The University of Oklahoma Graduate College Geology

Total Page:16

File Type:pdf, Size:1020Kb

The University of Oklahoma Graduate College Geology THE UNIVERSITY OF OKLAHOMA GRADUATE COLLEGE GEOLOGY OF WAGONER COUNTY, OKLAHOMA A DISSERTATION SUBMITTED TO THE GRADUATE FACULTY in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY BY RAYMOND W. GOVETT Norman, Oklahoma 1959 GEOLOGY OF WAGONER COUNTY, OKLAHOMA APPROVED BY DISSERTATION COMMITTEE ACKNOWLEDGMENTS The writer wishes to express his appreciation to the Oklahoma Geological Survey for the assistance given while working on th is p ro je c t. Dr. Carl C. Branson checked the work and served as chairman of the doctoral committee. The following men served on the doctoral committee and offered constructive criticism : Dr. E. A. Frederickson, Dr. George G. Huffman, Dr. Charles J. Mankin and Dr. Clifford A. M erritt. Dr. P. K. Sutherland helped to identify the inverte­ brate fossils. Thanks are due to the many farmers and ranchers in the County who gave permission to enter their land and aided in locating outcrops. The writer wishes to thank his father, Mr. Sam E. Govett, for assistance in preparation of the manuscript. The writer is especially indebted to his wife, Lenora, for help in several phases of this project. iii TABLE OF CONTENTS Page ACKNOWLEDGMENTS ................................................................................. i i i LIST OF PLATES ................................................................................... v i i LIST OF TABLES ................................................................................... v i i i LIST OF ILLUSTRATIONS .................................................................... ix Chapter I . INTRODUCTION .......................................................................... 1 Scope and Purpose ....................................................... 1 L ocation .......................................................................... 1 Accessibility ............................................................... 3 Previous Investigations .......................................... 6 Present Investigation .............................................. 10 I I . GEOGRAPHY................................................................................ 12 Topographic Features ................................................ 12 D rainage ........................................................................... 13 C lim ate ............................................................................. 15. S o ils ................................................................................. 17 Economic Development ................................................ 19 I I I . SURFACE STRATIGRAPHY........................................................ 21 General Statement ....................................................... 21 M ississippian System ................................................ 22 Osage Series ............................................................. 23 Reeds Spring Formation ............................... 23 Keokuk Formation ............................................ 24 iv Chapter Page Meramec S eries ......................................................... 25 Mayes Group ........................................................... 25 Moorefield Formation ................................... 26 Bayou Manard Member ................................. 29 Lindsey Bridge Member ............................. 30 Ordnance Plant Member ............................. 30 Chester Series ......................................................... 31 Hindsville Formation .......... 31 Fayetteville Formation ................................. 33 Pitkin Formation ............................................ 34 Pennsylvanian System ..................................... 36 Morrowan Series ....................................................... 38 Hale Formation ................................................ 38 Bloyd Formation .............................................. 41 Atokan Series ........................................................... 42 Atoka Formation .............................................. 42 Desmoinesian Series .............................................. 45 Hartshorne Formation ................................... 46 McAlester Formation ..................................... 48 Warner Sandstone Member ........................ 50 Savanna Formation ...................................... 52 Spaniard Limestone Member .................... 53 Sam Creek Limestone Member .................. 58 Spiro Sandstone Member ........................ 61 Rowe Coal .................................................. 63 Doneley Limestone Member ...................... 64 Drywood Coal ................................................ 65 Boggy Form ation .............................................. 67 Bluejacket Sandstone Member ................ 69 Secor ? Coal ................................................ 72 Bluejacket Coal .......................................... 75 Inola Limestone Member ........................... 76 Taft Sandstone Member ............................. 79 Weir-Pittsburg ? Coal ............................. 82 Senora Formation ............................................ 82 Tebo Coal ....................................................... 85 Tiawah Limestone Member ........................ 86 Chelsea Sandstone Member ...................... 88 McNabb Limestone Member ......................... 90 Croweburg Coal ............................................ 92 Verdigris Limestone Member .................. 93 Lagonda Member ............................................ 96 Iron Post Coal ............................................ 