Dripping Springs Parcel, Gila and Pinal Counties, Arizona
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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______________________ . -
United States Department of the Interior U.S
United States Department of the Interior U.S. Fish and Wildlife Service 2321 West Royal Palm Road, Suite 103 Phoenix, Arizona 85021-4951 Telephone: (602) 242-0210 FAX: (602) 242-2513 In Reply Refer To: AESO/SE 22410-2007-F-0196 January 29, 2009 Memorandum To: Field Manager, Yuma Field Office, Bureau of Land Management, Yuma, Arizona From: Field Supervisor Subject: Biological Opinion for the Yuma Field Office Resource Management Plan Thank you for your request for formal consultation with the U.S. Fish and Wildlife Service (FWS) pursuant to section 7 of the Endangered Species Act of 1973 (16 U.S.C. 1531-1544), as amended (Act). Your request for formal consultation regarding effects of the Bureau of Land Management (BLM) Yuma Field Office Resource Management Plan (RMP) was dated November 26, 2007, and received by us on November 27, 2007. At issue are impacts that may result from the RMP on the following federally-listed species: • razorback sucker (Xyrauchen texanus) and its critical habitat; • desert tortoise – Mohave Desert population (Gopherus agassizii); • Yuma clapper rail (Rallus longirostris yumanensis); and, • southwestern willow flycatcher (Empidonax traillii extimus). We concur with your effects determination of “may affect, not likely to adversely affect” for the Sonoran pronghorn (Antilocapra americanus sonoriensis). Our rationale is presented in Appendix A. The November 26, 2007, memorandum also requested concurrence regarding your determination that implementation of the proposed action may affect, but is not likely to contribute to the need to list the candidate western yellow-billed cuckoo (Coccyzus americanus). Other than the applicable conservation measures included in the proposed action (Appendix B), this species is not addressed in this biological opinion (BO). -
Grand-Canyon-South-Rim-Map.Pdf
North Rim (see enlargement above) KAIBAB PLATEAU Point Imperial KAIBAB PLATEAU 8803ft Grama Point 2683 m Dragon Head North Rim Bright Angel Vista Encantada Point Sublime 7770 ft Point 7459 ft Tiyo Point Widforss Point Visitor Center 8480ft Confucius Temple 2368m 7900 ft 2585 m 2274 m 7766 ft Grand Canyon Lodge 7081 ft Shiva Temple 2367 m 2403 m Obi Point Chuar Butte Buddha Temple 6394ft Colorado River 2159 m 7570 ft 7928 ft Cape Solitude Little 2308m 7204 ft 2417 m Francois Matthes Point WALHALLA PLATEAU 1949m HINDU 2196 m 8020 ft 6144ft 2445 m 1873m AMPHITHEATER N Cape Final Temple of Osiris YO Temple of Ra Isis Temple N 7916ft From 6637 ft CA Temple Butte 6078 ft 7014 ft L 2413 m Lake 1853 m 2023 m 2138 m Hillers Butte GE Walhalla Overlook 5308ft Powell T N Brahma Temple 7998ft Jupiter Temple 1618m ri 5885 ft A ni T 7851ft Thor Temple ty H 2438 m 7081ft GR 1794 m G 2302 m 6741 ft ANIT I 2158 m E C R Cape Royal PALISADES OF GO r B Zoroaster Temple 2055m RG e k 7865 ft E Tower of Set e ee 7129 ft Venus Temple THE DESERT To k r C 2398 m 6257ft Lake 6026 ft Cheops Pyramid l 2173 m N Pha e Freya Castle Espejo Butte g O 1907 m Mead 1837m 5399 ft nto n m A Y t 7299 ft 1646m C N reek gh Sumner Butte Wotans Throne 2225m Apollo Temple i A Br OTTOMAN 5156 ft C 7633 ft 1572 m AMPHITHEATER 2327 m 2546 ft R E Cocopa Point 768 m T Angels Vishnu Temple Comanche Point M S Co TONTO PLATFOR 6800 ft Phantom Ranch Gate 7829 ft 7073ft lor 2073 m A ado O 2386 m 2156m R Yuma Point Riv Hopi ek er O e 6646 ft Z r Pima Mohave Point Maricopa C Krishna Shrine T -
Index 1 INDEX
