40 Ar 39 Ar AGES of SELECTED Tuffs of the GREEN RIVER

Total Page:16

File Type:pdf, Size:1020Kb

40 Ar 39 Ar AGES of SELECTED Tuffs of the GREEN RIVER 40 39 Ar Ar AGES Of SELECTED TUffS Of THE GREEN RIVER FORMATION: WYOMING, COLORADO, AND UTAH A Thesis Presented in Partial fulfillment of the Requirements for the Degree Master of Science by William Arthur O'Neill, B. s. The Ohio State University 1980 Approved by De Mineralogy ACKNOWLEDGEMENTS I would like to express my sincere appreciation to all those . who contributed to this study. I owe a great debt of gratitude to my advisor, Dr. John Sutter, whose assistance, ideas and experience were essential to this study. His unselfish donation of time in the field, in the laboratory and in editing this paper is greatly appreciated. Dr. Kenneth Stanley first suggested this subject as a thesis topic. He provided valuable assistance in the field, with petro­ graphy, with stratigraphic interpretation and in editing this manu­ script. Dr. Ronald Surdam provided assistance in the field in locating outcrops in the Washakie and Bridger Basins. He also willingly provided transportation to sampling locations in Wyoming and Utah that could not be reached by automobile. Dr. William Cashion of the u.s.G.S. gave invaluable assistance in the Uinta and Piceance Creek Basins in locating tuff outcrops. He also provided several topographic maps of sampling areas. Dr. Earnest Ehlers provided assistance in taking photo­ micrographs and in editing this manuscript. Larry Snee was almost a second advisor for this study. He willingly gave advice and assistance throughout all facets of the laboratory analyses. Carl Sheliga shared the use of his automobile and provided assistance in the field area. iii The friends of Orton and the Sigma Xi Society provided financial assistance for travel expenses. Many thanks to my brother, Brian, who provided the trans­ portation from Chicago to Wyoming and back and who shared the dangers of vicious house cats, grumbling motorcycle mufflers and trout stealing sea gulls. My deepest thanks go to my wife, Nancy, whose support, patience and love made the last two years all worthwhile. iv TABLE OF CONTENTS Page ACKNOWLEDGEMENTS • • • • • • • • • • • • • • • • • • • • • • • • • ii LIST OF FIGURES •••••••••••• • • •• • • • • • • • • • vi LIST OF TABLES • • • • • • • • • • • • • • • • • • • • • • • • • • x INTRODUCTION • • • • • • • • • • • • • • • • • • • • • • • • • • • l Location • • • • • • • • • • • • • • • • • • • • • • • • • l Purpose of Study • • • • • • • • • • • • • • • • • • • • • 4 Present and Previous Research • • • • • • • • • • • • • • 5 Methods of Investigation • • • • • • • • • • • • • • • • • 6 40 39 . Ar/ Ar Dating Technique • • • • • • • • • • • • 6 Petrographic Analysis • • • • • • • • • • • • • • 8 GEOLOGIC SETTING • • • • • • • • • • • • • • • • • • • • • • • • • 10 General Setting • • • • • • • • • • • • • • • • • • • • • 10 Lake Gosiute • • • • • • • • • • • • • • • • • • • • • • • 13 Wasatch Formation • • • • • • • • • • • • • • • • 14 Green River Formation • • • • • • • • • • • • • • 15 Tipton Shale Member • • • • • • • • • • • 15 Wilkins Peak • • • • • • • • • • • • • • • 16 Laney Member • • • • • • • • • • • • • • • 18 Washakie and Bridger Formations • • • • • • • • • 20 Lake Uinta • • • • • • • • • • • • • • • • • • • • • • • • 21 Wasatch Formation • • • • • • • • • • • • • • • • 21 Green River Formation • • • • • • • • • • • • • • 22 Douglas Creek Member • • • • • • • • • • • 22 Garden Gulch Member • • • • • • • • • • • 24 v Page Parachute Creek Member • • • • • • • • • • 24 Anvil Points Member • • • • • • • • • • • 25 Uinta Formation • • • • • • • • • • • • • • • • • 27 General History • • • • • • • • • • • • • • • • • • • • • 27 Tuff Beds • • • • • • • • • • • • • • • • • • • • • • • • 