99 Chapter Page Kinhison Shale Member ............................. 100 Bheezy^Hill Limestone Member ............. 100 E x c ^ ld Shale Member ............................... 103 Fort S^K^t Formation ................................... 103 Labette r^mation .......................................... 105 Calvin Fondation ............................................ 106 Wetumka Form ation .............. 106 Quaternary System ..................................\ ............... 108 Terrace Deposits ...............................v............. 109 Alluvial Deposits ................................................... I l l IV. STRUCTURAL GEOLOGY .................................................. 114 F a u lts ............................................................................... 114 Folds ................................................................. 122 J o in ts ............. 125 Pimple Mounds ................................................................ 125 V. HISTORICAL GEOLOGY ............................................................. 126 VI. ECONOMIC GEOLOGY ................................................................. 131 V II. SUMMARY..................................................................................... 138 REFERENCES ................................................................................................ 142 APPENDIX A. MEASURED SECTIONS ............................................................... 151 vi LIST OF PLATES Plate Page 1. Geologic Map of Wagoner County, Oklahoma .. In Pocket 2. Generalized Columnar Section ............................. In Pocket vii LIST OF TABLES Table Page 1. Average Mean Temperature in the City of Wagoner ..................................................................................... 16 2. Average Monthly Rainfall .......................................... 17 3. Fauna from the Spaniard Limestone ............................. 56 4. Fossils from the Sam Creek Limestone ....................... 61 5. Fauna from the Inola Limestone .................................... 78 6. Fauna from the Verdigris Limestone .......................... 96 7. Fauna from the Breezy Hill Limestone ...................... 102 viii LIST OF ILLUSTRATIONS Figure Page 1. Location Map of Wagoner County, Oklahoma .............. 2 2. Contrast in bedding characteristics of the Reeds Spring, below, and the Keokuk, above. Big Hollow Creek, sec. 2, T. 18 N., R. 19 E. ... 28 3. Bayou Manard member of the M oorefield formation. Cut on an abandoned railroad, center of the north side of sec. 2, T. 18 N ., R. 19 E ........................................................................ 28 4. Moorefield limestone. SE^ sec. 6, T. 18 N., R. 20 E ........................................................................ 39 5. Pitkin, Hale, Bloyd contact at the west end of Fort Gibson Dam. NE cor. sec. 13, T. 16 N., R. 19 E. Pitkin Hale contact at the break above the white sign. Bloyd-Hale contact at the top of the steep cliff .................... 39 6. Savanna formation exposed below the Blue­ jacket sandstone in the south bank of the Verdigris River. Center sec. 12, T. 17 N., R. 16 E. .................................... 54 7. Spaniard limestone. Center SE^ sec. 5, T, 16 N ,, R. 18 E. ..................... 54 8. Spaniard limestone in the bed of the Verdigris River. Center SW% sec. 5, T. 16 N ., R. 18 E ........................................................................ 60 ix Figure Page 9. A long crinoid stem in the Spaniard lime­ stone. Center SE^ sec. 5, T. 16 N., R. 18 E ........................................................................................... 60 10. Sam Creek limestone and the conglomeratic zone below it. The zone here contains brown chert pebbles. In the east bank of a creek, near the center of the north side of sec. 9, T. 16 N ., R. 17 E ................ 66 11. Base of the Bluejacket sandstone. Near the NW
Recommended publications
  • Geologic Map of the Hasty Quadrangle, Boone And
    U.S. DEPARTMENT OF THE INTERIOR SCIENTIFIC INVESTIGATIONS MAP 2847 U.S. GEOLOGICAL SURVEY Version 1.0 A 1370 CORRELATION OF MAP UNITS Fayetteville Shale (Upper Mississippian, Chesterian)—Fine-grained Contact mapped the eastern and western parts of this system as separate grabens. This study 1440 1260 1300 sandstone and siltstone of the Wedington Sandstone Member that grades 88 illustrates that the northern bounding fault is continuous across the area, with a curvilinear 1380 1420 1400 Qty downward into main body of black, slope-forming shale. Thickness varies 60 Normal fault—Showing fault dip (arrow) and rake (diamond-headed arrow) map trace. McKnight (1935) called the eastern extension of this northern fault the St. Joe 1450 2 1340 Mb Ql QUATERNARY where known. Bar and ball on downthrown side. Dashed where 1320 Mf Qtm from 250 to 370 ft fault and that name is adopted here. The southern boundary of the graben system within Mfw Wedington Sandstone Member—Brown, well-indurated, calcite-cemented approximately located the quadrangle is formed by two normal faults that partly overlap in sec. 7, T. 16 N., R. 19 2 1050 1490 QTto sandstone and siltstone. The Wedington caps a steep slope and is Normal, right-lateral, strike-slip fault—Bar and ball on downthrown side. W. Where observed, the main planes of faults forming the graben system dip steeply 950 1420 3 TERTIARY(?) 1290 1325 Mbv ° ° 1320 3 separated from the overlying Pitkin Limestone by thin black shale that Dashed where approximately located. In cross section A–A', A, movement (72 –83 ); where slip striations have been preserved on these faults or nearby smaller faults, Mf 1340 1335 Unconformity 1270 commonly forms a bench.
