Geohydrology of the Weldon Spring Ordnance Works, St. Charles County, Missouri
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Bedrock Geology of Altenburg Quadrangle, Jackson County
BEDROCK GEOLOGY OF ALTENBURG QUADRANGLE Institute of Natural Resource Sustainability William W. Shilts, Executive Director JACKSON COUNTY, ILLINOIS AND PERRY COUNTY, MISSOURI STATEMAP Altenburg-BG ILLINOIS STATE GEOLOGICAL SURVEY E. Donald McKay III, Interim Director Mary J. Seid, Joseph A. Devera, Allen L. Weedman, and Dewey H. Amos 2009 360 GEOLOGIC UNITS ) ) ) 14 Qal Alluvial deposits ) 13 18 Quaternary Pleistocene and Holocene 17 360 ) 15 360 16 14 0 36 ) 13 Qf Fan deposits ) Unconformity Qal ) & 350 tl Lower Tradewater Formation Atokan ) ) Pennsylvanian 360 ) &cv Caseyville Formation Morrowan 24 360 ) Unconformity ) 17 Upper Elviran undivided, Meu ) Waltersburg to top of Degonia 19 20 Qal 21 22 23 ) 24 ) Mv Vienna Limestone 360 o ) 3 Mts ) 350 Mts Tar Springs Sandstone ) 20 360 ) Mgd 360 30 ) Mgd Glen Dean Limestone ) 21 350 360 Mts 29 ) Qal Hardinsburg Sandstone and J N Mhg Chesterian ) Golconda Formations h Æ Qal Mav anc 28 27 Br ) N oJ 26 25 JN 85 N ) Cypress Sandstone through J Mcpc Dsl 500 Paint Creek Formation JN N ) J o Mts N 5 J s ) Dgt 600 J N 70 J N Mgd Yankeetown Formation s ) Myr Db 80 28 Æ and Renault Sandstone N J 29 N J N ) Sb J Mgd Mississippian o Dgt Ssc 25 Clines o N 25 Msg 27 ) Qal J 80 s 3 Mav Aux Vases Sandstone N J N Mts o MILL J MISSISSIPPI 34 ) Qal J N ) N J Dsl 35 N 26 J o N 25 J Mgd Mgd ) Msg Ste. Genevieve Limestone 500 o Db DITCH J 20 Mgd N N N ) J J o RIVER o N 600 J 80 N ) 10 o J Mav Æ Msl St. -
Columnals (PDF)
2248 22482 2 4 V. INDEX OF COLUMNALS 8 Remarks: In this section the stratigraphic range given under the genus is the compiled range of all named species based solely on columnals assigned to the genus. It should be noted that this range may and often differs considerably from the range given under the same genus in Section I, because that range is based on species identified on cups or crowns. All other abbreviations and format follow that of Section I. Generic names followed by the type species are based on columnals. Genera, not followed by the type species, are based on cups and crowns as given in Section I. There are a number of unlisted columnal taxa from the literature that are indexed as genera recognized on cups and crowns. Bassler and Moodey (1943) did not index columnal taxa that were not new names or identified genera with the species unnamed. I have included some of the omissions of Bassler and Moodey, but have not made a search of the extensive literature specifically for the omitted citations because of time constraints. Many of these unlisted taxa are illustrated in the early state surveys of the eastern and central United States. Many of the columnal species assigned to genera based on cups or crowns are incorrect assignments. An uncertain, but significant, number of the columnal genera are synonyms of other columnal genera as they are based on different parts of the stem of a single taxon. Also a number of the columnal genera are synonyms of genera based on cups and crowns as they come from more distal parts of the stem not currently known to be associated with the cup or crown. -
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 .......................................................................................................................... -
Faunas of the Boone Limestone
. DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR 598 FAUNAS OF THE BOONE LIMESTONE ST. JOE, ARKANSAS BY GEORGE H. GIRTY WASHINGTON GOVERNMENT PRINTING OFFICE 1915 CONTENTS. Page. Lower part of the Boone limestone......................................... 5 Introduction.......................................................... 5 Coelenterata........................................................... 7 Bryozoa............................................................... 8 Brachiopoda.........,................................................. H Pelecypoda .......................................................... 20 Gastropoda............................................................ 21 Cephalopoda.......................................................... 22 Trilobita............................................................. 22 The St. Joe limestone member ............................................ 24 Introduction.......................................................... 24 Coelenterata........................................................... 28 Echinoderrnata....................................................... 30 Bryozoa............................................................... 30 Brachiopoda.......................................................... 33 Gastropoda............................................................ 42 Index................................................................... 49 ILLUSTRATIONS. Fagc. PLATES I-11.T. Fossils from the Boone limestone ........................ -
