DOCSLIB.ORG

This Is a Digital Document from the Collections of the Wyoming Water Resources Data System (WRDS) Library

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
This Is a Digital Document from the Collections of the Wyoming Water Resources Data System (WRDS) Library This is a digital document from the collections of the Wyoming Water Resources Data System (WRDS) Library. For additional information about this document and the document conversion process, please contact WRDS at [email protected] and include the phrase “Digital Documents” in your subject heading. To view other documents please visit the WRDS Library online at: http://library.wrds.uwyo.edu Mailing Address: Water Resources Data System University of Wyoming, Dept 3943 1000 E University Avenue Laramie, WY 82071 Physical Address: Wyoming Hall, Room 249 University of Wyoming Laramie, WY 82071 Phone: (307) 766-6651 Fax: (307) 766-3785 Funding for WRDS and the creation of this electronic document was provided by the Wyoming Water Development Commission (http://wwdc.state.wy.us) VOLUME 11-A OCCURRENCE AND CHARACTERISTICS OF GROUND WATER IN THE BIGHORN BASIN, WYOMING Robert Libra, Dale Doremus , Craig Goodwin Project Manager Craig Eisen Water Resources Research Institute University of Wyoming Report to U.S. Environmental Protection Agency Contract Number G 008269-791 Project Officer Paul Osborne June, 1981 INTRODUCTION This report is the second of a series of hydrogeologic basin reports that define the occurrence and chemical quality of ground water within Wyoming. Information presented in this report has been obtained from several sources including available U.S. Geological Survey publications, the Wyoming State Engineer's Office, the Wyoming Geological Survey, and the Wyoming Oil and Gas Conservation Commission. The purpose of this report is to provide background information for implementation of the Underground Injection Control Program (UIC). The UIC program, authorized by the Safe Drinking Water Act (P.L. 93-523), is designed to improve the protection of ground-water resources from possible contamination caused by injection of waste brines, sewage, and other fluids. This report identifies the stratigraphic limits, hydraulic properties, chemical quality, and use of the major water-bearing units within the Bighorn basin, and can therefore be used to assist identification of the aquifers in need of protection. TABLE OF CONTENTS CHAPTER Page I . SUMMARY OF FINDINGS ................. I1 . GEOGRAPHIC AND GEOLOGIC SETTING ........... PHYSIOGRAPHY .................. Topography .................. Climate and Surface Drainage ......... HUMAN GEOGWHY ................. Population Distribution ........... Land Use and Ownership ............ GEOLOGY ..................... Stratigraphy and Depositional History .... Structure .................. Hydrostratigraphy .............. MAJOR GROUND-WATER USERS ............ Petroleum Industry .............. Agriculture ................. Irrigation ................ Livestock ................ Underground Drinking Water Supplies ..... Private Domestic Use ........... Public Drinking Water Supplies ...... Surface Water Use .............. IV. HYDROGEOLOGY .................... FLATHEAD AQUIFER ................ Hydrologic Properties ............ CHAPTER Page PALEOZOIC AQUIFER SYSTEM ............ Hydrologic Properties ............ Permeability. .............. Specific Capacity ............ Transmissivity. ............. Ground-Water Movement ............ UPPER PALEOZOIC AND LOWER AND MIDDLE MESOZOIC AQUIFERS. ............... Hydrologic Properties ............ Permeability. .............. Specific Capacity ............ Transmissivity. ............. Ground-Water Movement ............ UPPER CRETACEOUS-TERTIARY AQUIFER SYSTEM .... Hydrologic Properties ............ Specific Capacity ............ Ground-Water Movement ............ QUATERNARY AQUIFERS. .............. Hydrologic Properties ............ Specific Capacity ............ Transmissivities. ............ Ground-Water Movement ............ V. WATERQUALITY. ................... GENERAL WATER QUALITY. ............. Flathead Aquifer. .............. Paleozoic Aquifer System. .......... Upper Paleozoic and Lower and Middle Mesozoic Aquifers ............. Upper Cretaceous-Tertiary Aquifer System. .. Quaternary Aquifers ............. Absaroka Volcanics. ............. CHAPTER Page DRINKING WATER STANDARDS ............ Primary Standards .............. Fluoride ................. Nitrate ................. Other Primary Standards ......... Secondary Standards ............. Total Dissolved Solids .......... Sulfate ................. Chloride ................. Radionuclear Species ............. VI. REFERENCES ..................... APPENDIX A: Non-Municipal and Non-Community Public Drinking Water Supplies .......... APPENDIX B: Geologic Properties of Major Water-Bearing Strata ............... APPENDIX C: Chemical Analyses of Bighorn Basin Ground Waters Sampled by WRRI ........... APPENDIX D: Location and Numbering System ...... LIST OF FIGURES Page 11-1. Location and drainage map of the Bighorn basin . 9 11-2. Population map of the Bighorn basin. ....... 14 11-3, Stratigraphic section of the Bighorn basin .... 17 11-4. Geologic cross sections through the Bighorn basin. ...................... 11-5. Major structural features of the Bighorn basin, Wyoming. ..................... 11-6. Generalized hydrostratigraphy of the Bighorn basin, Wyoming .................. 111-1. Location of public drinking water supplies in the Bighorn basin. ................ IV-1. Potentiometric surface of the Tensleep aquifer in the Bighorn basin ............... IV-2. Generalized Upper Paleo zoic-Lower Mesozoic stratigraphy of the Bighorn basin. ........ V-1. Major ion composition of waters from the Paleozoic aquifer system, Bighorn basin, Wyoming. ..................... V-2. Major ion composition of waters from the Phosphoria Formation, Bighorn basin, Wyoming ... V-3. Major ion composition of waters from the Cloverly Formation, Bighorn basin, Wyoming .... V-4. Major ion composition of waters from the Frontier Formation, Bighorn basin, Wyoming .... V-5. Major ion composition of waters from the Upper Cretaceous-Tertiary aquifer system, Bighorn basin, Wyoming .................. V-6. Major ion composition of waters from Quaternary flood plain aquifers, Bighorn basin, Wyoming ... Figure Page v-7. Major ion composition of waters from Quaternary terrace aquifers, Bighorn basin, Wyoming ..... 95 . V-8. Location of ground-water fluoride concentrations greater than 2.0 mg/l. .............. 97 v-9. Variations in fluoride concentrat ions in Lance Formation waters, Manderson, Wyoming ....... 99 V-10. Location of ground-water nitrate concentrations inexcessof10mg/lN03-N ............ 100 vii LIST OF TABLES Table Page 11-1. Surface drainage in the Bighorn basin. ....... 11 11-2. Populations of counties and population centers in the Bighorn basin ............ 13 11-3. Land cover in the Bighorn basin. .......... 16 111-1. Summary of ground-water use, Bighorn basin, Wyoming. ...................... 27 111-2. Number of public drinking water supplies in the Bighorn basin by service category. ......... 33 111-3. Municipal ground-water supplies in the Bighorn basin. ................... 36 IV-1. Lithologic and hydrologic characteristics of rock units in the Bighorn basin, Wyoming ...... 41 IV-2. Hydrologic properties of Paleozoic aquifer system, Bighorn basin, Wyoming ........... 51 IV-3. Reported specific capacities of wells in the Paleozoic aquifer system, Bighorn basin, Wyoming . 53 IV-4. Transmissivities of members of Paleozoic aquifer system, Bighorn basin, Wyoming ........... 55 IV-5. Hydrologic properties of Upper Paleozoic and Lower and Middle Mesozoic aquifers, Bighorn basin, Wyoming ................... 