Database of the Uranium Mines, Prospects, Occurrences and Mills In
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Map 3.1 Travel Management Plan
TOADLENA SHEEP SPRINGS GREAT BENDTHE PILLAR 3 NW THE PILLAR 3 NE TANNER LAKE PRETTY ROCKPUEBLO BONITO NW B836108 B636108 B536108 B436108 KIMBETO LYBROOK NW LYBROOK COUNSELORTANCOSA WINDMILL B336108 B236108 B136108 FIVE LAKES CANYON NEREGINA GALLINA ARROYA DEL AGUAYOUNGSVILLE CANONES ABIQUIU Y 134 B836107 B736107 B636107 B536107 B436107 MEDANALES LYDEN VELARDE TRAMPAS PENASCO TRES RITOS CERRO VISTA CHACON W B336107 B136107 B836106 B736106 B636106 B536106 E H B436106 B336106 B236106 B136106 B836105 B736105 B636105 B536105 B436105 B336105 T TOADLENA FIVE LAKES CANYON NW U STA 8 S 6 SONSELA BUTTES B236107 CRYSTAL WASHINGTON PASS S H Y A136109 NASCHITTI CHACO CANYON T W W A836108 THE PILLAR 3 SW A H A736108 THE PILLAR 3 SE Y E A636108 LA VIDA MISSION T T E A436108 PUEBLO BONITO HW 8 A A336108 FIRE ROCK WELL Y 44 ABIQUIU 4 TAOS GREY HILL SPRING T A236108 A836107 LYBROOK SE MULE DAM DEER MESA A636107 TAYLOR RANCH CUBA S A536108 KIN KLIZHIN RUINS A536107 A436107 A336107 NACIMIENTO PEAK JAROSA POLVADERA PEAK SARGENT RANCH A236107 A836106 VALLECITOS CHILI SAN JUAN PUEBLO CHIMAYO TRUCHAS EL VALLE JICARITA PEAK HOLMAN A136108 A736106 A636106 A436106 COMANCHE PEAK A736107 ARROYO CHIJUILLITA A336106 A236106 A136106 A836105 A736105 A636105 A536105 A436105 S A336105 CERRO DEL GRANT 6 A136107 7 T A536106 Y A W T STATE H HWY STAT E E BUELL PARK TODILTO PARK 1 H CHUSKA PEAK 26 W H135109 H835108 EAR ROCK Y H735108 RED LAKE WELL 5 H535108 MILK LAKE NOSE ROCK 18 COYOTE CANYON NW H335108 SEVEN LAKES NEPUEBLO PINTADO STANDING ROCK NW H235108 H135108 STAR LAKE -
Southward-Directed Subduction of the Farallon–Aluk Spreading Ridge and Its Impact on Subduction Mechanics and Andean Arc Magmatism: Insights From
feart-08-00121 May 7, 2020 Time: 11:30 # 1 ORIGINAL RESEARCH published: 08 May 2020 doi: 10.3389/feart.2020.00121 Southward-Directed Subduction of the Farallon–Aluk Spreading Ridge and Its Impact on Subduction Mechanics and Andean Arc Magmatism: Insights From Edited by: Marina Manea, Geochemical and Seismic National Autonomous University of Mexico, Mexico Tomographic Data Reviewed by: 1,2 1,2 1,2 1,2 Luca Ferrari, Sofía B. Iannelli *, Lucía Fernández Paz , Vanesa D. Litvak , Guido Gianni , Geosciences Center, National Lucas M. Fennell1,2, Javiera González3, Friedrich Lucassen4, Simone Kasemann4, Autonomous University of Mexico, Verónica Oliveros3 and Andrés Folguera1,2 Mexico 1 2 Jiashun Hu, Departamento de Ciencias Geológicas, Universidad de Buenos Aires, Buenos Aires, Argentina, Instituto de Estudios 3 California Institute of Technology, Andinos ‘Don Pablo Groeber’, CONICET- Universidad de Buenos Aires, Buenos Aires, Argentina, Departamento 4 United States de Ciencias de la Tierra, Universidad de Concepción, Concepción, Chile, MARUM - Center for Marine Environmental Sciences and Faculty of Geosciences, University of Bremen, Bremen, Germany *Correspondence: Sofía B. Iannelli sofi[email protected] Since the initial proposal of the past existence of a southward-directed mid-ocean ridge–subduction interaction in the Andes during Late Cretaceous–Paleogene times, Specialty section: This article was submitted to several studies have been devoted to uncover the tectonomagmatic evidence of this Structural Geology and Tectonics, process. The collision of a spreading ridge against a subduction margin provokes a section of the journal important tectonomagmatic changes, including, between them, variations in arc-related Frontiers in Earth Science magmatic activity and in the plate-margin stress regime. -
The Grants Uranium District, New Mexico: Update on Source, Deposition, and Exploration 1
