A GEOLOGIC RECONNAISSANCE and MINERAL EVALUATION WHEELER WASH AREA, HUALPAI MOUNTAINS, MOHAVE COUNTY, ARIZONA by John Steven
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Arizona Missing Linkages (US-93: Wickenburg to Santa Maria River Linkage Design)
ARIZONA MISSING LINKAGES US-93: Wickenburg to Santa Maria River Linkage Design Paul Beier, Daniel Majka submitted July 2006 last revised March 14, 2007 US-93: WICKENBURG TO SANTA MARIA RIVER LINKAGE DESIGN Acknowledgments This project would not have been possible without the help of many individuals. We thank Dr. Phil Rosen, Matt Good, Chasa O’Brien, Dr. Jason Marshal, Ted McKinney, and Taylor Edwards for parameterizing models for focal species and suggesting focal species. Catherine Wightman, Fenner Yarborough, Janet Lynn, Mylea Bayless, Andi Rogers, Mikele Painter, Valerie Horncastle, Matthew Johnson, Jeff Gagnon, Erica Nowak, Lee Luedeker, Allen Haden, and Shaula Hedwall helped identify focal species and species experts. Robert Shantz provided photos for many of the species accounts. Shawn Newell, Jeff Jenness, Megan Friggens, and Matt Clark provided helpful advice on analyses and reviewed portions of the results. Funding This project was funded by a grant from Arizona Game and Fish Department to Northern Arizona University. Recommended Citation Beier, P., and D. Majka. 2006. Arizona Missing Linkages: US-93: Wickenburg to Santa Maria River Linkage Design. Report to Arizona Game and Fish Department. School of Forestry, Northern Arizona University. Table of Contents TABLE OF CONTENTS ............................................................................................................................................ I LIST OF TABLES & FIGURES...............................................................................................................................II -
Manganese Deposits in the Artillery Mountains Region Mohave County, Arizona
UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. E. Wrather. Director Bulletin 936-R MANGANESE DEPOSITS IN THE ARTILLERY MOUNTAINS REGION MOHAVE COUNTY, ARIZONA BY S. G. LASKY AND B. N. WEBBER Strategic Minerals Investigations. 1942 (Pages 417-448) UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1944 For sale by the Superintendent of Documents, U. S. Government Printing Office, Washington, D. C. Price $1.25 CONTENTS Page 4 Abstract................................................... 417 Introduction.............................................. 418 Acknowledgments....................................... 420 Geography................................................. 420 -* Geology................................................... 422 Manganese-bearing formation........................... 425 Manganese deposits........................................ 427 General character..................................... 428 Sandstone ore..................................... - 430 Clay ore.......................................... 431 Hard or supergene ore............................. 432 Extent and thickness................................... 433 Upper zone........................................ 433 Maggie block.................................. 434 Upper Chapin block............................ 435 Lower Chapin block............................ 435 Price block................................... 437 Sees. 23 and 26, T. UN., R. 13 W............ 437 Lower zone........................................ 437 Origin................................................ -
Miocene Slip History of the Eagle Eye Detachment Fault, Harquahala
PUBLICATIONS Tectonics RESEARCH ARTICLE Miocene slip history of the Eagle Eye detachment 10.1002/2016TC004241 fault, Harquahala Mountains metamorphic core Key Points: complex, west-central Arizona • Total displacement on the Eagle Eye detachment fault is ~44 ± 2 km Michael G. Prior1, Daniel F. Stockli1, and John S. Singleton2 • Apatite and zircon (U-Th)/He slip rates along the Eagle Eye detachment are 1Department of Geological Sciences, University of Texas at Austin, Austin, Texas, USA, 2Department of Geosciences, ~6.6 + 7.8/À2.3 km/Myr and ~6.6 + 7.1/À2.0 km/Myr, respectively Colorado State University, Fort Collins, Colorado, USA • Active extension along the Eagle Eye detachment fault from ~21 ± 1 Ma to ~14 Ma Abstract The structural and thermal evolution of major low-angle normal faults in the Colorado River extensional corridor has been a controversial topic since the pioneering studies of metamorphic core Supporting Information: complexes in the early 1980s. We present new geo-thermochronometry data from the Harquahala Mountains • Supporting Information S1 in west-central Arizona to determine the timing of extension, displacement magnitude, and slip rates along the • Table S1 Eagle Eye detachment fault (EED) during large-magnitude Miocene extension. Zircon and apatite (U-Th)/He • Table S2 • Table S3 data (ZHe and AHe, respectively) from 31 samples along a ~55 km extension-parallel transect indicate active • Table S4 slip along the EED occurred between ~21 ± 1 Ma and ~14 Ma. The spatial extent of ZHe ages and exhumation • Table S5 of the zircon partial retention zone indicated ~44 ± 2 km of total displacement, whereas lithologic similarity Correspondence to: and identical U-Pb ages between correlated footwall rocks in the Little Harquahala Mountains and breccia M. -