Geology of Des Moines County
GEOLOGY OF DES MOINES COUNTY. CHARLES ROLLIN KEYES. 280. Rep. ECONOMIC GEOLOGY OF DES MOINES COUNTY. BY CHARLES ROLLIN KEYES. CONTENTS. Introduction... ..................... 413 Situation and Extent. .. .. 413 Previous 'Vork. ......................... 413 Physiography.. .. .. .. .. .. .. _. _. ........ 4 T4 Surface Relief.. ..... ..... ........ 4'4 Table of Altitudes ... .. - ........ 4[8 Drainage ... ........... 418 Stratigraphy .. • •••.•.•.. 420 General Geological Relations ... .• 420 Classification of Formations .. .. ·421 General Section ...... _.. _......... _............. _............ 421 Standard Sections..... ........... 422 I. Prospect Hill...... .......... 423 n. Augusta.. ..... _.......... _.. 423 III. Southwest Corner of County. ............ _.. 4?!4 IV. Southwest of Danville. ... _..... 424 Mississippi RiverSections .. .. 424 V. Huron Section ... ...••.......... 4Z5 VI. Dolbee Creek Section .. .426 vn. Oak Creek Section ....................... .. 4 26 VIII. Patterson Sections. ... 427 Skunk River Sections... 427 Flint River Sections... .. 428 X. KnoUy Creek . 429 XI. Big Hollow..... ............................ 429 XII. Pleasant Grove. .. .. 430 Geological Fonnations ... • .•..... 430 Mississippian Series .. 431 Kinderhook ....... 431 Correlation of Kinderhook ... ,6 4I1 412 GEOLOGY OF DES MOINES COUNTY, Userul Deposits ........................................... 438 Augusta ...................................................... 439 Lower Burlington.... .. ..... 440 Upper.Burlington................ ........•.......•...... -
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 Middle Ordovician Section in East Central Missouri
Scholars' Mine Masters Theses Student Theses and Dissertations 1922 The Middle Ordovician section in east central Missouri Morris James Ingerson Josiah Bridge Follow this and additional works at: https://scholarsmine.mst.edu/masters_theses Part of the Geology Commons Department: Recommended Citation Ingerson, Morris James and Bridge, Josiah, "The Middle Ordovician section in east central Missouri" (1922). Masters Theses. 7088. https://scholarsmine.mst.edu/masters_theses/7088 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]. TRE ]HDDLE ORDOVICIAN SECTION IK EAST CEH'l'RAL MISSOURI BY Josiah Bridge , M. s. Assistant Professor of Geology and M. J. Ingerson Graduate Assistant in Geology A T HE S I S submitted to the Faculty of the SCHOOL OF MINES AND METALLURGY OF THE UNIVERSITY OF MISSOURI in partial fulfil~ent of the work required for the Degree of M&Bter or Science :M . J. Ingerson Rolla., Mo . 1 9 2 2 Approved by c. i . Clj-CJ-i/u:__ -----------------~ ------------ Profess~r of Geology LIST OF ILLUSTRATIONS Page Section of the Joachim at Pacific, Mo. in pocket Section of Joachim at Tavern Rock, Mo. in pocket Ledge of Plattin at Joa.chim-Plattin facing page contact near Pacific, Mo. 16 "Chimneys" of Plattin Limestone near facing page Port Royal, Mo. 1'7 Section of the Plattin at Hirnms Station, in pocket Mo. -
Mississippian: Osagean)
CHONDRICHTHYAN DIVERSITY WITHIN THE BURLINGTON- KEOKUK FISH BED OF SOUTHEAST IOWA AND NORTHWEST ILLINOIS (MISSISSIPPIAN: OSAGEAN) A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science By MATTHEW MICHAEL JAMES HOENIG B.S., Hillsdale College, 2017 2019 Wright State University WRIGHT STATE UNIVERSITY GRADUATE SCHOOL Thursday, September 5th, 2019 I HEREBY RECOMMEND THAT THE THESIS PREPARED UNDER MY SUPERVISION BY Matthew Michael James Hoenig ENTITLED Chondrichthyan diversity within the Burlington-Keokuk Fish Bed of Southeast Iowa and Northwest Illinois (Mississippian: Osagean) BE ACCEPTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF Master of Science Charles N. Ciampaglio, Ph.D. Thesis Director Doyle R. Watts, Ph.D. Chair, Department of Earth & Environmental