32 4 39 oAr/ Ar AGES OF TUFF UNITS • • • • • • • • • • • • • • • • • • • 34 Big Island Tuff • • • • • • • • • • • • • • • • • • • • • 34 Petrography • • • • • • • • • • • • • • • • • • • 39 Age Data • • • • • • • • • • • • • • • • • • • • • 40 Wilkins Peak Tuff NLnnber Six • • • • • • • • • • • • • • • 51 Petrography • • • • • • • • • • • • • • • • • • • 51 Age Data • • • • • • • • • • • • • • • • • • • • • 54 Flaming Gorge Tuff • • • • • • • • • • • • • • • • • • • • 56 Petrography • • • • • • • • • • • • • • • • • • • 56 Age Data • • • • • • • • • • • • • • • • • • • • • 60 Sand Butte Tuff • • • • • • • • • • • • • • • • • • • • • 60 Petrography • • • • • • • • • • • • • • • • • • • 66 Age Data • • • • • • • • • • • • • • • • • • • • • 68 Robin's Egg Blue Tuff • • • • • • • • • • • • • • • • • • 71 Petrography • • • • • • • • • • • • • • • • • • • 71 Age Data • • • • • • • • • • • • • • • • • • • • • 78 Curly Tuff • • • • • • • • • • • • • • • • • • • • • • • • 80 Petrography • • • • • • • • • • • • • • • • • • • 80 Age Data • • • • • • • • • • • • • • • • • • • • • 85 Wavy Tuff • • • • • • • • • • • • • • • • • • • • • • • • 85 vi Page Petrography • • • • • • • • • • • • • • • • • • • 85 Age Data • • • • • • • • • • • • • • • • • • • • • 92 EVALATION Of AGES • • • • • • • • • • • • • • • • • • • • • • • • 101 Reliability of Tuff Ages ••••••••••••••••• 101 Use of Tuff Ages • • • • • • • • • • • • • • • • • • • • • 106 Mahogany Zone • • • • • • • • • • • • • • • • • • 106 Correlation of High Stands • • • • • • • • • • • • 108 CONCLUSION • • • • • • • ••• • • • • • • • • • • • • • • • • • • 110 Results of This Study •••••••••••••••••• 110 Dating of Tuff Beds • • • • • • • • • • • • • • • • • • • 110 Recommendations • • • • • • • • • • • • • • • • • • • • • 111 REfERENCES • • • • • • • • • • • • • • • • • • • • • • • • • • • • 112 APPENDIX I • • • • •••• • • • • • • • • • • • • • • • • • • • • 113 Analytical Methods •••••••••••••••••••• 117 APPENDIX II • • • • • • • • • • • • • • • • • • • • • • • • • • • 123 40 39 Ar/ Ar Age 0 a t a • • • • • • • • • • • • • • • • • • • • 123 Locations of Samples • • • • • • • • • • • • • • • • • • • 139 vii TABLE OF FIGURES Figura Page 1. False color composite space photograph of study area • • • • • • • • • • • • • • • • 2 2. Generalized map showing surface and subsurface occurance • • • • • • • • • • • • • • • • • • 3 3. Temperature release spectrum for a sample of the Curly Tuff • • • • • • • • • • • • • • • • 9 4. Schematic cross section of Lake Gosuite • • • • • • • • • 11 5. Schematic cross section of Lake Uinta • • • • • • • • • • 12 6. Schematic cross section of Wilkins Peak Member with lens shape zone of trona deposits ••••••••••••••••••••• 17 7. Inferred boundary of hydrographic basin of Eocene Lake, Gosuite • • • • • • • • • • • • • • • • 19 a. Schematic north-south cross section of Uinta Basin • • • • • • • • • • • • • • • • • • • • • 23 9. Generalized stratigraphy of Green River Formation in Uinta and Piceance Creek Basins • • • • • • 26 10. Correlation of Eocene Age sediments with provincial land mammal ages • • • • • • • • • • • • • • 29 11. Diagramatic cross section of playa Lake Gosuite •••••••••• • • • • • • • • • • • • 30 12. Columnar sections of Wilkins Peak and Laney Members • • • • • • • • • • • • • • • • • • • • • 35 13. Columnar sections of Wilkins Peak Member • • • • • • • • • 36 14. Photograph of outcrop of Big Island Tuff • • • • • • • • • 37 15. Location map showing position of sampling of tuffs in Green River, Wyoming Area. • • • • • • • • • 38 16. Age spectrum diagrams for Big Island Tuff • • • • • • • • 41 17. Photomicrographs from samples of Big Island Tuff • • • • • • • • • • • • • • • • • • • • • • 44 viii Figure Page 18. Photograph of outcrop for tuff number six of Wilkins Peak Member • • • • • • • • • • • • • • • . 