Ore Deposits in Northern Yuma County, Arizona
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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 -
Mineral Resources of the Harquahala Mountains Wilderness Study Area, La Paz and Maricopa Counties, Arizona
2.SOB nH in ntoiOGIGM. JAN 3 1 1989 Mineral Resources of the Harquahala Mountains Wilderness Study Area, La Paz and Maricopa Counties, Arizona U.S. GEOLOGICAL SURVEY BULLETIN 1701-C Chapter C Mineral Resources of the Harquahala Mountains Wilderness Study Area, La Paz and Maricopa Counties, Arizona By ED DE WITT, S.M. RICHARD, J.R. HASSEMER, and W.F. HANNA U.S. Geological Survey J.R. THOMPSON U.S. Bureau of Mines U.S. GEOLOGICAL SURVEY BULLETIN 1701 MINERAL RESOURCES OF WILDERNESS STUDY AREAS- WEST-CENTRAL ARIZONA AND PART OF SAN BERNARDINO COUNTY, CALIFORNIA U. S. GEOLOGICAL SURVEY Dallas L Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE: 1988 For sale by the Books and Open-File Reports Section U.S. Geological Survey Federal Center Box 25425 Denver, CO 80225 Library of Congress Cataloging-in-Publlcatlon Data Mineral resources of the Harquahala Mountains wilderness study area, La Paz and Maricopa counties, Arizona. (Mineral resources of wilderness study areas west-central Arizona and part of San Bernardino County, California ; ch. C) (U.S. Geological Survey bulletin ; 1701-C) Bibliography: p. Supt. of Docs, no.: I 19.3:1701-C 1. Mines and mineral resources Arizona Harquahala Mountains Wilderness. 2. Harquahala Mountains (Ariz.) I. DeWitt, Ed. II. Series. III. Series: U.S. Geological Survey bulletin ; 1701. QE75.B9 no. 1701-C 557.3 s [553'.09791'72] 88-600012 [TN24.A6] STUDIES RELATED TO WILDERNESS Bureau of Land Management Wilderness Study Areas The Federal Land Policy and Management Act (Public Law 94-579, October 21, 1976) requires the U.S. Geological Survey and the U.S. -
Birds of Coniferous Forest on Mount Graham, Arizona
Wilson Bull., 107(4), 1995, pp. 719-723 SHORT COMMUNICATIONS Birds of coniferous forest on Mount Graham, Arizona.-Because of interest in the effect upon the biota of Mount Graham by current development for astronomy, I repeated observations and censuses made there forty years ago. Avifaunal changes have occurred. Unlike my companion study in the Sierra Nevada (Marshall 1988), the losses at Mount Graham of nesting species-all at the lower altitudinal limit of Pinus Zeiophylla chihuahuana and P. ponderosa arizonica-lack an obvious connection to human interference with the environment. Study area.-Mount Graham, in southeastern Arizona, is capped with old growth Engel- mann spruce and alpine fir from 3000 m to the summit at 3267 m. This boreal forest of 8 km* is at its southernmost limits on the North American continent. Descending, one passes through other vegetation zones in sequence: Douglas firs and white firs mixed with spruce, and then mixed with Mexican white pines; south slopes of New Mexican locust and Gambel oak; ponderosa pine with Gambel oak, ponderosa pine mixed with silver-leaf oak; and finally Chihuahua pine with Arizona oak (Martin and Fletcher 1943, Hoffmeister 1956, Marshall 1957, Mohlenbrock 1987). From memory, notes, and photographs I detect no change in vegetation during the forty-year study period. Specifically, the trees at the mapped census area in Wet Canyon (Fig. 1) have not closed ranks about the little openings suitable for those foothill birds that forage among grasses, boulders, manzanitas, and nolinas. The mesic luxuriance of Mount Graham’s vegetation is shown by running streams sup- porting tall groves of maples, by the enormous Douglas firs that remain, by the profusion of understory flowers and green forbs, and by the gigantic stature of clear-trunked alders dominating Wet Canyon. -
Southern Arizona, United States of America
Southern Arizona, United States of America 2 – ASSESSMENT AND RECOMMENDATIONS Assessment and recommendations Southern Arizona region: from a resource-based economy to a knowledge-based economy Southern Arizona is the southern-most part of the state of Arizona in the United States. bordering the Mexican state of Sonora, with a multi-cultural heritage and a major gateway for trade with Mexico. The vast desert region consists of Pima County, Cochise County and Santa Cruz County, and has a population of approximately 1.2 million, accounting for 18% of the state population. The engine of the region’s development is the Tucson metropolitan area, the second largest metropolitan area in the state, just behind the Phoenix metropolitan area. About 23% of the land in Southern Arizona is owned by Native Americans, Tohono O’odham and Pascua Yaqui Nations, who continue to feature low education, labour market and health outcomes. Population growth is a major strength in the region, an opportunity for many industry sectors, but at the same time it poses cultural, economic and political challenges. Since World War II, Arizona has had one of the fastest growing populations in the United States. Between 1990 and 2000, Arizona experienced a 40.0% population increase which slowed down to 26.7% between 2000 and 2008. In Southern Arizona, the corresponding figures were 26.0% and 18.4%. Arizona has the fastest growing Hispanic population in the US, comprising about 25% of the state population and 27% of that of Southern Arizona. In Tucson, 40% of the residents identify themselves as Hispanic, while in Santa Cruz the majority of population are Hispanic. -
