Of Mining Properties in Yuma County, Arizona
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The Lower Gila Region, Arizona
DEPARTMENT OF THE INTERIOR HUBERT WORK, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Water-Supply Paper 498 THE LOWER GILA REGION, ARIZONA A GEOGBAPHIC, GEOLOGIC, AND HTDBOLOGIC BECONNAISSANCE WITH A GUIDE TO DESEET WATEEING PIACES BY CLYDE P. ROSS WASHINGTON GOVERNMENT PRINTING OFFICE 1923 ADDITIONAL COPIES OF THIS PUBLICATION MAT BE PROCURED FROM THE SUPERINTENDENT OF DOCUMENTS GOVERNMENT PRINTING OFFICE WASHINGTON, D. C. AT 50 CENTS PEE COPY PURCHASER AGREES NOT TO RESELL OR DISTRIBUTE THIS COPT FOR PROFIT. PUB. RES. 57, APPROVED MAT 11, 1822 CONTENTS. I Page. Preface, by O. E. Melnzer_____________ __ xr Introduction_ _ ___ __ _ 1 Location and extent of the region_____._________ _ J. Scope of the report- 1 Plan _________________________________ 1 General chapters _ __ ___ _ '. , 1 ' Route'descriptions and logs ___ __ _ 2 Chapter on watering places _ , 3 Maps_____________,_______,_______._____ 3 Acknowledgments ______________'- __________,______ 4 General features of the region___ _ ______ _ ., _ _ 4 Climate__,_______________________________ 4 History _____'_____________________________,_ 7 Industrial development___ ____ _ _ _ __ _ 12 Mining __________________________________ 12 Agriculture__-_______'.____________________ 13 Stock raising __ 15 Flora _____________________________________ 15 Fauna _________________________ ,_________ 16 Topography . _ ___ _, 17 Geology_____________ _ _ '. ___ 19 Bock formations. _ _ '. __ '_ ----,----- 20 Basal complex___________, _____ 1 L __. 20 Tertiary lavas ___________________ _____ 21 Tertiary sedimentary formations___T_____1___,r 23 Quaternary sedimentary formations _'__ _ r- 24 > Quaternary basalt ______________._________ 27 Structure _______________________ ______ 27 Geologic history _____ _____________ _ _____ 28 Early pre-Cambrian time______________________ . -
Reconnaissance Geology of the Northern Plomosa Mountains
RECONNAISSANCE GEOLOGY OF THE NORTHERN PLOMOSA MOUNTAINS by Robert Scarborough and Norman Meader with assistance by Jan C. Wilt and Stanley B. Keith November 1983 BUREAU nrc (iT;f)LOGY AND MINERAL TECHNOL{]Yl)Y STATE OF ARIZONA BUREAU OF GEOLOGY AND MHNEPJJ,L TECHNOLOGY OPEN - FIL.E HEPOF<T This report is preliminary and has not been edited o.r reviewed for conformity with Arizona Bureau o.f Geology and Mineral Technology standards. __ ~ - 1 - Table of Contents :~ I i) Previous Work. Acknowledgments. General Stratigraphy in the Northern Plomosa Mountains ',' Precambrian .• Paleozoic. • Mesozoic . Cenozoic • . i IJ I Geologic Relations in the Northern Plomosa Mountains • • • J"7 structures . I .. l ! J General Dexcriptions of Lithologies Within Plates. I' , 1) Bighorn Plate . • • ... • I / , i 2) Plomosa Pass Plate. • • • • j' I 1 3) Tough Nut Plate •. / " 4a) and 4b) Deadman Plate. ! , ,I 5) Plomosa Plate. • • • 'iii .. • • • 2./ Dikes. .. ~/ ..",. ) '1 J structural Observations and Interpretations. .' ' 1. Plomosa Fault ••. " ( 2. Order of structural Stacking. 3. Vergence Indicators 4. Movement on Plomosa Fault q ; Economic Geology . I Base and Precious Metals "I j - 2 .- 1 Ferrous Metals Iron . Manganese. " ., . Industrial minerals. Barite Bentoni te. Uranium Potential. ) , Petroleum Potential. List of Figures A. Chronology of rock units and major events. 1. Reconnaissance geologic map of the northern Plomosa Mountains, La Paz County, Arizona. 2. Geologic map - Plomosa Pass area. 3. General sketch tectonic map of northern Plomosa Mountains. 4. Geologic cross-section of the Plomosa Mountains. 1983 AGS Fall Field Trip Route Led by Bob Scarborough, Steven Reynold8, and Jon Spencer Arizona Bureau of Geology and Minerai Technology Organized by Stanley B. -