The Grants Uranium District, New Mexico: Update on Source, Deposition, and Exploration 1 VIRGINIA T. M cLEMORE 2 1. Manuscript received September 2, 2010; Accepted November 28, 2010 2. NM Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, Socorro, NM, 87801; [email protected] ABSTRACT More than 340 million pounds (lbs) of U 3O8 have been produced from the Grants uranium deposits in New Mexico between 1948 and 2002, and at least 403 million lbs of U 3O8 remain as unmined resources. The Grants district is one of the largest uranium provinces in the world. The Grants district extends from east of Laguna to west of Gallup in the San Juan Basin of New Mexico. Three types of sandstone uranium deposits are recognized: tabular, redistributed (roll-front, fault- related), and remnant-primary. The tabular deposits formed during the Jurassic Westwater Canyon time. Subsequently, oxidizing solutions moved downdip, modifying tabular deposits into redistributed roll- front and fault-related deposits. Evidence, including age dates and geochemistry of the uranium deposits, suggests that redistributed deposits could have been formed shortly after deposition in the early Creta - ceous and from a second oxidation front during the mid-Tertiary. The source of uranium is important in understanding how the Grants deposits formed. Two possible sources exist: 1) the Zuni Mountains, which lie south of the district and consist of a Proterozoic granitic highland enriched in uranium with as much as 11 parts per million, and with high heat flow; and 2) vol - canic rocks erupted from a Jurassic arc volcanism, which formed southwest of the San Juan Basin, and deposited ash over much of the region. -
Preliminary Report on the July 10–11, 2015 Explosive Eruption at Volcán
ÔØ ÅÒÙ×Ö ÔØ Preliminary report on the July 10–11, 2015 explosive eruption at Volc´an de Colima: Pyroclastic density currents with exceptional runouts and volume. L. Capra, J.L. Mac´ıas, A. Cort´es, N. D´avila, R. Saucedo, S. Osorio-Ocampo, J.L. Arce, J.C. Gavilanes-Ru´ız, P. Corona-Ch´avez, L. Garc´ıa-S´anchez, G. Sosa-Ceballos, R. V´azquez PII: S0377-0273(15)00404-7 DOI: doi: 10.1016/j.jvolgeores.2015.11.022 Reference: VOLGEO 5716 To appear in: Journal of Volcanology and Geothermal Research Received date: 24 August 2015 Accepted date: 23 November 2015 Please cite this article as: Capra, L., Mac´ıas, J.L., Cort´es, A., D´avila, N., Saucedo, R., Osorio-Ocampo, S., Arce, J.L., Gavilanes-Ru´ız, J.C., Corona-Ch´avez, P., Garc´ıa- S´anchez, L., Sosa-Ceballos, G., V´azquez, R., Preliminary report on the July 10–11, 2015 explosive eruption at Volc´an de Colima: Pyroclastic density currents with excep- tional runouts and volume., Journal of Volcanology and Geothermal Research (2015), doi: 10.1016/j.jvolgeores.2015.11.022 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. -
Chaco Landscapes: Data, Theory and Management
Chaco Landscapes: Data, Theory and Management Ruth Van Dyke, Stephen Lekson, and Carrie Heitman with a contribution by Julian Thomas February 25, 2016 Draft report submitted as partial fulfillment of CESU Master Agreement P14AC00979, Project Number: UCOB-109 to Chaco Culture National Historical Park, New Mexico by the University of Colorado, Boulder, Colorado CONTENTS User’s Guide THE CHACO LANDSCAPE I. Introduction: Chaco in Time & Space II. Management History III. Landscape: Theoretical Background IV. Defining the Chaco Landscape: Part I – Materials V. Anthropological Research Issues on the Chacoan Landscape A. Chaco’s Boundaries in Time and Space B. Sociopolitical Organization/Complexity C. Exchange & Interaction D. Indigenous Relationships to the Chacoan Landscape E. Dwellings in Places VI. Defining the Chacoan Landscape: Part II – Experiences A. Viewsheds B. Day and Night Skies C. Soundscapes D. Oral Histories VII. Management Considerations APPENDICES Appendix I: Landscape in Canyon-Outlier Models Appendix II: Management Considerations Appendix III: Landscape: Theoretical Background A. Settlement Pattern Studies and GIS B. Cultural Landscapes C. Phenomenology Appendix IV: Defining the Chacoan Landscape A. An Outlier List and Map Example B. Examples of Outlier Diversity C. Roads D. Shrines and Related Features Appendix V: Chaco Landscapes - Some Suggestions from the Old World, by Julian Thomas Appendix VI: Defining the Chacoan Landscape: Part II – Experiences A. Viewsheds B. Day and Night Skies C. Soundscapes REFERENCES i ii User’s Guide This paper, informally termed the “White Paper,” presents current anthropological theory, methods, and research on Chacoan landscapes at several scales. The paper consists of 17 pages of text which summarize anthropological and management issues, supported by 45 pages of Appendices and a list of References cited. -