Brenda SEZ Analysis: Draft PEIS
1 8 AFFECTED ENVIRONMENT AND IMPACT ASSESSMENT FOR 2 PROPOSED SOLAR ENERGY ZONES IN ARIZONA 3 4 5 8.1 BRENDA 6 7 8 8.1.1 Background and Summary of Impacts 9 10 11 8.1.1.1 General Information 12 13 The proposed Brenda Solar Energy Zone (SEZ) is located in La Paz County in west- 14 central Arizona (Figure 8.1.1.1-1), 32 mi (52 km) east of the California border. The SEZ has a 15 total area of 3,878 acres (16 km2). In 2008, the county population was 20,005, while adjacent 16 Riverside County to the west in California had a population of 2,087,917. The towns of 17 Quartzsite and Salome in La Paz County are about 18 mi (29 km) west of, and 18 mi (29 km) 18 east of, the SEZ respectively. The Phoenix metropolitan area is approximately 100 mi (161 km) 19 to the east of the SEZ, and Los Angeles is approximately 230 mi (370 km) to the west. 20 21 The nearest major road access to the SEZ is via U.S. 60, which runs southwest to 22 northeast, along the southeast border of the Brenda SEZ. The nearest railroad stop is 11 mi 23 (18 km) away. The nearest airports serving the area are the Blythe and Parker (Avi Suquilla) 24 Airports, both approximately 50 mi (80 km) from the SEZ, and neither of which have scheduled 25 commercial passenger service. The Sky Harbor Airport in Phoenix is 125 mi (201 km) to the 26 east, and Yuma International Airport in Yuma is 104 mi (167 km) to the south, of the SEZ. -
The Southern Arizona Guest Ranch As a Symbol of the West
The Southern Arizona guest ranch as a symbol of the West Item Type text; Thesis-Reproduction (electronic) Authors Norris, Frank B. (Frank Blaine), 1950-. 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 07/10/2021 15:00:58 Link to Item http://hdl.handle.net/10150/555065 THE SOUTHERN ARIZONA GUEST RANCH AS A SYMBOL OF THE WEST by Frank Blaine Norris A Thesis Submitted to the Faculty of the DEPARTMENT OF GEOGRAPHY, REGIONAL DEVELOPMENT, AND URBAN PLANNING In Partial Fulfillment of the Requirements For the Degree of MASTER OF ARTS WITH A MAJOR IN GEOGRAPHY In the Graduate College THE UNIVERSITY OF ARIZONA 1 9 7 6 Copyright 1976 Frank Blaine Norris STATEMENT BY AUTHOR This thesis has been submitted in partial fulfill ment of requirements for an advanced degree at The University of Arizona and is deposited in the University Library to be made available to borrowers under rules of the Library. Brief quotations from this thesis are allowable without special permission, provided that accurate acknowl edgment of source is made. Requests for permission for extended quotation from or reproduction of this manuscript in whole or in part may be granted by the copyright holder. SIGNED: APPROVAL BY THESIS DIRECTOR This thesis has been approved on the date shown below: ACKNOWLEDGMENTS This thesis is the collective effort of many, and to each who played a part in its compilation, I am indebted. -
Saddlebrooke Hiking Club Hike Database 11-15-2020 Hike Location Hike Rating Hike Name Hike Description
SaddleBrooke Hiking Club Hike Database 11-15-2020 Hike Location Hike Rating Hike Name Hike Description AZ Trail B Arizona Trail: Alamo Canyon This passage begins at a point west of the White Canyon Wilderness on the Tonto (Passage 17) National Forest boundary about 0.6 miles due east of Ajax Peak. From here the trail heads west and north for about 1.5 miles, eventually dropping into a two- track road and drainage. Follow the drainage north for about 100 feet until it turns left (west) via the rocky drainage and follow this rocky two-track for approximately 150 feet. At this point there is new signage installed leading north (uphill) to a saddle. This is a newly constructed trail which passes through the saddle and leads downhill across a rugged and lush hillside, eventually arriving at FR4. After crossing FR4, the trail continues west and turns north as you work your way toward Picketpost Mountain. The trail will continue north and eventually wraps around to the west side of Picketpost and somewhat paralleling Alamo Canyon drainage until reaching the Picketpost Trailhead. Hike 13.6 miles; trailhead elevations 3471 feet south and 2399 feet north; net elevation change 1371 feet; accumulated gains 1214 northward and 2707 feet southward; RTD __ miles (dirt). AZ Trail A Arizona Trail: Babbitt Ranch This passage begins just east of the Cedar Ranch area where FR 417 and FR (Passage 35) 9008A intersect. From here the route follows a pipeline road north to the Tub Ranch Camp. The route continues towards the corrals (east of the buildings). -
236 Pinaleño Mountains in the Twentieth Century Atalanta Hoyt
