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INFORMATION TO USERS This manuscript has bean raproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event tfiat tfie author did not send UMI a complete manuscript and there are missing pages, these wilt be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand comer and continuing from left to right in equal sections with small overlaps. Photographs included in the original manuscript have been reproduced xerographically in this copy. Higher quality 6* x 9* black and white photographic prints are available for any photographs or illustrations appearing in this copy for an additional charge. Contact UMI directly to order. Bell & Howell Infbrmation and Learning 300 North Zeab Road. Ann Arbor. Ml 48106-1346 USA 800-521-0600 u m t NOTE TO USERS This reproduction Is the best copy available. UMI UNIVERSITY OF OKLAHOMA GRADUATE COLLEGE THE GEOARCHAEOLOGY OF DAY CREEK CHERT: LITHOSTRATIGRAFHY, PETROLOGY, AND THE INDIGENOUS LANDSCAPE OF NORTHWEST OKLAHOMA AND SOUTHWEST KANSAS A Dissertation SUBMITTED TO THE GRADUATE FACULTY in partial fulfilment of the requirements for the degree of Doctor of Philosophy By BERKLEY BARNETT BAILEY Norman, Oklahoma 200 0 UMI Number 9975805 UMI* UMI MiCFOform9975805 Copyright 2000 by Bell & Howell Information and Learning Company. -
Please Pass the Salt: Using Oil Fields for the Disposal of Concentrate from Desalination Plants
FINAL REPORT - June 2005 Please Pass the Salt: Using Oil Fields for the Disposal of Concentrate from Desalination Plants PRESSURE 8 0 % % 0 8 0 500 1,000 1,500 2,000 2,500 3,000 3,500 4,000 6 J l 0 C % % a 0 C 0 J + 6 + J J M 4 JJ J O 4 JJ J JJ J J J g 0 J JJ J J J J S JJ JJ J % % J J J J JJ J 1,000 J JJJJJJ J JJJ J J 0 JJJ J JJJJJ JJJJ J J J J 4 JJJ JJJJJ JJ JJ J J J JJJJJJJJJ JJJJJJJJJ JJ 2 JJJJ JJJ JJ J J 0 J JJJJJ JJ JJJJ J J JJ J JJJJJJJJ J J % % J J JJJJJJJJJJ J JJ 2,000 JJ JJJ JJJJJ J J JJJ J 0 J JJJ JJJJJJJJJ JJJ J J JJ 2 JJ JJJJ J J J J JJJ JJ J J JJ J J J JJJJJ J JJ J J J JJ JJJJJJJJ J JJ J J JJJ J J JJJ J J 3,000 JJ JJ JJ J J J J JJ JJ J JJ J J JJ J J J J J J JJ J J J J J J J J JJ J JJJJ J J J JJ J JJ JJ JJJ JJJ J J JJJ J J J J JJ J JJ J J J J 4,000 J J J JJ JJJJJ J J J J JJJJ J J J J J JJ JJJJJ J J JJJJ DEPTH J J J J JJ JJJJ 5,000 J JJJ JJ JJ 2 JJJJ 0 % J JJ % 0 J JJJJ 2 J J J J 80% N JJJ 80% a JJ JJJ 3 6,000 JJJ J + J J O 4 JJ C 0 % K JJJ % J 0 J JJ H S g 4 JJ J O 60% JJ JJ J 60% M 4 7,000 6 JJ 0 J JJ J J J % % J JJ J J J J J 0 J JJ JJJ J J J J 6 JJJJ J 40% J J J J J J J J J J JJ 40% J J J JJ J JJ JJ J JJ 8,000 J J J J J 8 J J J J J JJJJJJ J J J J J J J 0 J J J J JJ JJ J J J J % J JJ J J J J JJ J JJ JJ J % J J JJJ JJJJ JJJJ J JJ J J J JJJJ JJJ J J 0 J JJJJJJ JJJJJJ J J JJJ J J JJ JJJ JJJJJJJ J JJ J 8 J JJ JJJJ JJJJJJ J JJ JJJ J JJ 20% J J JJJ JJJJJJJJJJ JJ JJJJJJ J J J J J JJJ JJJJJJ JJJJJJJ JJJ J JJJJ J 20% J JJ JJJJ JJJJJJJJJJJJJ J JJJ JJJ JJJJ J JJ JJJJJ JJJJJJJJJJJJJJJJJJJ JJJJJJJ J J J JJJJJJJJJJJJJJJJJJJJJJJJ JJJJJJJJJJ -
SPRING 1963 Bulletin 4 BURR A. SILVER
SPRING 1963 Bulletin 4 The Bluehonnet Lake Waco Formation {Upper Central Lagoonal Deposit BURR A. SILVER thinking is more important than elaborate equipment-" Frank Carney, Ph.D. Professor of Geology Baylor University 1929-1934 Objectives of Geological at Baylor The of a geologist in a university covers but a few years; his education continues throughout his active life. The purposes of training geologists at Baylor University are to provide a sound basis of un derstanding and to foster a truly geological point of view, both of which are essential for continued professional growth. The staff considers geology to be unique among sciences since it is primarily a field science. All geologic research including that done in laboratories must be firmly supported by field observations. The student is encouraged to develop an inquiring objective attitude and to examine critically all geological concepts and principles. The development of a mature and professional attitude toward geology and geological research is a principal concern of the department. PRESS WACO, TEXAS BAYLOR GEOLOGICAL