Uranium Provinces of North America— Their Definition, Distribution, and Models by Warren I

Total Page:16

File Type:pdf, Size:1020Kb

Uranium Provinces of North America— Their Definition, Distribution, and Models by Warren I Uranium Provinces of North America— Their Definition, Distribution, and Models By Warren I. Finch U.S. GEOLOGICAL SURVEY BULLETIN 2141 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1996 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, 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 Finch, Warren Irvin, 1924– Uranium provinces of North America : their definition, distribution, and models / by Warren I. Finch. p. cm. — (U.S. Geological Survey bulletin ; 2141) Includes bibliographical references. Supt. of Docs. no.: I 19.3:2141 1. Uranium ores—North America. I. Title. II. Series. QE75.B9 no. 2141 [QE390.2.U7] 557.3 s—dc20 [551.4′932′097] 95-37553 CIP CONTENTS Abstract ........................................................................................................................... 1 Introduction..................................................................................................................... 1 Methods of Study .................................................................................................... 2 Acknowledgments................................................................................................... 2 Brief Review of Concepts of Metallogenic and Mineral Provinces ............................... 2 Definition of a Uranium Province................................................................................... 3 Description of Uranium Province Model........................................................................ 3 Definitions and Models of North American Uranium Provinces ................................... 4 Athabasca Basin Uranium Province, Canada ......................................................... 4 Definition ........................................................................................................ 4 The Model ....................................................................................................... 4 Blind River–Elliot Lake Uranium Province, Canada.............................................. 5 Definition ........................................................................................................ 5 The Model ....................................................................................................... 5 Colorado Plateau Uranium Province, United States ............................................... 6 Definition ........................................................................................................ 6 The Model ....................................................................................................... 7 Rocky Mountain and Intermontane Basins Uranium Province, United States ....... 7 Definition ........................................................................................................ 7 The Model ....................................................................................................... 8 Gulf Coast Uranium Province, United States and Mexico ..................................... 8 Definition ........................................................................................................ 8 The Model ....................................................................................................... 9 Basin and Range Uranium Province, United States and Mexico............................ 10 Definition ........................................................................................................ 10 The Model ....................................................................................................... 10 Florida Phosphorite Uranium Province, United States, by Warren I. Finch and James B. Cathcart.................................................................................................. 11 Definition ........................................................................................................ 11 The Model ....................................................................................................... 11 Distribution of Uranium in North America..................................................................... 12 Tectonostratigraphic and Plate Tectonic Perspective of the Distribution of North American Uranium Provinces........................................................................... 13 References Cited ............................................................................................................. 15 PLATES 1. Map showing locations of uranium provinces and the major uranium clusters in North America. 2. Map showing details of the Colorado Plateau, Rocky Mountain and Intermontane Basins, and Basin and Range Uranium Provinces. III IV CONTENTS FIGURES 1–3. Maps showing: 1. Details of the Athabasca Basin Uranium Province, Canada ..................................................................................... 5 2. Details of the Blind River–Elliot Lake Uranium Province, Canada ......................................................................... 6 3. Details of the Gulf Coast Uranium Province, United States and Mexico ................................................................. 9 4. Graph showing distribution of uranium in North America....................................................................................... 