DOCSLIB.ORG

The Phosphoria, Park City and Shedhorn Formations in the Western Phosphate Field

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
The Phosphoria, Park City and Shedhorn Formations in the Western Phosphate Field The Phosphoria, Park City and Shedhorn Formations in the Western Phosphate Field GEOLOGICAL SURVEY PROFESSIONAL PAPER 313-A This report concerns work done as part of the program of the Department of the Interior for development of the Missouri River basin and work done partly on behalf of the U. S. Atomic Energy Commission. It is published with the permission of the Commission The Phosphoria, Park City and Shedhorn Formations in the Western Phosphate Field By V. E. McKELVEY and others GEOLOGY OF PERMIAN ROCKS IN THE WESTERN PHOSPHATE FIELD GEOLOGICAL SURVEY PROFESSIONAL PAPER 313-A With Sections by JAMES STEELE WILLIAMS, R. P. SHELDON, E. R. CRESSMAN, T. M. CHENEY, and R. W. SWANSON This report concerns work done as part of the program of the Department of the Interiorfor development of the Missouri River basin and work done partly on behalf of the U. S. Atomic Energy Commission. It is published with the permission of the Commission UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1959 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1 (paper cover; PREFACE Phosphorus is vital to the national economy because were measured and sampled, however, where natural it is required to sustain the agricultural productivity of exposures and prospect pits permitted. our soils. It is also used extensively in the chemical Similar work continued intermittently and on a re­ industry, particularly in the manufacture of detergents. duced scale until World War II. During W. W. Nearly all the phosphorus and phosphate compounds Rubey's work in the Afton quadrangle of western produced in this country are derived from sedimentary Wyoming the Public Works Administration provided phosphorites, such as those in the western field. In funds to sample the phosphatic beds and associated addition to phosphate, some phosphorites contain minor rocks. Several trenches were dug in 1938. Analyses amounts of certain elements that are now or may even­ of some of the samples collected from these trenches tually be recovered during the production of phosphate. showed the presence of as much as 1 percent V2O5, 0.3 Chief among these are fluorine, uranium, vanadium, and percent NiO2, and 0.1 percent Mo2O3 in a nonphos- rare earths. Some of the black shales associated with phatic black shale zone. Because of the strategic im­ the phosphorites also contain vanadium, zinc, nickel, portance of vanadium at that time, an extensive molybdenum, selenium, and distillable hydrocarbons. sampling program was begun in 1942 under Mr. Moreover, the oil in some important fields may have Rubey's direction to explore the vanadium content of the been derived from source beds associated with phos­ Phosphoria formation. A well-defined vanadiferous phorites. For these several reasons, then, phosphorite zone was found in several areas in western Wyoming formations are among our most valuable natural re­ and southeastern Idaho; this zone was explored in sources. more detail in some areas by the Bureau of Mines and The most extensive phosphorite beds in the United the Wyodak Coal and Manufacturing Co., agent for States are in the Phosphoria formation of Permian age, the Metals Reserve Corporation. Analyses of samples which crops out in many areas in Idaho, Montana, collected showed the vanadiferous zone to contain as Wyoming, and Utah. The importance of the phos­ much as 1.3 percent ZnO and some of the phosphate phate deposits in this formation was recognized early beds to contain 0.01 to 0.02 percent U. in the present century, and in 1908 the Secretary of the As a result of the great wartime expansion in agri­ Interior withdrew from public entry large areas in the culture, domestic consumption of phosphate fertilizer region in which the phosphate deposits are found. increased sharply in the early 1940's. Most of this in­ Ownership rights to phosphate and certain other min­ crease was supported by production from the Florida erals were separated from the surface rights in 1914 and field, but by 1946 it was clear that production in the leasing laws were passed later to permit mining of the western field also would undergo considerable expan­ phosphate deposits. As a result of the 1908 land with­ sion. Because better information on the distribution, drawal, it was necessary to classify the phosphate lands quality, and thickness of phosphorite beds in different and separate them from nonphosphate lands as expedi- parts of the field would facilitate this expansion, and tiously as possible. With this as the main objective because the phosphorite and associated rocks evidently the Geological Survey undertook much geologic map­ contained other minerals of great potential importance ping in the western field between 1908 and 1916. Much to the Nation, the Geological Survey decided in 1947 to of this work was summarized by G. R. Mansfield in resume investigations of the western phosphate field. Professional Paper 152 and most of