Grand Canyon Council Oa Where to Go Camping Guide
GRAND CANYON COUNCIL OA WHERE TO GO CAMPING GUIDE GRAND CANYON COUNCIL, BSA OA WHERE TO GO CAMPING GUIDE Table of Contents Introduction to The Order of the Arrow ....................................................................... 1 Wipala Wiki, The Man .................................................................................................. 1 General Information ...................................................................................................... 3 Desert Survival Safety Tips ........................................................................................... 4 Further Information ....................................................................................................... 4 Contact Agencies and Organizations ............................................................................. 5 National Forests ............................................................................................................. 5 U. S. Department Of The Interior - Bureau Of Land Management ................................ 7 Maricopa County Parks And Recreation System: .......................................................... 8 Arizona State Parks: .................................................................................................... 10 National Parks & National Monuments: ...................................................................... 11 Tribal Jurisdictions: ..................................................................................................... 13 On the Road: National -
Geologic Framework of West-Central Arizona
Arizona Geological Society Digest, Volume XII, 1980 1 Geologic Framework of West-Central Arizona by Stephen J. Reynolds 1 Abstract The geology of west-central Arizona is complex and understood only in a reconnais sance fashion. The oldest rocks are Precambrian (approximately 1. 7 b. y . B.P.) gneiss, schist, quartzite, and amphibolite, which in the Precambrian were metamorphosed, de formed, and intruded by several generations of plutons. These rocks and structures are unconformably overlain by a cratonic sequence of Paleozoic carbonate and clastic strata. Representatives of Mesozoic rocks include intermediate to felsic volcanic and plutonic rocks of probably mid-Mesozoic age and overlying thick sections of clastic rocks, which are intruded by Late Cretaceous plutons. At least three deformational and metamorphic events of probably Cretaceous and Tertiary ages affected the region after deposition of the Mesozoic clastic rocks. Evidence for Tertiary mylonitization and subsequent dislocational phenomena is exposed in at least four mountain ranges that have characteristics of metamorphic core complexes. Dislocation was accompanied by listric normal faulting and tilting of mid- Tertiary volcanic and sedimentary sections. Late Tertiary Basin and Range faulting occurred after 15 m. y. B. P. and has eVidently been inactive for at least several million years. Introduction 1976; Varga, 1976, 1977; Rehrig and Reynolds, 1977, in press; Harding, 1978; Eberly and The geology of west-central Arizona, al Stanley, 1978; Keith, 1978; Otton, 1978; though incompletely understood, provides Crowl, 1979; Marshak, 1979; Robison, 1979; insight into the variety of geologic components Suneson and Lucchitta, 1979; Davis and that constitute the regional tectonic framework others, in press; Shafiqullah and others, this of southwestern North America. -
Selected Papers on the Geology of Washington
SELECTED PAPERS ON THE GEOLOGY OF WASHINGTON J. ERIC SCHUSTER, Editor WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES BULLETIN 77 1987 •• WASHINGTON STATE DEPARTMENT OF =~;;;arf;t Natural Resources Brian Boyle • Commlnloner ol Public Land> Art Sleoms · Supervisor Division ol Geology and Earth Resources Raymond Lamianis. Stale Geologist This report is for sale by: Publications Washington Deparbnent of Natural Resources Division of Geology and Earth Resources Mail Stop PY-12 Olympia, WA 98504 Price $ 14.84 Tax 1.16 Total $ 16.00 Mail orders must be prepaid; please add $1.00 to each order for postage and handling. Make checks payable to the Department of Natural Resources. This book is printed on acid-free paper. Printed in the United States of America. ii This volume is in memory of Randall L. Gresens (1935-1982) E. Bates