Minerals in Arizona Through Geologic History
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CENTRAL ARIZONA SALINITY STUDY --- PHASE I Technical Appendix C HYDROLOGIC REPORT on the PHOENIX
CENTRAL ARIZONA SALINITY STUDY --- PHASE I Technical Appendix C HYDROLOGIC REPORT ON THE PHOENIX AMA Prepared for: United States Department of Interior Bureau of Reclamation Prepared by: Brown and Caldwell 201 East Washington Street, Suite 500 Phoenix, Arizona 85004 Brown and Caldwell Project No. 23481.001 C-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 ................................................................................ 9 4.1 GROUNDWATER OCCURRENCE .................................................................... -
Alteration of Spodumene, Montebrasite and Lithiophilite In
American Mineralogist, Volume 67, pages 97-113, 1982 Alteration of spodumene,montebrasite and lithiophilite in pegmatites of the White PicachoDistrict, Arizona Davrp Lor.rooxrnNo DoNer-uM. Bunr Department of Geology Arizona State University Tempe, Arizona 85281 Abstract The crystallization sequence and metasomatic alteration of spodumene (LiAlSizOe), montebrasite(LiAIPO4(OH,F)), and lithiophilite (Li(Mn,Fe)PO+)are describedfor nine zoned lithium pegmatitesin the White Picacho district, Arizona. The observedcrystalliza- tion trends suggesta progressiveincrease in the activities of lithium species(spodumene follows microcline as the principal alkali aluminosilicate), as well as an increase in the activities of the acidic volatiles phosphorus and fluorine (montebrasite succeedsspodu- mene as the stableprimary lithium phase).Much of the lithiophilite occurs with columbite, apatite, beryl, zircon, and tourmaline in cleavelanditecomplexes that formed in part at the expenseof quartz-spodumenepegmatite. Fracture-controlledpseudomorphic alteration of the primary lithium minerals is widespread and apparently is the result of subsolidus reactionswith residualpegmatitic fluids. Spodumenehas been replacedby eucryptite, albite, and micas. Alteration products of montebrasite include low-fluorine secondary montebrasite,crandallite (tentative), hydroxylapatite, muscovite, brazilianite, augelite (tentative),scorzalite, kulanite, wyllieite, and carbonate-apatite.Secondary phases identi- fied in altered lithiophilite include hureaulite, triploidite, eosphorite, -
Arizona 'Highways
Sc:~r1ic: VOL. XXXIII NO. 3 MARCH 1957 RAYMOND CARLSON, Editor U. S. Highway 89, Arizona's main artery of north GFORGE M. AV EY, Art Editor south trayel, is one of the most scenic of all 0~1r roads. Its JAJ\LCS E. STEVENS, Business Manager some 600 miles through the state offer a Yarietv of eleva LEGEND tion, terrain and scenic interest. Each mile unfoldi1we:, be- "89" ENT ERl'-'G HousEROCK VALLEY FRONT COVER fore the traveler is an interesting mile and different from ~ . R .,, y MANLEY'S PHOTOGRAPH SHOWS the one preceding. "89" brings :--·ou into the state at GLORIOUS NORTHERN ARIZONA VISTA. Fredonia. It leaves the state at Nogales. As eYen the most ARIZONA S CRAPBOOK . 2 S:-.:11PSHOTS OF SCEN IC INTEREST casual glance at a map ·will reveal, "89'' cuts right through ALO ~G "89," BORDER TO BORD ER . the heart of Arizona and covers a lot of interesting· coun PIPE SPRI NG NATIONAL MoNUJVIENT 4 try between Utah and J\1e.\'ico. The Strip, the cool J(aibab, \VF. PAY A VISIT TO HISTORIC the s,1 ·eeping panorama of Houserock Valley, Vermilion SHR INE GLORIFYING OUR PIONEERS. and Echo Cliffs, the lofty forested reg·ion ~f San Fran IO \VE TAKE A TRIP ON A HIGHWAY cisco Peaks, the high pla~eau countr:v ~bet\\·een vVillia1m OF INTE RNAT IONAL GRANDEUR. and Prescott, or by Alternate "89" Oak Creek and the OLD BrLL WrLLTAJVrs' FAVORITE MouNTAIN 34 Verde Va llev, the desert and then the historic Santa Cruz D ESC RIPTIO N OF A MOUNTAIN THAT Vallev- all of these and more, too, make up the travel JS LA NDM ARK IN NORTHERN ARIZONA. -
Arizona Wulfenite 2009 3 12
