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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 .................................................................... -
A's News Clips, Wednesday, November 16, 2011 Whodathunkit
A’s News Clips, Wednesday, November 16, 2011 Whodathunkit? Baseball a paragon of labor stability John Shea, Chronicle Columnist The NFL lockout lasted 136 days. The NBA lockout is in its 139th day. By contrast, baseball's collective bargaining agreement expires Dec. 11, but a new settlement through 2017 is expected soon. That means MLB, which had eight strikes/lockouts from 1972 to 1995, now is envisioning 22 years of labor peace. I asked Bill Gould, emeritus professor at Stanford Law School who was instrumental in ending baseball's 1994-95 strike, why basketball can't figure out, like baseball, how to peacefully divide the wealth. Few know sports labor like Gould, whose new book, "Bargaining With Baseball: Labor Relations in an Age of Prosperous Turmoil" illustrates law's impact on baseball history. He pointed to three differences between the sports. 1. The baseball union has maintained more aggressive stances than the basketball union. "The lack of which in basketball led (Commissioner David) Stern, who's a lawyer, to believe he could push the union around, and he's been right, until now at least," Gould said. "Baseball owners learned they can't push these (players) around." 2. The NBA has more "marginal franchises with economically perilous circumstances" than MLB - including Sacramento, Toronto and Memphis. "I don't think baseball has any teams like that," Gould said. I mentioned the A's, and he called them "an aberration. They seem to be calculating that they can go elsewhere." 3. Race. "Look at who comes to NBA games and who has the money," said Gould, who's African American. -
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 ....................................................................................................................... -
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 -
Minerals in Arizona Through Geologic History
Silver, Lucky Cuss m. Silver, Lucky Cuss m. Gold, Gold Basin, Mohave Co., AZ It’s not all copper! Copper , Bisbee by Jan C. Rasmussen Consulting Geologist Jan C. Rasmussen, Ph.D., R.G. December 8, 2014 www.janrasmussen.com >800 districts/ subdistricts Very rich mineral heritage Copper deposits made only 3 times in AZ geologic history Jan C. Rasmussen, Ph.D., R.G. December 8, 2014 www.janrasmussen.com Mineralization related to mountain building episodes . Precambrian = orogenies added to fringes of continent . Paleozoic = AZ on trailing edge - Eastern orogenies . Mesozoic-Cenozoic = AZ on leading edge = Cordilleran orogeny – many metals . Latest Cenozoic = subduction cutoff by San Andreas transform margin Jan C. Rasmussen, Ph.D., R.G. December 8, 2014 www.janrasmussen.com Orogeny Phase Age (Ma) Alkalinity Resources Mining districts San Francisco volcanic Basin San field, San Carlos & 13-0 Sand, gravel, salt, zeolites, gypsum Andreas M A olivine, Emerald Isle Range exotic Cu Cu-Au-Ag in veins; epithermal Au-Ag Oatman, Mammoth, Late) 18-13 M QA veins Rowley Silver (Red Cloud m.), Middle 28-18 M AC Pb-Zn-Ag F veins, replace.; epithermal Castle Dome, Stanley, Galiuro Aravaipa Early 30-22 M CA Au +/- Cu-W veins & disseminated Little Harquahala, Kofa Earlies Ajo Cornelia, Copper 38-28 - Uranium, clay, exotic copper t Butte (from Ray) Oracle (Wilderness granite), Boriana, Las Late 55-43 P C, CA Au dissem. & qtz veins; W veins, Guijas, Gold Basin, Copperstone Ajo, Ray, Christmas, San Manuel, Mineral large disseminated porphyry Cu Park, Pima, Bagdad, -
City Manager
Office of the City Manager TO: Mayor and Council FROM: Chris Hillman, City Manager DATE: October 11, 2013 SUBJECT: City Manager’s Weekly Items of Interest Fall League The Arizona Fall League season at Surprise Stadium began on October 8th. Due to renovations to the Peoria Sports Complex, Surprise is hosting 2 teams in this season. Both the Surprise Saguaros and the Peoria Javelinas will call Surprise Stadium home. A total of 30 games will be played in Surprise by the end of the season on November 14th. Surprise Stadium will also be hosting the 2013 Fall Stars Game which will take place on November 2nd. Tickets to games are $7 for adults and $6 for seniors and youth. The Arizona Fall League teams are comprised of the top prospects in minor league baseball. Each Major League team sends their top 6 prospects