12 TABLE 1. Distribution of uranium in North America...................................................................................................................... 13 URANIUM PROVINCES OF NORTH AMERICA— THEIR DEFINITION, DISTRIBUTION, AND MODELS By Warren I. Finch ABSTRACT ≈1,280–≈1,000, ≈575, and ≈225 Ma. Subsequently in North America, only minor uranium mineralization occurred until after continental collision in Permian time (255 Ma). Three Uranium resources in North America are principally in principal epochs of uranium mineralization occurred in the unconformity-related, quartz-pebble conglomerate, sand- CPUP: (1) ≈ 210–200 Ma, shortly after Late Triassic sedi- stone, volcanic, and phosphorite types of uranium deposits. mentation; (2) ≈ 155–150 Ma, in Late Jurassic time; and (3) Most are concentrated in separate, well-defined metallo- ≈ 135 Ma, after sedimentation of the Upper Jurassic Morri- genic provinces. Proterozoic quartz-pebble conglomerate son Formation. The most likely source of the uranium was and unconformity-related deposits are, respectively, in the silicic volcaniclastics for the three epochs derived from a Blind River–Elliot Lake (BRELUP) and the Athabasca volcanic island arc at the west edge of the North American Basin (ABUP) Uranium Provinces in Canada. Sandstone continent. Uranium mineralization occurred during Eocene, uranium deposits are of two principal subtypes, tabular and Miocene, and Pliocene times in the RMIBUP, GCUP, and roll-front. Tabular sandstone uranium deposits are mainly in BRUP. Volcanic activity took place near the west edge of the upper Paleozoic and Mesozoic rocks in the Colorado Plateau continent during and shortly after sedimentation of the host Uranium Province (CPUP). Roll-front sandstone uranium rocks in these three provinces. Some volcanic centers in the deposits are in Tertiary rocks of the Rocky Mountain and Sierra de Peña Blanca district within the BRUP may have Intermontane Basins Uranium Province (RMIBUP), and in a provided uranium-rich ash to host rocks in the GCUP. narrow belt of Tertiary rocks that form the Gulf Coastal Ura- Most of the uranium provinces in North America nium Province (GCUP) in south Texas and adjacent Mexico. appear to have a common theme of close associations to vol- Volcanic uranium deposits are concentrated in the Basin and canic activity related to the development of the western mar- Range Uranium Province (BRUP) stretching from the gin of the North American plate. The south and west margin McDermitt caldera at the Oregon-Nevada border through the of the Canadian Shield formed the leading edge of the Marysvale district of Utah and Date Creek Basin in Arizona progress of uranium source development and mineralization and south into the Sierra de Peña Blanca District, Chihuahua, from the Proterozoic to the present. The development of Mexico. Uraniferous phosphorite occurs in Tertiary sedi- favorable hosts and sources of uranium is related to various ments in Florida, Georgia, and North and South Carolina and tectonic elements developed over time. Periods of major in the Lower Permian Phosphoria Formation in Idaho and uranium mineralization in North America were Early Prot- adjacent States, but only in Florida has economic recovery erozoic, Middle Proterozoic, Late Triassic–Early Jurassic, been successful. The Florida Phosphorite Uranium Province Early Cretaceous, Oligocene, and Miocene. Tertiary miner- (FPUP) has yielded large quantities of uranium as a byprod- alization was the most pervasive, covering most of Western uct of the production of phosphoric acid fertilizer. Econom- and Southern North America. ically recoverable quantities of copper, gold, molybdenum, nickel, silver, thorium, and vanadium occur with the ura- nium deposits in some provinces. INTRODUCTION Many major epochs of uranium mineralization occurred in North America. In the BRELUP, uranium minerals were The uranium provinces of North America have been concentrated in placers during the Early
Recommended publications
  • Geologic Resource Evaluation Report, Capitol Reef National Park
    National Park Service U.S. Department of the Interior Natural Resource Program Center Capitol Reef National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2006/005 Capitol Reef National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2006/005 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 September 2006 U.S. Department of the Interior Washington, D.C. The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the NPS conservation and environmental constituencies. Manuscripts are peer-reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and is designed and published in a professional manner. Natural Resource Reports are the designated medium for disseminating high priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. Examples of the diverse array of reports published in this series include vital signs monitoring plans; "how to" resource management papers; proceedings of resource management workshops or conferences; annual reports of resource programs or divisions of the Natural Resource Program Center; resource action plans; fact sheets; and regularly-published newsletters. Views and conclusions in this report are those of the authors and do not necessarily reflect policies of the National Park Service. Mention of trade names or commercial products does not constitute endorsement or recommendation for use by the National Park Service.