Description of the Deming Quadrangle
DESCRIPTION OF THE DEMING QUADRANGLE, By N. H. Darton. INTRODUCTION. GENERAL GEOLOGY AND GEOGRAPHY OF SOUTHWESTERN Paleozoic rocks. The general relations of the Paleozoic rocks NEW MEXICO. are shown in figure 3. 2 All the earlier Paleozoic rocks appear RELATIONS OF THE QUADRANGLE. STRUCTURE. to be absent from northern New Mexico, where the Pennsyl- The Deming quadrangle is bounded by parallels 32° and The Rocky Mountains extend into northern New Mexico, vanian beds lie on the pre-Cambrian rocks, but Mississippian 32° 30' and by meridians 107° 30' and 108° and thus includes but the southern part of the State is characterized by detached and older rocks are extensively developed in the southern and one-fourth of a square degree of the earth's surface, an area, in mountain ridges separated by wide desert bolsons. Many of southwestern parts of the State, as shown in figure 3. The that latitude, of 1,008.69 square miles. It is in southwestern the ridges consist of uplifted Paleozoic strata lying on older Cambrian is represented by sandstone, which appears to extend New Mexico (see fig. 1), a few miles north of the international granites, but in some of them Mesozoic strata also are exposed, throughout the southern half of the State. At some places the and a large amount of volcanic material of several ages is sandstone has yielded Upper Cambrian fossils, and glauconite 109° 108° 107" generally included. The strata are deformed to some extent. in disseminated grains is a characteristic feature in many beds. Some of the ridges are fault blocks; others appear to be due Limestones of Ordovician age outcrop in all the larger ranges solely to flexure. -
Unm Sustainability Studies | Ra a Zine About Nuclear New Mexico
HOME A ZINE ABOUT NUCLEAR NEW MEXICO FALL 2015 | UNM SUSTAINABILITY STUDIES | R.A. New Mexico is famous for being the home of the world’s first atomic bomb, but it is also home to many people, animals, and natural wonders. Since the Manhattan Project, New Mexico has become a sacrifice zone for the nuclear industry. Not only are health risks not fully disclosed with New Mexico inhabitants, but accidents have destroyed livelihoods. I made this zine to spread awareness about the impact of nuclearism in the place I call home, the place my family has called home for many S A C R generations, the place I love with all of my heart. With its colorful rock formations, high desert landscapes, sunshine-filled days, summer rainstorms, and rich cultural history, it is so much more than a rural state. New Mexico has been home to a wide ray of ecosystems for millions of years, and I F I C E it is a place that deserves to be protected. Z O N E It’s okay, it’s rural. SACRFICEZONE: noun a geographic area that has been impaired by environmental damage or economic disinvestment, most commonly found in low-income and minority communities Mescalero Apache Reservation Sunspot N U C L E A R H O M E Mesilla Tularosa Nogal Tinnie TRINITY WATER Orogranda Weed 1945Eagle Creek Oscura 35 MI EAST OF SOCORRO Lake Arthur Radium Springs The world’s first atomic bomb detonation Lake Holloman Ruidoso of Gadget was tested in White Sands as Lake Lucero San Patricio Lost River Socorro a part of the Manhattan Project. -
Southwest NM Publication List