    [Show full text]
  • The Brachiopod Antiquatonia Coloradoensis (Girty) from the Upper Morrowan and Atokan (Lower Middle Pennsylvanian) of the United States
    U.S. Department of the Interior U.S. Geological Survey The Brachiopod Antiquatonia coloradoensis (Girty) from the Upper Morrowan and Atokan (Lower Middle Pennsylvanian) of the United States U.S. Geological Survey Professional Paper 1588 The Brachiopod Antiquatonia coloradoensis (Girty) from the Upper Morrowan and Atokan (Lower Middle Pennsylvanian) of the United States By Thomas W. Henry T OF EN TH U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1588 TM E R I A N P T E E D R . I O S . R Taxonomic and biostratigraphic analysis of a widespread and U stratigraphically restricted, semireticulate productid brachiopod M 9 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, Interim 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 Henry, Thomas W. The brachiopod Antiquatonia coloradoensis (Girty) from the upper Morrowan and Atokan (lower Middle Pennsylvanian) of the United States / by Thomas W. Henry. p. cm.—(U.S. Geological Survey professional paper ; 1588) Includes bibliographical references (p. – ). 1. Antiquatonia coloradoensis—United States. 2. Paleontology—Pennsylvanian. 3. Animals, Fossil—United States. I. Title. II. Series. QE797.S89H46 1988 564′.68—dc21 97–42005 CIP CONTENTS
    [Show full text]
  • Geology of the Coal Hill Hartman, and Clarksville Quadrangles, Johnson County and ,Vicinity, Arkansas
    Geology of the Coal Hill Hartman, and Clarksville Quadrangles, Johnson County and ,Vicinity, Arkansas GEOLOGICAL SURVEY PROFESSIONAL PAPER 536-C Prepared in cooperation with the Arkansas Geological Commission Geology of the Coal Hill Hartman, and Clarksville Quadrangles, Johnson cnunty and Vicinity, Arkansas By E. A. MEREWETHER and BOYD R. HALEY GEOLOGY OF THE ARKANSAS VALLEY COAL FIELD GEOLOGICAL SURVEY PROFESSIONAL PAPER 536-C Prepared in cooperation with the Arkansas Geological Commission UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1969 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Page Abstract__________________________________________ _ C1 Stratigraphy-Continued Introduction ______________________________________ _ 1 Pennsylvanian System---continued StratigraphY--------------------------------------- 4 Des Moines Series, Krebs Group-Continued Ordovician System_____________________________ _ 4 McAlester Formation __________________ _ C18 Everton Formation and St. Peter Sandstone un- Savanna Formation ____________________ _ 19 divided_________________________________ _ 4 Quaternary System _____________________________ _ 21 Plattin Limestone and Kimmswick Limestone Terrace deposits ___________________________ _ 21 undivided _______________________________ _ 4 Alluvium _________________________________ _ 21 Fernvale Limestone ________________________
    [Show full text]
  • Arkansas Geology: Bluffs, Crevices, Pedestals, and Fossils
    EWS - 08 STATE OF ARKANSAS ARKANSAS GEOLOGICAL SURVEY BEKKI WHITE, DIRECTOR AND STATE GEOLOGIST ______________________________________________________________________________ EDUCATIONAL WORKSHOP SERIES 08 ______________________________________________________________________________ Arkansas Geology: Blus, Crevices, Pedestals, and Fossils Angela Chandler Little Rock, Arkansas 2015 EWS - 08 STATE OF ARKANSAS ARKANSAS GEOLOGICAL SURVEY BEKKI WHITE, DIRECTOR AND STATE GEOLOGIST ______________________________________________________________________________ EDUCATIONAL WORKSHOP SERIES 08 ______________________________________________________________________________ Arkansas Geology: Blus, Crevices, Pedestals, and Fossils Angela Chandler Little Rock, Arkansas 2015 STATE OF ARKANSAS Mike Beebe, Governor Arkansas Geological Survey Bekki White, State Geologist and Director COMMISSIONERS Dr. Richard Cohoon, Chairman………………………. Russellville William Willis, Vice Chairman………………………… Hot Springs Gus Ludwig…….