the remainder has The aims of the new work were to determine the been published in several Geological Survey Bulletins.1 distribution of the phosphatic rocks, the reserves, the The chief aim of these early surveys was the delineation regional trends of phosphate and other important of the structure and position of the phosphatic rocks minerals, the structures in which the containing beds rather than the determination of their quality, thick­ lie, and the origin of the minerals and the rocks in ness, and detailed stratigraphy. The phosphatic rocks which they are found. These objectives have been ap­ proached by several types of work, chiefly: (1) 1 See Harris, R. A., Davidson, D. F., and Arnold, B. P., 1954, Bibliog­ measurement, description, sampling, and analysis of raphy of the geology of the western phosphate field: U. S. Geol. Survey Bull. 1018, 89 p. the phosphorites and associated rocks in trenches or IV PEEFACE other exposures at intervals of 3 to 25 miles over most form in U. S. Geological Survey bulletins, circulars, of the field; (2) geologic mapping, at scales of and open-file releases.2 The reports that make up 1:12,000 to 1:62,500 of several previously unmapped Professional Paper 313 present the data on the chemi­ areas, mostly in Montana and southeastern Idaho, and cal composition, thickness, and stratigraphy of the remapping at a scale of 1:24,000, of the area in south­ phosphorites and associated rocks in the western phos­ eastern Idaho that contains most of the thickest and phate field, together with estimates of resources of the richest deposits in the field; (3) laboratory studies of valuable minerals and interpretative discussions of the mineralogy, petrography, and chemical composition regional geologic relationships. of the rocks; and (4) reconnaissance examination of The investigations described herein have been sup­ previously unmapped areas in which phosphatic rocks might occur but had not been reported. The work was ported in part by the Raw Materials Division of the designed to acquire geologic information that would U. S. Atomic Energy Commission and the Missouri aid industry in making preliminary selections of de­ Eiver Basin Committee of the Department of the In­ posits and of combinations of beds suitable for mining terior. The contributions of the many individuals who and that would aid the Federal Government in national have participated in the work are described in the in­ planning and in the leasing of phosphate deposits on dividual chapters that follow. the public domain. Most of the field investigations planned have been * For a summary of the status of component investigations see Swanson, R. W., McKelvey, V. E., and Sheldon, R. P., 1953, Progress report on investigations of completed and the results summarized in preliminary western phosphate deposits: U. S. Qeol. Survey Oirc. 297. CONTENTS Page Page Abstract.----_-----_--__-______________________-___ 1 Phosphoria formation Continued Introduction.______________________________________ I Tosi chert member by R. P. Sheldon________ 30 Fieldwork and acknowledgments.___________________ 1 Shedhorn sandstone, by E. R. Cressman and R. W. Swan- Regional stratigraphy and facies__________________ 2 son_____-___-____________________________ 31 Nomenclature, by V. E. McKelvey, E. R. Cressman, Lower member.________________________________ 32 R. P. Sheldon, and T. M. Cheney______________ 5 Upper member___________________-___---_--_ . 33 History...___________________________________ 5 Nomenclature of other units of Park City age, by T. M. Problems._____________________________________ 8 Cheney and R. P. Sheldon.____________._ 33 Plan and justification___________________________ 9 Fauna, age, and correlation of rocks of Park City age, by Park City formation...______________________________ II James Steele Williams--_-____--_-_-_---_---------- 36 General description, by R. P. Sheldon and T. M. Park City formation-___________________________ 36 Cheney ___________________________________ 11 Grandeur member._________-_-__-_----_____ 36 Grandeur member, by T. M. Cheney, R. W. Swanson, Franson member__________________________ 37 R. P. Sheldon, and V. E. McKelvey-_________ 12 Ervay carbonate rock member ___________ 37 Franson member, by T. M. Cheney_______________ 15 Phosphoria formation.________ _______________ 38 Ervay carbonate rock member, by R. P. Sheldon. __ 19 Meade Peak phosphatic shale and lower chert Phosphoria formation_-_---__-_-___-_________________ 20 members______-_-__________________ 3& General description, by V. E. McKelvey___________ 20 Rex chert and cherty shale members __________ 38 Lower chert member, by R. P. Sheldon__________ 22 Retort phosphatic shale and Tosi chert members. 39 Meade Peak phosphatic shale member, by V. E. Underlying and overlying rocks ___________________ 39 McKelvey. __________________________________ 22 Regional and intercontinental correlation of rocks of Rex chert member, by V. E. McKelvey___________ 25 Park City age________________ _ 40 Cherty shale member, by V. E. McKelvey_________ 28 Literature cited.-.._________________________________ 41 Retort phosphatic shale member, by R.