52 Age spectrum for sample 706-7 of tuff number six • • • • • • • • • • • • • • • • • • • • • • • 20. Photomicrograph from sample 706-7 • • • • • • • • • • • • 55 21. Age spectrum diagrams of Flaming Gorge Tuff • • • • • • • • • • • • • • • • • • • • • • • 58 22. Photomicrographs from samples of Flaming Gorge Tuffs • • • • • • • • • • • • • • • • • • 61 23. Columnar section of portion of Laney Member • • • • • • • • • • • • • • • • • • • • • • • • • 63 24. Geologic map of Western half of Washakie Basin • • • • • • • • • • • • • • • • • • • • • 64 25. Photograph of outcrop of two inch thick tuff in Upper Laney Member • • • • • • • • • • • • • • • 65 26. Age spectra diagrams for sample 705-3, and 705-5 • • • • • • • • • • • • • • • • • • • • • • • 67 27. Photomicrograph of thin section from base of of sample 705-3 • • • • • • • • • • • • • • • • • • • • 69 28. Generalized stratigraphic column of Washakie Formation • • • • • • • • • • • • • • • • • • • • • • • 72 29. Geologic map of western two-thirds of Washakie Basin • • • • • • • • • • • • • • • • • • • 73 30. Disrupted age spectrum of sample 706-2 of Robin's Egg Blue Tuff • • • • • • • • • • • • • • • • 75 31. Photomicrographs from thin sections of samples of Robin's Egg Blue Tuff ••••• • • • • • • • 79 32. Outline map of Uinta Basin • • • • • • • • • • • • • • • • 81 33. Stratigraphic column of Parachute Creek Member • • • • • • • • • • • • • • • • • • • • • • 82 34. Age spectra diagrams for samples of Curly Tuff • • • • • • •• • • • • • • • • • • • • • 84 ix Figure Page 35. Photomicrograph of thin section of samples from Curly Tuff • • • • • • • • • • • • • • • 86 36. Outline map of Uinta and Piceance Creek Basins • • • • • • • • • • • • • • • • • • • • • • 90 37. Age spectra diagrams for samples of the Wavy Tuff • • • • • • • • • • • • • • • • • • • • 91 38. Photomicrographs of thin sections of samples from Wavy Tuff ••• • • • • • • • • • • • • 93 39. Generalized cross section for sediments for Eocene Lakes Uinta and Gosiute • • • • • • • • • • • 105 40. Geomagnetic polarity
Recommended publications
  • Download File
    Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Graduate School of Arts and Sciences COLUMBIA UNIVERSITY 2016 © 2015 Kaori Tsukui All rights reserved ABSTRACT Chronology and Faunal Evolution of the Middle Eocene Bridgerian North American Land Mammal “Age”: Achieving High Precision Geochronology Kaori Tsukui The age of the Bridgerian/Uintan boundary has been regarded as one of the most important outstanding problems in North American Land Mammal “Age” (NALMA) biochronology. The Bridger Basin in southwestern Wyoming preserves one of the best stratigraphic records of the faunal boundary as well as the preceding Bridgerian NALMA. In this dissertation, I first developed a chronological framework for the Eocene Bridger Formation including the age of the boundary, based on a combination of magnetostratigraphy and U-Pb ID-TIMS geochronology. Within the temporal framework, I attempted at making a regional correlation of the boundary-bearing strata within the western U.S., and also assessed the body size evolution of three representative taxa from the Bridger Basin within the context of Early Eocene Climatic Optimum. Integrating radioisotopic, magnetostratigraphic and astronomical data from the early to middle Eocene, I reviewed various calibration models for the Geological Time Scale and intercalibration of 40Ar/39Ar data among laboratories and against U-Pb data, toward the community goal of achieving a high precision and well integrated Geological Time Scale. In Chapter 2, I present a magnetostratigraphy and U-Pb zircon geochronology of the Bridger Formation from the Bridger Basin in southwestern Wyoming.
