June 4, 2014 ISGS FORMATION CODES and NAMES in CODE
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New Member Names for the Lower Silurian Hopkinton Dolomite of Eastern Iowa
Proceedings of the Iowa Academy of Science Volume 90 Number Article 4 1983 New Member Names for the Lower Silurian Hopkinton Dolomite of Eastern Iowa Markes E. Johnson William College Let us know how access to this document benefits ouy Copyright ©1983 Iowa Academy of Science, Inc. Follow this and additional works at: https://scholarworks.uni.edu/pias Recommended Citation Johnson, Markes E. (1983) "New Member Names for the Lower Silurian Hopkinton Dolomite of Eastern Iowa," Proceedings of the Iowa Academy of Science, 90(1), 13-18. Available at: https://scholarworks.uni.edu/pias/vol90/iss1/4 This Research is brought to you for free and open access by the Iowa Academy of Science at UNI ScholarWorks. It has been accepted for inclusion in Proceedings of the Iowa Academy of Science by an authorized editor of UNI ScholarWorks. For more information, please contact [email protected]. Johnson: New Member Names for the Lower Silurian Hopkinton Dolomite of Eas Proc. Iowa Acad. Sci. 90(1): 13-18, 1983 New Member Names for the Lower Silurian Hopkinton Dolomite of Eastern Iowa MARKES E. JOHNSON Department of Geology, Williams College, Williamstown, Massachusetts 01267. Previously divided primarily on the basis of paleontologic units, the approximately 60-80 m thick Hopkinton Dolomite in eastern Iowa also comprises a set oflithologically unique subunits. With the development of a new capability for inter-regional correlation of Lower Silurian strata based on the use of sea-level curves, it is especially appropriate to recognize these subdivisions of the Hopkinton Dolomite as formal member units. Locally, the relationships shown by these units may also contribute to a better understanding of the Plum River Fault Zone and its associated structures in Iowa and Illinois. -
Geology and Oil Production in the Tuscola Area, Illinois
124 KUItOfS GEOLOGICAL S SURVEY LIBRARY 14.GS: 4^ ^ CIR 424 :. 1 STATE OF ILLINOIS DEPARTMENT OF REGISTRATION AND EDUCATION Geology and Oil Production in the Tuscola Area, Illinois H. M. Bristol Ronald Prescott ILLINOIS STATE GEOLOGICAL SURVEY John C. Frye, Chief URBANA CIRCULAR 424 1968 Digitized by the Internet Archive in 2012 with funding from University of Illinois Urbana-Champaign http://archive.org/details/geologyoilproduc424bris GEOLOGY AND OIL PRODUCTION IN THE TUSCOLA AREA, ILLINOIS H. M. Bristol and Ronald Prescott ABSTRACT The Tuscola Anticline, in east-central Illinois, lies astride the complex LaSalle Anticlinal Belt and dips steeply westward into the Fairfield Basin and gradually eastward into the Murdock Syncline. The anticline is broken into two structural highs, the Hayes Dome and the Shaw Dome. Pleistocene sediments, 50 to 250 feet thick, cover the area. Pennsylvanian sediments cover much of the area, thinning to expose an inlier of Mississippian, Devonian, and Silurian rock north of Tuscola. The basal Cambrian for- mation, the Mt. Simon Sandstone, is penetrated by only two wells. Oil production from the Kimmswick (Trenton) com- menced in 1962 from the R. D. Ernest No. 1 Schweighart well, near Hayes, and as of January 1, 1968, approximately 30 wells were producing oil. Cumulative oil production as of January 1, 1968, is approximately 94,000 barrels. The potential pay zone is confined to the upper 5 to 100 feet of structure and to the upper 125 feet of the Kimmswick, whose permeability ranges from 0.1 to 2. millidarcys, av- eraging 0.6, and whose porosity ranges from 2 to 12 per- cent. -