61 IV-6. Reported specific capacity for wells in the Upper Paleozoic and Lower and Middle Mesozoic aquifers, Bighorn basin, Wyoming .......... 65 IV-7. Reported specific capacity of wells in the Willwood aquifer, Upper Cretaceous-Tertiary aquifer system, Bighorn basin, Wyoming ....... 69 IV-8. Reported specific capacity and estimated transmissivity for wells completed in the Quaternary aquifers, Bighorn basin, Wyoming. .... 74 Table Page V-1. Concentration ranges for sulfate, chloride, and total dissolved solids in ground waters from the Bighorn basin, Wyoming. 102 V-2. Concentrations of radionuclear species in ground waters from the Bighorn basin, Wyoming . 105 Plate 1. Structural contour map of the Bighorn basin. 2. Permitted domestic wells in the Bighorn basin. 3. Total dissolved solids map of the Paleozoic aquifer system, Bighorn basin. 4. Total dissolved solids map of the Upper Cretaceous- Tertiary aquifer system, Bighorn basin. 5. Total dissolved solids map of the Quaternary aquifers, Bighorn basin. 'plates contained in Volume 11-B. I. SUMMARY OF FINDINGS I. SUMMARY OF FINDINGS 1. Two major bedrock aquifer systems have been identified within the Bighorn basin. These are the Paleozoic and Upper Cretaceous- Tertiary aquifer systems. Additionally, several dispersed, hydro- logically isolated water-bearing units have been distinguished including the basal Cambrian sandstone, several sandstone and carbonate units within the Upper Paleozoic through Middle Mesozoic sequence, and unconsolidated deposits of Quaternary age. Aquifer recharge rates, ground-water flow paths, the extent of interformational mixing, and historic water level fluctuations are poorly known. Data concern- ing hydrologic properties are sparse, especially for pre-Tertiary strata in the central basin. 2. On the basis of available hydrologic and hydrochemical data, the Paleozoic aquifer system (Ordovician through Pennsylvanian strata) has excellent potential for producing large quantities of good quality water. The Pennsylvanian Tensleep Sandstone and Mississippian
Load more

Recommended publications
  • Morrison Formation 37 Cretaceous System 48 Cloverly Formation 48 Sykes Mountain Formation 51 Thermopolis Shale 55 Mowry Shale 56
    THE STRUCTURAL AND STRATIGRAPHIC FRAMEWORK OF THE WARM SPRINGS RANCH AREA, HOT SPRINGS COUNTY, WYOMING By CHRISTOPHER JAY CARSON Bachelor of Science Oklahoma State University 1998 Submitted to the Faculty of the Graduate College of the Oklahoma State University in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE July, 2000 THE STRUCTURAL AND STRATIGRAPHIC FRAMEWORK OF THE WARM SPRINGS RANCH AREA, HOT SPRINGS COUNTY, WYOMING Thesis Approved: Thesis Advisor ~~L. ... ~. ----'-"'-....D~e~e:.-g-e----- II ACKNOWLEDGEMENTS I wish to express appreciation to my advisor Dr. Arthur Cleaves for providing me with the opportunity to compile this thesis, and his help carrying out the fieldwork portion of the thesis. My sincere appreciation is extended to my advisory committee members: Dr. Stan Paxton, Dr. Gary Stewart, and Mr. David Schmude. I wish to thank Mr. Schmude especially for the great deal of personal effort he put forth toward the completion of this thesis. His efforts included financial, and time contributions, along with invaluable injections of enthusiasm, advice, and friendship. I extend my most sincere thank you to Dr. Burkhard Pohl, The Big Hom Basin Foundation, and the Wyoming Dinosaur Center. Without whose input and financial support this thesis would not have been possible. In conjunction I would like to thank the staff of the Wyoming Dinosaur Center for the great deal of help that I received during my stay in Thermopolis. Finally I wish to thank my friends and family. To my friends who have pursued this process before me, and with me; thank you very much.