    [Show full text]
  • The Great Plains As a Natural Region: the Basics
    Proceedings of the South Dakota Academy of Science,Vol. 80 (2001) 259 THE GREAT PLAINS AS A NATURAL REGION: THE BASICS Richard A. Peterson Wewela, SD 57578 ABSTRACT The need for this paper became apparent during a review of articles in the Prairie Naturalist(1986-1995), where the term, Great Plains, was used to de- scribe many different areas/regions, most of which were outside of established natural boundaries. The Rocky Mountains have long been the agreed upon western boundary of the Great Plains and the primary factor in the develop- ment of the Great Plains; indeed, without the uplift of the Rocky Mountains there would not be a Great Plains region. Consistent natural boundaries for the Great Plains, were in general use after 1931, when Nevin M. Fenneman de- scribed the region in Physiography of the Western United States, and reaffirmed the eastern boundary as originally fixed by John Wesley Powell in 1895. Typ- ical Great Plains landforms (plains and buttes) have resulted from the moun- tain uplift and subsequent sediment deposits that increased the elevation of the Great Plains relative to the Central Lowlands. The Great Plains, in the rain shadow of the Rocky Mountains, have been characterized by a dry subhumid to semiarid climate. The potential natural vegetation of the Great Plains has been, since the last retreat of the continental glaciers 8,000-10,000 years ago, grass/forb vegetation - mostly a mix of mid and short grasses. True Prairie has been limited to the moist side of the dry/moist boundary. These differences between the grasslands of the Great Plains and the grasslands of the Central Lowlands have resulted in differences in occurrence and abundance of grass- land animal species, such as black-tailed prairie dog, black-footed ferret, swift fox, pronghorn, ferruginous hawk, prairie falcon and lark bunting.
    [Show full text]
  • OVERVIEW Tectonics of the Himalaya and Southern Tibet from Two Perspectives
    OVERVIEW Tectonics of the Himalaya and southern Tibet from two perspectives K. V. Hodges Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139 ABSTRACT café or on the banks of a quiet pond, Impressionist art preserves an instan- taneous sensation. Claude Monet, perhaps the greatest of the Impressionists, The Himalaya and Tibet provide an unparalleled opportunity to ex- tried to go further by expressing the passage of time in his series paintings, amine the complex ways in which continents respond to collisional like those of the façade of the Rouen Cathedral. If Impressionism is a form orogenesis. This paper is an attempt to synthesize the known geology of of historical documentation, we might think of one of the great traditions of this orogenic system, with special attention paid to the tectonic evolu- tectonics research—the description of orogeny as a temporal progression of tion of the Himalaya and southernmost Tibet since India-Eurasia colli- deformational episodes—as an essentially Impressionist enterprise. Our sion at ca. 50 Ma. Two alternative perspectives are developed. The first ability to use the developmental sequence of major structures in one setting is largely historical. It includes brief (and necessarily subjective) re- to predict the sequence in others, as is the case for foreland fold-and-thrust views of the tectonic stratigraphy, the structural geology, and meta- belts worldwide (Dahlstrom, 1970), is ample testimony to the value of the morphic geology of the Himalaya. The second focuses on the processes Impressionist perspective. that dictate the behavior of the orogenic system today.
    [Show full text]
  • Plateau Uplift: Mode and Mechanism
    Papers Presented to the CONFERENCE ON PLATEAU UPLIFT: MODE AND MECHANISM Flagstaff, Arizona 14-16 August 1978 (NASA-CE-157468) PAPERS PRESENTED TO THE N178-29663 CONFERENCE ON PT.RTEAU UP1IFT: ODE AND MECHANISM (lunar and Planetary Inst) 92 p HC A05/MF A01 CSCL 08G nclas G3/46 27138 A LUNAR AND PLANETARY INSTITUTE TOPICAL CONFERENCE Co-Sponsored' by the International Committee on Geodynamics. A Working Group 7 p~uPU 178 Hodted by the 'RECEIVEO U.S. Geological Survey, Geologic Division 1 1 Branch of Astrogeologic Studies Universities Space Research Association The Lunar and Planetary Institute 3303 NASA Road 1 Houston, Texas 77058 PAPERS PRESENTED TO THE CONFERENCE ON PLATEAU UPLIFT: MODE AND MECHANISM A LUNAR AND PLANETARY INSTITUTE TOPICAL CONFERENCE Co-Sponsored by the INTERNATIONAL COMMITTEE ON GEODYNAMICS, WORKING GROUP 7 Hosted by the U.S. GEOLOGICAL SURVEY, GEOLOGIC DIVISION BRANCH OF ASTROGEOLOGIC STUDIES Flagstaff, Arizona 14-16 August 1978 Compiled by the Lunar and Planetary Institute 3303 NASA Road One Houston, Texas 77058 LPI Contribution 329 PREFACE This volume contains papers which have been accepted for publication by the Program Committee of the Conference on Plateau Uplifts* Mode and Mechanism. The Program Committee consists of K. Burke (State Universtty of New York), G. Eaton (U.S. Geological Survey), E. A. Flinn (NASA Headquarters), P. P. Jones (Lunar and Planetary Institute), I. Lucchitta (U.S. Geological Survey), T. R. McGetchin, Chairman (Lunar and Planetary Instttute), R. B. Merrill (Lunar and Planetary Institute), E. M. Shoemaker (Californta Instttute of Technology), L. T. Silver (CaZifornia Institute of Technology), G A.