Curriculum Vita - Stephen J
Curriculum Vita - Stephen J. Reynolds School of Earth and Space Exploration, Arizona State University, Tempe, Arizona 85287-1404 (480) 965-9049 (work) Website: http://reynolds.asu.edu email: [email protected] Degrees/Registration University of Texas, El Paso: B.S., Geology, 1974 University of Arizona: M.S., Geosciences, 1977, Ph.D., Geosciences,1982 Arizona Registered Geologist #26773 (1993-present) Recent Professional Experience Arizona State University, Dept. of Geology: Professor (6/97 to present), Associate Professor (8/91 to 6/97). Teaching responsibilities include Advanced Geologic Field Mapping, Advanced Structural Geology, Applied Arizona Geology, Cordilleran Regional Geology, Geology of Arizona, Geotectonics, Introductory Geology, Orogenic Systems, Summer Field Geology, Methods of Geoscience Teaching ASU Center for Research on Education in Science, Mathematics, Engineering, and Technology, Associate Director (6/99 to present); chairman of founding committee. Arizona Geological Survey and Arizona Bureau of Geology and Mineral Technology: Research Geologist (6/88 to 7/91), Associate Research Geologist (6/87 to 6/88); Assistant Research Geologist (2/81 to 6/87). University of Arizona, Dept. of Geosciences: Visiting Associate Professor, (1991 to ~1997); Adjunct Associate Research Scientist (1987 to 1991); Research Associate and Assistant (1/75 to 12/80); Teaching Assistant (8/74 to 7/75) Geologist and Consulting Geologist: Clients include Animas Resources (2007 to present), Pediment Exploration, Ltd. (2007 to present), Clear Creek -
Mineral Resources of the Harquahala Mountains Wilderness Study Area, La Paz and Maricopa Counties, Arizona
2.SOB nH in ntoiOGIGM. JAN 3 1 1989 Mineral Resources of the Harquahala Mountains Wilderness Study Area, La Paz and Maricopa Counties, Arizona U.S. GEOLOGICAL SURVEY BULLETIN 1701-C Chapter C Mineral Resources of the Harquahala Mountains Wilderness Study Area, La Paz and Maricopa Counties, Arizona By ED DE WITT, S.M. RICHARD, J.R. HASSEMER, and W.F. HANNA U.S. Geological Survey J.R. THOMPSON U.S. Bureau of Mines U.S. GEOLOGICAL SURVEY BULLETIN 1701 MINERAL RESOURCES OF WILDERNESS STUDY AREAS- WEST-CENTRAL ARIZONA AND PART OF SAN BERNARDINO COUNTY, CALIFORNIA U. S. GEOLOGICAL SURVEY Dallas L Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE: 1988 For sale by the Books and Open-File Reports Section U.S. Geological Survey Federal Center Box 25425 Denver, CO 80225 Library of Congress Cataloging-in-Publlcatlon Data Mineral resources of the Harquahala Mountains wilderness study area, La Paz and Maricopa counties, Arizona. (Mineral resources of wilderness study areas west-central Arizona and part of San Bernardino County, California ; ch. C) (U.S. Geological Survey bulletin ; 1701-C) Bibliography: p. Supt. of Docs, no.: I 19.3:1701-C 1. Mines and mineral resources Arizona Harquahala Mountains Wilderness. 2. Harquahala Mountains (Ariz.) I. DeWitt, Ed. II. Series. III. Series: U.S. Geological Survey bulletin ; 1701. QE75.B9 no. 1701-C 557.3 s [553'.09791'72] 88-600012 [TN24.A6] STUDIES RELATED TO WILDERNESS Bureau of Land Management Wilderness Study Areas The Federal Land Policy and Management Act (Public Law 94-579, October 21, 1976) requires the U.S. Geological Survey and the U.S. -