Geologic Settings of Wulfenite in Arizona by Jan C. Rasmussen Curator, Arizona Mining and Mineral Museum and Stanley B. Keith, MagmaChem Exploration March 21, 2009 Arizona is famous for its spectacular wulfenite specimens. The butterscotch-colored, bladed crystals from the Glove Mine in the Santa Rita Mountains south of Tucson and the bright red, chunky blades from the Red Cloud Mine in the Silver district north of Yuma are prized highlights of many mineral collections. Most of these famous mineral localities are no longer available to collectors, making the historic specimens even more valuable. Outline Figure 1. Wulfenite from the Glove mine, Santa Rita Alkali-calcic Pb-Zn-Ag Mountains Laramide (75-65 Ma) Glove, Tyndall, Turquoise, Empire dist. Wulfenite is lead molybdate, PbMoO4. It forms Mid-Tertiary (30-20 Ma) in the oxidized zones of lead deposits where the Hilltop, Tonopah, Hull, Red Cloud white needle-like crystals of cerussite (PbCO3) (Silver dist.), Ripsey, Grand Reef, Purple have developed. Surprisingly, the presence of Passion mines molybdenite is not required. Wulfenite rarely Quartz Alkalic Au-base metal occurs in the same mineral deposits as Jurassic (180-160 Ma) molybdenite, and then only in the later stages of Bisbee the deposits. Even there, wulfenite does not Laramide (75-70 Ma) occur unless cerussite or mimetite is present. Old Yuma There had to be enough lead in the system in a Mid-Tertiary (28-22 Ma) relatively soluble mineral to allow the Tiger, Rowley molybdenum in the ground water to combine Calc-alkalic porphyry copper stage 4 with lead and oxygen as wulfenite. -
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 ....................................................................................................................... -
Maricopa County Regional Trail System Plan
Maricopa County Regional Trail System Plan Adopted August 16, 2004 Maricopa Trail Maricopa County Trail Commission Maricopa County Department of Transportation Maricopa County Parks and Recreation Maricopa County Planning and Development Flood Control District of Maricopa County We have an obligation to protect open spaces for future generations. Maricopa County Regional Trail System Plan VISION Our vision is to connect the majestic open spaces of the Maricopa County Regional Parks with a nonmotorized trail system. The Maricopa Trail Maricopa County Regional Trail System Plan - page 1 Credits Maricopa County Board of Supervisors Andrew Kunasek, District 3, Chairman Fulton Brock, District 1 Don Stapley, District 2 Max Wilson, District 4 Mary Rose Wilcox, District 5 Maricopa County Trail Commission Supervisor Max Wilson, District 4 Chairman Supervisor Andrew Kunasek, District 3 Parks Commission Members: Citizen Members: Laurel Arndt, Chair Art Wirtz, District 2 Randy Virden, Vice-Chair Jim Burke, District 3 Felipe Zubia, District 5 Stakeholders: Carol Erwin, Bureau of Reclamation (BOR) Fred Pfeifer, Arizona Public Service (APS) James Duncan, Salt River Project (SRP) Teri Raml, Bureau of Land Management (BLM) Ex-officio Members: William Scalzo, Chief Community Services Officer Pictured from left to right Laurel Arndt, Supervisor Andy Kunasek, Fred Pfeifer, Carol Erwin, Arizona’s Official State Historian, Marshall Trimble, and Art Wirtz pose with the commemorative branded trail marker Mike Ellegood, Director, Public Works at the Maricopa Trail -
Ore Deposits of the Jerome and Bradshaw Mountains Quadrangles, Arizona
DEPARTMENT OF THE INTERIOR Hubert Work, Secretary U. S. GEOLOGICAL SURVEY George Otis Smith, Director Bulletin 782 ORE DEPOSITS OF THE JEROME AND BRADSHAW MOUNTAINS QUADRANGLES, ARIZONA BY WALDEMAR LINDGREN WITH STATISTICAL NOTES BY V. C. HEIKES WASHINGTON GOVERNMENT PRINTING OFFICE 1926 CONTENTS Page Introduction - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - 1 History of mining - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - -2 Production - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - 5 Mining districts near area here described - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - 6 General geology - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - -7 Physiography - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - -7 Paleozoic sediments - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - 9 Pre-Paleozoic peneplain - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - 10 Relation of the plateau province to the mountain region - - - - - - - - - - - - - - - - - - - - - 10 Post-Paleozoic erosion - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - 13 Volcanic flows - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - -
~Ui&£R5itt! of J\Rij!Oua
Minerals and metals of increasing interest, rare and radioactive minerals Authors Moore, R.T. Rights Arizona Geological Survey. All rights reserved. Download date 06/10/2021 17:57:35 Link to Item http://hdl.handle.net/10150/629904 Vol. XXIV, No.4 October, 1953 ~ui&£r5itt! of J\rij!oua ~ul1etiu ARIZONA BUREAU OF MINES MINERALS AND METALS OF INCREASING INTEREST RARE AND RADIOACTIVE MINERALS By RICHARD T. MOORE ARIZONA BUREAU OF MINES MINERAL TECHNOLOGY SERIES No. 47 BULLETIN No. 163 THIRTY CENTS (Free to Residents of Arizona) PUBLISHED BY ~tti£ll~r5itt! of ~rh!Omt TUCSON, ARIZONA TABLE OF CONTENTS INTRODUCTION 5 Acknowledgments 5 General Features 5 BERYLLIUM 7 General Features 7 Beryllium Minerals 7 Beryl 7 Phenacite 8 Gadolinite 8 Helvite 8 Occurrence 8 Prices and Possible Buyers ,........................................ 8 LITHIUM 9 General Features 9 Lithium Minerals 9 Amblygonite 9 Spodumene 10 Lepidolite 10 Triphylite 10 Zinnwaldite 10 Occurrence 10 Prices and Possible Buyers 10 CESIUM AND RUBIDIUM 11 General Features 11 Cesium and Rubidium Minerals 11 Pollucite ..................•.........................................................................., 11 Occurrence 12 Prices and Producers 12 TITANIUM 12 General Features 12 Titanium Minerals 13 Rutile 13 Ilmenite 13 Sphene 13 Occurrence 13 Prices and Buyers 14 GALLIUM, GERMANIUM, INDIUM, AND THALLIUM 14 General Features 14 Gallium, Germanium, Indium and Thallium Minerals 15 Germanite 15 Lorandite 15 Hutchinsonite : 15 Vrbaite 15 Occurrence 15 Prices and Producers ~ 16 RHENIUM 16 -
Geologic Map of the Northeastern Hieroglyphic Mountains, Central Ariz Ora
GEOLOGIC MAP OF THE NORTHEASTERN HIEROGLYPHIC MOUNTAINS, CENTRAL ARIZ ORA by Richard C. Capps, Stephen J. Reynolds, Curtis P. Kortemeier, and Elizabeth A. Scott Arizona Geological Survey Open-File Report 86·10 August 1986 Arizona Geological Survey 416 W. Congress, Suite #100, Tucson, Arizona 85701 Jointly funded by the Arizona Bureau o/Geology and Mineral Technology and the U.S. Geological Survey Cooperative Geologic Mapping Program (COGEOMAP) Contract No. 14-08-0001-A0378 Principal Investigators: Stephen J. Reynolds and lArry D. Fellows This report is preliminary and has not been edited or reviewed for conformity with Arizona Geological Survey standards INTROOOCTION This report presents a preliminary 1:24,OOO-scale geologic map of the northeastern Hieroglyphic Mountains in central Arizona. The mapping, completed between January and June, 1986, was jOintly funded by the U. S. Geological Survey and the Arizona Bureau of Geology and Mineral Technology as part of the cost-sharing, Cooperative Geologic Mapping Program (COGEOMAP). The aim of COGEOMAP is to produce high-quality geologic maps for areas that have been inadequately mapped and that have high mineral resource or natural hazard potential. The mapping was done on 1:24,OOO-scale topographic maps and on 1:24,000- scale color aerial photographs provided by Raymond A. Brady, U. S. Bureau of Land Management, Phoenix. GEOLOGIC OVERV][EW The Hieroglyphic Mountains are composed of a metamorphic-plutonic basement that is overlain by middle Tertiary volcanic and sedimentary rocks. The oldest rocks in the range are Proterozoic schist, gneiss, metasedimentary and metavolcanic rocks, and several generations of plutonic rocks. -
1 POST-MINERAL NORMAL FAULTING in ARIZONA PORPHYRY SYSTEMS by Phillip A. Nickerson a Dissertation Submitted To
