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Journal of Arizona History Index, M
Index to the Journal of Arizona History, M Arizona Historical Society, [email protected] 480-387-5355 NOTE: the index includes two citation formats. The format for Volumes 1-5 is: volume (issue): page number(s) The format for Volumes 6 -54 is: volume: page number(s) M McAdams, Cliff, book by, reviewed 26:242 McAdoo, Ellen W. 43:225 McAdoo, W. C. 18:194 McAdoo, William 36:52; 39:225; 43:225 McAhren, Ben 19:353 McAlister, M. J. 26:430 McAllester, David E., book coedited by, reviewed 20:144-46 McAllester, David P., book coedited by, reviewed 45:120 McAllister, James P. 49:4-6 McAllister, R. Burnell 43:51 McAllister, R. S. 43:47 McAllister, S. W. 8:171 n. 2 McAlpine, Tom 10:190 McAndrew, John “Boots”, photo of 36:288 McAnich, Fred, book reviewed by 49:74-75 books reviewed by 43:95-97 1 Index to the Journal of Arizona History, M Arizona Historical Society, [email protected] 480-387-5355 McArtan, Neill, develops Pastime Park 31:20-22 death of 31:36-37 photo of 31:21 McArthur, Arthur 10:20 McArthur, Charles H. 21:171-72, 178; 33:277 photos 21:177, 180 McArthur, Douglas 38:278 McArthur, Lorraine (daughter), photo of 34:428 McArthur, Lorraine (mother), photo of 34:428 McArthur, Louise, photo of 34:428 McArthur, Perry 43:349 McArthur, Warren, photo of 34:428 McArthur, Warren, Jr. 33:276 article by and about 21:171-88 photos 21:174-75, 177, 180, 187 McAuley, (Mother Superior) Mary Catherine 39:264, 265, 285 McAuley, Skeet, book by, reviewed 31:438 McAuliffe, Helen W. -
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 -
U-Pb Geochronologic Data from Zircons from Eleven Granitic Rocks in Central and Western Arizona
U-Pb geochronologic data from zircons from eleven granitic rocks in central and western Arizona 1 3 Clark E. Isachsenl, George E. Gehrels , Nancy R. Riggs , 2 2 Jon E. Spence~, Charles A. Ferguson , Steve J. Skotnicki , Stephen M. Richard2 Arizona Geological Survey Open-File Report 99-5 1999 Arizona Geological Survey 416 W. Congress, Suite #100, Tucson, Arizona 85701 Jointly funded by the Arizona Geological Survey and the U.S. Geological Survey STATEMAP Program. Cooperative Agreement #1434-HQ-96-AG-O 1474. Author Affiliations: 1. Dept. of Geosciences, University of Arizona, Tucson 2. Arizona Geological Survey, Tucson 3. Dept. of Geology, Northern Arizona University, Flagstaff This report Is preliminary and has not been edited or reviewed for confonnity with Arlzona Geological Survey standards U-Pb GEOCHRONOLOGIC DATA FROM ZIRCONS FROM ELEVEN GRANITIC ROCKS IN CENTRAL AND WESTERN ARIZONA INTRODUCTION The U-Pb data described in this report were produced to determine the ages of granitic rocks in Arizona and the timing of metamorphic and deformational events. Two developments emerge from the data reported here that are especially significant. Two granites, one from the Mazatzal Mountains east of Phoenix and one from the Santan Mountains southeast of Phoenix, yielded dates between 1630 and 1640 Ma. This is unusually young for early Proterozoic granites in Arizona, although two granites in the Maricopa Mountains southwest of Phoenix have yielded similar dates (Eisele and Isachsen, in review; Joe Wooden, written communication, 1998). Possi bly, these dated granites are part of a belt of similar-age granites that roughly occupy the boundary between Pi nal Schist on the southeast and metavolcanic and metasedimentary rocks of the Tonto Basin Supergroup to the northwest (Conway and Silver, 1989; Reynolds and Dewitt, 1991). -
Peak List Please Send Updates Or Corrections to Lat/Lon to Mike Heaton