Crystal Chemistry of Wulfenite (Pbmoo4) and Wolframite (Fe,Mn)WO4 Author Information – Darren A
Crystal Chemistry of Wulfenite (PbMoO4) and Wolframite (Fe,Mn)WO4 Author information – Darren A. Umbsaar Affiliation – University of Calgary Summary In this study, the crystal structure and chemistry of a selection of wulfenite (PbMoO4) and wolframite ((Fe,Mn)WO4) samples from various worldwide localities are examined. These 2+ minerals have the same general formula, ABO4, where A is a divalent metal cation (e.g. Mn , Fe2+, Pb2+, etc.) and B is a highly charged cation (W6+ or Mo6+). These minerals crystallize in two different space groups; (1) wulfenite crystallizes in the tetragonal scheelite-type structure (space group I41/a, formula units, Z, = 4), whereas (2) wolframite crystallizes in the monoclinic wolframite- type structure (space group P2/c, Z = 2). The space group symmetry and cell dimensions are largely dictated by the ionic radius of the A site cation. In general, when the A cation radius is >0.90Å the crystal will form the tetragonal scheelite-type structure, whereas an A cation radius <0.90Å will favor the monoclinic wolframite-type structure. X-ray diffraction analyses of these minerals have long been a challenge because they are composed of heavy atoms (Pb, Mo, and W) which dominate in scattering X-rays. This makes it challenging to precisely determine the atomic coordinates of oxygen, being a much lighter element with a weaker atomic scattering power. Therefore, in an effort to overcome the aforementioned obstacle, and to acquire accurate structural data for these minerals, this study uses synchrotron high resolution powder X-ray diffraction (HRPXRD). The natural wulfenite specimens analyzed so far in this study from various worldwide localities are very pure in composition, with all specimens being represented by the formula: Pb0.99- 5+ 6+ 6+ 6+ 1.00Mo0.99-1.00O4. -
Department of the Interior U.S
DEPARTMENT OF THE INTERIOR U.S. FISH AND WILDLIFE SERVICE REGION 2 DIVISION OF ENVIRONMENTAL CONTAMINANTS CONTAMINANTS IN BIGHORN SHEEP ON THE KOFA NATIONAL WIL DLIFE REFUGE, 2000-2001 By Carrie H. Marr, Anthony L. Velasco1, and Ron Kearns2 U.S. Fish and Wildlife Service Arizona Ecological Services Office 2321 W. Royal Palm Road, Suite 103 Phoenix, Arizona 85021 August 2004 2 ABSTRACT Soils of abandoned mines on the Kofa National Wildlife Refuge (KNWR) are contaminated with arsenic, barium, mercury, manganese, lead, and zinc. Previous studies have shown that trace element and metal concentrations in bats were elevated above threshold concentrations. High trace element and metal concentrations in bats suggested that bighorn sheep also may be exposed to these contaminants when using abandoned mines as resting areas. We found evidence of bighorn sheep use, bighorn sheep carcasses, and scat in several abandoned mines. To determine whether bighorn sheep are exposed to, and are accumulating hazardous levels of metals while using abandoned mines, we collected soil samples, as well as scat and bone samples when available. We compared mine soil concentrations to Arizona non-residential clean up levels. Hazard quotients were elevated in several mines and elevated for manganese in one Sheep Tank Mine sample. We analyzed bighorn sheep tissues for trace elements. We obtained blood, liver, and bone samples from hunter-harvested bighorn in 2000 and 2001. Arizona Game and Fish Department also collected blood from bighorn during a translocation operation in 2001. Iron and magnesium were elevated in tissues compared to reference literature concentrations in other species. Most often, domestic sheep baseline levels were used for comparison because of limited available data for bighorn sheep. -
