARDINSBURG FORMATION (LATE MISSISSIPPIAN) OF INDIANA John B. Droste and Alan Stanley Horowitz Department of Geology Indiana University Bloomington, Indiana 47405 INTRODUCTION The purpose of this report is to present the general stratigraphy of the Har- dinsburg Formation, Stephensport Group (Figure 1), in the subsurface of Indiana and to consider factors that have combined to create a belt of massive sandstones in the Hardinsburg in southwestern Indiana. These Mississippian rocks lie near the Lower Carboniferous Visean-Namurian series boundary of international ter- minology. The study area (Figure 2) is south of the northern boundaries of Sullivan and Greene Counties and west of the eastern boundaries of Greene, Martin, and Dubois Counties. The data for this report were taken from well information on file with the Indiana Geological Survey, Bloomington (Table 1). Initially, the records of ap- proximately 12,000 wells were inspected. A single well per section was selected for construction of the thickness maps, and no more than three wells per section were chosen to construct the cross sections. Intensive drilling for petroleum throughout much of the study area provides at least one well per section for which both well samples and a geophysical log are available. In areas of less dense drilling, we necessarily used wells for which either samples or wire-line logs existed. PREVIOUS WORK Reviews of Late Mississippian surface and subsurface stratigraphy and dep- ositional systems in the Illinois Basin area can be found in Swann (1963,1964), Potter (1962,1963), Willman, et al. -
A Rock Evaluation Schema for Transporting Planning in Kentucky
COMMONWEALTH OF KENTUCKY DEPARTMENT OF TRANSPORTATION JAMES E. GRAY WENDELL H. FORD FRANKFORT, KENTUCKY 40601 SECRETARY GOVERNOR May 29, 1974 H.3.13 MEMO TO: J. R. Harbison State Highway Engineer Chairman, Research Committee SUBJECT: Research Report No. 390; 11 A Rock Evaluation Schema for Transportation Planning in Kentucky; 11 Soil mantles and bedrock systems in Kentucky are being well defined pedologically and geologically. Agricultural soils maps, together with topographic and geological quadrangle maps, provide excellent, megascopic information for land-use guidance and site planning. In some respects, the agricultural and geologic technologies have surpassed or by-passed soil-and-rock mechanics -- that is, the engineering technology. During the past several years, the Soil Conservation Service in Kentucky has included engineering data and descriptions furnished by the Research Division in their publications. Also, U.S.G.S. notes some engineering information on the new, geological quadrangle maps. For instance, they note some aggregate sources and fossil slides and instances where highway embankments have shown a history of instability. As mentioned, engineering data on soils has been steadily accumulated during the past 25 years. It is now possible in many areas to indicate the most probable value of some properties and the expected range and variability. Rock data have not been accumulated; and, so, the purpose of the report submitted herewith is to bring into view the possibilities of beginning to assemble and catalog rock data in an orderly way for eventual reporting along with soils data. The Bureau of Highways is the principal source of engineering data for soils and produces extensive footages or rock cores from borings at bridge sites and along highway corridors. -
Proceedings of the Indiana Academy of Science
Proceedings of the Indiana Academy of Science (1990) Volume 99 p. 39-45 39 INFLUENCES ON THE POSITION OF CHESTERIAN SAND BELTS IN INDIANA John B. Droste and Alan S. Horowitz Department of Geological Sciences Indiana University 1005 East 10th Street Bloomington, Indiana 47405 ABSTRACT: The axial trend of belt sand bodies in the Hardinsburg Formation in Indiana shows striking similarities to the axial trends of belt sand bodies in earlier Chesterian formations of the West Baden Group and in the overlying Tar Springs and Waltersburg Formations. Droste and Horowitz (1990) postulated that the belt sand bodies of the Hardinsburg Formation in Indiana resulted from focussed current action on quartz sands funnelled along sea floor lows. The