Van Dyke 2011 Ideology on the Chacoan Landscape.Pdf
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Narbonapass.Pdf
FIRST-DAY ROAD LOG 1 FIRST-DAY ROAD LOG, FROM GALLUP TO GAMERCO, YAH-TA-HEY, WINDOW ROCK, FORT DEFIANCE, NAVAJO, TODILTO PARK, CRYSTAL, NARBONA PASS, SHEEP SPRINGS, TOHATCHI AND GALLUP SPENCER G. LUCAS, STEVEN C. SEMKEN, ANDREW B. HECKERT, WILLIAM R. BERGLOF, First-day Road Log GRETCHEN HOFFMAN, BARRY S. KUES, LARRY S. CRUMPLER AND JAYNE C. AUBELE ������ ������ ������ ������� ������ ������ ������ ������ �������� Distance: 141.8 miles ������� Stops: 5 ���� ������ ������ SUMMARY ������ �� ������ �� ����� �� The first day’s trip takes us around the southern �� �� flank of the Defiance uplift, back over it into the �� southwestern San Juan Basin and ends at the Hogback monocline at Gallup. The trip emphasizes Mesozoic— especially Jurassic—stratigraphy and sedimentation in NOTE: Most of this day’s trip will be conducted the Defiance uplift region. We also closely examine within the boundaries of the Navajo (Diné) Nation under Cenozoic volcanism of the Navajo volcanic field. a permit from the Navajo Nation Minerals Department. Stop 1 at Window Rock discusses the Laramide Persons wishing to conduct geological investigations Defiance uplift and introduces Jurassic eolianites near on the Navajo Nation, including stops described in this the preserved southern edge of the Middle-Upper guidebook, must first apply for and receive a permit Jurassic depositional basin. At Todilto Park, Stop 2, from the Navajo Nation Minerals Department, P.O. we examine the type area of the Jurassic Todilto For- Box 1910, Window Rock, Arizona, 86515, 928-871- mation and discuss Todilto deposition and economic 6587. Sample collection on Navajo land is forbidden. geology, a recurrent theme of this field conference. From Todilto Park we move on to the Green Knobs diatreme adjacent to the highway for Stop 3, and then to Stop 4 at the Narbona Pass maar at the crest of the Chuska Mountains. -
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 -
Geophysical Investigations of Ship Rock and Thumb Igneous Centers, New Mexico
Bank, C. 2007. 20th Annual Keck Symposium; http://keck.wooster.edu/publications GEOPHYSICAL INVESTIGATIONS OF SHIP ROCK AND THUMB IGNEOUS CENTERS, NEW MEXICO CARL-GEORG BANK, JEFF NOBLETT, GLENN KROEGER, STEVEN SEMKEN University of Toronto, Colorado College, Trinity University, Arizona State University INTRODUCTION minette plugs, it intruded the surrounding Cretaceous Mancos shale in middle Oligocene Imaging the subsurface structure of two times. Differential erosion has left Ship Rock important volcanic centers of the mid-Tertiary towering 550 m above the surrounding plains Navajo Volcanic Field, on the Colorado Plateau, (Fig. 1). serves several purposes. Besides having specific implications for the formation of these particular features, our project will aid in understanding similar structures across the Colorado Plateau. Various researchers [e.g., Rubin, 1991; Mériaux and Jaupart, 1998; Segall et al., 2001] imagine the emplacement of a dike as vertical movement through host rock, often along preexisting faults or cracks, driven by magma pressure, and modified by the change in stress regime with depth. Other models [e.g., Delaney and Pollard, 1981; Quareni et al., 2001] allow magma to flow in pipes in addition to, and possibly following, its emplacement in dikes. Our results will provide valuable data against which to test such competing models of magma emplacement, and Figure 1: View of the Ship Rock diatreme from the – in a wider sense – aid in understanding diverse South-East (Photo: Brett Mayhew) processes like hydraulic fracturing, tensile fracturing, and dike-generated seismicity [Baer, Seven dikes of mafic minette (a potassic mica 1991]. lamprophyre containing phlogopite) extend from the diatreme. The largest of these is up to GEOLOGICAL AND 30 m high, about 2 m wide, and can be followed for about 9 km to the South. -