    [Show full text]
  • VC Summer Nuclear Station Units 2 & 3 COLA
    V. C. Summer Nuclear Station, Units 2 and 3 COL Application Part 2, FSAR SUBSECTION 2.5.1 BASIC GEOLOGIC AND SEISMIC INFORMATION TABLE OF CONTENTS Section Title Page 2.5.1 BASIC GEOLOGIC AND SEISMIC INFORMATION .................... 2.5.1-1 2.5.1.1 Regional Geology ....................................................................... 2.5.1-1 2.5.1.1.1 Regional Physiography, Geomorphology, and Stratigraphy.............................................................................. 2.5.1-1 2.5.1.1.1.1 The Appalachian Plateau Physiographic Province ............... 2.5.1-2 2.5.1.1.1.2 The Valley and Ridge Physiographic Province..................... 2.5.1-3 2.5.1.1.1.3 The Blue Ridge Physiographic Province .............................. 2.5.1-3 2.5.1.1.1.4 The Piedmont Physiographic Province................................. 2.5.1-4 2.5.1.1.1.5 The Atlantic Coastal Plain Physiographic Province .............. 2.5.1-8 2.5.1.1.1.6 Mesozoic Rift Basins ............................................................ 2.5.1-8 2.5.1.1.2 Regional Tectonic Setting ........................................................ 2.5.1-9 2.5.1.1.2.1 Regional Geologic History .................................................... 2.5.1-9 2.5.1.1.2.2 Tectonic Stress in the Mid-Continent Region ..................... 2.5.1-12 2.5.1.1.2.3 Gravity and Magnetic Data of the Site Region and Site Vicinity .................................................................. 2.5.1-14 2.5.1.1.2.3.1 Regional Gravity Data............................................. 2.5.1-15 2.5.1.1.2.3.2 Regional Magnetic Data.......................................... 2.5.1-17 2.5.1.1.2.4 Principal Regional Tectonic Structures............................... 2.5.1-19 2.5.1.1.2.4.1 Regional Paleozoic Tectonic Structures ................
    [Show full text]
  • Geologic Resource Evaluation Report, Zion National Park
    National Park Service U.S. Department of the Interior Natural Resource Program Center Zion National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2006/014 Zion National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2006/014 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 March 2006 U.S. Department of the Interior Washington, D.C. The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the NPS conservation and environmental constituencies. Manuscripts are peer-reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and is designed and published in a professional manner. Natural Resource Reports are the designated medium for disseminating high priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. Examples of the diverse array of reports published in this series include vital signs monitoring plans; "how to" resource management papers; proceedings of resource management workshops or conferences; annual reports of resource programs or divisions of the Natural Resource Program Center; resource action plans; fact sheets; and regularly-published newsletters. Views and conclusions in this report are those of the authors and do not necessarily reflect policies of the National Park Service. Mention of trade names or commercial products does not constitute endorsement or recommendation for use by the National Park Service.