McKee, Jr. (1934-1982) and in honor of Julian D. Barksdale (1904-1983) Howard A. Coombs Peter Misch A. Lincoln Washburn and Harry E. Wheeler (1907-1987) for their service to the University of Washington, Department of Geological Sciences, and their contributions to the geological sciences. iii iv CONTENTS page Preface J. Eric Schuster and Eric S. Cheney vii A tectonic and geochronologic overview of the Priest River crystalline complex, northeastern Washington and northern Idaho William A. Rehrig, Stephen J. Reynolds, and Richard L. Armstrong ......................... I Rb-Sr and U-Pb geochronometry of the Priest River metamorphic complex Precambrian X basement and its Mesozoic-Cenozoic plutonic-metamorphic overprint, northeastern Washington and northern Idaho Richard Lee Armstrong, Randall R. Parrish, Peter van der Heyden, Stephen J. -
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. -
K-Ar and Fission-Track Ages (Dates) of Volcanic Intrusive, Altered, and Metamorphic Rocks in the Mohave Mountains Area, West- Central Arizona J.K
K-Ar and fission-track ages (dates) of volcanic intrusive, altered, and metamorphic rocks in the Mohave Mountains area, west- central Arizona J.K. Nakata, M.A. Pernokas, K.A. Howard, J.E. Nielson, and J.R. Shannon Isochron/West, Bulletin of Isotopic Geochronology, v. 57, pp. 21-32 Downloaded from: https://geoinfo.nmt.edu/publications/periodicals/isochronwest/home.cfml?Issue=57 Isochron/West was published at irregular intervals from 1971 to 1996. The journal was patterned after the journal Radiocarbon and covered isotopic age-dating (except carbon-14) on rocks and minerals from the Western Hemisphere. Initially, the geographic scope of papers was restricted to the western half of the United States, but was later expanded. The journal was sponsored and staffed by the New Mexico Bureau of Mines (now Geology) & Mineral Resources and the Nevada Bureau of Mines & Geology. All back-issue papers are available for free: https://geoinfo.nmt.edu/publications/periodicals/isochronwest This page is intentionally left blank to maintain order of facing pages. 21 K-Ar AND FISSION-TRACK AGES (DATES) OF VOLCANIC INTRUSIVE, ALTERED, AND METAMORPHIC ROCKS IN THE MOHAVE MOUNTAINS AREA, WEST-CENTRAL ARIZONA J. K. NAKATA M. A. PERNOKAS U,S. Geological Survey, Menio Park, CA 94025 K. A. HOWARD J. E. NIELSON U.S. Geological Survey, Denver, CO 80225 J. R. SHANNON Current address: Crown Resource Corp., Republic, WA 99166 114^30' The Mohave Mountains and adjacent ranges of west-central Arizona (fig. 1) occupy a key area for unraveling the evolution of Tertiary tectonics in the SSS3S333SSS8S3SS$S!sOUTLINE OF FIGURE 2. -
And La Paz County, Arizona
~ Min.era] urces of t'he Cactu Plain »and East Cact s Plain Wild rness Study Areas, La Paz County, Arizona ARIZONA AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the cur rent-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Sur vey publications released prior to the current year are listed in the most recent annual "Price and Availability List" Publications that are listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" are no longer available. Prices of reports released to the open files are given in the listing "U.S. Geological Survey Open-File Reports," updated month ly, which is for sale in microfiche from the U.S. Geological Survey, Books and Open-File Reports Section, Federal Center, Box 25425, Denver, CO 80225. Reports released through the NTIS may be obtained by writing to the National Technical Information Service, U.S. Department of Commerce, Springfield, VA 22161; please include NTIS report number with inquiry. Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL OVER THE COUNTER Books Books Professional Papers, Bulletins, Water-Supply Papers, Techniques of Water-Resources Investigations, Circulars, publications of general in Books of the U.S. Geological Survey are available over the terest (such as leaflets, pamphlets, booklets), single copies of Earthquakes counter at the following Geological Survey Public Inquiries Offices, all & Volcanoes, Preliminary Determination of Epicenters, and some mis of which are authorized agents of the Superintendent of Documents: cellaneous reports, including some of the foregoing series that have gone out of print at the Superintendent of Documents, are obtainable by mail from • WASHINGTON, D.C.--Main Interior Bldg., 2600 corridor, 18th and C Sts., NW. -
Geologic Interpretation of Gravity Data from the Date Creek Basin and Adjacent Area, West-Central Arizona