Operation On Target Arizona Peak List Please send updates or corrections to Lat/Lon to Mike Heaton Description Comment Latitude Longitude Elevation "A" Mountain (Tempe) ASU campus by Sun Devil Stadium 33.42801 -111.93565 1495 AAA Temp Temp Location 33.42234 -111.8227 1244 Agassiz Peak @ Snow Bowl Tram Stop (No access to peak) 35.32587 -111.67795 12353 Al Fulton Point 1 Near where SR260 tops the Rim 34.29558 -110.8956 7513 Al Fulton Point 2 Near where SR260 tops the rim 34.29558 -110.8956 7513 Alta Mesa Peak For Alta Mesa Sign-up 33.905 -111.40933 7128 Apache Maid Mountain South of Stoneman Lake - Hike/Drive? 34.72588 -111.55128 7305 Apache Peak, Whetstone Mountain Tallest Peak, Whetstone Mountain 31.824583 -110.429517 7711 Aspen Canyon Point Rim W. of Kehl Springs Point 34.422204 -111.337874 7600 Aztec Peak Sierra Ancha Mountains South of Young 33.8123 -110.90541 7692 Battleship Mountain High Point visible above the Flat Iron 33.43936 -111.44836 5024 Big Pine Flat South of Four Peaks on County Line 33.74931 -111.37304 6040 Black (Chocolate) Mountain, CA Drive up and park, near Yuma 33.055 -114.82833 2119 Black Butte, CA East of Palm Springs - Hike 33.56167 -115.345 4458 Black Mountain North of Oracle 32.77899 -110.96319 5586 Black Rock Mountain South of St. George 36.77305 -113.80802 7373 Blue Jay Ridge North end of Mount Graham 32.75872 -110.03344 8033 Blue Vista White Mtns. S. of Hannagan Medow 33.56667 -109.35 8000 Browns Peak (Four Peaks) North Peak of Four Peaks Range 33.68567 -111.32633 7650 Brunckow Hill NE of Sierra Vista, AZ 31.61736 -110.15788 4470 Bryce Mountain Northwest of Safford 33.02012 -109.67232 7298 Buckeye Mountain North of Globe 33.4262 -110.75763 4693 Burnt Point On the Rim East of Milk Ranch Point 34.40895 -111.20478 7758 Camelback Mountain North Phoenix Mountain - Hike 33.51463 -111.96164 2703 Carol Spring Mountain North of Globe East of Highway 77 33.66064 -110.56151 6629 Carr Peak S. -
Structural Evolution of the Mcdowell Mountains Maricopa County
Structural Evolution of the McDowell Mountains Maricopa County, Arizona by Brad Vance A Thesis Presented in Partial Fulfillment of the Requirements for the Degree Master of Science Approved November 2012 by the Graduate Supervisory Committee: Stephen Reynolds, Chair Steven Semken Edmund Stump ARIZONA STATE UNIVERSITY December 2012 ABSTRACT The accretion of juvenile island-arc lithosphere by convergent tectonism during the Paleoproterozoic, in conjunction with felsic volcanism, resulted in the assembly, ductile to partial brittle deformation, uplift, and northwest-directed thrusting of rocks in the McDowell Mountains region and adjacent areas in the Mazatzal Orogenic belt. Utilizing lithologic characteristics and petrographic analysis of the Proterozoic bedrock, a correlation to the Alder series was established, revising the stratigraphic sequences described by earlier works. The central fold belt, composed of an open, asymmetric syncline and an overturned, isoclinal anticline, is cut by an axial-plane parallel reactivated thrust zone that is intruded by a deformed Paleoproterozoic mafic dike. Finite strain analyses of fold geometries, shear fabrics, foliations, fold vergence, and strained clasts point to Paleoproterozoic northwest-directed thrusting associated with the Mazatzal orogen at approximately 1650 million years ago. Previous studies constrained the regional P-T conditions to at least the upper andalusite-kyanite boundary at peak metamorphic conditions, which ranged from 4-6 kilobars and 350-450⁰ Celsius, although the plasticity of deformation in a large anticlinal core suggests that this represents the low end of the P-T conditions. Subsequent to deformation, the rocks were intruded by several granitoid plutons, likely of Mesoproterozoic age (1300-1400 Ma). A detailed analysis of Proterozoic strain solidly places the structure of the McDowell Mountains within the confines of the Mazatzal Orogeny, pending any contradictory geochronological data. -
