Bedrock Geology of Bethalto Quadrangle
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Bedrock Geology of Edwardsville Quadrangle
Rod R. Blagojevich, Governor BEDROCK GEOLOGY OF EDWARDSVILLE QUADRANGLE Department of Natural Resources Joel Brunsvold, Director MADISON COUNTY, ILLINOIS Illinois State Geological Survey William W. Shilts, Chief Joseph A. Devera and F. Brett Denny 2003 BUNKER HILL 12 MI. 2 000m. 2 2 2 2 2 2 2 90°00' 40 E. 41 42 1.6 MI. TO ILL. 140 57' 30" 44 45 R. 8 W. 46 R. 7 W. 55' 48 49 580 000 FEET 89°52'30'' 38°52'30" 38°52'30" 159 Psb 400 Eberhart Cem St James Cem 4306 21 22 23 24 19 20 21 4306000m.N. HENKE LANDING STRIP 375 Psb Shelburn Formation 400 350 Pennsylvanian Desmoinsian ek 800 000 re C FEET Pcb Carbondale Formation Gard Pcb 400 I M Quercus Grove 4 Maple . 2 Cem L E 157 M A Quercus Grove H Park 4305 Line symbols: dashed where inferred Petroleum and Coal Resources a h i c 26 k 28 n o a h of Madison County 27 r a C 25 B Barnett (Resources have been removed) 30 29 Contact 375 28 43 Macoupin County 04 475 Bedrock topography (elevation in feet) Madison County 325 350 4304 325 Coal test (depth in feet) Oil test, dry hole (depth in feet) s Golf gh ou Course rr u 43 Oil test, show of oil (depth in feet) B 03 . I . I 33 M 35 M 2 7 1 2 N 36 31 D O 34 32 L Edwardsville T Mine shaft, abandoned E 33 I . S I F G M H Quadrangle N I C 5 V T I I . -
(A) Placement Above Uppermost Aquifer
AECOM 502-569-2301 tel 500 W Jefferson St. 502-569-2304 fax Suite 1600 Louisville, KY 40202 www.aecom.com October 17, 2018 Big Rivers Electric Corporation Sebree Generating Station 9000 Highway 2096 Robards, Kentucky 42452 Engineer’s Certification of Placement Above the Uppermost Aquifer Existing Green CCR Surface Impoundment EPA Final CCR Rule Sebree Station Robards, Kentucky 1.0 PURPOSE The purpose of this document is to certify that the Placement above Sebree “Green” Existing CCR Surface Impoundment is in compliance with the Placement above the Uppermost Aquifer requirement of the Final CCR Rule at 40 CFR §257.60. Presented below is the project background, summary of findings, limitations and certification. 2.0 BACKGROUND In accordance with 40 CFR §257.60, the owner/operator of an existing CCR Surface Impoundment must demonstrate that the base of the unit is located no less than 1.52 meters (five feet) above the upper limit of the uppermost aquifer, or must demonstrate that there will not be an intermittent, recurring, or sustained hydraulic connection between any portion of the base of the CCR unit and the uppermost aquifer due to normal fluctuations in groundwater elevations (including the seasonal high water table). In accordance with 40 CFR §257.60(c)(1), the demonstration must be made by October 17, 2018. If such demonstration cannot be made, the unit is subject to the closure or retrofit requirements of 40 CFR §257.101 3.0 SUMMARY OF FINDINGS Available data regarding site groundwater, site geology, and physical limits of the unit for the Green Surface Impoundment do not evidence a 5-foot separation between the base of the impoundment and the uppermost limit of the uppermost aquifer and they do not support a lack of hydraulic connectivity between the unit and the aquifer as specified in 40 CFR §257.60(a). -
Detailed Sedimentological Study of the West Franklin Limestone Member
Detailed Sedimentological Study of the West Franklin Limestone Member (Desmoinesian to Missourian) of the Shelburn Formation (Upper Pennsylvanian) of southwestern Indiana Grace L. Stone and William S. Elliott, Jr. Department of Geology and Physics, University of Southern Indiana, 8600 University Blvd., Evansville, Indiana 47712; [email protected] Introduction Results Discussion The West Franklin Limestone is a key marker bed in correlating Middle to Upper Southwest Indiana is underlain by gently, westward dipping (2° to 3°) Middle to Upper Photomicrograph of skeletal 76.4 to 76.9 feet depth: tan to gray, Pennsylvanian strata in the Illinois Basin (Wier & Ault, 1986; Brown & Rexroad, 2009). It is Pennsylvanian strata on the southern margin of the Illinois Basin consisting of recurring packstone showing broken bioturbated, skeletal packstone with typically identified by two limestone benches separated by an interval of siliciclastic deposits of limestone, sandstone, shale, and coal (Fig. 1). USI 1-32, an exploratory USI 1-32 Core Upper Bench of skeletal fragments that include, broken crinoid, brachiopod, sediment, but the number of benches is variable from the absence of the limestone to four coalbed methane well drilled in 2009, is located at 37.951° N and 87.670°W south of 75 bryozoans, gastropods, forams, West Franklin bryozoan, and gastropod fossils with discrete limestone intervals (Anderson, 1956; King, 1994; Heckel et al., 1998; Rexroad et al., the campus of the University of Southern Indiana in Vanderburgh County, Indiana (Fig. and algae, with a micrite mud traces of disseminated pyrite. 