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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______________________ . -
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. -
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. -
The Maricopa County Wildlife Connectivity Assessment: Report on Stakeholder Input January 2012
The Maricopa County Wildlife Connectivity Assessment: Report on Stakeholder Input January 2012 (Photographs: Arizona Game and Fish Department) Arizona Game and Fish Department In partnership with the Arizona Wildlife Linkages Workgroup TABLE OF CONTENTS LIST OF FIGURES ............................................................................................................................ i RECOMMENDED CITATION ........................................................................................................ ii ACKNOWLEDGMENTS ................................................................................................................. ii EXECUTIVE SUMMARY ................................................................................................................ iii DEFINITIONS ................................................................................................................................ iv BACKGROUND ................................................................................................................................ 1 THE MARICOPA COUNTY WILDLIFE CONNECTIVITY ASSESSMENT ................................... 8 HOW TO USE THIS REPORT AND ASSOCIATED GIS DATA ................................................... 10 METHODS ..................................................................................................................................... 12 MASTER LIST OF WILDLIFE LINKAGES AND HABITAT BLOCKSAND BARRIERS ................ 16 REFERENCE MAPS ....................................................................................................................... -
Animated Tectonic Reconstruction of the Lower Colorado River Region: Implications for Late Miocene to Present Deformation Scott E
Animated tectonic reconstruction of the Lower Colorado River region: implications for Late Miocene to Present deformation Scott E. K. Bennett,1 Michael H. Darin,2 Rebecca J. Dorsey,3 Lisa A. Skinner,2 Paul J. Umhoefer,2 and Michael E. Oskin4 1U.S. Geological Survey, 2Northern Arizona University, 3University of Oregon, 4University of California, Davis Introduction of upper crustal structures that accommodated Although the majority of late Miocene to present intracontinental strain and improves our understanding Pacic–North America plate boundary strain has been of the processes that promoted localized or diuse strain accommodated by faults of the San Andreas and Gulf during reorganization of the Pacic–North America of California systems, growing evidence of dextral shear plate boundary. east of the San Andreas Fault indicates that a component Map-view translations of crustal blocks inuence of plate boundary deformation occurred in the lower the relative motions of adjacent blocks, an approach Colorado River (LoCR) region. Large-scale tectonic adhered to in global plate-circuit models (Atwater and reconstructions across the Gulf of California and Salton Stock, 1998; 2013). us, a synthesis of the magnitude Trough (GCAST) region (Fig. 1), a ~500 km-wide and timing of horizontal strain across a broad zone zone of deformation that aected the western margin of distributed deformation can provide insight into of North America, provide important constraints on processes of strain partitioning and potential kinematic the location, timing, style, and magnitude of crustal links between adjacent structural domains. Furthermore, deformation in the LoCR region (Fig. 2). Characterizing it can help prioritize and guide future work by Miocene to present deformation in the LoCR region identifying gaps in our understanding of plate boundary is important to resolve the presence and kinematics deformation and provide a degree of predictability Figure 1. -
Reintroduction of the Tarahumara Frog (Rana Tarahumarae) in Arizona: Lessons Learned