…………………………………......... Quitman Ken Fritsche……………………………………………. Greenwood William Cains…………………………………………… Altus Quin Baber……………………………………………… Benton David Lumbert………………………………………….. Little Rock Little Rock, Arkansas 2015 Table of Contents Geologic Setting..…………………………………………………….. 1 Deposition of rock formations – Upper Mississippian (331-323 million years ago ).......................................................................... 4 Description of rock formations – Boston Mountain Plateau – Pitkin Limestone………………………………….. 5 Deposition of rock formations
    [Show full text]
  • Mississippian Cephalopods of Northern and Eastern Alaska
    Mississippian Cephalopods of Northern and Eastern Alaska By MACKENZIE GORDON, JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 283 Descr9tions and illustrations of nautiloids and ammonoids and correlation of the assemblages with European Carbonferous goniatite zones UNITED STATES GOVERNMENT PRINTING OF,FICE, 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 $1.50 (paper cover) CONTENTS Pane Page 1 Stratigraphic and geographic distribution-Continued Introduction - - - - - - .. - - - - ... - - - - - - - - - - - - .. - - - - - - - - - - - - - 1 Brooks Range-Continued Previous work-------------------------------------- 1 Kiruktagiak River basin--Chandler Lake area- - Composition of the cephalopod fauna ------------------ 2 Siksikpuk River basin ------- ---------- ------ Stratigraphic and geographic distribution of the cepha- Anaktuvuk River basin _------------..-..------ lopods------------------------------------------- Nanushuk River basin ...................... - Brooks Range---------------------------------- Echooka River basin --------- ----- - Cape Lisburne region ------- -- --- --------- - - - Eagle-Circle district ---__ _ -___ _- --- --- - - ---- - -- - - Lower Noatak Rlver basin -----------------..- Age and correlation of the cephalopod-bearing beds- ---- Western De Long Mountains_--__----- .------ Mississippian cephalopod-collecting localities in Alaska- -
    [Show full text]
  • Significance for International Correlation of the Perapertú Formation in Northern Palencia, Cantabrian Mountains
    PERAPERTÚ FM, CANTABRIAN MTS. GONIATITES 127 SIGNIFICANCE FOR INTERNATIONAL CORRELATION OF THE PERAPERTÚ FORMATION IN NORTHERN PALENCIA, CANTABRIAN MOUNTAINS. TECTONIC/STRATIGRAPHIC CONTEXT AND DESCRIPTION OF MISSISSIPPIAN AND UPPER BASHKIRIAN GONIATITES Jürgen KULLMANN1, Robert H. WAGNER2 and Cornelis F. WINKLER PRINS3 1 Institut für Geowissenschaften der Universität Tübingen, Sigwartstraβe 10, D 72076 Tübingen, Germany; e-mail: [email protected] 2 Corresponding author: Centro Paleobotánico, Jardín Botánico de Córdoba, Avda. de Linneo, s/n, E 1�00������������ Córdoba �Spain����������; e-mail: [email protected] 3 Nationaal Natuurhistorisch Museum, Postbus 9517, NL 2300 RA Leiden, The Netherlands; e-mail: [email protected] Kullmann, J., Wagner R. H. & Winkler Prins, C.F. 2007. Significance for international correlation of the Pera- pertú Formation in northern Palencia, Cantabrian Mountains. Tectonic/stratigraphic context and description of Mississippian and Upper Bashkirian goniatites. �������������������������������������������������������������El significado de la Formación Perapertú para la correlación internacional, norte de Palencia, Cordillera Cantábrica. Contexto tectónico/estratigráfico y descripción de go- niatítidos misisípicos y del Bashkiriense Superior.] Revista Española de Paleontología, 22 �2�, 127-1�5. ISSN 0213-6937. ABSTRACT Small ammonoid assemblages are recorded from the Perapertú Formation in northern Palencia. This is a mud- stone unit with local platform limestones characterised by carbonate debris flows