2008; Gray, 2011). 2). The total depth of the well is 780 feet with a core recovered from the West Franklin Limestone matrix from 76.45 feet depth. -
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 -
Geologic Names of North America Introduced in 19364955
Geologic Names of North America Introduced in 19364955 ^GEOLOGICAL SURVEY BULLETIN 1056-A Names of North America Introduced in 1936-1955 By DRUID WILSON, WILLIAM J. SANDO? and RUDOLPH W. KOPF Prepared with the assistance of BARBARA BEDETTE, JEAN L. EGGLETON, GRACE C. KEROHER, CAROLYN MANN, WILLIAM G. MELTON, JR., KATHERINE DENNISON PALMER, and JACK E. SMEDLEY GEOLOGIC NAMES OF NORTH AMERICA -G E O L O G I C AL SURVEY BULLETIN 1056-A A compilation of new geologic names of North America, including Greenland, the finest Indies, the Pacific Island pos sessions of the United States, and the Trust Territory of the Pacific Islands UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1957 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) FOEEWOBD The "Lexicon of geologic names of the United States" by M. Grace Wilmarth, published in 1938 and reprinted in 1951 and 1957, met a long standing need and continuing demand for a compilation of geologic names. Plans made for future compilations as new names and revisions appeared were interrupted during the years of World War II. In 1952 a sustained effort was begun toward review of geo logic publications necessary to furnish a background for preparation of a new edition. After the review was brought up to date in 1956, the present compilation was prepared in order to furnish to the geo logic profession, as quickly as possible, some of the essential data concerning the new names that have appeared since 1935. -
Geologic Overview
Chapter C National Coal Resource Assessment Geologic Overview By J.R. Hatch and R.H. Affolter Click here to return to Disc 1 Chapter C of Volume Table of Contents Resource Assessment of the Springfield, Herrin, Danville, and Baker Coals in the Illinois Basin Edited by J.R. Hatch and R.H. Affolter U.S. Geological Survey Professional Paper 1625–D U.S. Department of the Interior U.S. Geological Survey Contents Coal Formation ..................................................................................................................................... C1 Plant Material ............................................................................................................................. 1 Phases of Coal Formation ......................................................................................................... 1 Stratigraphic Framework of the Illinois Basin Coals ..................................................................... 1 Raccoon Creek Group ............................................................................................................... 4 Carbondale Formation or Group ............................................................................................... 6 McLeansboro Group................................................................................................................... 6 Structural Setting ............................................................................................................................... 6 Descriptions of the Springfield, Herrin, Danville, and -
BEDROCK GEOLOGY of PRAIRIETOWN QUADRANGLE As A