Index 1 INDEX A Blue Spring 76, 106, 110, 115 Bluff Spring Trail 184 Adeii Eechii Cliffs 124 Blythe 198 Agate House 140 Blythe Intaglios 199 Agathla Peak 256 Bonita Canyon Drive 221 Agua Fria Nat'l Monument 175 Booger Canyon 194 Ajo 203 Boundary Butte 299 Ajo Mountain Loop 204 Box Canyon 132 Alamo Canyon 205 Box (The) 51 Alamo Lake SP 201 Boyce-Thompson Arboretum 190 Alstrom Point 266, 302 Boynton Canyon 149, 161 Anasazi Bridge 73 Boy Scout Canyon 197 Anasazi Canyon 302 Bright Angel Canyon 25, 51 Anderson Dam 216 Bright Angel Point 15, 25 Angels Window 27 Bright Angel Trail 42, 46, 49, 61, 80, 90 Antelope Canyon 280, 297 Brins Mesa 160 Antelope House 231 Brins Mesa Trail 161 Antelope Point Marina 294, 297 Broken Arrow Trail 155 Apache Junction 184 Buck Farm Canyon 73 Apache Lake 187 Buck Farm Overlook 34, 73, 103 Apache-Sitgreaves Nat'l Forest 167 Buckskin Gulch Confluence 275 Apache Trail 187, 188 Buenos Aires Nat'l Wildlife Refuge 226 Aravaipa Canyon 192 Bulldog Cliffs 186 Aravaipa East trailhead 193 Bullfrog Marina 302 Arch Rock 366 Bull Pen 170 Arizona Canyon Hot Springs 197 Bush Head Canyon 278 Arizona-Sonora Desert Museum 216 Arizona Trail 167 C Artist's Point 250 Aspen Forest Overlook 257 Cabeza Prieta 206 Atlatl Rock 366 Cactus Forest Drive 218 Call of the Canyon 158 B Calloway Trail 171, 203 Cameron Visitor Center 114 Baboquivari Peak 226 Camp Verde 170 Baby Bell Rock 157 Canada Goose Drive 198 Baby Rocks 256 Canyon del Muerto 231 Badger Creek 72 Canyon X 290 Bajada Loop Drive 216 Cape Final 28 Bar-10-Ranch 19 Cape Royal 27 Barrio -
I2628 Pamphlet
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP I–2628 U.S. GEOLOGICAL SURVEY Version 1.0 GEOLOGIC MAP OF THE LITTLEFIELD 30' × 60' QUADRANGLE, MOHAVE COUNTY, NORTHWESTERN ARIZONA By George H. Billingsley and Jeremiah B. Workman INTRODUCTION 10 km north of the north-central part of the map and are the largest settlements near the map area. This map is one result of the U.S. Geological Survey’s Interstate Highway 15 and U.S. Highway 91 provide intent to provide geologic map coverage and a better under- access to the northwest corner of the map area, and Arizona standing of the transition in regional geology between the State Highway 389 provides access to the northeast corner. Basin and Range and Colorado Plateaus in southeastern Ne- Access to the rest of the map area is by dirt roads maintained vada, southwestern Utah, and northwestern Arizona. Infor- by the U.S. Bureau of Land Management, Arizona Strip Dis- mation gained from this regional study provides a better trict, St. George, Utah. The area is largely managed by the understanding of the tectonic and magmatic evolution of an U.S. Bureau of Land Management, the Arizona Strip Dis- area of extreme contrasts in late Mesozoic-early Tertiary trict, which includes sections of land controlled by the State compression, Cenozoic magmatism, and Cenozoic extension. of Arizona. There are several isolated sections of privately This map is a synthesis of 32 new geologic maps encom- owned lands, mainly near the communities of Littlefield, passing the Littlefield 30' x 60' quadrangle, Arizona. Geo- Beaver Dam, and Colorado City. -
Grand Canyon
ALT ALT To 389 To 389 To Jacob Lake, 89 To 89 K and South Rim a n a b Unpaved roads are impassable when wet. C Road closed r KAIBAB NATIONAL FOREST e in winter e K k L EA O N R O O B K NY O A E U C C N T E N C 67 I A H M N UT E Y SO N K O O A N House Rock Y N N A Buffalo Ranch B A KANAB PLATEAU C C E A L To St. George, Utah N B Y Kaibab Lodge R Mount Trumbull O A N KAIBAB M 8028ft De Motte C 2447m (USFS) O er GR C o Riv AN T PLATEAU K HUNDRED AND FIFTY MIL lorad ITE ap S NAVAJO E Co N eat C A s C Y RR C N O OW ree S k M INDIAN GRAND CANYON NATIONAL PARK B T Steamboat U Great Thumb Point Mountain C RESERVATION K 6749ft 7422ft U GREAT THUMB 2057m 2262m P Chikapanagi Point MESA C North Rim A 5889ft E N G Entrance Station 1795m M Y 1880ft FOSSIL R 8824ft O Mount Sinyala O U 573m G A k TUCKUP N 5434ft BAY Stanton Point e 2690m V re POINT 1656m 6311ft E U C SB T A C k 1924m I E e C N AT A e The Dome POINT A PL N r o L Y Holy Grail l 5486ft R EL Point Imperial C o Tuweep G W O Temple r 1672m PO N Nankoweap a p d H E o wea Mesa A L nko o V a Mooney D m N 6242ft A ID Mount Emma S Falls u 1903m U M n 7698ft i Havasu Falls h 2346m k TOROWEAP er C Navajo Falls GORGE S e v A Vista e i ITE r Kwagunt R VALLEY R N N Supai Falls A Encantada C iv o Y R nt Butte W d u e a O G g lor Supai 2159ft Unpaved roads are North Rim wa 6377ft r o N K h C Reservations required. -