    [Show full text]
  • Exhibit Specimen List FLORIDA SUBMERGED the Cretaceous, Paleocene, and Eocene (145 to 34 Million Years Ago) PARADISE ISLAND
    Exhibit Specimen List FLORIDA SUBMERGED The Cretaceous, Paleocene, and Eocene (145 to 34 million years ago) FLORIDA FORMATIONS Avon Park Formation, Dolostone from Eocene time; Citrus County, Florida; with echinoid sand dollar fossil (Periarchus lyelli); specimen from Florida Geological Survey Avon Park Formation, Limestone from Eocene time; Citrus County, Florida; with organic layers containing seagrass remains from formation in shallow marine environment; specimen from Florida Geological Survey Ocala Limestone (Upper), Limestone from Eocene time; Jackson County, Florida; with foraminifera; specimen from Florida Geological Survey Ocala Limestone (Lower), Limestone from Eocene time; Citrus County, Florida; specimens from Tanner Collection OTHER Anhydrite, Evaporite from early Cenozoic time; Unknown location, Florida; from subsurface core, showing evaporite sequence, older than Avon Park Formation; specimen from Florida Geological Survey FOSSILS Tethyan Gastropod Fossil, (Velates floridanus); In Ocala Limestone from Eocene time; Barge Canal spoil island, Levy County, Florida; specimen from Tanner Collection Echinoid Sea Biscuit Fossils, (Eupatagus antillarum); In Ocala Limestone from Eocene time; Barge Canal spoil island, Levy County, Florida; specimens from Tanner Collection Echinoid Sea Biscuit Fossils, (Eupatagus antillarum); In Ocala Limestone from Eocene time; Mouth of Withlacoochee River, Levy County, Florida; specimens from John Sacha Collection PARADISE ISLAND The Oligocene (34 to 23 million years ago) FLORIDA FORMATIONS Suwannee
    [Show full text]
  • Basin-Margin Depositional Environments of the Fort Union and Wasatch Formations in the Buffalo-Lake De Smet Area, Johnson County, Wyoming
    U.S. DEPARTMENT OF INTERIOR GEOLOGICAL SURVEY Basin-Margin Depositional Environments of the Fort Union and Wasatch Formations in the Buffalo-Lake De Smet area, Johnson County, Wyoming By Stanley L. Obernyer Open-File Report 79-712 1979 Contents Page Abstract 1 Introduction 5 Methods of investigation 8 Previ ous work - 9 General geol ogy 10 Acknowledgments 16 Descriptive stratigraphy of the Fort Union and Wasatch Formations 18 Fort Union Formation- 18 Lower member 20 Conglomerate member 21 Wasatch Formation 30 Kingsbury Conglomerate Member 32 Moncrief Member 38 Coal-bearing strata Wasatch Formation 45 Conglomeratic sandstone sequence 46 The Lake De Smet coal bed 53 Very fine to medium-grained sandstone sequence 69 Fossil marker beds 78 Environments of Deposition 79 General 79 Alluvial fan environment 82 Braided stream environments 86 Alluvial valley environments 89 Tectonics and Sedimentation 92 Conglomerates and tectonics- 92 Coals and tectonics 98 Conclusions 108 References 111 11 ILLUSTRATIONS Plates Plate 1. Bedrock geologic map of the Buffalo-Lake De Smet area, Johnson County, Wyoming In pocket 2. Geologic cross sections along the Bighorn Mountain Front, Buffalo-Lake De Smet area, Johnson County, Wyoming In pocket FIGURES Page Figure 1. Location map sh wing the major structural units surround­ ing the Powder River Basin, Wyoming and Montana 7 2. Composite geologic section of the rocks exposed in in the Buffalo-Lake De Smet area- 11 3. Generalized geologic map of the Powder River Basin 12 4. Isopach map of the Fort Union and Wasatch Formations, Powder River Basin, from Curry (1971) 14 5. Generalized stratigraphic column of the conglomerate sequences 19 6.