BEDROCK GEOLOGY OF PRAIRIETOWN QUADRANGLE Department of Natural Resources Illinois Preliminary Geologic Map ILLINOIS STATE GEOLOGICAL SURVEY MADISON AND MACOUPIN COUNTIES, ILLINOIS IPGM Prairietown-BG William W. Shilts, Chief F. Brett Denny Introduction ���������������������������� 2004 Bedrock Geology of Prairietown Quadrangle was prepared as part of a statewide 1:24,000-scale �� geologic mapping program by the Illinois State Geological Survey (ISGS). This geologic map was funded in part through a contract with the United States Geological Survey. Bedrock geolog- ��� ��� ��� ��� ���������������� ���������� ic maps may aid in the exploration for economic minerals including coal, petroleum, and natural ��� ��� gas and may facilitate regional planning by locating groundwater resources and aggregate materi- als for infrastructure support. ��� ��� ������������������ ��� ��� ������������� ����������� Several data sources have been used to construct this map. Well records from files of the ISGS ���� were the primary source. Most data locations are shown on the map sheet, but locations from ��� ��� ��� �������������������� ��� several confidential records used to construct the geologic and structural contour maps are not shown. In addition, bedrock outcrops were observed along the east side of Sherry Creek (Secs. 6 ��� ���� ������������������ � and 7, T6N, R7W). ��� ��� ��� Bedrock topographic surface contours at 25-foot intervals were generated and overlain on the �� �������������������� ������ geologic map. Unconsolidated or surficial material thickness may be estimated by subtracting ��� bedrock elevations from surface elevations on the topographic base map. ������������ ��� ��� ��� ���������� Economic Geology ��� ��������������������������� ��� ��� ������������� Coal The primary economic coal is the Herrin Coal, located near the top of the Carbondale Formation. ��� ��� ���������� ��� ��������������������������� The Herrin averages 5 feet in thickness, but is eroded or not deposited in a few locations (see inset map of Herrin structure on top of the Herrin Coal). -
Bedrock Aquifer Systems of Pike County, Indiana
Bedrock Aquifer Systems of Pike County, Indiana by Gregory P. Schrader and William C. Herring Division of Water, Resource Assessment Section June 2003 The occurrence of bedrock aquifers depends on the original composition of the rocks and subsequent changes which influence the hydraulic properties. Post-depositional processes, which promote jointing, fracturing, and solution activity of exposed bedrock, generally increase the hydraulic conductivity (permeability) of the upper portion of bedrock aquifer systems. Because permeability is generally greatest near the bedrock surface, bedrock units within the upper 100 feet are usually the most productive aquifers. In Pike County, rock types exposed at the bedrock surface range from relatively unproductive shales to moderately productive sandstones. Thin limestone and coal seams are sometimes noted as water-bearing. Bedrock aquifer systems in the county are overlain by unconsolidated deposits of varying thickness. Refer to the map for unconsolidated aquifer systems for more information. Most of the bedrock aquifers in the county are under confined conditions. In other words, the potentiometric surface (water level) in most wells completed in bedrock rises above the top of the water-bearing formation. The yield of a bedrock aquifer depends on its hydraulic characteristics and the nature of the overlying deposits. Shale and glacial till act as aquitards, restricting recharge to underlying bedrock aquifers. However, fracturing and/or jointing may occur in aquitards, which can increase recharge to the underlying aquifers. Hydraulic properties of the bedrock aquifers are highly variable. Three bedrock aquifer systems are identified for Pike County based on bedrock surface lithology. They are, from east to west and oldest to youngest: Raccoon Creek Group of Pennsylvanian age; Carbondale Group of Pennsylvanian age; and McLeansboro Group of Pennsylvanian age. -
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. -
Index to the Geologic Names of North America