    [Show full text]
  • Secondary Carbonate Accumulations in Soils of the Baikal Region: Formation Processes and Significance for Paleosoil Investigations
    Вестник Томского государственного университета. Биология. 2017. № 39. С. 6–28 АГРОХИМИЯ И ПОЧВОВЕДЕНИЕ УДК 631.48 (571.5) doi: 10.17223/19988591/39/1 В.А. Голубцов Институт географии им. В.Б. Сочавы СО РАН, г. Иркутск, Россия Карбонатные новообразования в почвах Байкальского региона: процессы формирования и значение для палеопочвенных исследований Работа выполнена при поддержке РФФИ (проект № 17-04-00092). На данный момент вопросы, касающиеся строения, хронологии и специфики формирования педогенных карбонатов в резкоконтинентальных областях юга Восточной Сибири, остаются практически незатронутыми. Выполнено обобщение сформировавшихся за последние годы представлений о механизмах формирования карбонатных новообразований почв, а также их связи с условиями среды и процессами почвообразования. Оценены пути поступления карбонатов и основные факторы их аккумуляции в профиле почв. Описаны особенности вещественного и изотопного состава карбонатных новообразований в почвах, формирующихся в различных климатических условиях. На основании собственных исследований приводятся данные о разнообразии карбонатных аккумуляций в почвах Байкальского региона, их вещественном составе и роли в качестве палеогеографических индикаторов. Детально рассмотрены следующие формы карбонатных новообразований: ризолиты, игольчатый кальцит, гипокутаны, белоглазка, нодули, кутаны, лессовые куколки. Ключевые слова: карбонаты; педогенные карбонатные новообразования; стабильные изотопы; почвы; палеореконструкции. Введение Первостепенное значение при изучении эволюции почв имеет
    [Show full text]
  • A New Microvertebrate Assemblage from the Mussentuchit
    A new microvertebrate assemblage from the Mussentuchit Member, Cedar Mountain Formation: insights into the paleobiodiversity and paleobiogeography of early Late Cretaceous ecosystems in western North America Haviv M. Avrahami1,2,3, Terry A. Gates1, Andrew B. Heckert3, Peter J. Makovicky4 and Lindsay E. Zanno1,2 1 Department of Biological Sciences, North Carolina State University, Raleigh, NC, USA 2 North Carolina Museum of Natural Sciences, Raleigh, NC, USA 3 Department of Geological and Environmental Sciences, Appalachian State University, Boone, NC, USA 4 Field Museum of Natural History, Chicago, IL, USA ABSTRACT The vertebrate fauna of the Late Cretaceous Mussentuchit Member of the Cedar Mountain Formation has been studied for nearly three decades, yet the fossil-rich unit continues to produce new information about life in western North America approximately 97 million years ago. Here we report on the composition of the Cliffs of Insanity (COI) microvertebrate locality, a newly sampled site containing perhaps one of the densest concentrations of microvertebrate fossils yet discovered in the Mussentuchit Member. The COI locality preserves osteichthyan, lissamphibian, testudinatan, mesoeucrocodylian, dinosaurian, metatherian, and trace fossil remains and is among the most taxonomically rich microvertebrate localities in the Mussentuchit Submitted 30 May 2018 fi fi Accepted 8 October 2018 Member. To better re ne taxonomic identi cations of isolated theropod dinosaur Published 16 November 2018 teeth, we used quantitative analyses of taxonomically comprehensive databases of Corresponding authors theropod tooth measurements, adding new data on theropod tooth morphodiversity in Haviv M. Avrahami, this poorly understood interval. We further provide the first descriptions of [email protected] tyrannosauroid premaxillary teeth and document the earliest North American record of Lindsay E.