    [Show full text]
  • Geological Survey of Wyoming
    GEOLOGICAL SURVEY OF WYOMING SELECTED REFERENCES USED TO CO~IPILE THE ~IETALLIC AND INDUSTRIAL MI ERALS ~IAP OF WYOMING by Ray E. Harris and W. Dan Hausel OPEN FILE REPORT 85-1 1985 This report has no~ been reviewed for conformity with the editorial standards of the Geological Survey of Wyoming. CONTENTS District or Region Page Introduction . iii Absaroka Mountains ...........................•.......................... 1 Aladdin District . 1 Barlow Canyon District . 1 Bear Lodge District . 1 Big Creek District . 2 Bighorn Basin . 2 Bighorn Mountains ...•................................................... 3 Black Hills . 4 Carlile District ...........•............................................ 5 Centennial Ridge District . 5 Clay Spur District ...................................•.................. 5 Colony District . 6 Cooke City - New World District . 6 Copper Mountain District .........................................•...... 7 Cooper Hill District . 7 Crooks Gap-Green Mountain District . 7 Deer Creek District . 8 Denver Basin . 8 Elkhorn Creek District . 8 Esterbrook District . 8 Gas Hills District . 8 Gold Hill District . 9 Grand Encampment District . 9 Granite Mountains . 9 Green River Basin ................................•...................... 10 Gras Ventre Mountains ..................•...............•................ 11 Hanna Basin . 11 Hartville Uplift . 12 Hulett Creek District .........................................•......... 13 Iron Mountain District . 13 Iron Mountain Kimberlite District ......•...............................
    [Show full text]
  • Related Magmatism in the Upper Wind River Basin, Wyoming (USA), GEOSPHERE; V
    Research Paper THEMED ISSUE: Cenozoic Tectonics, Magmatism, and Stratigraphy of the Snake River Plain–Yellowstone Region and Adjacent Areas GEOSPHERE The leading wisps of Yellowstone: Post–ca. 5 Ma extension- related magmatism in the upper Wind River Basin, Wyoming (USA), GEOSPHERE; v. 14, no. 1 associated with the Yellowstone hotspot tectonic parabola doi:10.1130/GES01553.1 Matthew E. Brueseke1, Anna C. Downey1, Zachary C. Dodd1, William K. Hart2, Dave C. Adams3, and Jeff A. Benowitz4 12 figures; 2 tables; 1 supplemental file 1Department of Geology, Kansas State University, 108 Thompson Hall, Manhattan, Kansas 66506, USA 2Department of Geology and Environmental Earth Science, Miami University, 118C Shideler Hall, Oxford, Ohio 45056, USA 3Box 155, Teton Village, Wyoming 83025, USA CORRESPONDENCE: brueseke@ ksu .edu 4Geophysical Institute and Geochronology Laboratory, University of Alaska Fairbanks, Fairbanks, Alaska 99775, USA CITATION: Brueseke, M.E., Downey, A.C., Dodd, Z.C., Hart, W.K., Adams, D.C., and Benowitz, J.A., 2018, The leading wisps of Yellowstone: Post–ca. 5 Ma ABSTRACT the issue of linking volcanic events to a specific driving mechanism (Fouch, extension-related magmatism in the upper Wind River 2012; Kuehn et al., 2015). Complicating matters, magmatism often continues Basin, Wyoming (USA), associated with the Yellow- The upper Wind River Basin in northwest Wyoming (USA) is located ~80– long after (e.g., millions of years) the upper plate has been translated away stone hotspot tectonic parabola: Geosphere, v. 14, no. 1, p. 74–94, doi:10.1130/GES01553.1. 100 km southeast of the Yellowstone Plateau volcanic field. While the upper from an upwelling plume (Bercovici and Mahoney, 1994; Sleep, 2003; Shervais Wind River Basin is a manifestation of primarily Cretaceous to Eocene Lara- and Hanan, 2008; Jean et al., 2014).