    [Show full text]
  • ADAMS Accession Nos. ML14309A441
    Fermi 3 Combined License Application Part 2: Final Safety Analysis Report 2.5 Geology, Seismology, and Geotechnical Engineering EF3 COL 2.0-26-A 2.5.1 Basic Geology and Seismic Information Subsection 2.5.1 presents a geological and seismological characterization of the Fermi 3 site divided into two parts. Subsection 2.5.1.1 describes the geology including the physiographic, geologic, and tectonic setting of the (320 km [200 mi] radius) site region and Subsection 2.5.1.2 describes the geology including stratigraphy, structural geology, and engineering geology of the (40 km [25 mi] radius) site vicinity to (1 km [0.6 mi] radius) site location. The geological and seismological characterization was developed in accordance with the guidance provided in RG 1.206, Section C.I.2.5.1 “Basic Geologic and Seismic Information,” and is intended to fulfill the requirements of 10 CFR 52 “Licenses, Certifications, and Approvals for Nuclear Power Plants” Section 52.79. The geological and seismological characterization presented in this section provides the basis for evaluating the geologic, seismic, and man-made hazards at the site. The geological and seismological characterization presented in this section is developed from previously published reports for the Fermi 2 power plant, recent and historic geologic literature, field and aerial reconnaissance, and subsurface hydrogeologic and geotechnical investigations conducted in 2007 for the preparation of this FSAR. The review of recent literature was facilitated by using GeoRef electronic database (American Geological Institute). Additionally, the Michigan and Ohio Geological Survey offices were contacted for relevant unpublished geologic literature, studies, and projects.
    [Show full text]
  • The Nature Conservancy's Watershed Approach To
    THE NATURE CONSERVANCY’S WATERSHED APPROACH TO COMPENSATION PLANNING FOR THE VIRGINIA AQUATIC RESTORATION TRUST FUND December 2009 TABLE OF CONTENTS PART ONE: THE NATURE CONSERVANCY’S CONSERVATION BY DESIGN .... 2 Background ..................................................................................................................... 2 The Nature Conservancy’s Conservation By Design ..................................................... 3 Element I: Geographic service area delineation ............................................................ 4 Elements ii, iii and iv: Threats Assessment ................................................................... 8 Elements v and vi: Aquatic resource goals / objectives and a prioritization strategy.. 10 Element xii. Satisfying Criteria for Use of Preservation ............................................. 13 Element viii. A description of any public and private stakeholder involvement in the plan ................................................................................................................................ 13 Element ix. Long-term protection and management strategies ................................... 15 Element x. Monitoring and Evaluating Progress .......................................................... 15 Conclusion .................................................................................................................... 17 PART II. OVERVIEW OF ECOREGIONAL PRIORITY CONSERVATION AREAS BY DEQ/CORPS SERVICE AREAS .............................................................................
    [Show full text]
  • Geologic Map of East Tennessee with Explanatory Text
    STATE OF TENNESSEE DEPARTMENT OF ENVIRONMENT AND CONSERVATION DIVISION OF GEOLOGY BULLETIN 58, PART II Geologic Map of East Tennessee With Explanatory Text Compiled by JOHN RODGERS Geologist, U. S. Geological Survey with the Collaboration of Geologists of the Tennessee Division of Geology Tennessee Valley Authority and United States Geological Survey Prepared under the Joint Auspices of the United States Geological Survey and the Tennessee Division of Geology Nashville, Tennessee 1953 Reprinted 1993 STATE OF TENNESSEE FRANK G. CLEMENT, Governor DEPARTMENT OF CONSERVATION Jim McCORD, Commissioner DIVISION OF GEOLOGY W. D. HARDEMAN, State Geologist 1993 STATE OF TENNESSEE Ned McWherter Governor DEPARTMENT OF ENVIRONMENT AND CONSERVATION J. W. Luna Commissioner DIVISION OF GEOLOGY Edward T. Luther State Geologist CONTENTS Page Abstract…………………………………………………...…………………………………………………1 Introduction ………………………………………………………...……………………………………… 3 Area covered by present map…………………………………………………………………...…………. 3 Compilation of the map ……………………………………………………………………………………. 3 Map units…………………………………………………………………………………………………… 6 Acknowledgments……………………………………………………………………………………….…. 8 Physical geography …...........…………………………………………………………........................…… 11 Regional setting .........................…............…………………………………………………….…. 11 Unaka Mountains .............................................……………………………………………….….. 11 Valley of East Tennessee ........................................………………………………………………. 14 Cumberland Plateau ..............................……………………………………………………….….