Brenda SEZ Analysis: Draft PEIS
1 8 AFFECTED ENVIRONMENT AND IMPACT ASSESSMENT FOR 2 PROPOSED SOLAR ENERGY ZONES IN ARIZONA 3 4 5 8.1 BRENDA 6 7 8 8.1.1 Background and Summary of Impacts 9 10 11 8.1.1.1 General Information 12 13 The proposed Brenda Solar Energy Zone (SEZ) is located in La Paz County in west- 14 central Arizona (Figure 8.1.1.1-1), 32 mi (52 km) east of the California border. The SEZ has a 15 total area of 3,878 acres (16 km2). In 2008, the county population was 20,005, while adjacent 16 Riverside County to the west in California had a population of 2,087,917. The towns of 17 Quartzsite and Salome in La Paz County are about 18 mi (29 km) west of, and 18 mi (29 km) 18 east of, the SEZ respectively. The Phoenix metropolitan area is approximately 100 mi (161 km) 19 to the east of the SEZ, and Los Angeles is approximately 230 mi (370 km) to the west. 20 21 The nearest major road access to the SEZ is via U.S. 60, which runs southwest to 22 northeast, along the southeast border of the Brenda SEZ. The nearest railroad stop is 11 mi 23 (18 km) away. The nearest airports serving the area are the Blythe and Parker (Avi Suquilla) 24 Airports, both approximately 50 mi (80 km) from the SEZ, and neither of which have scheduled 25 commercial passenger service. The Sky Harbor Airport in Phoenix is 125 mi (201 km) to the 26 east, and Yuma International Airport in Yuma is 104 mi (167 km) to the south, of the SEZ. -
GSA ROCKY MOUNTAIN/CORDILLERAN JOINT SECTION MEETING 15–17 May Double Tree by Hilton Hotel and Conference Center, Flagstaff, Arizona, USA
Volume 50, Number 5 GSA ROCKY MOUNTAIN/CORDILLERAN JOINT SECTION MEETING 15–17 May Double Tree by Hilton Hotel and Conference Center, Flagstaff, Arizona, USA www.geosociety.org/rm-mtg Sunset Crater is a cinder cone located north of Flagstaff, Arizona, USA. Program 05-RM-cvr.indd 1 2/27/2018 4:17:06 PM Program Joint Meeting Rocky Mountain Section, 70th Meeting Cordilleran Section, 114th Meeting Flagstaff, Arizona, USA 15–17 May 2018 2018 Meeting Committee General Chair . Paul Umhoefer Rocky Mountain Co-Chair . Dennis Newell Technical Program Co-Chairs . Nancy Riggs, Ryan Crow, David Elliott Field Trip Co-Chairs . Mike Smith, Steven Semken Short Courses, Student Volunteer . Lisa Skinner Exhibits, Sponsorship . Stephen Reynolds GSA Rocky Mountain Section Officers for 2018–2019 Chair . Janet Dewey Vice Chair . Kevin Mahan Past Chair . Amy Ellwein Secretary/Treasurer . Shannon Mahan GSA Cordilleran Section Officers for 2018–2019 Chair . Susan Cashman Vice Chair . Michael Wells Past Chair . Kathleen Surpless Secretary/Treasurer . Calvin Barnes Sponors We thank our sponsors below for their generous support. School of Earth and Space Exploration - Arizona State University College of Engineering, Forestry, and Natural Sciences University of Arizona Geosciences (Arizona LaserChron Laboratory - ALC, Arizona Radiogenic Helium Dating Lab - ARHDL) School of Earth Sciences & Environmental Sustainability - Northern Arizona University Arizona Geological Survey - sponsorship of the banquet Prof . Stephen J Reynolds, author of Exploring Geology, Exploring Earth Science, and Exploring Physical Geography - sponsorship of the banquet NOTICE By registering for this meeting, you have acknowledged that you have read and will comply with the GSA Code of Conduct for Events (full code of conduct listed on page 31) . -