IGS 2015B-Maquoketa Group
,QGLDQD*HRORJLFDO6XUYH\ $ERXW8V_,*66WDII_6LWH0DS_6LJQ,Q ,*6:HEVLWHIGS Website Search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
Geology for Planning in St. Clair County, Illinois
465 � JSGS-- -OIL & 6AS s SECJIGN--=fltES 14.GS: STATE OF ILLINOIS CIR465 c.4 DEPARTMENT OF REGISTRATION AND ED UCATION GEOLOGY FOR PLANNING IN ST. CLAIR COUNTY, ILLINOIS Alan M. Jacobs, compiler ILLINOIS ST ATE GEOLOGIC AL SURVEY John C. Frye, Chief Urbana, IL 61801 CIRCULAR 465 1971 GEOLOGY FOR PLANNING IN ST. CLAIR COUNTY, ILLINOIS Alan M. Jacobs, compiler ABSTRACT St. Clair County lies in southwestern Illinois across the Mississippi River from St. Louis, Missouri . One-fifth of the total land surface of 673 square miles is on flood plains of the Mississippi and Kaskaskia Rivers and Silver Creek. The floodplains are underlain by as much as 120 feet of gravel, sand, silt, and clay. The remaining fo ur fifths of the land surface is on uplands that contain flat or dissected plains, low ridges and mound-shaped hills, about 20 square miles of strip mines , and an area of karst topog raphy. The uplands are underlain by as much as 75 feet of till and sand and gravel, and generally 12 to 3 0 feet of loess and related silt; however, near the Mississippi River bluffs there are more than 100 feet of loes s and related silt. These deposits have been redistributed into spoil piles in the strip mines. Ben<ilath these deposits or cropping out in places are gently sloping beds of limestone, shale, sand stone, siltstone, clay stone, and coal. Thinly layered, frac tured limestone underlies the area of karst topography. Mineral and water resources are abundant in the county . Limestone of the St. -
Upper Ordovician) at Wequiock Creek, Eastern Wisconsin
~rnooij~~~mij~rnoo~ ~oorn~rn~rn~~ rnoo~~rnrn~rn~~ Number 35 September, 1980 Stratigraphy and Paleontology of the Maquoketa Group (Upper Ordovician) at Wequiock Creek, Eastern Wisconsin Paul A. Sivon Department of Geology University of Illinois Urbana, Illinois REVIEW COMMITTEE FOR THIS CONTRIBUTION: T.N. Bayer, Winona State College University, Winona Minnesota M.E. Ostrom, Wisconsin Geological Survey, Madison, Wisconsin Peter Sheehan, Milwaukee Public Museum· ISBN :0-89326-016-4 Milwaukee Public Museum Press Published by the Order of the Board of Trustees Milwaukee Public Museum Accepted for publication July, 1980 Stratigraphy and Paleontology of the Maquoketa Group (Upper Ordovician) at Wequiock Creek, Eastern Wisconsin Paul A. Sivon Department of Geology University of Illinois Urbana, Illinois Abstract: The Maquoketa Group (Upper Ordovician) is poorly exposed in eastern Wisconsin. The most extensive exposure is found along Wequiock Creek, about 10 kilometers north of Green Bay. There the selection includes a small part of the upper Scales Shale and good exposures of the Fort Atkinson Limestone and Brainard Shale. The exposed Scales Shale is 2.4 m of clay, uniform in appearance and containing no apparent fossils. Limestone and dolomite dominate the 3.9 m thick Fort Atkinson Limestone. The carbonate beds alternate with layers of dolomitic shale that contain little to no fauna. The shales represent times of peak terrigenous clastic deposition in a quiet water environment. The car- bonates are predominantly biogenic dolomite and biomicrite. Biotic succession within single carbonate beds includes replacement of a strophomenid-Lepidocyclus dominated bottom community by a trep- ostome bryozoan-Plaesiomys-Lepidocyclus dominated community. Transported echinoderm and cryptostome bryozoan biocalcarenites are common. -