    [Show full text]
  • Pre-Atoka Rocks of Northern Arkansas
    Pre-Atoka Rocks of Northern Arkansas GEOLOGICAL SURVEY PROFESSIONAL PAPER 314-H Pre-Atoka Rocks of Northern Arkansas By SHERWOOD E. FREZON and ERNEST E. CLICK SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 314-H Thickness, lithofacies, and geologic history of potential oil and gas producing rocks of Paleozoic age in northern Arkansas UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1959 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U. S. Geological Survey Library has cataloged this publication as follows: Frezon, Sherwood Earl, 1921- Pre-Atoka rocks of northern Arkansas, by Sherwood E. Frezon and Ernest E. Glick. Washington, U. S. Govt. Print. Off., 1959. iii, 171-189 p. maps, diagrs., table. 30 cm. (U. S. Geological Sur­ vey. Professional paper 314-H. Shorter contributions to general geology) Part of illustrative matter fold, col., in pocket. Bibliography: p. 186-187. 1. Geology Arkansas. 2. Rocks, Sedimentary. 3. Geology, Strati- graphic Paleozoic. i. Glick, Ernest Earwood, 1922- joint author, n. Title. (Series: U. S. Geological Survey. Professional paper 314-H. Series: U. S. Geological Survey. Shorter contribu­ tions to general geology) 551.7209767 For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. CONTENTS Page Abstract .__----_ ---_-_._--._---__-_-____ 171 Stratigraphy Continued Page Introduction. ___ ___________________________________ 171 Probable latest Mississippian and early
    [Show full text]
  • Geologic Map of the Mountain View Quadrangle, Stone County, Arkansas
    Digital Geologic Quadrangle Map Arkansas Geological Survey Mountain View Quadrangle, Arkansas Bekki White, State Geologist and Director Geologic Map of the Mountain View Quadrangle, DGM-AR-00604 Stone County, Arkansas Richard S. Hutto and Daniel S. Rains 2013 Correlation of Map Units Description of Map Units Stratigraphic Column Alluvial terrace (Quaternary) - Unconsolidated clay, silt, Holocene Qat Qat Qls Quaternary sand and gravel on either the modern floodplain or the Pleistocene modern floodplain and one or more terrace levels. SystemSeries Member Formation Unconformity 1500 Landslide deposits (Quaternary) - A mass of rock and Qls Ùhc Morrowan Pennsylvanian debris that has moved downslope due to gravity. Only the largest landslide deposits are depicted. 1400 Cane Hill Unconformity Hale Morrowan 400 Pennsylvanian Mpi Hale Formation (Pennsylvanian, Morrowan) – Consists 1300 of two members, the Prairie Grove and the Cane Hill. Only Mp the Cane Hill Member is present on this quadrangle. 1200 Chesterian Cane Hill Member consists of very thin to Ù Imo interval Mf hc medium-bedded, and rarely thick-bedded, very fine 1100 grained, silty sandstone with shale interbeds. The Mbv Mississippian sandstone is buff to brown on freshly broken and 1000 weathered surfaces, characteristically ripple- or 300 Mm Meramecian flat-bedded, and typically weathers to flagstone; locally thick-bedded and cross bedded; Other rare features 900 Unconformity include liesegang boxwork, bioturbation, and plant Pitkin Limestone Mb Osagean fossils. The shale is typically not exposed but mostly 800 Chesterian clayey and black to dark-gray with rare liesegang Mississippian boxwork. Unconformable with the underlying Imo Unconformity 700 interval. Up to 220 feet (67 meters) thick.