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]
  • 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]
  • 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 wrds@uwyo.edu 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.
    [Show full text]
  • The Track of the Yellowstone Hot Spot: Volcanism, Faulting, and Uplift
    Geological Society of America Memoir 179 1992 Chapter 1 The track of the Yellowstone hot spot: Volcanism, faulting, and uplift Kenneth L. Pierce and Lisa A. Morgan US. Geological Survey, MS 913, Box 25046, Federal Center, Denver, Colorado 80225 ABSTRACT The track of the Yellowstone hot spot is represented by a systematic northeast-trending linear belt of silicic, caldera-forming volcanism that arrived at Yel- lowstone 2 Ma, was near American Falls, Idaho about 10 Ma, and started about 16 Ma near the Nevada-Oregon-Idaho border. From 16 to 10 Ma, particularly 16 to 14 Ma, volcanism was widely dispersed around the inferred hot-spot track in a region that now forms a moderately high volcanic plateau. From 10 to 2 Ma, silicic volcanism migrated N54OE toward Yellowstone at about 3 cm/year, leaving in its wake the topographic and structural depression of the eastern Snake River Plain (SRP). This <lo-Ma hot-spot track has the same rate and direction as that predicted by motion of the North American plate over a thermal plume fixed in the mantle. The eastern SRP is a linear, mountain- bounded, 90-km-wide trench almost entirely(?) floored by calderas that are thinly cov- ered by basalt flows. The current hot-spot position at Yellowstone is spatially related to active faulting and uplift. Basin-and-range faults in the Yellowstone-SRP region are classified into six types based on both recency of offset and height of the associated bedrock escarpment. The distribution of these fault types permits definition of three adjoining belts of faults and a pattern of waxing, culminating, and waning fault activity.
    [Show full text]
  • The Geologic History of Fossil Butte National Monument and Fossil Basin
    The Geologic History of Fossil Butte National Monument and Fossil Basin FOSSIL BUTTE The Geologic History of Fossil Butte National Monument and Fossil Basin NPS Occasional Paper No. 3 THE GEOLOGIC HISTORY OF FOSSIL BUTTE NATIONAL MONUMENT AND FOSSIL BASIN Paul O. McGrew Michael Casilliano Department of Geology, University of Wyoming National Park Service Occasional Paper Number Three 1975 TABLE OF CONTENTS index.htm Last Updated: 01-Mar-2005 http://www.nps.gov/history/history/online_books/fobu/index.htm[6/17/2013 12:42:49 PM] The Geologic History of Fossil Butte National Monument and Fossil Basin (Tables of Contents) FOSSIL BUTTE The Geologic History of Fossil Butte National Monument and Fossil Basin NPS Occasional Paper No. 3 CONTENTS COVER INTRODUCTION LOCATION HISTORICAL BACKGROUND OF RESEARCH STRATIGRAPHY Thaynes Limestone Evanston Formation Wasatch Formation Basal Conglomerate Member Lower Member Main Body Sandstone Tongue Mudstone Tongue Bullpen Member Tunp Member Age of the Wasatch Formation Depositional Environment Green River Formation Fossil Butte Member Angelo Member Age of the Green River Formation Depositional Environment Fowkes Formation Sillem Member Bulldog Hollow Member Gooseberry Member Age of the Fowkes Formation Depositional Environment QUATERNARY THE GEOLOGIC STRUCTURE OF FOSSIL BASIN PALEONTOLOGY Flora Invertebrates http://www.nps.gov/history/history/online_books/fobu/contents.htm[6/17/2013 12:42:58 PM] The Geologic History of Fossil Butte National Monument and Fossil Basin (Tables of Contents) Vertebrates Fish Amphibians Reptiles Birds Mammals PALEOECOLOGY AND TAPHONOMY ACKNOWLEDGMENTS GLOSSARY REFERENCES BIBLIOGRAPHY Library of Congress Cataloging in Publication Data McGrew, Paul Orman, 1909- The geological history of Fossil Butte National Monument and Fossil Basin.