    [Show full text]
  • Artesian Pressures and Water Quality in Paleozoic Aquifers in the Ten Sleep Area of the Bighorn Basin, North-Central Wyoming
    Artesian Pressures and Water Quality in Paleozoic Aquifers in the Ten Sleep Area of the Bighorn Basin, North-Central Wyoming By MAURICE E. COOLEY Prepared in cooperation with the WYOMING STATE ENGINEER U.S. GEOLOGICAL SURVEY WATER-SUPPLY PAPER 2289 DEPARTMENT OF THE INTERIOR DONALD PAUL MODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE: 1986 For sale by the Books and Open-File Reports Section, U.S. Geological Survey, Federal Center, Box 25425, Denver, CO 80225 Library of Congress Cataloging-in-Publication Data Cooley, M.E. (Maurice E.) Artesian pressures and water quality in Paleozoic aquifers in the Ten Sleep area of the Bighorn Basin, north-central Wyoming. (U.S. Geological Survey water-supply paper; 2289 Bibliography: p. 21 Supt. of Docs, no.: I 19.13:2289 1. Artesian basins Bighorn River Watershed (Wyo. and Mont.) 2. Artesian basins Wyoming. 3. Water quality Bighorn River Watershed (Wyo. and Mont.) 4. Water quality Wyo­ ming. 5. Geology, Stratigraphic Paleozoic. I. Wyoming. State Engineer. II. Title. III. Series. GB1199.3.W8C66 1986 551.49 85-600193 CONTENTS Abstract 1 Introduction 1 Purpose and scope 2 Previous investigations 2 Acknowledgments 3 Well-numbering system 3 Geohydrologic setting 3 Major aquifers 4 Tensleep Sandstone 4 Madison-Bighorn aquifer 4 Flathead Sandstone 4 Minor aquifers 5 Goose Egg Formation 5 Park City Formation 5 Amsden Formation 5 Confining layers 5 Geologic structures 5 Linear features 6 Ground-water hydrology 8 Recharge 8 Potentiometric surfaces and water movement 8 Hydraulic characteristics of aquifers 11 Discharge 12 Springs 12 Wells 13 Changes in artesian pressure or yield 15 Goose Egg Formation 15 Tensleep Sandstone 15 Madison-Bighorn aquifer 15 Flathead Sandstone 16 Seasonal fluctuation 16 Chemical quality of water 17 Springs, spring-sustained streams, ponds, and reservoirs 17 Wells 17 Geothermal gradient 18 Aquifers most favorable for continued development 19 Summary 20 References cited 21 Metric conversion factors 54 PLATES [Plates are in pocket] 1.
    [Show full text]
  • Stratigraphic Framework of the Cretaceous Mowry Shale, Frontier
    Chapter 15 Stratigraphic Framework of the Cretaceous Mowry Shale, Frontier Formation and Adjacent Units, Southwestern Wyoming Province, Volume Title Page Wyoming, Colorado, and Utah By Mark A. Kirschbaum and Laura N.R. Roberts Chapter 15 of Petroleum Systems and Geologic Assessment of Oil and Gas in the Southwestern Wyoming Province, Wyoming, Colorado, and Utah By USGS Southwestern Wyoming Province Assessment Team U.S. Geological Survey Digital Data Series DDS–69–D U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey Charles G. Groat, Director U.S. Geological Survey, Denver, Colorado: Version 1, 2005 For sale by U.S. Geological Survey, Information Services Box 25286, Denver Federal Center Denver, CO 80225 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. 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. Manuscript approved for publication May 10, 2005 ISBN= 0-607-99027-9 Contents Abstract ………………………………………………………………………………………
    [Show full text]
  • Montana Bureau of Mines and Geology PRELIMINARY
    Montana Bureau of Mines and Geology PRELIMINARY GEOLOGIC MAP OF PARADISE VALLEY SOUTH-CENTRAL MONTANA by David A. Lopez and Jon C. Reiten Montana Bureau of Mines and Geology Open File Report MBMG 480 2003 This report has been reviewed for conformity with Montana Bureau of Mines and Geology’s technical and editorial standards. Partial support has been provided by the STATEMAP component of the National Cooperative Geologic Mapping Program of the U.S. Geological Survey under Contract Number: 02HQAG0038. Montana 15 90 Map area 90 15 111° Bozeman Livingston 90 Map area r e 89 v i 45°30' R e n o t s w o l l e Y Emigrant Park Co. Gallatin Co. Pray Chico Miner Corwin Springs Jardine Gardiner YELLOWSTONE NATIONAL PARK 45° MT 3 0 3 6 Miles WY Location of the Paradise Valley map area. 1 CORRELATION OF MAP UNITS Qal Qdf Qrs Qc Qaf Qta Qls Holocene Qat1 Qpg Qgtc Qgoc Qgt Qat2 Qgt8 Qgo8 ? Qat Qat3 Qtr Qat4 QUATERNARY Pleistocene Qat5 Unconformity Qba Unconformity Thr Unconformity Tba Pliocene Tgr Unconformity Ts Miocene Unconformity TERTIARY Thpa Thpb Thpv Td Tdf Tqla Tgcs Tgca Eocene Tslc Tse Unconformity Tft Paleocene Unconformity Kho Kbc Kmi Kcd Unconformity Kls Unconformity Kevt Upper Cretaceous Ke CRETACEOUS Ktc Kco Kcf Kf Km Kmfr Ktf Unconformity Lower Cretaceous Kk Jm Upper Jurassic JURASSIC Je Middle Jurassic JT s R Unconformity TRc Lower Triassic TRIASSIC Unconformity Permi an PERMIAN lPq PMpa PMqa Pennsylvani an PENNSYLVANIAN lPMa Upper Miss. Unconformity MISSISSIPPIAN Mm Lower Miss. Unconformity DOs Dev.—Ord. DEV. --ORD Unconformity U & Mid.Cambrian CAMBRIAN Cs Unconformity Early Proterozoic Xmy PRECAMBRIAN Unconformity Archean Ag Anc Aqa Asg Aga As 2 DESCRIPTIONS OF MAP UNITS Qal Alluvium of modern channels and flood plains (Holocene) – Younger alluvium generally confined to the present flood plain developed along active rivers and streams.