    [Show full text]
  • Stratigraphy and Depositional Characterization of the Moorefield
    University of Arkansas, Fayetteville ScholarWorks@UARK Theses and Dissertations 5-2019 Stratigraphy and Depositional Characterization of the Moorefield hS ale (Middle-Late Mississippian) in its Type Area, Northeastern Arkansas (Eastern Arkoma Basin) Griffina W rner Follow this and additional works at: https://scholarworks.uark.edu/etd Part of the Geology Commons, Sedimentology Commons, and the Stratigraphy Commons Stratigraphy and Depositional Characterization of the Moorefield Shale (Middle-Late Mississippian) in its Type Area, Northeastern Arkansas (Eastern Arkoma Basin) A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology by Griffin Warner University of Arkansas Bachelor of Science in Geology, 2017 May 2019 University of Arkansas This thesis is approved for recommendation to the Graduate Council Walter L. Manger, Ph.D. Thesis Advisor T.A. “Mac” McGilvery, Ph.D. Committee Member Glenn Sharman, Ph.D. Committee Member Abstract The Moorefield Shale represents the Meramecian Series in the Eastern Arkoma Basin in northern Arkansas. Lying on the margin of the Mississippi Embayment and Reelfoot Rift, sequence stratigraphic interpretations have labelled the Moorefield Shale a lowstand wedge succeeding the Early Mississippian (Osagean) Boone Limestone conformably and overlain conformably by the Hindsville Limestone/Batesville Sandstone. The unit contains a basal brown- black limestone and succeeding brown-black phosphatic shale. The Moorefield Shale was deposited along the broad, stable cratonic platform on the southern flank of Laurasia, before it’s collision with Gondwanaland to form the supercontinent Pangea at the end of the Paleozoic. During this time, the midcontinent region was covered by shallow seas and carbonates covered most of the region.
    [Show full text]
  • THE UNIVERSITY of Oklahœia GRADUATE COLLEGE the ATOKA FORMATION W the N Œ T H SIDE of the Mcalester BASIN a DISSERTATION SUBMI
    THE UNIVERSITY OF OKlAHŒiA GRADUATE COLLEGE THE ATOKA FORMATION W THE N Œ T H SIDE OF THE McALESTER BASIN A DISSERTATION SUBMITTED TO THE ŒIADUATE FACULTY in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY BY JACK GORDON BLYTHE Norman, Oklahoma 1957 THE ATOKA FORMATION ON THE NORTH SIDE OF THE McALESTER BASIN APPROVED BY j /•) • DISSERTATION CCMMITTEE ACKNOWLEDGMENTS Dr. Carl C. Branson directed this dissertation problem. Dr. George G. Huffman, Dr. E. L. Lucas, Dr. Doris Curtis, and Dr. Reginald Harris contributed helpful advice and information. The Oklahoma Geo­ logical Survey employed the author as field geologist during the summer of 1954. Assistance was rendered in the field by Richard Beveridge during the month of June in 1953; and Mr. A. H. Hanson of Muskogee, Oklahoma, spent a portion of one day in the field with the author, directing his attention to several fossil localities in the Atoka for­ mation. Mr. Irwin Gold photographed the thin sections and the fossils, Mr. June D. King took some of the field photographs, Mr. Raymond Kune instructed the author in certain procedures of drafting, and Mr. Roy Davis and Mr. Kent Gregg assisted with much of the drafting. The author's wife, Ruth, assisted in certain phases of the field work, typed preliminary drafts of the dissertation, and continually en­ couraged the author during all phases of the dissertation program. Ill TABLE OF CONTENTS Page LIST OF ILLUSTRATIONS .................................... vi LIST OF MAPS xiii Chapter I . INTRODUCTION 1 II. STRATIGRAPHY 10 III. SEDIMENTATIOMAL ASPECTS AND ENVIRONMENTS OF DEPOSITION 52 IV.