    [Show full text]
  • Phosphate Rock in Wyoming
    Phosphate Rock in Wyoming Jacob D. Carnes Report of Investigations No. 68 • 2015 WYOMING STATE GEOLOGICAL SURVEY Thomas A. Drean, Director and State Geologist Director and State Geologist Thomas A. Drean Editing by: Sarah R. Garlick Design and layout by: James R. Rodgers Photomicrograph of phosphate rock from the Poison Creek trench in Lincoln County, Wyo., showing the concentric structure of ap- atite grains commonly found in phosphorites of the Phosphoria Formation. Photomicrograph by Jacob Carnes, 2015. Cover photo: Outcrop of the Meade Peak Member of the Phosphoria Formation along U.S. Hwy 26, approximately 3 miles southwest of Hoback Junction, in Teton County, Wyo. Photo by Jacob Carnes, 2015. Phosphate Rock in Wyoming Wyoming State Geological Survey (WSGS) Report of Investigations No. 68, 2015 Suggested citation: Carnes, J.D., 2015, Phosphate rock in Wyoming: Wyoming State Geological Survey Report of Investigations No. 68, 34 p. The WSGS encourages fair use of its material. We request that credit be expressly given to the “Wyoming State Geological Survey” when citing information from this publication. Please contact the WSGS at 307- 766-2286, ext. 224, or by email at wsgs-info@wyo.gov, if you have any questions about citing materials, preparing acknowledgments, or extensive use of this material. We appreciate your cooperation. Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement or approval by the State of Wyoming or the WSGS. Individuals with disabilities who require an alternate form of this publication should contact the WSGS. TTY relay operator 800-877-9975.
    [Show full text]
  • Sequence Stratigraphy and Geochemistry of The
    Report of Investigations 2007-1 SEQUENCE STRATIGRAPHY AND GEOCHEMISTRY OF THE UPPER LOWER THROUGH UPPER TRIASSIC OF NORTHERN ALASKA: IMPLICATIONS FOR PALEOREDOX HISTORY, SOURCE ROCK ACCUMULATION, AND PALEOCEANOGRAPHY by Landon N. Kelly, Michael T. Whalen, Christopher A. McRoberts, Emily Hopkin, and Carla Susanne Tomsich ASK AL A G N S E Y O E L O V G R U IC S A L L A A N SIC D GEOPHY Published by STATE OF ALASKA DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL & GEOPHYSICAL SURVEYS 2007 Report of Investigations 2007-1 SEQUENCE STRATIGRAPHY AND GEOCHEMISTRY OF THE UPPER LOWER THROUGH UPPER TRIASSIC OF NORTHERN ALASKA: IMPLICATIONS FOR PALEOREDOX HISTORY, SOURCE ROCK ACCUMULATION, AND PALEOCEANOGRAPHY by Landon N. Kelly, Michael T. Whalen, Christopher A. McRoberts, Emily Hopkin, and Carla Susanne Tomsich 2007 This DGGS Report of Investigations is a final report of scientific research. It has received technical review and may be cited as an agency publication. STATE OF ALASKA Sarah Palin, Governor DEPARTMENT OF NATURAL RESOURCES Tom Irwin, Commissioner DIVISION OF GEOLOGICAL & GEOPHYSICAL SURVEYS Robert F. Swenson, State Geologist and Acting Director Division of Geological & Geophysical Surveys publications can be inspected at the following locations. Address mail orders to the Fairbanks office. Alaska Division of Geological University of Alaska Anchorage Library & Geophysical Surveys 3211 Providence Drive 3354 College Road Anchorage, Alaska 99508 Fairbanks, Alaska 99709-3707 Elmer E. Rasmuson Library Alaska Resource Library University of Alaska Fairbanks 3150 C Street, Suite 100 Fairbanks, Alaska 99775-1005 Anchorage, Alaska 99503 Alaska State Library State Office Building, 8th Floor 333 Willoughby Avenue Juneau, Alaska 99811-0571 This publication released by the Division of Geological & Geophysical Surveys was produced and printed in Fairbanks, Alaska at a cost of $5.00 per copy.