    [Show full text]
  • Threatened, Endangered, Candidate & Proposed Plant Species of Utah
    TECHNICAL NOTE USDA - Natural Resources Conservation Service Boise, Idaho and Salt Lake City, Utah TN PLANT MATERIALS NO. 52 MARCH 2011 THREATENED, ENDANGERED, CANDIDATE & PROPOSED PLANT SPECIES OF UTAH Derek Tilley, Agronomist, NRCS, Aberdeen, Idaho Loren St. John, PMC Team Leader, NRCS, Aberdeen, Idaho Dan Ogle, Plant Materials Specialist, NRCS, Boise, Idaho Casey Burns, State Biologist, NRCS, Salt Lake City, Utah Last Chance Townsendia (Townsendia aprica). Photo by Megan Robinson. This technical note identifies the current threatened, endangered, candidate and proposed plant species listed by the U.S.D.I. Fish and Wildlife Service (USDI FWS) in Utah. Review your county list of threatened and endangered species and the Utah Division of Wildlife Resources Conservation Data Center (CDC) GIS T&E database to see if any of these species have been identified in your area of work. Additional information on these listed species can be found on the USDI FWS web site under “endangered species”. Consideration of these species during the planning process and determination of potential impacts related to scheduled work will help in the conservation of these rare plants. Contact your Plant Material Specialist, Plant Materials Center, State Biologist and Area Biologist for additional guidance on identification of these plants and NRCS responsibilities related to the Endangered Species Act. 2 Table of Contents Map of Utah Threatened, Endangered and Candidate Plant Species 4 Threatened & Endangered Species Profiles Arctomecon humilis Dwarf Bear-poppy ARHU3 6 Asclepias welshii Welsh’s Milkweed ASWE3 8 Astragalus ampullarioides Shivwits Milkvetch ASAM14 10 Astragalus desereticus Deseret Milkvetch ASDE2 12 Astragalus holmgreniorum Holmgren Milkvetch ASHO5 14 Astragalus limnocharis var.
    [Show full text]
  • Revision of the Lower Part of the Tertiary System in the Central and \Vestern Uinta Basin, Utah______
    Revision of the Lower Part of the Tertiary System in the Central and \Vestern Uinta Basin, Utah_____ __________ GEOLOGICAL SURVEY BULLETIN 1405G Revision of the Lower Part of the Tertiary System in the Central and \Vfestern Uinta Basin, Utah By THOMAS D. FOUCH CONTRIBUTIONS TO STRATIGRAPHY GEOLOGICAL SURVEY BULLETIN 1405-C Correlation of lower Tertiary stratigraphic units recently penetrated in northeastern Utah UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1976 UNITED STATES DEPARTMENT OF THE INTERIOR THOMAS S. KLEPPE, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Fouch, Thomas D. Revision of the lower part of the Tertiary system in the central and western Uinta Basin, Utah. (Contributions to stratigraphy) (Geological Survey Bulletin 1405-C) Bibliography: p. Supt. of Docs, no.: I 19.3:1405-C 1. Geology, Stratigraphic Tertiary. 2. Geology, Stratigraphic Nomenclature Utah Uinta Basin. I. Title. II. Series. III. Series: United States Geological Survey Bulletin 1405-C. QE75.B9 No. 1405-C [QE691] 557.3'08s [ 551.7'8'0979221] 75-619374 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D. C. 20402 Stock Number 024-001-02770-4 CONTENTS Page Abstract....................................................................................................................... Cl Introduction................................................................................................................ 1 North Horn Formation .............................................................................................