Affected Environment 4
Section 4 AFFECTED ENVIRONMENT 4. Affected Environment 4.0 Affected Environment The study corridor used to identify various resources within the program’s affected environment is comprised of the seven sections described in Chapter 3, Section 3.3.7.1 and illustrated in Exhibit 3.3‐10. Depending on the resource and the available information collected, the width of the study corridor ranges from 100 feet to the counties in which the study corridor traversed. The study corridors are described in each of the resource sections. 4.1 Existing Land Use 4.1.1 Development Patterns Historically, Chicago and St. Louis have served as major continental transportation centers, both tracing their origins to water and rail transportation routes. Chicago prospered from its strategic location on Lake Michigan and access to eastern markets through the Erie Canal and the Great Lakes. St. Louis originally developed from its role as a port on the Mississippi River that provided access to domestic and foreign markets. During the 19th Century, the addition of railroads linking these cities forged an economic lifeline between Chicago and St. Louis. Construction of the rail network spawned the growth of numerous communities that served as regional centers for the collection and distribution of goods for a rich agricultural region. The influence of the railroad remained strong until interstate highways joined the transportation system in the 1950s and 1960s. In contrast to the railroads, which created new communities along their length to maintain and support the railroads, interstate highways were constructed around, and often bypassed some communities. Because the interstates had limited points of access, county roads that connected with or crossed over them linking existing communities, became particularly important to the rural areas. -
Dolomite Resources of Boone and De Kalb Counties
View metadata, citation and similar papersbrought at core.ac.uk to you by CORE nUNOfS SSOLOCrCAL provided by Illinois Digital... SURVEY tlBRARY STATE OF ILLINOIS DEPARTMENT OF REGISTRATION AND EDUCATION DOLOMITE RESOURCES OF BOONE AND DE KALB COUNTIES James C. Bradbur/ ILLINOIS STATE GEOLOGICAL SURVEY John C. Frye, Chief URBANA CIRCULAR 379 1965 Digitized by the Internet Archive in 2012 with funding from University of Illinois Urbana-Champaign http://archive.org/details/dolomiteresource379brad DOLOMITE RESOURCES OF BOONE AND DE KALB COUNTIES James C. Bradbury ABSTRACT The dolomite resources of Boone and DeKalb Counties are of interest because of their location near the greater Chicago area. As natural exposures are rare and quarries are limited chiefly to one area within the two counties, much of the information on the distribution and character of the dolomite formations must come from drill records. Maps in this report show distribution of bedrock formations, depth to bedrock, and depth to and thickness of dolomites. Chemical analyses of samples from active and abandoned quarries are presented. Three or more dolomite rock units up to 300 or more feet in thickness are present in the area. Places where each of the carbonate units may be found with relatively thin overburden are suggested. INTRODUCTION The limestone resources of Boone and DeKalb Counties in north-central Illinois are of interest because of their location near the western margin of the Chicago metropolitan area (fig. 1). Widespread deposits of glacial drift and a lack of pronounced topographic relief generally result in a scarcity of outcrops. Thus, although there are several quarries, both active and abandoned, they are mostly limited to a narrow belt in western Boone County. -