STUDIES BULLETIN NO. 4 The Member, Lake Waco Formation {Upper Central Texas - - A Lagoonal Deposit BURR A. SILVER BAYLOR UNIVERSITY Department of Geology Waco, Texas Spring, 1963 Baylor Geological Studies EDITORIAL STAFF F. Brown, Jr., Ph.D., Editor stratigraphy, paleontology O. T. Hayward, Ph.D., Adviser stratigraphy-sedimentation, structure, geophysics-petroleum, groundwater R. M. A., Business Manager archeology, geomorphology, vertebrate paleontology James W. Dixon, Jr., Ph.D. stratigraphy, paleontology, structure Walter T. Huang, Ph.D. mineralogy, petrology, metallic minerals Jean M. Spencer, B.S., Associate Editor Bulletin No. 4 The Baylor Geological Studies Bulletin is published Spring and Fall, by the Department of Geology at Baylor University. -
Mollusks from the Pepper Shale Member of the Woodbine Formation Mclennan County, Texas
Mollusks From the Pepper Shale Member of the Woodbine Formation McLennan County, Texas GEOLOGICAL SURVEY PROFESSIONAL PAPER 243-E Mollusks From the Pepper Shale Member of the Woodbine Formation McLennan County, Texas By LLOYD WILLIAM STEPHENSON SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY, 1952, PAGES 57-68 GEOLOGICAL SURVEY PROFESSIONAL PAPER 243-E Descriptions and illustrations of new species offossils of Cenomanian age UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1953 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price 25 cents (paper cover) CONTENTS Page Abstract________________________________________________________________ 57 Historical sketch__-___-_-__--__--_l________________-__-_-__---__--_-______ 57 Type section of the Pepper shale member.____________________________________ 58 Section of Pepper shale at Haunted Hill._______________-____-__-___---_------- 58 Systematic descriptions._______.._______________-_-__-_-_-____---__-_-_-_----_ 59 Pelecypoda_ ________________________________________________________ 59 Gastropoda.______-____-_-_____________--_____-___--__-___--__-______ 64 Cephalopoda-_______-_______________________-___--__---_---_-__-— 65 References......___________________________________________________________ 65 Index.__________________________________________________ 67 ILLUSTRATIONS Plate 13. Molluscan fossils, mainly from the Pepper shale__________ -
Late Cretaceous and Tertiary Burial History, Central Texas 143
A Publication of the Gulf Coast Association of Geological Societies www.gcags.org L C T B H, C T Peter R. Rose 718 Yaupon Valley Rd., Austin, Texas 78746, U.S.A. ABSTRACT In Central Texas, the Balcones Fault Zone separates the Gulf Coastal Plain from the elevated Central Texas Platform, comprising the Hill Country, Llano Uplift, and Edwards Plateau provinces to the west and north. The youngest geologic for- mations common to both regions are of Albian and Cenomanian age, the thick, widespread Edwards Limestone, and the thin overlying Georgetown, Del Rio, Buda, and Eagle Ford–Boquillas formations. Younger Cretaceous and Tertiary formations that overlie the Edwards and associated formations on and beneath the Gulf Coastal Plain have no known counterparts to the west and north of the Balcones Fault Zone, owing mostly to subaerial erosion following Oligocene and Miocene uplift during Balcones faulting, and secondarily to updip stratigraphic thinning and pinchouts during the Late Cretaceous and Tertiary. This study attempts to reconstruct the burial history of the Central Texas Platform (once entirely covered by carbonates of the thick Edwards Group and thin Buda Limestone), based mostly on indirect geological evidence: (1) Regional geologic maps showing structure, isopachs and lithofacies; (2) Regional stratigraphic analysis of the Edwards Limestone and associated formations demonstrating that the Central Texas Platform was a topographic high surrounded by gentle clinoform slopes into peripheral depositional areas; (3) Analysis and projection -
An Early Bothremydid from the Arlington Archosaur Site of Texas Brent Adrian1*, Heather F