    [Show full text]
  • Uppermost Cretaceous and Tertiary Stratigraphy of Fossil Basin, Southwestern Wyoming
    Uppermost Cretaceous and Tertiary Stratigraphy of Fossil Basin, Southwestern Wyoming By STEVEN S. ORIEL and JOSHUA I. TRACEY, JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 635 New subdivisions of the J,ooo-Joot-thick continental Evanston, Wasatch, Green River, and Fowkes Formations facilitate understanding of sediment genesis and Jl7yoming thrust-belt tectonic events UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1970 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. 70-604646 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 65 cents (paper cover) CONTENTS Page Wasatch Formation-Continued Abstract __________________________________________ _ 1 Fossils and age-Continued· Page Introduction ______________________________________ _ 2 Tunp Member______________________________ 28 Purpose ______________________________________ _ 2 Origin--------~-------------------------------- 28 Earlier work_ .. __ - __ - ___________________ - _-- _- __ 2 Tectonic implications ____________ -_-------------- 29 Acknowledgments __ . ___________________________ _ 2 Green River Formation ___ .. _______ ------------------ 30 General relations ___ -- _________________________ _ 5 Name and usage __________________ -------------- 30 Evanston Formation _______________________________ _ 5 Definition __________________ -_-------------- 30 N arne and usage _______________________________ _ 5 Lithologic heterogeneity.
    [Show full text]
  • Brighan Young University Geology Studies
    BRIGHAM GEOLOGY YOUNG STUDIES UNIVERSITY Volume 19: Part 1 - December 1972 CONTENTS An Ealy Cembrian Trilobite Faunule from Utah .................... .... ......................... R. A. Robism and L. F. Hintze 3 Cbeirscystelld antiqm gn. d sp. nev. from the Lower Ordovician of Western Utah, and Its Bearing en the Evsluti~nof the Cheirocrinidae (Rhombifera: Glyptocystitida) ................... ...... ......................... C. R. C. Paul 15 Gc~lta~of the Mill Fork Area, Utah ................................ W. C. Metrill 65 Geology ef the Thistle Quadrangle, Utah ........................ M. L. Pinnell 89 Study of Internal Structures of Fine-Grained Clastic Rocks by X-radiography ........................................... A. M. Jones 131 Publications and Maps of the Geology Department ............................. 159 Brigham Young University Geology Studies Volume 19, Part 1 - December, 1972 Contents An Early Cambrian Trilobite Faunule from Utah ........................................................ R. A. Robison and L. F. Hintze 3 Cheit.orystella a~ztiua gen. et sp. nov. from the Lower Ordovician o Y Western Utah, and Its Bearing on the Evolution of the Cheirocrinidae (Rhombifera: Glyptocystitida) ........................................................ C. R. C. Paul 15 Geology of the Mill Fork Area, Utah ................................ R. C. Merrill 65 Geology of the Thistle Quadrangle, Utah .......................... M. L. Pinnell 89 Study of Internal Structures of Fine-Grained Clastic Rocks by X-radiography ...........................................
    [Show full text]
  • EPA's Fish and Shellfish Program Newsletter
    Fish and Shellfish Program NEWSLETTER March 2018 This issue of the Fish and Shellfish Program Newsletter generally focuses on the Pacific EPA 823-N-18-003 Northwest. In This Issue Recent Advisory News Recent Advisory News ............... 1 Liberty Bay Commercial Shellfish Beds Open EPA News ................................. 2 for First Time in Decades Other News .............................. 4 On September 14, 2017, improved water quality prompted Washington health officials to Recently Awarded Research .... 13 open 760 acres of commercial shellfish beds in Liberty Bay near Poulsbo in Kitsap County. Recent Publications ............... 15 In an effort to address water quality issues that have plagued Liberty Bay for decades, Upcoming Meetings Kitsap County officials teamed up with stakeholders to apply progressive pollution and Conferences .................... 17 identification and correction strategies. The result is improved marine water quality that meets the strict standards for harvesting shellfish. Clean Water Kitsap (a partnership of Kitsap County, the Kitsap Public Health District, the Kitsap County Conservation District, and the Washington State University Extension), the Suquamish Tribe, the City of Poulsbo, and hundreds of property owners began working toward the collective goal of improving water quality over a decade ago. Determining the sources of pollution led to individual on-site sewage system repairs, the implementation of manure management practices, and improvements to Poulsbo’s wastewater collection system. While the water quality has improved, federal rules require harvest area closure from May This newsletter provides information through September each year due to the large number of boats in the bay. only. This newsletter does not impose legally binding requirements on the U.S.
