Bedrock Geology of Herod Quadrangle
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CONODONT BIOSTRATIGRAPHY and ... -.: Palaeontologia Polonica
CONODONT BIOSTRATIGRAPHY AND PALEOECOLOGY OF THE PERTH LIMESTONE MEMBER, STAUNTON FORMATION (PENNSYLVANIAN) OF THE ILLINOIS BASIN, U.S.A. CARl B. REXROAD. lEWIS M. BROWN. JOE DEVERA. and REBECCA J. SUMAN Rexroad , c.. Brown . L.. Devera, 1.. and Suman, R. 1998. Conodont biostrati graph y and paleoec ology of the Perth Limestone Member. Staunt on Form ation (Pennsy lvanian) of the Illinois Basin. U.S.A. Ill: H. Szaniawski (ed .), Proceedings of the Sixth European Conodont Symposium (ECOS VI). - Palaeont ologia Polonica, 58 . 247-259. Th e Perth Limestone Member of the Staunton Formation in the southeastern part of the Illinois Basin co nsists ofargill aceous limestone s that are in a facies relati on ship with shales and sandstones that commonly are ca lcareous and fossiliferous. Th e Perth conodo nts are do minated by Idiognathodus incurvus. Hindeodus minutus and Neognathodu s bothrops eac h comprises slightly less than 10% of the fauna. Th e other spec ies are minor consti tuents. The Perth is ass igned to the Neog nathodus bothrops- N. bassleri Sub zon e of the N. bothrops Zo ne. but we were unable to co nfirm its assignment to earliest Desmoin esian as oppose d to latest Atokan. Co nodo nt biofacies associations of the Perth refle ct a shallow near- shore marine environment of generally low to moderate energy. but locali zed areas are more variable. particul ar ly in regard to salinity. K e y w o r d s : Co nodo nta. biozonation. paleoecology. Desmoinesian , Penn sylvanian. Illinois Basin. U.S.A. -
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 -
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. -
A.A.S.P. Newsletter
A.A.S.P. NEWSLETTER Published Quarterly by the American Association of Stratigraphic Palynologists Inc. December 2000 Volume 33, Number 4 Presidential address - 2000 AASP Meeting, Reno -3- Secretary -Treasurer report -6- Report of activities, 2000 AASP Annual Meeting -6- News from the UK -8- A new working group: Tropical Dinocysts -9- New members and address updates -9- Recieve your AASP newsletter electronically -11- AASP member missing in action -11- Book reviews -12- Announcements -19- Agenda -20- 1 A.A.S.P. American Association of Stratigraphic Palynologists Inc. The American Association of Stratigraphic Palynologists, Inc. - AASP - was established in 1967 by a group of 31 founding members to promote the science of palynology. Today AASP has a world-wide membership of about 800 and is run by an executive comprising an elected Board of Directors and subsidiary boards and committees. AASP welcomes new members. The AASP Foundation publishes the journal Palynology (annually), the AASP Newsletter (quarterly), and the AASP Contributions Series (mostly monographs, issued irregularly), as well as several books and miscellaneous items. AASP organises an Annual Meeting which usually includes a field trip, a business luncheon, social events, and technical sessions where research results are presented on all aspects of palynology. AASP Scientific Medal recipients Professor William R. Evitt (awarded 1982) AASP Board of Directors Award recipient Professor William G. Chaloner (awarded 1984) Dr. Robert T. Clarke (awarded 1994) Dr. Lewis E. Stover (awarded 1988) Dr. Graham Lee Williams (awarded 1996) Teaching medal recipients Dr. Hans Gocht (awarded 1996) Professor Aureal T. Cross (awarded 1999) AASP Honorary Members AASP Distinguished Service Award recipients Professor Dr. -
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. -
B2150-B FRONT Final