Pinaleño Mountains in the Twentieth Century Atalanta Hoyt Throughout the twentieth century, a few major events dominated the history of the Forest Service. First, the founding of the National Forest Service in 1905 replaced the Bureau of Forestry and led to the creation of modern National Forests. The new service was created under the jurisdiction of the Department of Agriculture with the purpose of securing a long term supply of timber for the American people.1 Second, the great depression of the 1930s, Franklin Roosevelt’s creation of the Civilian Conservation Corps (CCC) and the expansion of the Forest Service changed the shape of National Forests.2 This time period featured a major transition from timber management to hands on putting resources into the forest. The Forest Service and CCC planted trees, carved trails, built roads, and conducted research; actively molding forests and applying the latest forestry techniques instead of letting the forest take its course.3 A third period of great change came in the 1970s during the environmental era.4 The emphasis changed from conceptualizing the forests as resources to be converted into marketable goods to seeing them as wilderness in need of preservation. While conservation has always been an important part of the Forest Service - advocated by both those who saw an intrinsic value in wilderness and by those who used the wilderness for recreational purposes - increased urbanization highlighted the uniqueness of forests. Efforts to catalog and protect the environments of forests became a main priority while ecologists and conservationists gained status.5 These three main shifts defined the Forest Service in the twentieth century. -
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. -
Tucson Cactus and Succulent Society Guide to Common Cactus and Succulents of Tucson
Tucson Cactus and Succulent Society Guide to Common Cactus and Succulents of Tucson http://www.tucsoncactus.org/c-s_database/index.html Item ID: 1 Item ID: 2 Family: Cactaceae Family: Cactaceae Genus: Ferocactus Genus: Echinocactus Species: wislizenii Species: grusonii Common Name: Fishhook Barrel Common Name: Golden Barrel Habitat: Various soil types from 1,000 Cactus to 6,000 feet elevation from grasslands Habitat: Located on rolling hills to rocky mountainous areas. and cliffs. Range: Arizona, southwestern New Range: Limited to small areas in Mexico, limited extremes of western Queretaro, Mexico. The popula- Texas, Sonora, northwest Chihuahua tion had become very low in num- and northern Sinaloa, Mexico bers over the years but is just Care: An extremely easy plant to grow now beginning to increase due to in and around the Tucson area. It re- protective laws and the fact that Photo Courtesy of Vonn Watkins quires little attention or special care as this plant is now in mass cultiva- ©1999 it is perfectly at home in almost any tion all over the world. garden setting. It is very tolerant of ex- Photo Courtesy of American Desert Care: The Golden Barrel has slow- Description treme heat as well as cold. Cold hardi- Plants ly become one of the most pur- This popular barrel cactus is noted ness tolerance is at around 10 degrees chased plants for home landscape for the beautiful golden yellow farenheit. Description in Tucson. It is an easy plant to spines that thickly surround the Propagation: Propagation of this cac- This plant is most recognized by the grow and takes no special care. -
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 -
Geochronology, Geology, and Listric Normal Faulting of the Vulture Mountains, Maricopa County, Arizona
Arizona Geological Society Digest, Volume XII, 1980 89 Geochronology, Geology, and Listric Normal Faulting of the Vulture Mountains, Maricopa County, Arizona by WA. Rehrigi, M. Shafiqullah2, and P.E. Damon2 Abstract Geologic mapping and geochronologic studies in the Vulture Mountains near Wickenburg, Arizona, have led to the recognition of a large, northeast-trending batholith of 68.4-m.y. age that intrudes complex gneissic and granitic rocks of probably Precambrian age. Over- lying the denuded crystalline terrane is a sequence of late Oligocene to Miocene ( .'26 to 16 m.y.) volcanic rocks (vitrophyres, ash-flow tuffs, welded tuffs, breccias, agglomerates, and lava flows) that vary locally. Nearby source areas are suggested. A swarm of north- to north-northwest-trending porphyritic dikes intrudes the volcanics and crystalline basement. Overlying this volcanic sequence in angular unconformity is a thin section of basal conglom- erate and basalt lava flows dated at 13.5 m.y. B.P. The older, tuffaceous sequence is generally calc-alkalic but with a high proportion of rhyolites that are exceptionally rich in potassium and silica. These silicic units are peral- kaline or nearly so, and those with K20/Na2O >3 are ultrapotassic. Initial strontium ratios average 0.7081, whereas an initial ratio for the younger basalt sequence is significantly lower at 0.7054. The silicic volcanics have been severely tilted on multiple, low-angle listric normal faults. The youngest basalt flows are relatively flat lying and postdate this deformation. By geo- logic and radiometric criteria, the transition from tilted silicic volcanics to untilted basalts occurred between about 16 and 14 m.y.