Michael Kenney Paleozoic Stratigraphy of the Grand Canyon
Michael Kenney Paleozoic Stratigraphy of the Grand Canyon The Paleozoic Era spans about 250 Myrs of Earth History from 541 Ma to 254 Ma (Figure 1). Within Grand Canyon National Park, there is a fragmented record of this time, which has undergone little to no deformation. These still relatively flat-lying, stratified layers, have been the focus of over 100 years of geologic studies. Much of what we know today began with the work of famed naturalist and geologist, Edwin Mckee (Beus and Middleton, 2003). His work, in addition to those before and after, have led to a greater understanding of sedimentation processes, fossil preservation, the evolution of life, and the drastic changes to Earth’s climate during the Paleozoic. This paper seeks to summarize, generally, the Paleozoic strata, the environments in which they were deposited, and the sources from which the sediments were derived. Tapeats Sandstone (~525 Ma – 515 Ma) The Tapeats Sandstone is a buff colored, quartz-rich sandstone and conglomerate, deposited unconformably on the Grand Canyon Supergroup and Vishnu metamorphic basement (Middleton and Elliott, 2003). Thickness varies from ~100 m to ~350 m depending on the paleotopography of the basement rocks upon which the sandstone was deposited. The base of the unit contains the highest abundance of conglomerates. Cobbles and pebbles sourced from the underlying basement rocks are common in the basal unit. Grain size and bed thickness thins upwards (Middleton and Elliott, 2003). Common sedimentary structures include planar and trough cross-bedding, which both decrease in thickness up-sequence. Fossils are rare but within the upper part of the sequence, body fossils date to the early Cambrian (Middleton and Elliott, 2003). -
Akimel O'odham
Akimel O’odham - Pee Posh OUR COMMUNITY OUR FUTURE Governor Lieutenant Governor William Rhodes Jennifer Allison-Ray ANew Direction CONTENTS www.gric.nsn.us | FALL 2007 4 Community Profi le 13 Tribal Government + Executive Offi ce 5 History + Legislative Offi ce + Judicial Offi ce + Pre-History + Early Contact 16 Community Portfolio + 19th and 20th Centuries 9 Water Settlement 17 Tribal Enterprises 10 Tribal Culture 23 Tribal Community 27 Tribal Districts View of Sacaton Mountains from Olberg Gila River farms - District 2, Blackwater Bridge District 2 A MESSAGE FROM THE GOVERNOR We welcome you to experience the rug- ged, awe-inspiring vistas of the South- west and the rich heritage of the Akimel O’odham (Pima) and Pee-Posh (Mari- copa). Historically, the strength of our culture has been the community spirit, industriousness, and maintaining our traditions and languages. Today, we con- tinue to face the challenge of preserving these core values while also meeting the demands of a rapidly changing world. Throughout Gila River’s history, our tribe has made innumerable contribu- tions and will continue to play an inte- gral role in the decades ahead. Governor William R. Rhodes 5 COMMUNITYFACTSHEET COMMUNITY PROFILE The Gila River Indian Community is located on 372,000 acres in south-central Arizona, south of Phoenix, Tempe, and Chandler. The reservation was established by an act of Congress in 1859. The Tribal administrative offi ces and departments are located in Sacaton, and serve residents throughout the seven community districts. The Gila River casinos are both owned and managed by the Gila River Indian Com- munity. -
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 -
Pinal County, Arizona