www.nature.com/scientificreports OPEN An early bothremydid from the Arlington Archosaur Site of Texas Brent Adrian1*, Heather F. Smith1, Christopher R. Noto2 & Aryeh Grossman1 Four turtle taxa are previously documented from the Cenomanian Arlington Archosaur Site (AAS) of the Lewisville Formation (Woodbine Group) in Texas. Herein, we describe a new side-necked turtle (Pleurodira), Pleurochayah appalachius gen. et sp. nov., which is a basal member of the Bothremydidae. Pleurochayah appalachius gen. et sp. nov. shares synapomorphic characters with other bothremydids, including shared traits with Kurmademydini and Cearachelyini, but has a unique combination of skull and shell traits. The new taxon is signifcant because it is the oldest crown pleurodiran turtle from North America and Laurasia, predating bothremynines Algorachelus peregrinus and Paiutemys tibert from Europe and North America respectively. This discovery also documents the oldest evidence of dispersal of crown Pleurodira from Gondwana to Laurasia. Pleurochayah appalachius gen. et sp. nov. is compared to previously described fossil pleurodires, placed in a modifed phylogenetic analysis of pelomedusoid turtles, and discussed in the context of pleurodiran distribution in the mid-Cretaceous. Its unique combination of characters demonstrates marine adaptation and dispersal capability among basal bothremydids. Pleurodira, colloquially known as “side-necked” turtles, form one of two major clades of turtles known from the Early Cretaceous to present 1,2. Pleurodires are Gondwanan in origin, with the oldest unambiguous crown pleurodire dated to the Barremian in the Early Cretaceous2. Pleurodiran fossils typically come from relatively warm regions, and have a more limited distribution than Cryptodira (hidden-neck turtles)3–6. Living pleurodires are restricted to tropical regions once belonging to Gondwana 7,8. -
Stratigraphy of the Taylor Formation {Upper Cretaceous), East-Central Texas
Na Montmorillonite-Kaolinite Facies SPRING 1964 Bulletin No. 6 Stratigraphy of the Taylor [Upper Cretaceous), East-Central Texas ARTHUR 0. BEALL JR. thinking is more important than elaborate FRANK CARNEY, PH.D. OF GEOLOGY BAYLOR UNIVERSITY Objectives of Geological Training at Baylor The training of a geologist in a university covers but a few years; his education continues throughout his active life. The purposes of training geologists at Baylor University are to provide a sound basis of understanding and to foster a truly geological point of view, both of which are essential for continued pro fessional growth. The staff considers geology to be unique among sciences since it is primarily a field science. All geologic research in cluding that done in laboratories must be firmly supported by field observations. The student is encouraged to develop an inquiring objective attitude and to examine critically all geological concepts and principles. The development of a mature and professional attitude toward geology and geological research is a principal concern of the department. THE BAYLOR UNIVERSITY PRESS TEXAS BAYLOR GEOLOGICAL STUDIES BULLETIN NO. 6 Stratigraphy of the Taylor Formation {Upper Cretaceous), East-Central Texas ARTHUR O. JR. BAYLOR UNIVERSITY Department of Geology Waco, Texas Spring, 1964 Baylor Geological Studies EDITORIAL STAFF L. F. Brown, Jr., Ph.D., Editor stratigraphy, paleontology O. T. Hayward, Ph.D., Adviser stratigraphy-sedimentation, structure, groundwater R. L. Bronaugh, M.A., Business Manager archeology, geomorphology, vertebrate paleontology James W. Dixon, Jr., Ph.D. stratigraphy, paleontology, structure Walter T. Huang, Ph.D. mineralogy, petrology, metallic minerals lean M. Spencer, M.S., Associate Editor Moice A. -
Learning About the Earth As a System. International Conference on Geoscience Education Conference Proceedings (2Nd, Hilo, HI, July 28-31, 1997)