Geology of Cienega Mining District, Northwestern Yuma County, Arizona
Scholars' Mine Masters Theses Student Theses and Dissertations 1965 Geology of Cienega Mining District, Northwestern Yuma County, Arizona Elias Zambrano Follow this and additional works at: https://scholarsmine.mst.edu/masters_theses Part of the Geology Commons Department: Recommended Citation Zambrano, Elias, "Geology of Cienega Mining District, Northwestern Yuma County, Arizona" (1965). Masters Theses. 7104. https://scholarsmine.mst.edu/masters_theses/7104 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. GEOLOGY OF CIENEGA MINING DISTRICT, NORTHWESTERN YUM.1\, COUNTY, ARIZONA BY ELIAS ZAMBRANO I J'i~& A THESIS submitted to the faculty of the UNIVERSITY OF MISSOURI AT ROLLA in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE IN GEOLOGY Rolla, Missouri 1965 ~!'Approved by ~2/~advisor) ~ ~·-~~ ii ABSTRACT In the mapped area three metamorphic units crop out: calc-silicates and marble, gneiss, and a conglomerate- schist section. The first one consists of a series of intercalations of calc-silicate rocks, local marbles, and greenschist. Quartzite appears in the upper part of the section. This section passes transitionally to the gneiss, which is believed to be of sedimentary origin. Features indicative of sedimentary origin include inter calation with marble, relic bedding which can be observed locally, intercalation of greenschist clearly of sedimentary origin, lack of homogeneity in composition with both lateral and vertical variation occurring, roundness of zircon grains, and lack of zoning in the feldspars. -
Ajo Peak to Tinajas Altas: a Flora of Southwestern Arizona
Felger, R.S., S. Rutman, and J. Malusa. 2014. Ajo Peak to Tinajas Altas: A flora of southwestern Arizona. Part 6. Poaceae – grass family. Phytoneuron 2014-35: 1–139. Published 17 March 2014. ISSN 2153 733X AJO PEAK TO TINAJAS ALTAS: A FLORA OF SOUTHWESTERN ARIZONA Part 6. POACEAE – GRASS FAMILY RICHARD STEPHEN FELGER Herbarium, University of Arizona Tucson, Arizona 85721 & Sky Island Alliance P.O. Box 41165, Tucson, Arizona 85717 *Author for correspondence: [email protected] SUSAN RUTMAN 90 West 10th Street Ajo, Arizona 85321 JIM MALUSA School of Natural Resources and the Environment University of Arizona Tucson, Arizona 85721 [email protected] ABSTRACT A floristic account is provided for the grass family as part of the vascular plant flora of the contiguous protected areas of Organ Pipe Cactus National Monument, Cabeza Prieta National Wildlife Refuge, and the Tinajas Altas Region in southwestern Arizona. This is the second largest family in the flora area after Asteraceae. A total of 97 taxa in 46 genera of grasses are included in this publication, which includes ones established and reproducing in the modern flora (86 taxa in 43 genera), some occurring at the margins of the flora area or no long known from the area, and ice age fossils. At least 28 taxa are known by fossils recovered from packrat middens, five of which have not been found in the modern flora: little barley ( Hordeum pusillum ), cliff muhly ( Muhlenbergia polycaulis ), Paspalum sp., mutton bluegrass ( Poa fendleriana ), and bulb panic grass ( Zuloagaea bulbosa ). Non-native grasses are represented by 27 species, or 28% of the modern grass flora. -