Sciences Committee on Final Examination David A. Schmidt, Ph.D. Stephen J. Jacquemin, Ph.D. Barry Milligan, Ph.D. Professor and Interim Dean of the Graduate School ABSTRACT Hoenig, Matthew Michael James. M.S. Department of Earth & Environmental Sciences, Wright State University, 2019. Chondrichthyan diversity within the Burlington-Keokuk Fish Bed of Southeast Iowa and Northwest Illinois (Mississippian: Osagean) Chondrichthyan remains occur in abundance within a thin layer of limestone at the top of the Burlington Limestone at the point of the contact with the overlying Keokuk Limestone. This layer of rock, the “Burlington-Keokuk Fish Bed,”1 is stratigraphically consistent and laterally extensive in exposures of the Burlington Limestone near its type section along the Iowa-Illinois border. Deposition of the fish bed occurred on the Burlington Continental Shelf carbonate ramp off the subtropical western coast of Laurussia during the Lower Carboniferous (Late Tournaisian; Osagean) due to a drop in sea level, although the specific mechanism(s) that concentrated the vertebrate fossils remain(s) unknown. -
Guide to the Geology of the Pere Marquette State Park Area, Jersey County
557 IL6gui 991-D uuide to the Geology of the Pere Marquette State Park Area, Jersey County David L. Reinertsen Jan is D. Treworgy Field Trip Guidebook 1991 D, October 26, 1991 Department of Energy and Natural Resources ILLINOIS STATE GEOLOGICAL SURVEY Cover photo by J. D. Treworgy Bluff of Mississippian strata along the Great River Road at Chautauqua, Jersey County, Illinois. Geological Science Field Trips The Educational Extension Unit ot the Illinois State Geological Survey conducts four free tours each year to acquaint the public with the rocks, mineral resources, and landscapes of various regions of the state and the geological processes that have led to their origin. Each field trip is an all-day excursion through one or more Illinois counties. Frequent stops are made to explore interesting phenomena, explain the processes that shape our environment, discuss principles of earth science, and collect rocks and fossils. People of all ages and interests are welcome. The trips are especially helpful to teachers preparing earth science units. Grade school students are welcome, but each must be accompanied by a parent or guardian. High school science classes should be supervised by at least one adult for each ten students. A list of earlier field trip guide leaflets for planning class tours and private outings may be obtained by contacting the Educational Extension Unit, Illinois State Geological Survey, Natural Resources Building, 615 East Peabody Drive, Champaign, IL 61820. Telephone: (217) 244- 2407 or 333-7372. primed on recycled paper ) Printed by the authority of the State of Illinois/1991/500 Guide to the Geology of the Pere Marquette State Park Area, Jersey County David L. -
OZARK UPLIFT PROVINCE (057) by Joseph R
OZARK UPLIFT PROVINCE (057) By Joseph R. Hatch INTRODUCTION The Ozark Uplift Province covers approximately 53,000 sq mi in eastern and southern Missouri (76 counties) and northern Arkansas (10 counties). The province is bounded on the north by the Iowa Shelf Province (052), on the east by the Illinois Basin Province (064), on the south by the Arkoma Basin Province (058), and on the west by the Cherokee Platform (060) and Forest City Basin (056) Provinces. The major structural element in the province is the domal Ozark Uplift, from which sedimentary rocks have been eroded, leaving approximately 350 sq mi of Precambrian granite exposed in the core area. The sedimentary cover in the Ozark Uplift Province averages less than 2000 ft and primarily consists of dolomites and sandstones of Cambrian and lower Ordovician age. A generalized stratigraphic column for the province is shown in figure 2. In the western part of the Ozark area, Mississippian rocks overlap lower Ordovician rocks, and Middle Ordovician, Silurian, and Devonian rocks are absent. Middle Ordovician, Middle Devonian, Mississippian, and Pennsylvanian rocks are generally present in the counties north of the Missouri River (Adler and others, 1971). One conventional hypothetical play has been defined for this province, Middle Ordovician (Champlainian) Play (5701). ACKNOWLEDGMENTS Scientists affiliated with the American Association of Petroleum Geologists and from various State geological surveys contributed significantly to play concepts and definitions. Their contributions are gratefully acknowledged. CONVENTIONAL PLAYS 5701. MIDDLE ORDOVICIAN (CHAMPLAINIAN) PLAY (HYPOTHETICAL) The hypothetical Middle Ordovician (Champlainian) Play in the Ozark Uplift Province is based on (1) current hydrocarbon production from age-equivalent rocks in the adjacent Illinois Basin and Forest City Basin Provinces (064 and 056); (2) the presence of potentially good to excellent hydrocarbon source rocks in the Middle Ordovician section; and (3) the presence of potential sandstone and porous dolomite and limestone reservoirs. -