    [Show full text]
  • Biostratigraphy of the Morrow Group of Northern Arkansas James Harrison Quinn University of Arkansas, Fayetteville
    Journal of the Arkansas Academy of Science Volume 23 Article 32 1969 Biostratigraphy of the Morrow Group of Northern Arkansas James Harrison Quinn University of Arkansas, Fayetteville Follow this and additional works at: http://scholarworks.uark.edu/jaas Part of the Stratigraphy Commons Recommended Citation Quinn, James Harrison (1969) "Biostratigraphy of the Morrow Group of Northern Arkansas," Journal of the Arkansas Academy of Science: Vol. 23 , Article 32. Available at: http://scholarworks.uark.edu/jaas/vol23/iss1/32 This article is available for use under the Creative Commons license: Attribution-NoDerivatives 4.0 International (CC BY-ND 4.0). Users are able to read, download, copy, print, distribute, search, link to the full texts of these articles, or use them for any other lawful purpose, without asking prior permission from the publisher or the author. This Article is brought to you for free and open access by ScholarWorks@UARK. It has been accepted for inclusion in Journal of the Arkansas Academy of Science by an authorized editor of ScholarWorks@UARK. For more information, please contact [email protected], [email protected]. Journal of the Arkansas Academy of Science, Vol. 23 [1969], Art. 32 183 Arkansas Academy of Science Proceedings, Vol. 23, 1969 BIOSTRATIGRAPHY OF THE MORROW GROUP OF NORTHERN ARKANSAS James Harrison Quinn Dept. of Geology, University of Arkansas The Morrow Group of northwest Arkansas (p. 184, fig. 1) is of early Pennsylvanian age (300 M. Y., Kulp et. al. 1961, p.lll, fig. 1) and includes the Hale and Bloyd Formations. The term Morrow was introduced by Adams (1904, p.
    [Show full text]
  • Aquifer List
    ARKANSAS NATURAL RESOURCES COMMISSION 101 East Capitol Avenue, Suite 350; Little Rock, AR 72201 Phone: (501) 682-1611 Fax: (501) 682-3991 www.anrc.arkansas.gov T T Arkansas Aquifer Codes E This is a list of the identified underground aquifers and their code numbers in the state. E ALLUVIUM 112ALVM EVERTON FORMATION 364EVRN PENTERS CHERT 347PNRS ANNONA CHALK 211ANNN FAYETTEVILLE SHALE 332FTVL PIKE GRAVEL 217PIKE ARKADELPHIA MARL 211AKDP FERNVALE LIMESTONE 361FRVL PITKIN LIMESTONE 331PTKN E E ARKANSAS NOVACULITE 330ARKS GASCONADE DOLOMITE 367GSCK PLATTIN LIMESTONE 364PLTN ATOKA FORMATION 326ATOK GOODLAND LIMESTONE 218GDLD PLEISTOCENE SERIES 112PLSC ATOKAN SERIES 326ATKN GUNTER SANDSTONE 367GNTR PLIOCENE SERIES 121PLCN BATESVILLE SANDSTONE 331BSVL HALE FORMATION 328HALE POLK CREEK SHALE 361PKCK H H BIGFORK CHERT 364BGFK HARTSHORNE SANDSTONE 325HRSR PORTERS CREEK CLAY 125PRCK BLACK ROCK FORMATION 367PKRK HATTON TUFF LENTIL 330HNTF POTOSI DOLOMITE 371POTS BLAKELY SANDSTONE 367BLKL HINDSVILLE LIMESTONE 331HDVL POWELL DOLOMITE 368PWLL BLAYLOCK SANDSTONE 350BLCK HOLLY CREEK FORMATION 218HLCK PRAIRIE GROVE 328PRGV S S BLOYD SHALE 328BLVD HOLOCENE ALLUVIUM 111ALVM PRECAMBRIAN ERATHEM 400PCMB BOGGY SHALE 325BGGY HOLOCENE SERIES 111HLCN PRECAMBRIAN IGNEOUS ROCKS 400IGNS BONNETERRE DOLOMITE 371BNTR HOT SPRINGS SANDSTONE 330HSPG QUATERNARY ALLUVIUM 110ALVM BOONE FORMATION 330BOON JACKFORK SANDSTONE 328JKFK REDFIELD FORMATION 124RDFD BRASSFIELD LIMESTONE 357BFLD JACKSON GROUP 124JCKS ROUBIDOUX FORMATION 367RBDX T T BRENTWOOD LIMESTONE 328 BRND JEFFERSON
    [Show full text]