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Geologic Interpretation of Gravity Data from the Date Creek Basin and Adjacent Area, West-central Arizona By James K. Otton and Jeffrey C. Wynn Open-File Report 78-845 1978 This report is preliminary and has not been edited or reviewed for conformity with U.S. Geological Survey standards and nomenclature. Contents Page Abstract 1 Data processing, modeling, and contouring 3 Physiographic and geologic setting 4 yffVaTTI x. d v x <i-»i_y » - - _ T^ The Date Creek Basin 10 ^3 *^*"t ^ t^ OClO J.I1 Implications for uranium exploration 15 Conclus ions 17 References 18 Illustrations Figure 1. Area of gravity survey in west-central Arizona 5 2. Generalized geologic map of the Date Creek Bas in 6 3. Complete Bouguer gravity for the Date Creek Basin and vicinity 9 4. Second-order residual gravity for the Date Creek Basin and vicinity 11 5. Anderson mine gravity model 14 6. Two-basins gravity model 16 Table Table 1. Stratigraphy of the Date Creek Basin 8 Geologic Interpretation of Gravity Data from the Date Creek Basin and adjacent area, west-central Arizona by James K. Otton and Jeffrey C. Wynn Abstract A gravity survey of the Date Creek Basin and adjacent areas was conducted in June 1977 to provide information for the inter pretation of basin geology. A comparison of facies relations in the locally uraniferous Chapin Wash Formation and the position of the Anderson-mine gravity anomaly in the Date Creek Basin sug gested that a relationship between gravity lows and the develop ment of thick lacustrine sections in the region might exist. -
K-Ar Geochronology and Geologic History of Southwestern Arizona and Adjacent Areas
Arizona Geological Society Digest, Volume XII, 1980 201 K-Ar Geochronology and Geologic History of Southwestern Arizona and Adjacent Areas by 2 3 M. Shafiqullah , P.E. Damonl , D.J. Lynch l, S.J. Reynolds , WA. Rehrig , 4 and R.N. Raymond A bstract This paper presents K-Ar ages of 174 samples from 154 localities in southwestern Ari- zona and adjacent areas with a summary of the geologic history. Ages are given for many rock units that had been "dated" previously only by lithologic correlations. These ages establish the timing of the magmatic and tectonic events that created and deformed the rocks. We interpret the older Precambrian history of Arizona as the result of a long-enduring and evolving convergent continental margin with accretion to the southeast at the rate of 2 km/m.y. This process was terminated 1.4 b.y. ago by the intrusion of vast batholiths ex- tending in a northeasterly direction far beyond Arizona. Younger Precambrian rocks ac- cumulated in an epicontinental sea along the trend of the Cordilleran geosyncline. These rocks were intruded by extensive diabase sills that are best preserved in the central moun- tain region. There is no further record of Precambrian magmatism or sedimentation after intrusion of the diabase sills. Some Precambrian K-Ar dates have been reset by the thermal disturbance that accompanied these intrusions. K-Ar ages that fall within the Paleozoic are reset ages and there is no evidence for any Paleozoic magmatism in the region. K-Ar ages of most of the pre-Laramide Mesozoic igneous rocks in the region have been reset by Laramide magmatism but evidence has been found for Early to Late Jurassic magmatism. -
Frontiers in Geology and Ore Deposits of Arizona and the Southwest
FRONTIERS IN GEOLOGY AND ORE DEPOSITS OF ARIZONA AND THE SOUTHWEST Arizona Geological Society and the University of Arizona 1986 Symposium FIELD TRIP GUIDEBOOK #8 Mesozoic Through Miocene Low-angle Tectonics and Related Mineralization. Harguahala-Granite Wash Buckskin Mountains. West Central Arizona March 21-23, 1986 Leaders: J. Spencer and S. Reynolds (Az.BGMT) and N. Lehman (Consul tant) Coordinator: J. Welty (AzBGMT) ARIZONA GEOLOGICAL SOCIETY TUCSON, ARIZONA Cover preparation by Beverly Morgan, modified from J. Mehulka and P. Mirocha, AGS Digest Volume XVI ARIZONA GEOLOGICAL SOCIETY P.O. BOX 40952, UNIVERSITY STATION TUCSON, ARIZONA 85719 To: Field Trip Participants Welcome to Arizona and the 1986 Arizona Geological Society Symposium "Frontiers in Geology and Ore Deposits of Arizona and the Southwest. 11 As field trip chairman I would like to wish you an enjoyable and informative con ference and a worthwhile field trip experience. The field trip committee set out many months ago to provide field expo sure to a broad spectrum of geological disciplines. The results include trips to recent precious-metal discoveries, areas of new and developing stratigraph ic and structure concepts, industrial mineral resources, lithologic features significant to the petroleum potential in the Southwest, geologic hazards in the community, and an opportunity to attend trips from previous Arizona Geo logical Society meetings. We hope you find your chosen field trip as exciting as we intended. At this time of very limited support from industry, it is especially im portant to acknowledge the personal efforts of so many. I include in those the planning and follow through of the field trip committee, the many hours of preparation by the trip leaders, and the commitment of the trip coordina tors to a smooth-running trip.