to participate. The Surprise Saguaros are made up of prospects from the Brewers, Indians, Orioles, Rangers, and Red Sox. The Peoria Javelinas are made up of players from the Astros, Mariners, Padres, Phillies, and Royals. Adaptive Recreation CRS will host the Arizona Special Olympics Fall Games for the 9th consecutive year, next Friday and Saturday, October 18th and 19th. The swimming competition will take place at the Surprise Aquatic Center, softball will be held at Surprise Farms and Bocce will take place at DreamCatcher Park. At the completion of competition on Friday, the official Opening Ceremonies will be held in Surprise Stadium starting at 7:00 p.m. The event features the parade of teams, the lighting of the Olympic torch and special guests. -
Desert Botanical Garden Press
DESERT BOTANICAL GARDEN PRESS KIT OVERVIEW THE GARDEN: Discover the tranquil vibrancy of 50,000 desert plants nestled amid the red rocks of the Papago Buttes at Desert Botanical Garden. Visitors can stroll through five thematic trails to explore plants, including towering cactus, alluring succulents and brilliant desert wildflowers. Delve deeper to experience world-class art exhibitions, festive events, fascinating classes and so much more. MISSION: The Garden’s commitment to the community is to advance excellence in education, research, exhibition and conservation of desert plants of the world with emphasis on the Southwestern United States. We will ensure that the Garden is always a compelling attraction that brings to life the many wonders of the desert. LOCATION | WEBSITE: 1201 N. Galvin Parkway, Phoenix, AZ 85008 | dbg.org | 480.941.1225 MEDIA CONTACTS: Dana Terrazas, Director of Marketing Communications Clare Hahne, Marketing Communications Manager 480.481.8101 | [email protected] 480.481.8102 | [email protected] YOUR GARDEN BY THE NUMBERS (Reflective of 2017): 450,578 32,575 122 4,357 379 68,432 80 SPECIES CARED FOR TOTAL ATTENDANCE MEMBERS NEW SPECIES ADDED SPECIES IN THE VOLUNTEER HOURS CELEBRATING GARDEN’S LIVING THAT ARE RARE AND CONTRIBUTED 80 YEARS IN 2019 COLLECTION ENDANGERED DESERT BOTANICAL GARDEN | PRESS KIT | OVERVIEW 1 HISTORY In the 1930s, a small group of passionate local citizens saw the need to conserve the beautiful desert environment. One was Swedish botanist Gustaf Starck, who found like-minded residents by posting a sign that said “Save the desert,” with an arrow pointing to his home. Nearly eight decades later, thanks to leadership and investments from many individuals, Desert Botanical Garden has blossomed from a dream into a living museum unlike any other. -
Geologic Map of the Wickenburg, Southern Buckhorn, and Northwestern Hieroglyphic Mountains, Central Arizona
Geologic Map of the Wickenburg, southern Buckhorn, and northwestern Hieroglyphic Mountains, central Arizona _ by James A. Stimac, Joan E. Fryxell. Stephen J. Reynolds, Stephen M. Richard, Michael J. GrubenskY, and Elizabeth A. Scott Arizona Geological Survey Open-File Report 87-9 October, 1987 Arizona Geological Survey 416 W. Congress, Suite #100, Tucson, Arizona 85701 This report is preliminalY and has not been edited or reviewed for conformity with Arizona Geological Survey standards INTRODUCTION This report describes the geology of the Red Picacho quadrangle and parts of the Wickenburg, Garfias Mountain, and Wittmann quadrangles (Fig. 1). Geologic mapping was completed between January and April of 1987, and was jointly funded by the U.S. Geological Survey and the Arizona Bureau of Geology and Mineral Technology as part of the cost-sharing COGEOMAP program. Mapping was done on 1:24,000-scale topographic maps and on 1:24,000-scale color aerial photographs provided by Raymond A. Brady of the U.S. Bureau of Land Management. GEOLOGIC OVERVIEW The map area includes the Wickenburg Mountains and contiguous parts of the Buckhorn and Hieroglyphic Mountains (Fig. 1). Adjacent parts of the Vulture Mountains were mapped by Grubensky and oth_ers (1987) and adjacent parts of the Hieroglyphic Mountains were mapped by Capps and others (1986). The overall geologic history of the area is complex, but the regional stratigraphy developed in these reports carries well from range to range. The map area is composed of a metamorphic-plutonic basement unconformably overlain by Tertiary volcanic and sedimentary rocks. The oldest rocks, assigned to the Proterozoic (1.8-1.7 b.y.) Yavapai Supergroup, consist of amphibolite, schist, and gneiss, intruded by granite, leucogranite, and pegmatite.