1 POST-MINERAL NORMAL FAULTING IN ARIZONA PORPHYRY SYSTEMS By Phillip A. Nickerson _________________ A Dissertation Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements For the Degree of DOCTOR OF PHILOSOPHY In the Graduate College THE UNIVERSITY OF ARIZONA 2012 2 THE UNIVERSITY OF ARIZONA GRADUATE COLLEGE As members of the Dissertation Committee, we certify that we have read the dissertation prepared by Phillip A. Nickerson entitled Post-Mineral Normal Faulting in Arizona Porphyry Systems and recommend that it be accepted as fulfilling the dissertation requirement for the Degree of Doctor of Philosophy _______________________________________________________________________ Date: 04/30/2012 Eric Seedorff _______________________________________________________________________ Date: 04/30/2012 Mark Barton _______________________________________________________________________ Date: 04/30/2012 George Davis _______________________________________________________________________ Date: 04/30/2012 Peter Reiners _______________________________________________________________________ Date: 04/30/2012 Charles Ferguson Final approval and acceptance of this dissertation is contingent upon the candidate’s submission of the final copies of the dissertation to the Graduate College. I hereby certify that I have read this dissertation prepared under my direction and recommend that it be accepted as fulfilling the dissertation requirement. ________________________________________________ Date: 04/30/2012 -
General Monitoring and Discovery Plan for the City of Phoenix, Maricopa County, Arizona
General Monitoring and Discovery Plan for the City of Phoenix, Maricopa County, Arizona Prepared for City of Phoenix City Archaeology Office Parks and Recreation Department Pueblo Grande Museum 4619 E. Washington Street Phoenix, Arizona 85034 Pueblo Grande Museum Project No. 2017-009 Project Report No. 19-120 Desert Archaeology, Inc. Prepared by: T. Kathleen Henderson Submitted by: Patricia Castalia Desert Archaeology, Inc. 3975 N. Tucson Boulevard Tucson, Arizona 85716 July 31, 2020 ABSTRACT Report Title: General Monitoring and Discovery Plan for the City of Phoenix, Maricopa County, Arizona Project Name: General Monitoring and Discovery Plan Update Project Location: Phoenix, Maricopa County, Arizona Project Sponsor: City of Phoenix Sponsor Project Number(s): None (Pueblo Grande Museum No. 2017-009) Lead Agency: City of Phoenix Other Involved Agencies: Arizona State Historic Preservation Office; Arizona State Museum Applicable Regulations: City of Phoenix Historic Preservation Ordinance (Zoning Ordinance Chapter 8); Arizona Antiquities Act (ARS §41-841 et seq.); Arizona state burial laws (ARS §41-844 and ARS §41-865) Funding Source: City Description of the Project/Undertaking: Provide an updated general monitoring and discovery plan for the city of Phoenix Project Area/Area of Potential Effects (APE): Lands inside the boundary of the city of Phoenix and city-owned facilities that lie outside this boundary; acreage to be established by individual projects conducted under this updated plan Legal Description: To be established by individual -
A HISTORY of WELLIAMS, ARIZONA 1876-1951 James R. Fuchs A
A history of Williams, Arizona, 1876-1951 Item Type text; Thesis-Reproduction (electronic); maps Authors Fuchs, James R. Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 09/10/2021 06:46:33 Link to Item http://hdl.handle.net/10150/551188 A HISTORY OF WELLIAMS, ARIZONA 1876-1951 James R. Fuchs A Thesis submitted to the faculty of the Department of History in partial fulfillment of the requirements for the degree of MASTER OF ARTS in the Graduate College, University of Arizona 1952 3 - % TAB IE OF CONTENTS Page LIST OF ILLUSTRATIONS.......................... ill TABLE OF MAPS.................................. lv INTRODUCTION .................................. v Chapter I. NORTHERN ARIZONA, 1540-1870.............. 1 II. PIONEERS IN THE WILLIAMS AREA, 1869-1881 . 25 III. CHARLES T. ROGERS AND THE WILLIAMS TOWNSITE................................. 38 IV. FORMATIVE YEARS, 1881-1890 .............. 56 V. GROWING PAINS, 1891-1900 ................ 104 VI. COMING OF AGE, 1901-1910.................. 154 VII. ERA OF CIVIC IMPROVEMENT, 1911-1930. 206 VIII. RECENT PROGRESS, 1931-1951.............. 259 IX. GATEWAY TO THE GRAND CANYON(CONCLUSION) . 296 APPENDICES......................................... 304 BIBLIOGRAPHY....................................... 312 22321S LIST OF ILLUSTRATIONS Follows Page 1 1.-.' John Clark............ .......................... 28 Charles Thomas Rogers, 1827-1905. 58 Gurley Street- Prescott, Showing Rogers' Market . 40 Frank Lansing'Rogers in 1876. ., . ..... 45 Williams in 1882 (Looking West) . 55- First Bridge in Johnson Canyon, At Simms Tunnel . 58 Completed Bridge in Johnson Canyon.