Structural Framework of the Mississippi Embayment of Southern Illinois ^
<Olo£ 4.GV- Su&O&Ml STRUCTURAL FRAMEWORK OF THE MISSISSIPPI EMBAYMENT OF SOUTHERN ILLINOIS ^ Dennis R. Kolata, Janis D. Treworgy, and John M. Masters f^a>i^ < Illinois Institute of Natural Resources STATE GEOLOGICAL SURVEY DIVISION CIRCULAR 516 Jack A. Simon, Chief 1981 . COVER PHOTO: Exposure of Mississippian limestone along the Post Creek Cutoff in eastern Pulaski County, Illinois. The limestone is overlain (in ascending order) by the Little Bear Soil and the Gulfian (late Cretaceous) Tuscaloosa and McNairy Formations. Cover and illustrations by Sandra Stecyk. Kolata, Dennis R. Structural framework of the Mississippi Embayment of southern Illinois / by Dennis R. Kolata, Janis D. Treworgy, and John M. Masters. — Champaign, III. : State Geological Survey Division, 1981 — 38 p. ; 28 cm. (Circular / Illinois. State Geological Survey Division ; 516) 1. Geology — Mississippi Embayment. 2. Geology, Structural — Illinois, Southern. 3. Mississippi Embayment. I. Treworgy, Janis D. II. Masters, John M. III. Title. IV. Series. GEOLOGICAL SURVEY ILLINOIS STATE Printed by authority of State of Illinois (3,000/1981) 5018 3 3051 00003 STRUCTURAL FRAMEWORK OF THE MISSISSIPPI EMBAYMENT OF SOUTHERN ILLINOIS -*** t**- ILLINOIS STATE GEOLOGICAL SURVEY CIRCULAR 516 Natural Resources Building 1981 615 East Peabody Drive Champaign, IL 61820 Digitized by the Internet Archive in 2012 with funding from University of Illinois Urbana-Champaign http://archive.org/details/structuralframew516kola CONTENTS ABSTRACT 1 INTRODUCTION 1 METHOD OF STUDY 2 GEOLOGIC SETTING -
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). -
Preliminary Geologic Map of the Buried Bedrock Surface, Wisconsin Geological and Natural History Survey Brown County, Wisconsin Open-File Report 2011-02
Preliminary Geologic Map of the Buried Bedrock Surface, Wisconsin Geological and Natural History Survey Brown County, Wisconsin Open-File Report 2011-02 John A. Luczaj The bedrock surface in Brown County is typically overlain by Quaternary glacial sediment, ranging in thickness from 0 to 300 feet. These deposits include Pleistocene glacial till, outwash, and glaciolacustrine sediments from tens of feet to at least 300 feet in thickness in preglacial river valleys. Bedrock is best exposed along the Niagara Escarpment, which is 87°50'W DOOR CO 88°0'W produced by the resistant eastward-dipping Silurian Mayville Formation that overlies the ! ! ! ! BOUNDARY ! OCONTO CO!! !! ! INDEFINITE weaker Ordovician Maquoketa Shale. ! ! ! ! ! ! ! ! !! ! ! ! ! ! ! ! ! ! 88°10'W !!! ! ! ! !! ! ! ! ! ! ! ! ! L ! ! ! ! ! !! ! !! !!!! ! ! !! ! ! ! i ! ! ! ! ! ! ! !! ! t ! ! ! !! ! ! t ! ! ! ! ! ! ! ! ! 44°40'N !! ! !! ! ! !!! l ! ! ! ! ! ! ! ! e ! ! ! !!! !! ! ! ! ! ! ! ! !! ! ! ! ! ! ! ! ! ! ! T ! ! !! ! !! ! ! ! ! ! ! !! !! ! a ! ! ! ! ! ! ! ! !! ! ! ! i ! ! ! ! ! ! ! ! l ! ! ! ! ! !! P ! ! ! ! ! ! ! ! ! ! ! ! ! !!!! ! ! ! !! ! o ! ! ! ! ! ! ! ! ! ! EXPLANATION ! ! i 44°40'N ! ! ! ! ! n ! ! ! ! !!! ! ! ! ! ! !! ! ! t ! !! ! ! !! !! ! ! ! ! ! ! !! ! ! ! !! ! ! ! ! ! !! ! ! ! !!!!! ! !! ! ! ! ! ! ! ! ! Op ! ! ! ! ! ! ! ! ! ! !! ! ! ! !! ! ! ! ! ! ! ! ! ! SILURIAN ! ! ! ! ! ! ! ! ! ! ! !! ! ! ! !! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! !! ! ! ! ! ! ! ! ! ! ! Dyckesville!! Engadine Formation ! ! ! ! ! -
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.