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. -
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81 THE WASHINGTON PASS VOLCANIC CENTER: EVOLUTION AND ERUPTION OF MINETTE MAGMAS OF THE NAVAJO VOLCANIC FIELD S.N. Ehrenberg (Department of Earth and Space Sciences, University of California, Los Angeles, California 90024) Minettes of the Navajo Volcanic Field are of interest because they formed at depths of at least 150 km and appear to be genetically related to kimberlite diatremes. Minettes and their extrusive equivalents (tra- chybasalts) at the 2 km diameter subsidence crater at Washington Pass were chosen for detailed study because of the relatively well-developed eruptive history displayed in the crater stratigraphy and the presence of contrasting mafic and trachytic lavas. Eruption began with ejection of voluminous pyroclastic deposits, including both tuff-breccias, composed predominantly of comminuted sediments with subordinate minette and cry¬ stalline basement fragments, and agglomerates, composed mainly of minette clasts. These deposits are thickest (>100 m) on the east and west sides of the crater, where they are exposed in cliffs produced by landsliding. On the west, tuff-breccias predominate and exhibit a remark¬ able alternation of coarse- and fine-grained beds 0.1 - 1 m thick, suggest¬ ive of rhythmic variation in the physical properties in the eruptive med¬ ium. On the east, the pyroclastic materials are mostly agglo¬ merates. Low-angle cross-bedding is common in all the pyroclastic beds, but in the eastern agglomerates this feature is accompanied by dune structures. Some of these formed by accretion on the lee side, while others display accretion on the side facing the crater. Asymmetrical bomb sags are also abundant in this area. -
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. -
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. -
Shiprock Disposal Site Observational Site Visit
U.S. DEPARTMENT OF Legacy EN ERGYI Management Shiprock, New Mexico, Disposal Site This fact sheet provides information about the Uranium Mill Tailings Radiation ControlAct of 1978 Title I disposalsite at Shiprock, New Mexico. This site is managed by the U.S. Department of Energy Office of Legacy Management. Site Description and History The Shiprock site is the location of a former uranium- and vanadium-ore-processing facility within the Navajo Nation in the northwest corner of New Mexico near the town of Shiprock, approximately 28 miles west of Farmington. Kerr-McGee built the mill and operated the facility from 1954 until 1963. Vanadium Corporation of America purchased the mill and operated it until it closed in 1968. The milling operations created process- related wastes and radioactive tailings, a predominantly sandy material. The mill, ore storage area, raffinate ponds (ponds that contain spent liquids from the milling process), and tailings piles occupied approximately 230 acres leased from the Navajo Nation. In 1983, the U.S. Department of Energy (DOE) and the Navajo Nation entered into an agreement for site cleanup. By September 1986, all tailings and associ- ated materials (including contaminated materials from offsite vicinity properties) were encapsulated in the disposal cell built on top of the existing tailings piles. Regulatory Setting Location of the Shiprock Disposal Site Congress passed the Uranium Mill Tailings Radiation from the disposal cell to the San Juan River is about Control Act (UMTRCA) in 1978 (Public Law 95-604) 600 feet. and DOE remediated 22 inactive uranium-ore- Groundwater in the terrace area is thought to be a processing sites under the Uranium Mill Tailings result of human activities. -