    [Show full text]
  • From the Western of the United
    from the Western of the United GEOLOGICAL SURVEY P R® BES&lON AL PAPER 1057 Early Triassic Terebratulid Brachiopods from the Western Interior of the United States By PETER R. HOOVER GEOLOGICAL SURVEY PROFESSIONAL PAPER 1057 Description and illustration offive species of terebratulid brachiopods, and discussion of their distribution and developmental and evolutionary history UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1979 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director Library of Congress Cataloging in Publication Data Hoover, Peter R. Early Triassic Terebratulid Brachiopods from the Western Interior of the United States (Geological Survey Professional Paper 1057) Bibliography: p. 19 Includes index Supt. of Docs. No.: I 19:16:1057 1. Terebratulida, Fossil. 2. Paleontology Triassic. 3. Paleontology The West. I. Title. II. Series: United States Geological Survey Professional Paper 1057 QE797.T29H66 564'.8 77-608314 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-03182-5 CONTENTS Page Page Systematic paleontology Continued Abstract ....................... 1 Family Dielasmatidae Continued Introduction .................... 1 Subfamily Dielasmatinae. Previous work................ 1 Rhaetina Waagen ..... Present study ................ 3 Family Terebratulidae ......... 9 Acknowledgments ............ 3 Subfamily Plectoconchiinae. 9 Fossil localities cited in this report. .... 3 Vex, n. gen. ......... 9 Stratigraphic setting of the brachiopods 4 Family Cryptonellidae ......... 11 Faunal relationships. .............. 6 Subfamily Cryptacanthiinae . 11 Biostratigraphic implications........ 6 Obnixia, n. gen. ...... 11 Systematic paleontology............ 7 Family Zeilleriidae ............ 17 Family Dielasmatidae.......... 7 Periallus, n. gen. ......... 17 Subfamily Zugmayeriinae . 7 References cited. ................. 19 Portneufia, n. gen. .... 7 Index ......................... 21 ILLUSTRATIONS [Plates follow index] PLATE 1.