DOCUMENT RESUME ED 422 163 SE 061 669 AUTHOR Fortner, Rosanne W., Ed.; Mayer, Victor J., Ed. TITLE Learning about the Earth as a System. International Conference on Geoscience Education Conference Proceedings (2nd, Hilo, HI, July 28-31, 1997). INSTITUTION Ohio State Univ., Columbus. PUB DATE 1998-00-00 NOTE 190p. PUB TYPE Collected Works Proceedings (021) EDRS PRICE MF01/PC08 Plus Postage. DESCRIPTORS *Earth Science; *Educational Strategies; Elementary Secondary Education; Geology; Higher Education; Learning Strategies; Public Policy; Science and Society; *Science Curriculum; *Science Education ABSTRACT Learning about the earth as a system was the/focus of the 1997 International Conference on Geoscience Education. This proceedings contains details on the organization of the conference as well as five general sessions by various participants. The interactive poster sessions are organized according to three themes:(1) Earth Systems/Science Programs; (2) Earth Systems/Science Instruction; and (3) Public Information, Research, and Innovation. Addresses related to the conferring of four lifetime service awards are also included along with conference highlights, participants' evaluation of the conference, participant addresses, and an index to program contributors. (DDR) ******************************************************************************** * Reproductions supplied by EDRS are the best that can be made * * from the original document. * ******************************************************************************** . , arra2.m' a -
Ground-Water Resources of Navarro County, Texas
TEXAS WATER DEVELOPMENT BOARD REPORT 160 GROUND-WATER RESOURCES OF NAVARRO COUNTY, TEXAS By Gerald L. Thompson United States Geological Survey This repon was prepared by the U.S. Geological Survey under cooperative agl"eement with the Texas Water Development Board November 1972 Reprinted January 1987 TEXAS WATER DEVELOPMENT BOARD w. E. Tinsley, Chairman Marvin Shurbet, Vice Chairman Robert B. Gilmore John H. McCoy Milton T. Potts Carl Illig Harry P. Burleigh, Executive Director Authorization for use or reproduction of any original material contained in this publication, i.e., not obtained from other sources, is freely granted. The Board would appreciate acknowledgement. Published and distributed by the Texas Water Development Board Post Office Box 13087 Austin, Texas 78711 TABLE OF CONTENTS Page ABSTRACT ........•.••.•.•.••••.•....•....•.•....•.•....•.•..•.•......•......•.•. '" INTRODUCTION 3 Purpose and Scope of the Investigation __ . 3 Location and Extent of the Area ..... _.........•.•... 3 Climate , ................................................•.. 3 Physiography and Drainage ....•.•....•.•..•.•.•......•..•......•.•....•.•.•..•...... 4 Economic Development ......•.•......•..................•.............•........... 4 Previous Investigations .........•.•......•...........•......•....•......•......•.... 5 Well-Numbering System .....•..•.•. _..•.•....•.•....•..... 5 Acknowledgments . 5 GEOLOGY AS RELATED TO GROUND WATER ........•......•....................•....... 7 General Stratigraphy and Structure . 7 Physical Characteristics and -
South Texas Project Units 3 & 4 COLA
Rev. 08 STP 3 & 4 Final Safety Analysis Report 2.5S.1 Basic Geologic and Seismic Information The geological and seismological information presented in this section was developed from a review of previous reports prepared for the existing units, published geologic literature, interpretation of aerial photography, a subsurface investigation, and an aerial reconnaissance conducted for preparation of this STP 3 & 4 application. Previous site-specific reports reviewed include the STP 1 & 2 FSAR, Revision 13 (Reference 2.5S.1-7). A review of published geologic literature and seismologic data supplements and updates the existing geological and seismological information. A list of references used to compile the geological and seismological information presented in the following pages is provided at the end of Subsection 2.5S.1. It is intended in this section of the STP 3 & 4 FSAR to demonstrate compliance with the requirements of 10 CFR 100.23 (c). Presented in this section is information of the geological and seismological characteristics of the STP 3 & 4 site region, site vicinity, site area, and site. Subsection 2.5S.1.1 describes the geologic and tectonic characteristics of the site region and site vicinity. Subsection 2.5S.1.2 describes the geologic and tectonic characteristics of the STP 3 & 4 site area and site. The geological and seismological information was developed in accordance with NRC guidance documents RG-1.206 and RG-1.208. 2.5S.1.1 Regional Geology (200 mile radius) Using Texas Bureau of Economic Geology Terminology, this subsection discusses the physiography, geologic history, stratigraphy, and tectonic setting within a 200 mi radius of the STP 3 & 4 site. -