Profile: Pinal County, Arizona Pinal County was formed from portions of Maricopa and Pima counties on Feb. 1, 1875, in response to the petition of residents of the upper Gila River Valley, as "Act #1" of the Eighth Territorial Legislature. Florence, established in 1866, was designated and has remained the county seat. The county encompasses 5,374 square miles, of which 4.5 are water. In both economy and geography, Pinal County has two distinct regions. The eastern portion is characterized by mountains with elevations to 6,000 feet and copper mining. The western area is primarily low desert valleys and irrigatedagriculture. The communities of Mammoth, Oracle, San Manuel, and Kearny have traditionally been active in copper mining, smelting, milling and refining. Arizona City, Eloy, Maricopa, Picacho, Red Rock and Stanfield have agriculture based-economies. Apache Junction, Arizona City, Coolidge, Eloy, and particularly Casa Grande have diversified their economic base to include manufacturing, trade and services. This expansion and diversification has been facilitated by their location in the major growth corridor between Phoenix and Tucson near the junction of I-10 and I-8, except for Apache Junction, which is to the east of burgeoning Mesa. Most of the southern ¾ of Pinal County and a small area in Apache Junction are designated as Enterprise Zones. The county is home to many interesting attractions, including the Old West Highway 60, Casa Grande Ruins National Monument, Picacho Peak State Park, Picacho Reservoir, Boyce Thompson Southwestern Arboretum, Oracle State Park and Columbia University’s Biosphere II, McFarland State Park, Lost Dutchman State Park, Skydive Arizona, the world’s largest skydiving drop-zone, and the Florence Historical District, with 120 buildings on the National Register. -
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 - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - -
Issues Concerning Phreatophyte Clearing, Revegetation, and Water Savings Along the Gila River, Arizona William L
University of South Carolina Scholar Commons Faculty Publications Geography, Department of 4-1-1984 Issues Concerning Phreatophyte Clearing, Revegetation, and Water Savings Along the Gila River, Arizona William L. Graf University of South Carolina - Columbia, [email protected] Duncan T. Patten Bonnie Turner Follow this and additional works at: http://scholarcommons.sc.edu/geog_facpub Part of the Geography Commons Publication Info 1984, pages Cover-69. This Paper is brought to you for free and open access by the Geography, Department of at Scholar Commons. It has been accepted for inclusion in Faculty Publications by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. ISSUES CONCERNING PHREATOPHYTE CLEARING, REVEGETATION, AND WATER-SAVINGS ALONG THE GILA RIVER, ARIZONA W.... LGraf Duncan T. Patten Bonnie Turner Submitted by the Forum In partial fu1fliiment of U. S.. Army Corps of Engineer. Contract DACW09-83-M-2823 April 1984 -------- ISSUES CONCERNING PHREATOPHYTE CLEARING, REVEGETATION, AND WATER SAVINGS ALONG THE GILA RIVER, ARIZONA William L. Graf Department of Geography Duncan T. Patten Center for Environmental Studies Bonnie Turner Center for Environmental Studies Arizona State University Tempe, Arizona 85287 A report submitted in partial fulfillment of U.S. Army Corps of Engineers Contract DACW09-83-M-2623. April 1984 EXECUTIVE SUMMARY A detailed analysis of the published results of the U. S. Geological Survey Phreatophyte Project conducted in the area of interest for the Corps of Engineers Camelsback Dam study provides the following results. It appears that the figure of 18.53 inches per year for water savings from phreatophyte clearing along the Gila River in southeast Arizona should not be used for predicting potential water salvage because of large sampling errors, measurement errors, and the inherent variability of the natural processes of evapotranspiration.