sea floor lows marked locations where local increased rates of subsidence were produced by subtle adjust- ments in basement structures. We infer that all the belt sands in the Indiana Chesterian resulted from deposition controlled by the same factors and that their trends mark locations of changing loci of minor basement structural adjustments These trends are generally parallel to the tectonic movements that produced the structures associated with the LaSalle Anticlinal Belt and Wabash Valley Fault System. INTRODUCTION In this review, our principal purpose is to illustrate that the axial trend of belt sand bodies in the Hardinsburg Formation in Indiana shows striking similarities to the axial trends of several other belt sand bodies in other Chesterian formations in Indiana. Potter (1962, 1963) has published a classification of elongate sand bodies, and we use herein his characterization of belt sand bodies. CHESTERIAN BELT SANDSTONES Major belt sand bodies in the subsurface of Indiana occur in the West Baden Group, the Stephensport Group, and in the lower part of the Buffalo Wallow Group (Figure 1). -
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 -
Geology of the Lick Creek Quadrangle Johnson, Union, and Williamson Counties, Southern Illinois
GEOLOGY OF THE LICK CREEK QUADRANGLE JOHNSON, UNION, AND WILLIAMSON COUNTIES, SOUTHERN ILLINOIS W. John Nelson and C. Pius Weibel Department of Natural Resources ILLINOIS STATE GEOLOGICAL SURVEY GEOLOGY OF THE LICK CREEK QUADRANGLE JOHNSON, UNION, AND WILLIAMSON COUNTIE SOUTHERN ILLINOIS W. John Nelson and C. Pius Weibel BULLETIN 103 1996 ILLINOIS STATE GEOLOGICAL SURVEY William W. Shilts, Chief 615 East Peabody Drive Champaign, IL 61820-6964 ACKNOWLEDGMENTS Acknowledgments are due to Russel Peppers, who analyzed palynology of coals and provided biostratigraphic data. Jack Masters and Joe Devera care- fully critiqued the geological map. Heinz Damberger, as project leader of COGEOMAP, provided continuous encouragement and advice. Private land- owners in the study area are gratefully acknowledged for permitting access to outcrops on their land. In particular, we thank Sam Michaels, Herman Stokes, and Leonard Jones, who allowed us to drill stratigraphic tests on their land. Cover Photo Graben created by landslide on north side of Grassy Creek Printed by authority of the State of Illinois/l996/1200 printed with soybean ink on recycled paper ACKNOWLEDGMENTS ABSTRACT 1 INTRODUCTION Geography and Physiography General Geologic Setting Previous Geologic Studies Methodology STRATIGRAPHY Mississippian System Ste. Genevieve Limestone Pope Group Aux Vases Sandstone Renault Limestone Yankeetown Formation and Downeys Bluff Limestone Bethel Sandstone Ridenhower Shale Cypress Sandstone Golconda Formation Hardinsburg Formation Glen Dean Limestone Tar Springs -
Paleozoic Species of Bairata and Related Genera
Paleozoic Species of BairataD ' 7* andJ Related Genera GEOLOGICAL SURVEY PROFESSIONAL PAPER 330-A Paleozoic Species of natrdiaD 7* andJ Related Genera By I. G. SOHN REVISION OF SOME PALEOZOIC OSTRACODE GENERA GEOLOGICAL SURVEY PROFESSIONAL PAPER 3 3 0-A A monographic subjective revision of genera and species, including identification keys and stratigraphic ranges UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1960 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. - Price $1 (paper cover) CONTENTS Page Abstract ______ _ _ ____ 1 Introduction. ._ _________ __ 1 Page Acknowledgments _______ _____ _ __ 1 57 Methods of study _ _ _ _ _ ___ 2 60 Punched cards __ _ _ _ _ ______ 3 Orthobairdia n. gen _ ___ ________ 65 Definition of terms ______ 6 69 Internal casts ___________ _____ 7 69 Discrimination of species _ ___ ___ __ 7 69 Individual variation ._ __ __ _ __ _ ____ _ 7 72 Muscle scars. _ _ ____ _ __ __ ____ 8 72 Surface texture _________ 8 74 Paleontological nomenclature _ _ _ 8 74 8 76 Homonymy ______ q 76 10 76 Homonyms not renamed. 10 Rishona n. gen. ._ __ __ ______ 79 Collection localities. ... _ _ _ 11 80 Systematic descriptions _______ 11 81 Key to genera ______ 11 81 Family Bairdiidae _ _ 12 81 12 83 Stratigraphic range 12 Species assigned to genera not described in this paper 84 17 84 Key to Bairdia s.s 1Q 84 Assigned species ..