Herpetological Conservation and Biology 15(2):372–389. Submitted: 12 December 2019; Accepted: 11 June 2020; Published: 31 August 2020. REINTRODUCTION OF THE TARAHUMARA FROG (RANA TARAHUMARAE) IN ARIZONA: LESSONS LEARNED JAMES C. RORABAUGH1,8, AUDREY K. OWENS2, ABIGAIL KING3, STEPHEN F. HALE4, STEPHANE POULIN5, MICHAEL J. SREDL6, AND JULIO A. LEMOS-ESPINAL7 1Post Office Box 31, Saint David, Arizona 85630, USA 2Arizona Game and Fish Department, 5000 West Carefree Highway, Phoenix, Arizona 85086, USA 3Jack Creek Preserve Foundation, Post Office Box 3, Ennis, Montana 59716, USA 4EcoPlan Associates, Inc., 3610 North Prince Village Place, Suite 140, Tucson, Arizona 85719, USA 5Arizona-Sonora Desert Museum, 2021 North Kinney Road, Tucson, Arizona 85743, USA 6Arizona Game and Fish Department (retired), 5000 West Carefree Highway, Phoenix, Arizona 85086, USA 7Laboratorio de Ecología, Unidad de Biotecnología y Prototipos, Facultad de Estudios Superiores Iztacala, Avenida De Los Barrios No. 1, Colonia Los Reyes Iztacala, Tlalnepantla, Estado de México 54090, México 8Corresponding author, e-mail: [email protected] Abstract.—The Tarahumara Frog (Rana tarahumarae) disappeared from the northern edge of its range in south- central Arizona, USA, after observed declines and die-offs from 1974 to 1983. Similar declines were noted in Sonora, Mexico; however, the species still persists at many sites in Mexico. Chytridiomycosis was detected during some declines and implicated in others; however, airborne pollutants from copper smelters, predation, competition, and extreme weather may have also been contributing factors. We collected Tarahumara Frogs in Sonora for captive rearing and propagation beginning in 1999, and released frogs to two historical localities in Arizona, including Big Casa Blanca Canyon and vicinity, Santa Rita Mountains, and Sycamore Canyon, Atascosa Mountains. -
Summits on the Air – ARM for the USA (W7A
Summits on the Air – ARM for the U.S.A (W7A - Arizona) Summits on the Air U.S.A. (W7A - Arizona) Association Reference Manual Document Reference S53.1 Issue number 5.0 Date of issue 31-October 2020 Participation start date 01-Aug 2010 Authorized Date: 31-October 2020 Association Manager Pete Scola, WA7JTM Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged. Document S53.1 Page 1 of 15 Summits on the Air – ARM for the U.S.A (W7A - Arizona) TABLE OF CONTENTS CHANGE CONTROL....................................................................................................................................... 3 DISCLAIMER................................................................................................................................................. 4 1 ASSOCIATION REFERENCE DATA ........................................................................................................... 5 1.1 Program Derivation ...................................................................................................................................................................................... 6 1.2 General Information ..................................................................................................................................................................................... 6 1.3 Final Ascent -
Central Arizona Salinity Study --- Phase I
CENTRAL ARIZONA SALINITY STUDY --- PHASE I Technical Appendix D HYDROLOGIC REPORT ON THE GILA BEND BASIN Prepared for: United States Department of Interior Bureau of Reclamation Prepared by: Brown and Caldwell 201 East Washington Street, Suite 500 Phoenix, Arizona 85004 D-1 TABLE OF CONTENTS PAGE TABLE OF CONTENTS ................................................................................................................ 2 LIST OF TABLES .......................................................................................................................... 3 LIST OF FIGURES ........................................................................................................................ 3 1.0 INTRODUCTION .............................................................................................................. 4 2.0 PHYSICAL SETTING ....................................................................................................... 5 3.0 GENERALIZED GEOLOGY ............................................................................................ 6 3.1 BEDROCK GEOLOGY ......................................................................................... 6 3.2 BASIN GEOLOGY ................................................................................................ 6 4.0 HYDROGEOLOGIC CONDITIONS ................................................................................ 8 4.1 GROUNDWATER OCCURRENCE AND MOVEMENT ................................... 8 4.2 GROUNDWATER QUALITY ............................................................................. -
Federal Register/Vol. 76, No. 87/Thursday, May 5, 2011/Rules
