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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 .................................................................... -
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 -
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. -
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) . -
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 ....................................................................................................................... -
Arizona Public Service Sun Valley to Morgan 500/230 Kilovolt
TABLE OF CONTENTS CHAPTER 3 AFFECTED ENVIRONMENT ................................................................. 3-1 3.1 Introduction ......................................................................................................... 3-1 3.1.1 General Setting of Project Area .............................................................. 3-1 3.1.2 Resource Values and Uses Brought Forward for Analysis ..................... 3-1 3.1.3 Analysis Area ......................................................................................... 3-2 3.2 Air Quality and Climate Change ......................................................................... 3-2 3.2.1 Laws, Ordinances, Regulations, and Standards ..................................... 3-3 3.2.1.1 State and Local Air Quality Regulations ................................. 3-3 3.2.1.2 Federal Rules ......................................................................... 3-5 3.2.2 Study Area .............................................................................................. 3-7 3.2.3 Study Area Overview .............................................................................. 3-8 3.2.4 Existing Air and Climate Quality ............................................................. 3-8 3.2.4.1 National Ambient Air Quality Standards ................................. 3-8 3.2.4.2 Clean Air Act Attainment Status ........................................... 3-11 3.2.5 Climate Change .................................................................................... 3-12 3.2.5.1 -
Geologic Mapping in the Hieroglyphic and Wickenburg Mountains in Yavapai and Maricopa Counties; Partial Support Was Provided by the U.S
I .. Annual Report '- Arizona Geological Survey * ,-- I I L Fiscal Year 1986 - 1987 (July 1, 1986-June 30, 1987) ARIZONA GEOLOGICAL SURVEY OPEN·FILE REPORT 1I..- 87-13 , Cover Illustration: earth fissures formed in response L to ground-water withdrawal near Chandler Heights; artwork by Peter F. Corrao. L * The Arizona Geological Survey is the Geological Survey Branch of the Bureau of Geology and Mineral Technology, a Division of the University of Arizona, Tucson. This report is preliminary and has not been edited or reviewed for conformity with Arizona Geological Survey standards Highlights • Provided information or assistance to more than 3,200 persons who visited the office, telephoned, or wrote; sold publications totalling $19,431. • Completed 36 geologic maps and reports; presented 9 technical papers and talks and gave 10 non-technical talks; conducted or participated in 5 workshops or field trips. • Published map showing land subsidence and earth-fissure zones; project was done cooperatively with the u.s. Geological Survey, U.S. Bureau of Reclamation, and the Arizona Departments of Water Resources and Transportation. • Assisted Pima County Health Department in investigating potential indoor radon occurrences in southwestern Tucson by determining location and natural radioactivity levels of a uranium-bearing limestone. • Assisted Arizona Radiation Regulatory Agency in planning a statewide indoor radon survey by providing information about the distribution of rocks that contain elevated uranium content. • Assisted State Land Department in minerals ownership exchanges by assessing potential for mineral resources in specified areas. Published bibliographies of metallic mineral districts • for Yuma, La Paz, Mohave, Pima, and Santa Cruz Counties. • Completed detailed geologic mapping in the Hieroglyphic and Wickenburg Mountains in Yavapai and Maricopa Counties; partial support was provided by the U.S. -
Appendix / Attachment 1A
ATTACHMENT 1A (Supplemental Documentation to the: Mogollon Rim Water Resource, Management Study Report of Findings) Geology and Structural Controls of Groundwater, Mogollon Rim Water Resources Management Study by Gaeaorama, Inc., July, 2006 GEOLOGY AND STRUCTURAL CONTROLS OF GROUNDWATER, MOGOLLON RIM WATER RESOURCES MANAGEMENT STUDY Prepared for the Bureau of Reclamation GÆAORAMA, INC. Blanding, Utah DRAFT FOR REVIEW 22 July 2006 CONTENTS page Executive Summary…………………………………………………………………………….. 1 MRWRMS ii 1/18/11 Introduction……………………………………………………………………………………... 2 GIS database……………………………………………………………………………………. 5 Faults and fault systems………………………………………………………………………… 6 Proterozoic faults…………………………………………………………………………… 6 Re-activated Proterozoic faults……………………………………………………………... 6 Post-Paleozoic faults of likely Proterozoic inheritance…………………………………….. 7 Tertiary fault systems……………………………………………………………………….. 8 Verde graben system……………………………………………………………………. 8 East- to northeast-trending system……………………………………………………… 9 North-trending system…………………………………………………………………...9 Regional disposition of Paleozoic strata………………………………………………………. 10 Mogollon Rim Formation – distribution and implications……………………………………..10 Relation of springs to faults…………………………………………………………………… 11 Fossil Springs……………………………………………………………………………… 13 Tonto Bridge Spring………………………………………………………………………..14 Webber Spring and Flowing Spring………………………………………………………..15 Cold Spring………………………………………………………………………………... 16 Fossil Canyon-Strawberry-Pine area…………………………………………………………...17 Speculations on aquifer systems………………………………………………………………. -
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 -
Incorporated Municipality Highpoints Compiled by Scott
Maricopa County (AZ) Incorporated Municipality Highpoints Compiled by Scott Surgent, Initial draft: December 4, 2012. There are 24 incorporated towns and cities (municipalities) within Maricopa County. The highpoints of each municipality was determined by referencing http://www.citypopulation.de/php/usa-arizona.php , which shows the boundary of each municipality in detail, then referencing the topographical maps at www.mytopo.com , and carefully matching the boundaries from both sources together. The highpoint is within (or on) the boundaries, and excludes any higher ground within unincorporated county enclaves. Some municipality highpoints have a strong “permanency” since the boundaries are unlikely to grow, or impossible if the municipality is locked in by surrounding municipalities. On the other hand, some municipal boundaries may grow and absorb higher land. A note regarding each municipality highpoint is given at the end. Latitude and longitude coordinates are derived from mytopo.com. Avondale: Unnamed Peak 3,650+ feet, Estrella Mountains Regional Park, N33.294114, W112.32197. Buckeye: Unnamed Peak 3,671 feet, south of White Tank Mountains Regional Park boundary near “Tower Road”, N33.544232, W112.55086. Carefree: Black Mountain 3,398 feet, N33.815126, W111.94119 Cave Creek: Elephant Mountain 3,926 feet, Spur Cross Ranch Conservation Area, N33.895877, W111.98233 Chandler: Spot elevation 1,293 feet, Northwest corner of Val Vista Drive and Hunt Highway at southeast corner of city, N33.204713, W111.75527. El Mirage: Spot elevation 1,168 feet, Southeast corner of Dysart and Greenway Roads, northwest corner of city, N33.623470, W112.34196. Fountain Hills: Inferred elevation 3,180+ feet (20-ft intervals), on southeast ridge of Peak 3804 in the McDowell Mountains, on Fountain Hills-Scottsdale city limits, N33.627723, W111.78733. -
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.