    [Show full text]
  • Geology and Ground-Water Resources of the Greybull River-Dry Creek Area Wyoming
    ~ ~ te ~... Geology and Ground-Water ~"' 0... P-. P. p. Resources of the Greybull !Zl"' ~ 2 e::"' River-Dry Creek Area P-. ~ !Zl"' ";;; Wyoming 'b'j,""' 0 '¢ Cl:5"' 1. ;;:: GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1596 ~ Prepared in cooperation with the Wyoming Natural Resource Board and Wyoming State Engineer, and as part of the program of the Interior Department for the develop­ ment of the Missouri River basin Wl.SCONSIN - GeOLOGICAL SURVEY Geology and Ground-Water Resources of the Greybull River-Dry Creek Area Wyoming By CHARLES ]. ROBINOVE and RUSSELL H. LANGFORD GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1596 Prepared in cooperation with the Wyoming Natural Resource Board and Wyoming State Engineer, and as part of the program of the Interior Department for the develop­ ment of the Missouri River basin UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1963 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geolo!!.lcal Survey Library cards for this publication appear after pal!.e 88 For sale by the Superintendent of Documents, U.S. Government Println!l Office Washinl!.ton 25, D.C. CONTENTS Page Abstract__________________________________________________________ 1 Introduction______________________________________________________ 2 Purpose and scope of the investigation___________________________ 2 Location and extent of the area_________________________________ 3 Previous investigations_________________________________________ 3 Acknowledgments ____________________________________________
    [Show full text]
  • Wyoming-Skye Dinosaurs
    Clark, N.D.L. and Brett-Surman, M.K. (2008) A comparison between dinosaur footprints from the Middle Jurassic of the Isle of Skye, Scotland, UK, and Shell, Wyoming, USA. Scottish Journal of Geology, 44 (2). pp. 139-150. ISSN 0036-9276 http://eprints.gla.ac.uk/4807/ Deposited on: 14 April 2009 Enlighten – Research publications by members of the University of Glasgow http://eprints.gla.ac.uk A comparison between dinosaur footprints from the Middle Jurassic of the Isle of Skye, Scotland, UK, and Shell, Wyoming, USA N. D. L. CLARK1 & M. K. BRETT-SURMAN2 1Hunterian Museum and Art Gallery, University of Glasgow, University Avenue, Glasgow, G12 8QQ, UK (e-mail: [email protected]) 2Smithsonian Institution, Department of Paleobiology, PO Box 37012, MRC 121 Washington, DC 20013-7012, USA Synopsis Measurements of Middle Jurassic tridactyl dinosaur tracks from the Bathonian, Lealt Shale, Valtos Sandstone, Duntulm and Kilmaluag formations of the Isle of Skye, UK, are compared to the same measurements taken for dinosaur footprints from the Bajocian, Gypsum Spring and the Bathonian, Sundance Formation of the Bighorn Basin, Wyoming, USA. Principal component analysis of the data suggests that the smaller footprints from the Valtos Sandstone and Kilmaluag formations are indistinguishable from the footprints of the Sundance Formation. The single footprint from the Lealt Shale Formation is similar to the larger footprints from the Valtos Sandstone Formation. The footprints from the Duntulm and Gypsum Springs formations form distinct groupings from all other footprints. Four different groupings of dinosaur footprints can be recognized from the principal component analysis that may represent at least four different types of dinosaur.
    [Show full text]
  • Paleobios 34: 1–26, April 11, 2017
    PaleoBios 34: 1–26, April 11, 2017 PaleoBios OFFICIAL PUBLICATION OF THE UNIVERSITY OF CALIFORNIA MUSEUM OF PALEONTOLOGY William A. Clemens (2017). Procerberus (Cimolestidae, Mammalia) from the Latest Cretaceous and Earliest Paleocene of the Northern Western Interior, USA. Cover photo: Left maxillary of Procerberus sp. cf. P. grandis (UCMP 137189) from the Fort Union Formation, Montana, USA in buccal (A), occlusal (B) and lingual (C) views. Photo credit: Dave Strauss. Citation: Clemens, W.A. 2017. Procerberus (Cimolestidae, Mammalia) from the Latest Cretaceous and Earliest Paleocene of the Northern Western Interior, USA. PaleoBios, 34. ucmp_paleobios_34494 PaleoBios 34: 1–26, April 11, 2017 Procerberus (Cimolestidae, Mammalia) from the Latest Cretaceous and Earliest Paleocene of the Northern Western Interior, USA WILLIAM A. CLEMENS University of California Museum of Paleontology and Department of Integrative Biology, 1101 Valley Life Sciences Building, University of California, Berkeley, CA 94720-4780 email: [email protected] Three species of the cimolestid Procerberus are currently recognized in the northern North American Western Interior in latest Cretaceous and earliest Paleocene (Puercan North American Land Mammal Age) faunas: P. formicarum, P. andesiticus, and P. g randi s . Analysis of a new topotypic sample of P. formicarum from the Bug Creek Anthills locality provides an estimate of the range of variation of its postcanine denti- tion. The three currently recognized species occur in Puercan 1 (Pu1) interval zone faunas, but two other occurrences indicate that the genus originated and initially diversified prior to the Cretaceous/Paleogene boundary. Rare occurrences at several localities and entries in faunal lists suggest even greater taxonomic diversity. Limited evidence suggests continued diversification in the later Puercan and possible survival of the genus into the Torrejonian.