Southwest New Mexico Publication Inventory Draft Source of Document/Search Purchase Topic Category Keywords County Title Author Date Publication/Journal/Publisher Type of Document Method Price Geology 1 Geology geology, seismic Southwestern NM Six regionally extensive upper-crustal Ackermann, H.D., L.W. 1994 U.S. Geological Survey, Open-File Report 94- Electronic file USGS publication search refraction profiles, seismic refraction profiles in Southwest New Pankratz, D.P. Klein 695 (DJVU) http://pubs.er.usgs.gov/usgspubs/ southwestern New Mexico ofr/ofr94695 Mexico, 2 Geology Geology, Southwestern NM Magmatism and metamorphism at 1.46 Ga in Amato, J.M., A.O. 2008 In New Mexico Geological Society Fall Field Paper in Book http://nmgs.nmt.edu/publications/g $45.00 magmatism, the Burro Mountains, southwestern New Boullion, and A.E. Conference Guidebook - 59, Geology of the Gila uidebooks/59/ metamorphism, Mexico Sanders Wilderness-Silver City area, 107-116. Burro Mountains, southwestern New Mexico 3 Geology Geology, mineral Catron County Geology and mineral resources of York Anderson, O.J. 1986 New Mexico Bureau of Mines and Mineral Electronic file (PDF) NMBGMR search $10.00 for resources, York Ranch SE quadrangle, Cibola and Catron Resources Open File Report 220A, 22 pages. <http://geoinfo.nmt.edu/publicatio CD Ranch, Fence Counties, New Mexico ns/openfile/details.cfml?Volume=2 Lake, Catron, 20A> Cibola 4 Geology Geology, Zuni Salt Catron County Geology of the Zuni Salt Lake 7 1/2 Minute Anderson, O.J. 1994 New Mexico Bureau of Mines and -
Geohydrology of the San Agustin Basin, Alamosa Creek Basin
Geohydrology of the San Agustin Basin, Alamosa Creek Basin upstream from Monticello Box, and upper Gila Basin in parts of Catron, Socorro, and Sierra Counties, New Mexico By R.G. Myers, J.T. Everheart, and C.A. Wilson U.S. GEOLOGICAL SURVEY WATER-RESOURCES INVESTIGATIONS REPORT 94-4125 Prepared in cooperation with the NEW MEXICO STATE ENGINEER OFFICE Albuquerque, New Mexico 1994 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director For additional information Copies of this report can write to: be purchased from: U.S. Geological Survey District Chief Earth Science Information Center U.S. Geological Survey Open-File Reports Section Water Resources Division Box 25286, MS 517 4501 Indian School Rd. NE, Suite 200 Denver Federal Center Albuquerque, New Mexico 87110 Denver, Colorado 80225 CONTENTS Page Abstract.................................................................................................................................................. 1 Introduction........................................................................................................................................... 1 Purpose and scope...................................................................................................................... 3 Location and extent.................................................................................................................... 3 Ctimate....................................^ 3 Previous hydrologic investigations......................................................................................... -
Cultural Resources Overview Desert Peaks Complex of the Organ Mountains – Desert Peaks National Monument Doña Ana County, New Mexico
Cultural Resources Overview Desert Peaks Complex of the Organ Mountains – Desert Peaks National Monument Doña Ana County, New Mexico Myles R. Miller, Lawrence L. Loendorf, Tim Graves, Mark Sechrist, Mark Willis, and Margaret Berrier Report submitted to the Wilderness Society Sacred Sites Research, Inc. July 18, 2017 Public Version This version of the Cultural Resources overview is intended for public distribution. Sensitive information on site locations, including maps and geographic coordinates, has been removed in accordance with State and Federal antiquities regulations. Executive Summary Since the passage of the National Historic Preservation Act (NHPA) in 1966, at least 50 cultural resource surveys or reviews have been conducted within the boundaries of the Desert Peaks Complex. These surveys were conducted under Sections 106 and 110 of the NHPA. More recently, local avocational archaeologists and supporters of the Organ Monument-Desert Peaks National Monument have recorded several significant rock art sites along Broad and Valles canyons. A review of site records on file at the New Mexico Historic Preservation Division and consultations with regional archaeologists compiled information on over 160 