Chapter Land Use Plan and Housing Planning Project
NAHASDA (NATIVE AMERICAN HOUSING ASSISTANCE AND SELF DETERMINATION ACT) CHAPTER LAND USE PLAN AND HOUSING PLANNING PROJECT MASTER LAND USE PLAN SHIPROCK CHAPTER, NAVAJO NATION Prepared by: DUANE H. YAZZIE CONSULTANT Rez Star Point SHIPROCK, NAVAJO NATION 1 NAHASDA (NATIVE AMERICAN HOUSING ASSISTANCE AND SELF DETERMINATION ACT) CHAPTER LAND USE PLAN AND HOUSING PLANNING PROJECT MASTER LAND USE PLAN SHIPROCK CHAPTER, NAVAJO NATION TABLE OF CONTENTS SPECTRUM 1: Introduction, Authority, Purpose and Process Page No. 1.1 Introduction 7 1.2 Background 7 1.3 Authority 8 1.4 Purpose 10 1.5 Planning Process 10 1.6 Community Participation Process 14 1.7 Conclusion 16 1.8 Definitions 17 1.9 Exhibits 20 SPECTRUM 2: Community Assessment 2.1 Vision Statement 27 2.2 Existing Land Status Information 29 2.3 Demographics Data 30 2.4 Existing and Future Residential Needs 30 2.5 Grazing and Agriculture Information 35 2.6 Community and Public Facilities Information 36 2.7 Commercial and Industrial Development Information 45 2.8 Exhibits 47 SPECTRUM 3: Land Suitability Analysis 3.1 Background 56 3.2 Existing Environment 56 3.3 Site Analysis Elements 57 3.3.1 Hydrologic Features 57 3.3.2 Soils 58 3.3.3 Slopes and Topography 58 3.3.4 Vegetation and Wildlife 59 3.3.5 Culturally Sensitive Areas 61 3.3.6 Traditionally Sensitive Areas 61 3.3.7 Environmentally Sensitive Areas 62 2 3.4 Accessibility 67 3.5 Conclusion 67 3.6 Consultation Coordination 67 3.7 Bibliography 68 3.8 Exhibits 70 SPECTRUM 4: Infrastructure Analysis 4.1 Background 81 4.2 Infrastructure Analysis -
Lloyd L. Lee Native American Studies 7-1-21
Lloyd L. Lee Native American Studies 7-1-21 Educational History Ph.D., 2004, University of New Mexico, Albuquerque, NM, American Studies, Dissertation title: 21st Century Diné Cultural Identity: Defining and Practicing Sa’ah Naaghai Bik’eh Hozhoon, Amanda Cobb, Ph.D. M.A., 1995, Stanford University, Palo Alto, CA, Teacher Education and California Teaching Credential in Social Studies B.A., 1994, Dartmouth College, Hanover, NH, Major: History, Minor: Native American Studies Employment History, Part I Professor, 7/1/21 – present, University of New Mexico, Albuquerque, NM Associate Professor, 7/1/14 – 6/30/21, University of New Mexico, Albuquerque, NM Assistant Professor, 8/1/08 – 6/30/14, University of New Mexico, Albuquerque, NM Assistant Professor, 8/1/04 – 7/31/07, Arizona State University, Phoenix, AZ Social Studies Teacher, 8/1/95 – 5/31/99, Wingate High School, Fort Wingate, NM Employment History Part II Visiting Assistant Professor in Native American Studies, 8/1/07 -7/31/08, University of New Mexico, Albuquerque, NM Professional Recognition and Honors Presidential Teaching Fellow Award, promotes excellence in teaching and given the highest recognition for effective teaching, 2017 – 2019, Center for Teaching Excellence – University of New Mexico Honorary Stars, Special thank you and recognition from students, 2012 – 2013, American Indian Student Services – University of New Mexico Outstanding Commitment to Students Award, Recognition and honor of faculty and staff, 2005 -2006, Arizona State University at the West Campus 1 Short Narrative Description of Research, Teaching, and Service Interests My philosophy is to develop an individual’s critical consciousness through my teaching, research, and service. -
Executive Branch Third Quarterly Report