Late Albian Kiowa-Skull Creek Marine Transgression, Lower Dakota Formation, Eastern Margin of Western Interior Seaway R.L
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Papers in Natural Resources Natural Resources, School of 2000 Late Albian Kiowa-Skull Creek Marine Transgression, Lower Dakota Formation, Eastern Margin of Western Interior Seaway R.L. Brenner Iowa Department of Natural Resources G.A. Ludvigson Iowa Department of Natural Resources B.J. Witzke Iowa Department of Natural Resources A.N. Zawistoski Indiana University E.P. Kvale Indiana University See next page for additional authors Follow this and additional works at: https://digitalcommons.unl.edu/natrespapers Part of the Natural Resources and Conservation Commons, Natural Resources Management and Policy Commons, and the Other Environmental Sciences Commons Brenner, R.L.; Ludvigson, G.A.; Witzke, B.J.; Zawistoski, A.N.; Kvale, E.P.; Ravn, R.L.; and Joeckel, R.M., "Late Albian Kiowa-Skull Creek Marine Transgression, Lower Dakota Formation, Eastern Margin of Western Interior Seaway" (2000). Papers in Natural Resources. 1009. https://digitalcommons.unl.edu/natrespapers/1009 This Article is brought to you for free and open access by the Natural Resources, School of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Papers in Natural Resources by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Authors R.L. Brenner, G.A. Ludvigson, B.J. Witzke, A.N. Zawistoski, E.P. Kvale, R.L. Ravn, and R.M. Joeckel This article is available at DigitalCommons@University of Nebraska - Lincoln: https://digitalcommons.unl.edu/natrespapers/1009 LATE ALBIAN KIOWA±SKULL CREEK MARINE TRANSGRESSION, LOWER DAKOTA FORMATION, EASTERN MARGIN OF WESTERN INTERIOR SEAWAY, U.S.A. R.L. BRENNER1, G.A. -
New Species of Late Cretaceous Gypraeacea (Mollusca: Gastropoda) from California and Mississippi, and a Review of Cretaceous Gypraeaceans of North America
• \ ^rtM^T: IWO ' • - THE VELIGER © CMS, Inc., 1990 The Veliger 33(3):272-285 (July 2, 1990) New Species of Late Cretaceous Gypraeacea (Mollusca: Gastropoda) from California and Mississippi, and a Review of Cretaceous Gypraeaceans of North America by LINDSEY T. GROVES Malacology Section, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, California 90007, USA Abstract. Cypraeacean mollusks are rare in Cretaceous deposits of North America. Only 15 species are recognized, of which four are new and are described herein. Six species of Palaeocypraea s.s. have been previously described, and Palaeocypraea (P.) fontana (Anderson, 1958) from the Lower Cretaceous (uppermost Lower Albian), Budden Canyon Formation, Shasta County, California, is the earliest known cypraeacean from the Western Hemisphere. Bernaya s.s. is represented by two species and Bernaya (.Protocypraea) comprises five species. Eocypraea s.s. is represented by two species. New species described herein are as follows: Bernaya (B.) crawfordcatei from the Upper Cretaceous (Campanian/Maastrichtian), Point Loma Formation, San Diego County, California; Bernaya (Proto- cypraea) mississippiensis from the Upper Cretaceous (Campanian), Coffee Formation, Lee County, Mississippi; B. (P.) rineyi from the Upper Cretaceous (Campanian/Maastrichtian), Point Loma For- mation, San Diego County, California; and Eocypraea (E.) louellae from the Upper Cretaceous (Tu- ronian), Yolo Formation, Yolo County, California. Eocypraea (E.) louellae is the earliest known ovulid from the Western Hemisphere. INTRODUCTION Historical Review Four new species of cypraeacean gastropods, rare in Cre- The first cypraeacean species described from the Cre- taceous deposits of North America, are described from taceous of North America was Cypraea mortoni Gabb, 1860.