prehistoric and historic archaeological sites in the Desert Peaks Complex. Hundreds of additional sites have yet to be discovered and recorded throughout the complex. The known sites represent over 13,000 years of prehistory and history, from the first New World hunters who gazed at the nighttime stars to modern astronomers who studied the same stars while peering through telescopes on Magdalena Peak. Prehistoric sites in the complex include ancient hunting and gathering sites, earth oven pits where agave and yucca were baked for food and fermented mescal, pithouse and pueblo villages occupied by early farmers of the Southwest, quarry sites where materials for stone tools were obtained, and caves and shrines used for rituals and ceremonies. -
Fighting the Good Fight
www.nmwild.org NEW MEXICO CONGRESSMAN TOM UDALL FIGHTING THE G O O D F I G H T by Stephen Capra hen it comes to conservation, wilderness and the protection of W wildlands in America, few fami- lies have the same pedigree as the name Udall. Here in New Mexico Congressman Tom Udall is the latest in the Udall family to fi ght hard for the protection of wildlands in the West. His Father, Stewart Udall was Secretary of Interior during the Kennedy and Johnson Administrations. His uncle Mo Udall is fondly remembered for his efforts on national wilderness issues and his work on the monumental Alaska Lands Act. And today, during what many people consider a conservation crisis under the Bush Administration, few Congressmen are working harder and voting consistently for the protection of our National Forests and our public lands than our own New Mexico Congressman Tom Udall. Even before being elected to Congress, Udall worked diligently as Attorney Gen- eral of New Mexico to slow sprawl and enact tough new measures for develop- ers. Land use and subdivisions at that time had been loosely regulated in New Mexico, as in many parts of the West. A series of attempts in the early 1990’s to amend New Mexico’s subdivision laws failed. Interest groups such as the New Mexico Homebuilders Association and the New Mexico Association of Realtors had long been a powerful force in the state. But in 1995, the New Mexico State Legislature passed a sweeping set of amendments to the State’s subdivision laws. -
Plan for the Recovery of Desert Bighorn Sheep in New Mexico 2003-2013
PLAN FOR THE RECOVERY OF DESERT BIGHORN SHEEP IN NEW MEXICO 2003-2013 New Mexico Department of Game and Fish August 2003 Executive Summary Desert bighorn sheep (Ovis canadensis mexicana) were once prolific in New Mexico, occupying most arid mountain ranges in the southern part of the state. Over-hunting, and disease transmission from livestock are 2 primary reasons for the dramatic decline in bighorn sheep numbers throughout the west during the early 1900s. In 1980, desert bighorn were placed on New Mexico’s endangered species list. From 1992-2003, approximately 25% of bighorn were radiocollared to learn causes of mortality driving this species towards extinction. Approximately 85% of all known-cause non-hunter killed radiocollared individuals have been killed by mountain lions. Despite the lack of a native ungulate prey base in desert bighorn range, mountain lion populations remain high, leading to the hypothesis that mountain lions are subsidized predators feeding on exotic ungulates, including cattle. Lack of fine fuels from cattle grazing have resulted in a lack of fire on the landscape. This has lead to increased woody vegetation which inhibits bighorn’s ability to detect and escape from predators. Bighorn numbers in spring 2003 in New Mexico totaled 213 in the wild, and 91 at the Red Rock captive breeding facility. This is in spite of releasing 266 bighorn from Red Rock and 30 bighorn from Arizona between 1979 and 2002. Several existing herds of desert bighorn likely need an augmentation to prevent them from going extinct. The presence of domestic sheep and Barbary sheep, which pose risks to bighorn from fatal disease transmission and aggression, respectively, preclude reintroduction onto many unoccupied mountain ranges.