Goldfield Area Plan (PDF)
ACKNOWLEDGEMENTS AREAGOLDFIELD PLAN 2020 Eye To The Future DECEMBER, 2007 MARICOPA COUNTY, ARIZONA GOLDFIELD AREA PLAN i ACKNOWLEDGEMENTS This page intentionally left blank. ii GOLDFIELD AREA PLAN ACKNOWLEDGEMENTS ACKNOWLEDGEMENTS Preparation of the Goldfield Area Plan was made possible through the cooperative efforts of many public and private stakeholders. Maricopa County extends its appreciation to all those that participated in the process, including the Maricopa County Board of Supervisors, Planning and Zoning Commission, citizens, property owners, Indian communities, cities, towns, state and federal agencies, and other stakeholders. Board of Supervisors • Fulton Brock, Chairman (District 1) • Don Stapley, (District 2) • Andrew Kunasek, (District 3) • Max W. Wilson, (District 4) • Mary Rose Wilcox, (District 5) Planning and Zoning Commission • Mark Pugmire (District 1) • Jerry Brooks (District 1) • Russell Bowers (District 2) • Jason Barney, (District 2) • Jerry Aster (District 3) • Dick Smith, Chairman (District 3) • Robert L. Jones (District 4) • Ella Makula (District 4) • Jimmie Munoz (District 5) • Murray Johnson (District 5) Comprehensive Planning Team Planning and Development Department • Joy Rich, AICP, Director • Darren Gerard, AICP, Deputy Director • Matthew Holm, AICP, Principal Planner • John Verdugo, AICP, Senior Planner • Andy Piper, Planner • Brian McCabe, Planner • Jeff Clawson, Planner • Jose Macias, Planner • Leo Donahue, GIS Analyst GOLDFIELD AREA PLAN iii ACKNOWLEDGEMENTS Flood Control District of Maricopa County -
COPPER OXIDE RESOURCES Open-File Report 92-10 July, 1992
COPPER OXIDE RESOURCES Open-file Report 92-10 July, 1992 by Nyal J. Niemuth and Ken A. Phillips Arizona Department of Mines and Mineral Resourses 1502 West Washington Phoenix, Arizona 85007 This is a preliminary report, silbject to technical and editorial revision. TABLE OF CONTENTS Introduction . 1 Arizona Copper Deposits 1 Figure 1. Map showing copper oxide resources in Arizona 2 Figures 2-4. Maps showing the distribution of Arizona's principal copper-producing metallic mineral districts for the following deposit types: Figure 2. Porphyry copper . .. 3 Figure 3. Stratabound volcanogenic massive sulfide .. 3 Figure 4. Stratabound copper, veins, and replacement ....... 3 Table 1. Arizona copper oxide deposits Cochise County . 4 Coconino County 6 Gila County . 7 Graham County . 7 Greenlee County 8 La Paz County . 8 Maricopa County 9 Mohave County 10 Navajo County 11 Pima County. 11 Pinal County. 13 Santa Cruz County 16 Yavapai County 16 Yuma County . 18 Commodity Abbreviations AU - gold F - flourine AG - silver FE - iron CU - copper PB - lead BA - barium U - uranium SI - silicon V - vanadium W - tungsten HG - mercury MN - manganese MCA-mica STN - stone ASB - asbestos ZN - zinc MO - molybdenum COPPER OXIDE RESOURCES Open File Report 92-10 July, 1992 by Nyal J. Niemuth and Ken. A. Phillips Exploration and mining companies are showing renewed interest in Arizona copper deposits. Strong copper prices, averaging more than $l.(X)/pound since the late 1980's, are the primary reasonfor the increased activity. Another factor is the widespread recognition ofthe advantages of the solvent extraction-electrowinning process (SX-EW). Copper oxide deposits, and certain sUlfide deposits, are amenable to treatment by heap ,leaching and SX-Ew. -
Region 9 Tribal Underground Storage Tank Sites