    [Show full text]
  • A Window to the Appalachians
    I-68/I-70: A WINDOW TO THE APPALACHIANS by Dr. John J. Renton Dept. of Geology & Geography West Virginia University Morgantown, WV Introduction The Appalachian Mountains are probably the most studied mountains on Earth. Many of our modern ideas as to the origin of major mountain systems evolved from early investigations of the Appalachian region. The Appalachians offer a unique opportunity to experience the various components of an entire mountain system within a relatively short distance and period of time. Compared to the extensive areas occupied by other mountain systems such as the Rockies and the Alps, the Appalachians are relatively narrow and can be easily crossed within a few hours driving time. Following I-68 and I-70 between Morgantown, WV, and Frederick, Maryland, for example, one can visit all of the major structural components within the Appalachians within a distance of about 160 miles. Before I continue, I would like to clarify references to the Allegheny and Appalachian mountains. The Allegheny Mountains were created about 250 million years ago when continents collided during the Alleghenian Orogeny to form the super-continent of Pangea (Figure 1). As the continents collided, a range of mountains were created in much the same fashion that the Himalaya Mountains are now being formed by the collision of India and Asia. About 50 million years after its Figure 1 1 creation, Pangea began to break up with the break occurring parallel to the axis of the original mountains. As the pieces that were to become our present continents moved away from each other, the Indian, Atlantic, and Arctic oceans were created (Figure 2).
    [Show full text]
  • Section 2.5.1 Geologic Characterization Information
    Clinch River Nuclear Site Early Site Permit Application Part 2, Site Safety Analysis Report SUBSECTION 2.5.1 TABLE OF CONTENTS Section Title Page 2.5 Geology, Seismology, and Geotechnical Engineering ............................... 2.5.1-1 2.5.1 Geologic Characterization Information ...................................... 2.5.1-1 2.5.1.1 Regional Geology (within the 200-Mile Regional Radius) ................................................................... 2.5.1-1 2.5.1.2 Local Geology ....................................................... 2.5.1-32 2.5.1.3 References ........................................................... 2.5.1-82 2.5.1-i Revision 0 Clinch River Nuclear Site Early Site Permit Application Part 2, Site Safety Analysis Report SUBSECTION 2.5.1 LIST OF TABLES Number Title 2.5.1-1 Stratigraphic Units Encountered at the Clinch River Nuclear Site 2.5.1-2 Clinch River Nuclear Stratigraphic Boundaries 2.5.1-3 Average Thickness and Variability of Each Stratigraphic Unit 2.5.1-4 Lithologic Adjectives and Modifiers 2.5.1-5 Summary of Petrographic Examination 2.5.1-6 Description of Mapped Karst Features 2.5.1-7 Occurrence of Karst Depressions by Geologic Unit in the 5-Mile Site Radius 2.5.1-8 Occurrence of Cave Entrances by Geologic Unit in the 5-Mile Site Radius 2.5.1-9 Chemistry, Mineralogy, and Petrography of Rock Core 2.5.1-10 Mineralogy of Rock Core from Clinch River Breeder Reactor Project 2.5.1-11 Cavities in Boreholes Drilled at Clinch River Nuclear Site, 1973–1978 and 2013 2.5.1-12 Definition of Joint Condition Ratings
    [Show full text]
  • Friendship Hill National Historic Site Geologic Resource Evaluation Report
    National Park Service U.S. Department of the Interior Natural Resource Program Center Friendship Hill National Historic Site Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2008/022 THIS PAGE: Waterfall on Ice Pond Run, Friendship Hill NHP. ON THE COVER: Gallatin House, Friendship Hill NHP NPS Photos Friendship Hill National Historic Site Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2008/022 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 February 2008 U.S. Department of the Interior Washington, D.C. The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the NPS conservation and environmental constituencies. Manuscripts are peer- reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and is designed and published in a professional manner. Natural Resource Reports are the designated medium for disseminating high priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. Examples of the diverse array of reports published in this series include vital signs monitoring plans; "how to" resource management papers; proceedings of resource management workshops or conferences; annual reports of resource programs or divisions of the Natural Resource Program Center; resource action plans; fact sheets; and regularly- published newsletters. Views and conclusions in this report are those of the authors and do not necessarily reflect policies of the National Park Service.
    [Show full text]