Federal Register / Vol. 76, No. 87 / Thursday, May 5, 2011 / Rules and Regulations 25593 DEPARTMENT OF THE INTERIOR Service’s Arizona Ecological Services or result in the destruction or adverse Office at 2321 W. Royal Palm Road, modification of designated critical Fish and Wildlife Service Suite 103, Phoenix, AZ 85021. habitat. Section 7 of the Act does not FOR FURTHER INFORMATION CONTACT: affect activities undertaken on private or 50 CFR Part 17 Steve Spangle, Field Supervisor, other non-Federal land unless they are [Docket No. FWS–R2–ES–2009–0077; Arizona Ecological Services Office, 2321 authorized, funded, or carried out by a 92220–1113–0000; ABC Code: C3] W. Royal Palm Road, Suite 103, Federal agency. Phoenix, AZ 85021 (telephone 602– Under section 10(j) of the Act, the RIN 1018–AW63 242–0210, facsimile 602–242–2513). If Secretary of the Department of the Interior can reestablish populations Endangered and Threatened Wildlife you use a telecommunications device for the deaf (TDD), call the Federal outside the species’ current range and and Plants; Establishment of a designate them as ‘‘experimental.’’ With Nonessential Experimental Population Information Relay Service (FIRS) at 800–877–8339. the experimental population of Sonoran Pronghorn in designation, the relevant population is Southwestern Arizona SUPPLEMENTARY INFORMATION: treated as threatened for purposes of AGENCY: Fish and Wildlife Service, Background section 9 of the Act, regardless of the species’ designation elsewhere in its Interior. It is our intent to discuss only those ACTION: Final rule. range. Threatened designation allows us topics directly relevant to this final rule discretion in devising management establishing a Sonoran pronghorn SUMMARY: We, the U.S. -
Of Our Favorite Things
TALON AGENTS: THE MAJESTIC ARTIST ROBERT SHIELDS: AUGUST 1909: WILDLIFE ECOLOGY BIRDS OF CAVE CREEK CANYON NOPE. HE’S NOT ALL MIME IS BORN IN THE WHITE MOUNTAINS AUGUST 2009 ESCAPE. EXPLORE. EXPERIENCE BEST ofAZ of our favorite things 100featuring BRANDON WEBB & ROGER CLYNE plus DIERKS BENTLEY: The Coolest Dude in Country Music and A Pulitzer Winner and a Camera Went Into the Catalinas … contents 08.09 features 14 BEST OF AZ Our first-ever guide to the best of everything in Arizona, from eco-friendly accommodations to secret hide- aways and margaritas. The latter, by the way, come courtesy of Roger Clyne, the Tempe-based rock star. Cy Young Award-winner Brandon Webb pitched in on this piece as well, and so did NFL referee Ed Hochuli. Grand Canyon Some of the choices you’ll agree with. Others, prob - National Park ably not. Either way, this is our take on the “Best of Flagstaff Arizona.” EDITED BY KELLY KRAMER Sedona Springerville 36 A PULITZER WINNER AND A Camp Verde Globe CAMERA WENT INTO THE CATALINAS ... PHOENIX It sounds like a joke, doesn’t it? It’s not. We just wrote departments that to get your attention. When it comes to photography, 2 EDITOR’S LETTER 3 CONTRIBUTORS 4 LETTERS TO THE EDITOR Santa Catalina Jack Dykinga is dead serious. That’s why he has a Pulitzer Mountains sitting on his mantel. Or maybe it’s shoved in a drawer — 5 THE JOURNAL www.arizonahighways.com People, places and things from around the state, that’s more Jack’s style. -
Orocopia Schist in the Northern Plomosa Mountains, West-Central Arizona: a Laramide Subduction Complex Exhumed in a Miocene Metamorphic Core Complex
RESEARCH Orocopia Schist in the northern Plomosa Mountains, west-central Arizona: A Laramide subduction complex exhumed in a Miocene metamorphic core complex E.D. Strickland1, J.S. Singleton1, and G.B. Haxel2,3 1DEPARTMENT OF GEOSCIENCES, COLORADO STATE UNIVERSITY, FORT COLLINS, COLORADO 80523, USA 2U.S. GEOLOGICAL SURVEY, FLAGSTAFF, ARIZONA 86001, USA 3GEOLOGY PROGRAM, SCHOOL OF EARTH SCIENCES AND ENVIRONMENTAL SUSTAINABILITY, NORTHERN ARIZONA UNIVERSITY, FLAGSTAFF, ARIZONA 86011, USA ABSTRACT We document field relationships, petrography, and geochemistry of a newly identified exposure of Orocopia Schist, a Laramide subduction complex, in the northern Plomosa Mountains metamorphic core complex of west-central Arizona (USA). This core complex is character- ized by pervasive mylonitic fabrics associated with early Miocene intrusions. The quartzofeldspathic Orocopia Schist records top-to-the-NE mylonitization throughout its entire ~2–3 km structural thickness and 10 km2 of exposure in the footwall of the top-to-the-NE Plomosa detachment fault. The schist of the northern Plomosa Mountains locally contains graphitic plagioclase poikiloblasts and scattered coarse- grained actinolitite pods, both of which are characteristic of the Orocopia and related schists. Actinolitite pods are high in Mg, Ni, and Cr, and are interpreted as metasomatized peridotite—an association observed in Orocopia Schist at nearby Cemetery Ridge. A 3.5-km-long unit of amphibolite with minor interlayered ferromanganiferous quartzite is localized along a SE-dipping contact between the Orocopia Schist and gneiss. Based on their lithologic and geochemical characteristics, we interpret the amphibolite and quartzite as metabasalt and meta chert, respectively. The top of the Orocopia Schist is only ~3–4 km below a ca.