AltFacilityID TankID TankStatusDesc SubstanceDesc OverfillInstalled SpillInstalled AGUA001 1 Permanently Out of Use Used Oil FALSE FALSE AGUA002 1 Permanently Out of Use Gasoline FALSE FALSE AGUA002 2 Permanently Out of Use Diesel FALSE FALSE AGUA002 3 Permanently Out of Use Gasoline FALSE FALSE AGUA002 4 Permanently Out of Use Used Oil FALSE FALSE AGUA003 1 Permanently Out of Use Used Oil FALSE FALSE AGUA003 2 Permanently Out of Use Gasoline FALSE TRUE AGUA004 1 Currently In Use Gasoline TRUE TRUE AGUA004 2 Currently In Use Gasoline TRUE TRUE AGUA004 3 Currently In Use Gasoline TRUE TRUE AGUA004 4 Currently In Use Diesel TRUE TRUE AGUA005 1 Permanently Out of Use Gasoline FALSE FALSE AGUA005 2 Permanently Out of Use Diesel FALSE FALSE AGUA006 1 Permanently Out of Use Used Oil TRUE TRUE AGUA006 2 Permanently Out of Use Gasoline TRUE TRUE AGUA006 3 Permanently Out of Use Gasoline TRUE TRUE AGUA006 4 Permanently Out of Use Gasoline TRUE TRUE AGUA007 1 Permanently Out of Use Diesel FALSE FALSE AGUA008 1 Permanently Out of Use Gasoline TRUE TRUE AGUA008 2 Permanently Out of Use Diesel TRUE TRUE AGUA009 1 Permanently Out of Use Gasoline FALSE FALSE AGUA010 1 Currently In Use Used Oil TRUE TRUE AGUA010 2 Currently In Use Gasoline TRUE TRUE AGUA010 3 Currently In Use Gasoline TRUE TRUE AGUA010 4 Currently In Use Gasoline TRUE TRUE AGUA010 5 Currently In Use Gasoline TRUE TRUE AGUA011 1 Permanently Out of Use Diesel TRUE TRUE AGUA011 2 Currently In Use Diesel TRUE TRUE AGUA012 1 Permanently Out of Use Diesel FALSE FALSE AGUA012 2 Permanently -
4Great Hikes
Our Bark Beetle, a Tiny Bug with a Tree-killing Instinct arizonahighways.com OCT0BER 2004 great hikes Arizona Trail 4Snake Gulch Garden Canyon PLUS Hike of the Month {also inside} OCTOBER 2004 46 DESTINATION Pueblo Grande Museum and Archaeological Park The Hohokam people had a way with water — in fact, their canal technology still amazes us. 42 BACK ROAD ADVENTURE SPECIAL FALL HIKING FEATURES Outlaws hid out and Indians battled the Army Into the Woods and Canyons in and around Mount Ord in central Arizona. When somebody in Arizona tells you to “go take a hike,” 48 HIKE OF THE MONTH say “Amen, let’s go!” In this issue, we feature a rugged Hikers and fly fishermen share the pleasure trail north of the Grand Canyon, a lush path through the along Thompson Trail in the White Mountains. Huachuca Mountains near Sierra Vista and the soon-to- Snake be-completed mother of all our wild footpaths — the Gulch 2 LETTERS & E-MAIL Arizona Trail, from the Utah to Mexico borders. Also see our regular department, “Hike of the Month,” which 3 TAKING THE Grand Canyon Arizona Trail takes you to the Thompson Trail in eastern Arizona. National Park OFF-RAMP Thompson Trail Explore Arizona Mt. Ord 14 North to South — oddities, PHOENIX attractions Pueblo Grande Museum the Arizona Trail and Archaeological Park When a writer and some friends tackle parts and pleasures. of the meandering route bisecting the state, 40 HUMOR TUCSON Garden they find it full of lessons — including why we Canyon should preserve our scenic lands. POINTS OF INTEREST FEATURED IN THIS ISSUE 6 A Paradise for Hikers {more stories online} in Garden Canyon at arizonahighways.com Indians and U.S. -
Geologic Map of the Fountain Hills
GEOLOGIC MAP OF. THE FOUNTAIN HILLS I MOUNT McDOWELL AREA, MARICOPA COUNTY, ARIZONA by Steven J. Skotnicki Arizona Geological Survey Open-File Report 95-16 October, 1995 Arizona Geological Survey 416 W. Congress, Suite #100, Tucson, Arizona 85701 Includes 28 page text and 1:24,000 scale geologic map Partially funded by the Arizona Geological Survey and the U.S. Geological Survey STATEMAP Program Contract #1434-94-A-2222 This report is preliminary and has not been edited or reviewed for conformity with Arizona Geological Survey standards Introduction Most of central Arizona is covered with basin sediments composed largely of unconsolidated sands and gravels. These deposits are important to planners, engineers, and