    [Show full text]
  • Ainsworth House National Register Form Size
    NFS Form 10-900 (3-82) OMB No. 1024-0018 Expires 10-31-87 United States Department of the Interior National Park Service For NPS use only National Register of Historic Places received fljQ 1 5 Inventory Nomination Form date entered <^pn f \ See instructions in How to Complete National Register Forms Type all entries complete applicable sections_______________ 1. Name historic Ainsworth House and or common Greet Ranch Smithsonian Number: 48WA823 2. Location street & number Spring Creek Road not for publication city, town Big Trails vicinity of state Wyoming code 056 county Washakie code 043 3. Classification Category Ownership Status Present Use district public x occupied x agriculture __ museum x building(s) x private unoccupied commercial park structure both work in progress educational private residence site Public Acquisition Accessible entertainment religious object n/a in process x yes: restricted government scientific n/a being considered _ yes: unrestricted industrial "no transportation military other: 4. Owner of Property name Mr. and Mrs. George Greet street & number Box 3840 city, town Ten Sleep state Wyoming 5. Location of Legal Description courthouse, registry of deeds, etc. Washakie County ConrthnnsP, Hnnnt-y street & number Box 260 city, town Worland state Wyoming 6. Representation in Existing Surveys title not represented has this property been determined eligible? yes no date N/A n/a federal n/a state n/a county n/a local depository for survey records N/A city, town N/A state Wyoming^ 7. Description Condition Check one Check one excellent deteriorated unaltered x original site _JLgood ruins x altered moved date N/A fair unexposed Describe the present and original (if known) physical appearance "I kept on moving down the Big Horn and trapping as I went until I reached the junction of the Nowood...then I worked my way up the Nowood Valley..
    [Show full text]
  • South Fork and Heart Mountain Faults: Examples of Catastrophic, Gravity-Driven “Overthrusts,” Northwest Wyoming, Usa
    Proceedings of the Seventh International Conference on Creationism. Pittsburgh, PA: Creation Science Fellowship SOUTH FORK AND HEART MOUNTAIN FAULTS: EXAMPLES OF CATASTROPHIC, GRAVITY-DRIVEN “OVERTHRUSTS,” NORTHWEST WYOMING, USA Timothy L. Clarey, PhD, MS, MS, BS, 2878 Oaklawn Park, Saginaw, MI, 48603, KEYWORDS: break-away fault, denudation, detachment, gravity slide, gypsum dehydration, overthrust ABSTRACT Overthrust faults have been a source of debate and discussion in creation literature for many years. Their interpretation demands a better explanation in a Flood context. Two fault systems are examined as analogies for an “overthrust” model. The South Fork Fault System (SFFS) and the Heart Mountain Fault System (HMFS) exhibit folding and faulting consistent with thin- skinned overthrust systems. Both systems moved catastrophically under the influence of gravity. The South Fork Fault system (SFFS, southwest of Cody, Wyoming, exhibits tear faults, tight folds, a triangle zone, and flat-ramp geometries along the leading edge of the system. Transport was southeast, down a gentle slope during early to middle Eocene time (Late Flood), approximately coeval with the Heart Mountain Fault system (HMFS). The SFFS detaches in lower Jurassic strata, rich in gypsum-anhydrite, overlain by about 1250 m of Jurassic through Tertiary sedimentary and volcanic rocks. Movement between 5 km and 10 km to the southeast spread the allochthonous mass over an area exceeding 1400 km2. A break-away fault and an area of tectonic denudation mark the upper northwest part of the system. The exposed denuded surface was buried by additional Eocene-age volcanic rocks soon after slip. Catastrophic rear- loading during emplacement of HMFS may have initiated subsequent movement on the SFFS, with dehydration processes trapping water in a near frictionless anhydrite-water slurry.
    [Show full text]