OFFICE OF THE PRESIDENT AND VICE PRESIDENT JONATHAN NEZ | PRESIDENT MYRON LIZER |VICE PRESIDENT EXECUTIVE BRANCH THIRD QUARTERLY REPORT SUMMER COUNCIL SESSION JULY 2021 NAVAJO NATION OFFICE OF THE PRESIDENT AND VICE PRESIDENT SUMMER COUNCIL SESSION 2021 TABLE OF CONTENTS PAGE NO. I. Department of Diné Education 2 II. Department of Human Resources 32 III. Diné Uranium Remediation Advisory Commission 39 IV. Division of Community Development 42 V. Division of Economic Development 58 VI. Division of General Services 78 VII. Division of Public Safety 82 VIII. NavaJo Department of Health 94 IX. NavaJo Division of Social Services 108 X. NavaJo Division of Transportation 116 XI. NavaJo Gaming Regulatory Office 120 XII. NavaJo Nation Department of Justice 125 XIII. NavaJo Nation Division of Natural Resources 130 XIV. NavaJo Nation Environmental Protection Agency 156 XV. NavaJo Nation Telecommunications Regulatory Commission 161 XVI. NavaJo Nation Veterans Administration 164 XVII. NavaJo Nation Washington Office 166 XVIII. NavaJo-Hopi Land Commission Office 173 XIX. Office of Hearing and Appeals 185 XX. Office of Management and Budget 187 XXI. Office of Miss NavaJo Nation 190 XXII. Office of NavaJo Public Defender 195 XXIII. Office of NavaJo Tax Commission 198 XXIV. Office of The Controller 201 1 Department of Diné Education SUMMER COUNCIL SESSION 2021 I. MAJOR ACCOMPLISHMENTS II. CHALLENGES III. OUTREACH AND COMMUNICATION 2 DODE hosted a live forum regarding the state of education on the Navajo Nation amid the ongoing COVID-19 pandemic with Navajo Nation school leaders and health experts the evening of June 17, 2021. The panel took questions and concerns from the audience as well as points brainstormed by DODE staff that parents may have about sending their children back to school for in-person instruction. -
A Reconnaissance Survey of the Western Part of the Durango-Gallup Coal Field of Colo Rado and New Mexico."
A RECONNAISSANCE SURVEY OF THE WESTERN PART OF THE DURANGO-GALLUP COAL FIELD OF COLO RADO AND NEW MEXICO." By MILLARD K. SHALER. INTRODUCTION. The area of the Durango-Gallup coal field includes 13,500 square miles, of which 1,900 lie in Colorado and the remainder in New Mexico. The total production of coal in this field in 1905 b was about 660,600 short tons, valued at nearly $1,000,000, exclusive of coke, of which about 12,000 short tons were produced. The entire tonnage of the field is estimated at 80,000,000,000 short tons, by figuring con servatively on a total workable thickness of 6 feet underlying the area, although 10 feet is probably a closer approximation of the average. The Durango-Gallup coal field extends from the latitude of Durango, Colo., on the north to the latitude pf Salt Lake, 70 miles south of Gallup, N. Mex., on the south, a distance of about 200 miles. Chama, Elvado, and the Sierra Nacimiento, in longitude 106° 45', are situated near the eastern boundary of the field, and its western limit is the New Mexico-Arizona boundary line. The width of the field is about 150 miles. (See PI. XXII.) In altitude the surface ranges from 5,000 to 9,000 feet, with an average of about 6,500 feet. The topography is varied, but on the whole the country is an open plateau in which the streams have cut valleys nearly 1,000 feet in depth. This paper, as may be seen by reference to the map, treats only of that part of the Durango-Gallup field lying west of longitude 107° 30'; Hence the remainder of the area will be given no further consid eration.0 The principal towns in Colorado within the region here considered are Durango and Mancos, located on the Denver and Rio "This preliminary report will be followed by a fuller description of the entire field, now in prepa ration, which will appear at an early date as a publication of the Survey.