geologists as they are the reservoir for vast amounts of groundwater, the source of important industrial materials, and the physical matrix that supports roads and buildings for most of Arizona's inhabitants. In addition, the bedrock geology of this area is complex and interesting, and hosts potentially economic mineral resources. Expanding population and burgeoning development in the Greater Phoenix metropolitan area requires more information regarding its geological resources and the spatial distribution of geologic hazards such as flooding that are common to basin environments. The Arizona Geological Survey is conducting a systematic geologic mapping program in the Mesa 1 :250,000 quadrangle, which includes the eastern half of the Phoenix area. This report presents the results of geologic mapping of the Fountain Hills and Mt. McDowell areas in the eastern part of the metropolitan Phoenix area (Figure 1). Field work was carried out from June through September, 1995. -
W D Qal Qtc Qls Qycr Qyc Qyr Qy3r Qy2r Qy1r Qi3r Qi2r Qi1r
Geologic map of the southwestern part of the Tonto National Forest, Gila, Maricopa, Pinal and Yavapai Counties, Arizona Authors Richard, S.M. Citation Richard, S.M. (compiler), 2015, Geologic map of the southwestern part of the Tonto National Forest, Gila, Maricopa, Pinal and Yavapai Counties, Arizona. Arizona Geological Survey Digital Geologic Map, DGM-76 & DI-41, map scale 1:130,000. Rights Arizona Geological Survey. All rights reserved. Download date 29/09/2021 14:36:53 Link to Item http://hdl.handle.net/10150/630066 Map Unit Explanation Legend: Map Units for Tonto National Forest Geology w Water Water d Disturbed ground (recent) Heavily disturbed ground due to agriculture, extensive excavation, or construction of earth dams Quaternary sedimentary deposits Typically non marine clastic sedimentary rocks deposited in late Pliocene to Quaternary time, in depositional systems reflected in the modern geomorphology Qal Alluvium Sand and gravel deposits along valley and canyon floors Qtc Colluvium and talus (Holocene) Unconsolidated to weakly consolidated, very poorly sorted angular rock debris on hill slopes Qls Landslides Landslides and other mass-movement or rock-avalanche deposits River alluvium Sandy and gravelly deposits of major streams, characterized by rounded cobbles and mixing of rock types from many sources Qycr Modern river channel deposits (< 100 yr) Unconsolidated, rounded to subangular, moderately sorted to poorly sorted, clast-supported sand, cobbles, and small boulders. Low terraces typically covered by sand and silt. Minimal carbonate accumulation. Little vegetation in channels, bars and terraces may have abundant riparian vegetation Qyc Active piedmont channel alluvium Unconsolidated, very poorly sorted sandy to cobble-like ephemeral piedmont channel deposits Qyr Holocene river terrace deposits (0 to 10 ka) Equivalent to the Lehi Terrace of Pewe (1978). -
INFORMATION to USERS the Most Advanced Technology Has Been Used to Photo Graph and Reproduce This Manuscript from the Microfilm Master
Pre-development hydrologic conditions of the Salt River Indian Reservation, East Salt River Valley, central Arizona, with an emphasis on the groundwater flow regime Item Type text; Thesis-Reproduction (electronic) Authors Porcello, John Joseph, 1963- 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 05/10/2021 08:42:28 Link to Item http://hdl.handle.net/10150/277174 INFORMATION TO USERS The most advanced technology has been used to photo graph and reproduce this manuscript from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are re produced by sectioning the original, beginning at the upper left-hand corner and continuing from left to right in equal sections with small overlaps.