A Study of Uranium Favorability of Cenozoic Sedimentary Rocks, Basin
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY A Study of Uranium Favorability of Cenozoic Sedimentary Rocks Basin and Range Province, Arizona Part I General Geology and Chronology of Pre-late Miocene Cenozoic Sedimentary Rocks By Robert Scarborough and Jan Carol Wilt Open File Report 79-1429 1979 This report was funded by U.S. Geological Survey Grant No. 14-08-0001528. It;has not been edited for conformity with U.S. Geological Survey standards or with accepted U.S. Geological Survey stratigraphic nomenclature. FOREWORD This report by Robert Scarborough and Jan Carol Wilt summarizes the results of a study made for the U.S. Geological Survey jointly by the Bureau of Geology and Mineral Technology and the Laboratory of Isotope Geochemistry, College of Earth Sciences, University of Arizona, under Grant No. 14-08-0001528. Age dating by the K/Ar method was cost-shared with. NSF Grant No. EAR78-11535 which supports volcanic rock studies by the Laboratory of Isotope Geochemistry. It is considered that this report adequately fulfills the agreement objectives. Principal Investigator: H. Wesley Peirce, Principal Geologist Geological Survey Branch Bureau of Geology and Mineral Technology University of Arizona, Tucson Co-Principal Investigator: Paul E. Damon, Chief Scientist Laboratory of Isotope Geochemistry Department of Geosciences College of Earth Sciences University of Arizona, Tucson CONTENTS Page Abstract ,....,,...,...,........« « 1 Introduction ...,.,..*....««..« «« 3 General statement ........ , ».....,....». 3 Purpose and scope .«..,,.....,.......... 3 Acknowledgments ..................... * . 4 Location and physiographic setting .............. 4 Approach ........................... 5 General Cenozoic geology of Basin and Range Province sediments . General statement ...................... 7 Group I localities with radioactive anomalies ........ 9 Mineta Formation ..................... 9 Cardinal Avenue sediments ................ -
Mottramite Pbcu(VO4)(OH) C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Orthorhombic
Mottramite PbCu(VO4)(OH) c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: 2/m 2/m 2/m. As crystals, equant or dipyramidal {111}, prismatic [001] or [100], with {101}, {201}, many others, to 3 mm, in drusy crusts, botryoidal, usually granular to compact, massive. Physical Properties: Fracture: Small conchoidal to uneven. Tenacity: Brittle. Hardness = 3–3.5 D(meas.) = ∼5.9 D(calc.) = 6.187 Optical Properties: Transparent to nearly opaque. Color: Grass-green, olive-green, yellow- green, siskin-green, blackish brown, nearly black. Streak: Yellowish green. Luster: Greasy. Optical Class: Biaxial (–), rarely biaxial (+). Pleochroism: Weak to strong; X = Y = canary-yellow to greenish yellow; Z = brownish yellow. Orientation: X = c; Y = b; Z = a. Dispersion: r> v,strong; rarely r< v.α= 2.17(2) β = 2.26(2) γ = 2.32(2) 2V(meas.) = ∼73◦ Cell Data: Space Group: P nma. a = 7.667–7.730 b = 6.034–6.067 c = 9.278–9.332 Z=4 X-ray Powder Pattern: Mottram St. Andrew, England; close to descloizite. 3.24 (vvs), 5.07 (vs), 2.87 (vs), 2.68 (vs), 2.66 (vs), 2.59 (vs), 1.648 (vs) Chemistry: (1) (2) (1) (2) CrO3 0.50 ZnO 0.31 10.08 P2O5 0.24 PbO 55.64 55.30 As2O5 1.33 H2O 3.57 2.23 V2O5 21.21 22.53 insol. 0.17 CuO 17.05 9.86 Total 100.02 100.00 (1) Bisbee, Arizona, USA; average of three analyses. (2) Pb(Cu, Zn)(VO4)(OH) with Zn:Cu = 1:1.