Bedrock Geology of the Paducah 1°×2° CUSMAP Quadrangle, Illinois, Indiana, Kentucky, and Missouri By W. John Nelson THE PADUCAH CUSMAP QUADRANGLE: RESOURCE AND TOPICAL INVESTIGATIONS Martin B. Goldhaber, Project Coordinator T OF EN TH TM E U.S. GEOLOGICAL SURVEY BULLETIN 2150–B R I A N P T E E R D . I O S . R A joint study conducted in collaboration with the Illinois State Geological U Survey, the Indiana Geological Survey, the Kentucky Geological Survey, and the Missouri M 9 Division of Geology and Land Survey A 8 4 R C H 3, 1 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1998 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Mark Schaefer, Acting 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 Nelson, W. John Bedrock geology of the Paducah 1°×2° CUSMAP Quadrangle, Illinois, Indiana, Ken- tucky, and Missouri / by W. John Nelson. p. cm.—(U.S. Geological Survey bulletin ; 2150–B) (The Paducah CUSMAP Quadrangle, resource and topical investigations ; B) Includes bibliographical references. Supt. of Docs. no. : I 19.3:2150–B 1. Geology—Middle West. I. Title. II. Series. III. Series: The Paducah CUSMAP Quadrangle, resource and topical investigations ; B QE75.B9 no. 2150–B [QE78.7] [557.3 s—dc21 97–7724 [557.7] CIP CONTENTS Abstract .......................................................................................................................... -
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. -
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 P.H. von Bitter and J. Burke PALAEOBIOLOGY DIVISION, DEPARTMENT OF NATURAL HISTORY, ROYAL ONTARIO MUSEUM, TORONTO, ON, CANADA M5S 2C6 Number 41 May 2009 www.conodont.net Webmaster Mark Purnell, University of Leicester 2 Chief Panderer’s Remarks May 1, 2009 Dear Colleagues: It is again spring in southern Canada, that very positive time of year that allows us to forget our winter hibernation & the climatic hardships endured. It is also the time when Joan Burke and I get to harvest and see the results of our winter labours, as we integrate all the information & contributions sent in by you (Thank You) into a new and hopefully ever better Newsletter. Through the hard work of editor Jeffrey Over, Paleontographica Americana, vol. no. 62, has just been published to celebrate the 40th Anniversary of the Pander Society and the 150th Anniversary of the first conodont paper by Christian Pander in 1856; the titles and abstracts are here reproduced courtesy of the Paleontological Research Institution in Ithica, N.Y. Glen Merrill and others represented the Pander Society at a conference entitled “Geologic Problem Solving with Microfossils”, sponsored by NAMS, the North American Micropaleontology Section of SEPM, in Houston, Texas, March 15-18, 2009; the titles of papers that dealt with or mentioned conodonts, are included in this Newsletter. Although there have been no official Pander Society meetings since newsletter # 40, a year ago, there were undoubtedly many unofficial ones; many of these would have been helped by suitable refreshments, the latter likely being the reason I didn’t get to hear about the meetings. -
The Geology of the Interstate Highway 244 and 44 Exchange, Kirkwood, Missouri
Scholars' Mine Masters Theses Student Theses and Dissertations 1965 The geology of the interstate highway 244 and 44 exchange, Kirkwood, Missouri John Neil Thomas Follow this and additional works at: https://scholarsmine.mst.edu/masters_theses Part of the Geology Commons Department: Recommended Citation Thomas, John Neil, "The geology of the interstate highway 244 and 44 exchange, Kirkwood, Missouri" (1965). Masters Theses. 5338. https://scholarsmine.mst.edu/masters_theses/5338 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. THE GEOLOGY OF THE INTERSTATE HIGHWAY 244 AND 44 INTERCHANGE, KIRKWOOD MISSOURI BY JOHN NEIL THOMAS A THESIS submitted to the faculty of the UNIVERSITY OF MISSOURI AT ROLLA in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE, GEOLOGY MAJOR Rolla, Missouri 1965 Approved by ~~ (advisor) ~.Ad~ ii ABSTRACT During the summer of 1964, construction was completed on the intersection of Interstate Highways 244, 44 and u.s. Highway 66, one mile southwest of Kirkwood, Missouri. Dur ing the construction of the interchange, numerous artificial exposures of rocks of the middle Mississippian Meramecian Series were exposed. This provided an excellent opportunity for examining fresh exposures near the type Meramecian Ser ies. The formations of the area were studied, and starti graphic sections were prepared from three of the more com plete sections that were measured and described. The high way cuts expose complete sections of the Warsaw and Salem formations, and the lower part of the St. -
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 -
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. -
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.