Geologic Map of the Harrison 1° X2° Quadrangle, Missouri and Arkansas
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Geologic map of the Harrison 1° x2° quadrangle, Missouri and Arkansas by Mark A. Middendorf1, Kenneth C. Thomson2, Charles E. Robertson1, John W. Whitfield1, Ernest E. Glick3, William V. Bush4, Boyd R. Haley3, and John David McFarland HI4 Open-File Report 94-430 Prepared in cooperation with the Missouri Department of Natural Resources, Division of Geology and Land Survey, and the Arkansas Geological Commission This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards. Missouri Department of Natural Resources, Division of Geology and Land Survey 2Southwest Missouri State University 3U.S. Geological Survey, Little Rock, Ark. 4Arkansas Geological Commission 1994 FOLIO NOTE This map is the fifth in a folio of maps of the Harrison 1° x2° quadrangle, Arkansas and Missouri, prepared under the Conterminous United States Mineral Assessment Program. Previously published maps in this folio relate to the geochemistry of the subsurface carbonate rocks (Erickson and others, 1988), the geophysics of the basement terranes (McCafferty and others, 1989), the carbonate depositional lithofacies and mineralization in the Caulfield district (Hayes and others, 1992), and the mineral-resource potential of the quadrangle (Pratt and others, 1993). A multicolor version of this map is being processed for publication in the U.S. Geological Survey Miscellaneous Investigations Map series. Additional maps showing various other geologic aspects of the Harrison quadrangle will be published as U.S. Geological Survey Miscellaneous Field Studies Maps bearing the same serial number with different letter suffixes (MF-1994-E, -F, etc.). -
Katian GSSP and Carbonates of the Simpson and Arbuckle Groups in Oklahoma Jesse R
University of Dayton eCommons Geology Faculty Publications Department of Geology 2015 Katian GSSP and Carbonates of the Simpson and Arbuckle Groups in Oklahoma Jesse R. Carlucci Midwestern State University Daniel Goldman University of Dayton, [email protected] Carlton E. Brett University of Cincinnati - Main Campus Stephen R. Westrop University of Oklahoma Stephen A. Leslie James Madison University Follow this and additional works at: https://ecommons.udayton.edu/geo_fac_pub Part of the Geology Commons, and the Stratigraphy Commons eCommons Citation Carlucci, Jesse R.; Goldman, Daniel; Brett, Carlton E.; Westrop, Stephen R.; and Leslie, Stephen A., "Katian GSSP and Carbonates of the Simpson and Arbuckle Groups in Oklahoma" (2015). Geology Faculty Publications. 5. https://ecommons.udayton.edu/geo_fac_pub/5 This Article is brought to you for free and open access by the Department of Geology at eCommons. It has been accepted for inclusion in Geology Faculty Publications by an authorized administrator of eCommons. For more information, please contact [email protected], [email protected]. Stratigraphy, 12 (2) 12th International Symposium on the Ordovician System Katian GSSP and Carbonates of the Simpson and Arbuckle Groups in Oklahoma Jesse R. Carlucci1 Daniel Goldman2 Carlton E. Brett3 Stephen R. Westrop4 Stephen A. Leslie5 1Assistant Professor, Kimbell School of Geosciences, Midwestern State University, Wichita Falls TX, [email protected] 2Professor & Chair, Department of Geology, University of Dayton, Dayton OH, [email protected] 3Professor, Department of Geology, University of Cincinnati, Cincinnati OH, [email protected] 4Professor & Curator of Invertebrate Paleontology, University of Oklahoma, Sam Noble Oklahoma Museum of Natural History, Norman OK, [email protected] 5Professor & Department Head, Department of Geology and Environmental Science, James Madison University, Harrisonburg VA, [email protected] 144 Stratigraphy, 12 (2) TABLE OF CONTENTS & GPS COORDINATES pg.