Index to the Geologic Names of North America GEOLOGICAL SURVEY BULLETIN 1056-B Index to the Geologic Names of North America By DRUID WILSON, GRACE C. KEROHER, and BLANCHE E. HANSEN GEOLOGIC NAMES OF NORTH AMERICA GEOLOGICAL SURVEY BULLETIN 10S6-B Geologic names arranged by age and by area containing type locality. Includes names in Greenland, the West Indies, the Pacific Island possessions of the United States, and the Trust Territory of the Pacific Islands UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1959 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.G. - Price 60 cents (paper cover) CONTENTS Page Major stratigraphic and time divisions in use by the U.S. Geological Survey._ iv Introduction______________________________________ 407 Acknowledgments. _--__ _______ _________________________________ 410 Bibliography________________________________________________ 410 Symbols___________________________________ 413 Geologic time and time-stratigraphic (time-rock) units________________ 415 Time terms of nongeographic origin_______________________-______ 415 Cenozoic_________________________________________________ 415 Pleistocene (glacial)______________________________________ 415 Cenozoic (marine)_______________________________________ 418 Eastern North America_______________________________ 418 Western North America__-__-_____----------__-----____ 419 Cenozoic (continental)___________________________________ -
Pander Society Newsletter
Pander Society Newsletter S O E R C D I E N T A Y P 1 9 6 7 Compiled and edited by M.C. Perri, M. Matteucci and C. Spalletta DIPARTIMENTO DI SCIENZE DELLA TERRA E GEOLOGICO-AMBIENTALI, ALMA MATER STUDIORUM-UNIVERSITÀ DI BOLOGNA, BOLOGNA, ITALY Number 42 August 2010 www.conodont.net pdf layout and web delivery Mark Purnell, University of Leicester 1 Chief Panderer’s Remarks July 8, 2010 Dear Pander Society people, It is again summer and I am at the end of the first year in a new role―since ICOS 2009 in Calgary when the honour of Chief Panderer was bestowed upon me. I am much honoured to be the first woman to have this honour bestowed on her. As I wrote in my first communication to all Panderers, it was with a sense of awe that I accepted this task ― to attempt to follow in the footsteps of a remarkable sequence of Chief Panderers who gave so much time to improving communication between conodont workers around the globe. I thank very much Peter von Bitter for the excellence of the job he did during his tenure, superbly keeping "all of the Panderers connected and in harmony”. A special thanks to Peter also for the help he offered me during this year, and hope he will excuse me for 'plagiarising' some parts of his previous beautifully crafted newsletter. Many thanks too for the help that other Panderers have offered me. My previous role as member of the Committee for deciding Pander Society Medal has now passed to Susana Garcia Lopez (University of Oviedo, Spain). -
Storage, Retrieval, and Analysis of Compacted Shale Data
14 Storage, Retrieval, and Analysis of Compacted Shale Data Dirk J. A. van Zyl, L.E. Wood, and C. W. Lovell, Department of Civil Engineering, Purdue University, West Lafayette, Indiana W. J. Sisiliano, Indiana State Highway Commission La1ge amounts of soil test data aro beir,g gonoroted by states testing materials fr-om three Joint Highway Research Project (J.HRP) reports for new highway facillties. Of particular Interest to ,omo states Is tho occur completed at Purdue University @, !, ID. A complete rence of shale os a highway motorlal. This paper describes a storage and rotrioval system for compacted lndlnnn shale data (163 setsl. Statistical analyses in summary of all the data available and descriptions of the cluded frequency analysis, bivariate correlation analysis, nnd multiple rogres, geology of Indiana shales and the physiography of Indiana sion analysis. Histograms of the frequency distributions and o summary table are given by van Zyl (§). The table below gives a summary of all the dlfferont statistical descriptors of the parameters are given. Bivariate of the data sets according to geological description. correlation analysis (ono•to-one torrolations) was done for all dota lumped and for data grouped by geologic unit. The multiple regression, concentrated on five-parameter models for predicting Califomla bearing rotio values. It was Geological No. of also found by multlple tllgrenion that the various value, of sloko durabilily in System Geological Stage Data Sets dices can be estimated by using second•ordor equotions. The analyses aro of potontia! value to practicing engineers as a first approximation in design and Pennsylvanian Shelburn formation 3 moy prove useful to engineers rosoarching compacted shale behavior.