    [Show full text]
  • Stratigraphic Correlation Chart for Western Colorado and Northwestern New Mexico
    New Mexico Geological Society Guidebook, 32nd Field Conference, Western Slope Colorado, 1981 75 STRATIGRAPHIC CORRELATION CHART FOR WESTERN COLORADO AND NORTHWESTERN NEW MEXICO M. E. MacLACHLAN U.S. Geological Survey Denver, Colorado 80225 INTRODUCTION De Chelly Sandstone (or De Chelly Sandstone Member of the The stratigraphic nomenclature applied in various parts of west- Cutler Formation) of the west side of the basin is thought to ern Colorado, northwestern New Mexico, and a small part of east- correlate with the Glorieta Sandstone of the south side of the central Utah is summarized in the accompanying chart (fig. 1). The basin. locations of the areas, indicated by letters, are shown on the index map (fig. 2). Sources of information used in compiling the chart are Cols. B.-C. shown by numbers in brackets beneath the headings for the col- Age determinations on the Hinsdale Formation in parts of the umns. The numbers are keyed to references in an accompanying volcanic field range from 4.7 to 23.4 m.y. on basalts and 4.8 to list. Ages where known are shown by numbers in parentheses in 22.4 m.y. on rhyolites (Lipman, 1975, p. 6, p. 90-100). millions of years after the rock name or in parentheses on the line The early intermediate-composition volcanics and related rocks separating two chronostratigraphic units. include several named units of limited areal extent, but of simi- No Quaternary rocks nor small igneous bodies, such as dikes, lar age and petrology—the West Elk Breccia at Powderhorn; the have been included on this chart.
    [Show full text]
  • Introduction to Greater Green River Basin Geology, Physiography, and History of Investigations
    Introduction to Greater Green River Basin Geology, Physiography, and History of Investigations U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1506-A Introduction to Greater Green River Basin Geology, Physiography, and History of Investigations By HENRY W. ROEHLER GEOLOGY OF THE EOCENE WASATCH, GREEN RIVER, AND BRIDGER (WASHAKIE) FORMATIONS, GREATER GREEN RIVER BASIN, WYOMING, UTAH, AND COLORADO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1506-A UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1992 U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director 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 Roehler, Henry W. Introduction to greater Green River basin geology, physiography, and history of investigations / by Henry W. Roehler. p. cm. (Geology of the Eocene Wasatch, Green River, and Bridger (Washakie) formations, greater Green River basin, Wyoming, Utah, and Colorado) (U.S. Geological Survey professional paper ; 1506-A) Includes bibliographical references (p. ). Supt. of Docs, no.: I 19.16:1506A 1. Geology, Stratigraphic Eocene. 2. Geology Green River Watershed (Wyo.-Utah). I. Title. II. Series. III. Series: U.S. Geological Survey professional paper ; 1506-A. QE692.2.R625 1992 551.7'84'097925 dc20 91-23181 CIP For sale by Book and Open-File Report Sales, U.S. Geological Survey, Federal Center, Box 25286, Denver, CO 80225 CONTENTS Page Abstract ........................................................................................................................................ Al Purpose and scope of investigation ............................................................................................ 1 Location and accessibility of the greater Green River basin ................................................... 2 Geologic setting ...........................................................................................................................
    [Show full text]