    [Show full text]
  • Paleozoic Rocks in the Black Pine Mountains, Cassia County, Idaho
    Paleozoic Rocks in the Black Pine Mountains, Cassia County, Idaho GEOLOGICAL SURVEY BULLETIN 1536 Paleozoic Rocks in the Black Pine Mountains, Cassia County, Idaho By]. FRED SMITH, JR. GEOLOGICAL SURVEY BULLETIN 1536 Descriptions of eleven rock units which range in age from Devonian to Permian, the thickest parts being Early Pennsylvanian to· Early Permian UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1983 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Smith, J. Fred (Joe Fred), 1911-1982 Paleowic rocks in the Black Pine Mountains, Cassia County, Idaho. (Geological Survey Bulletin 1536) Bibliography: 36 p. Supt. of Docs. No.: I 19.3: 1. Geology, Stratigraphic-Paleozoic. 2. Geology-Idaho-Black Pine Mountains. I. Title. II. Series. QE75.B9 no. 1536 557.3s [551.7'2'0979639] 81-607193 [QE.654] AACR2 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract . 1 Introduction . 2 Stratigraphy . 7 Rocks south of West Dry Canyon fault . 8 Lower plate . 8 Devonian System . 8 Jefferson Formation . 8 Mississippian and Pennsylvanian Systems . 9 Manning Canyon Shale . 9 Middle plate . 11 Pennsylvanian System . 11 Oquirrh Formation, limestone member . 11 Lower part . 11 Middle part . 13 Upper part . 15 Oquirrh Formation, limestone, sandstone, and quartzite mem- ber . 17 Oquirrh Formation, limestone and dolomite member . 18 Upper plate . 21 Pennsylvanian and Permian Systems . 21 Oquirrh Formation sandstone and siltstone member . 21 Rocks north of West Dry Canyon fault . 23 Plate I . 23 Pennsylvanian and Permian Systems .
    [Show full text]
  • Triassic-Jurassic 'Red Beds' of the Rocky Mountain Region": a Discussion
    University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln USGS Staff -- Published Research US Geological Survey 1929 "Triassic-Jurassic 'Red Beds' of the Rocky Mountain Region": A Discussion John B. Reeside Jr. U.S. Geological Survey Follow this and additional works at: https://digitalcommons.unl.edu/usgsstaffpub Part of the Earth Sciences Commons Reeside, John B. Jr., ""Triassic-Jurassic 'Red Beds' of the Rocky Mountain Region": A Discussion" (1929). USGS Staff -- Published Research. 498. https://digitalcommons.unl.edu/usgsstaffpub/498 This Article is brought to you for free and open access by the US Geological Survey at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in USGS Staff -- Published Research by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. The Journal of Geology, Vol. 37, No. 1 (Jan. - Feb., 1929), pp. 47-63 "TRIASSIC-JURASSIC 'RED BEDS' OF THE ROCKY MOUNTAIN REGION": A DISCUSSION' JOHN B. REESIDE, JR. U.S. Geological Survey ABSTRACT The conclusion drawn by Professor E. B. Branson in a recent paper on the "Red Beds" of the Rocky Mountain region that parts of these beds are marine is considered likely. The conclusion that there exists no basis for subdivision of the beds is not accepted, and a division of the Mesozoic part into Lower Triassic, Upper Triassic, and Jurassic units is advocated. The conclusion that no eolian deposits are present likewise is not accepted, and the interpretation of important parts of the Jurassic unit as eolian is advocated. Disagreement is expressed with much of Professor Branson's correlation table, and a substitute is offered.
    [Show full text]
  • Cassia County, Qs Idaho 113O00’10” O Qw 42 35’05” 86 Qw Ke Iver Ppsp Sna R O Pps 114 03’50” Qa Burley O Qb Sublett Rge
    Cassia County, Qs Idaho 113o0010 o Qw 42 3505 86 Qw ke iver PPsP Sna R o PPs 114 0350 Qa Burley o Qb Sublett Rge. 42 3055 Declo Qs 77 PPsP Qm PPsP Tov Zs Wm QTb Qa PPs QTb Tpf Idahome PPsP Qs Qs PPsP 27 Albion Tps Qs QTb Ps Qs 84 k Zs e Qw Qs e r Tpf 81 TsR Qw C Zs Sublett P Tpf Wm PPs e Malta Qs s Tov Cassia o Wm o Zs Wm Pzu G Tpf Mtns. or Mt. Harrison South Hills PPsP PPsP PPsP Qa Oakley PzZm Elba Ps Ps Qs Qs r e Pzu Tpf Zs Raft River Valley Ps PPsP Ps Blackpine Rge. v Zs i R Tps Tpf Qs Tpf Wm t PzZm f PPs Tpf Zs Tpf a Trapper Pk. Cache Pk. Tms R Qa Tpf Toi Toi PPsP Tpf Zs Tpf Toi Qs Qs Almo Tpf Ms PPsP Tpf Albion Mtns. Wm PPs Zs Zs Toi PPs PPs Almo Qs Qa PzZm Pluton Raft RiverTpf Narrows. Qa Tpf Zs City of Tms Qs Tps Tpf PPsP Qbo Qs Rocks Tpf Qs o o 42 0004 41 5932 o 114o1655 113 0005 Digital Atlas of Idaho, Nov. 2002 0 5 10 miles http://imnh.isu.edu/digitalatlas Compiled by Paul K. Link, 0 8 16 kilometers Idaho State University, Geosciences Dept. http://www.isu.edu/departments/geology/ Cassia County Cassia County, on the south side of the Snake River forms much of Idahos southern boundary with Utah and Nevada on the west. It contains a diverse assemblage of rocks, including the oldest rocks in Idaho, the metamorphic Green Creek gneiss in the Albion Mountains core complex.
    [Show full text]
  • Ground-Water Possibilities South of the Snake River Between Twin Falls and Pocatello, Idaho
    Ground-Water Possibilities South of the Snake River Between Twin Falls and Pocatello, Idaho By E. G. CROSTHWAITE CONTRIBUTIONS TO HYDROLOGY GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1460-C Prepared for the United States Bureau of Reclamation with the cooperation of the Idaho Department of Reclamation UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1957 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. CONTENTS Pag* Abstract _______________________ ...- _ . _____ - _ 99> Introduction-.... _________________________________________ _____ 100 Purpose and scope of report __ _________________________________ 100 Location of area_________________________________________ _ ____ 101 Previous investigations_____________________ ____________________ 102 Geography __ ___________________________________________________ 103' Surface features___-__-____-________--__-________-__--__-___- _ 108- Drainage. ___-___-__-__---_---_-__-_---______--_---_-____ __ _ 100 Climate.. ____________________ . ______________ 107 Precipitation _ ______________________________ _ _ __ ___ 107 Temperature _ ____________________________________ __ _ _ 109* Evaporation __ ___________________________________ _ ___ _ 110' Development ___ ____________________________________ _ _____ 111 Population __ _____________________________________ ___ __ 111 Agriculture. ___ __ _______________________________ _ _____ 113: Industry
    [Show full text]