New Mexico. Triangulation Stations
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Water and Natural Resources Committee
WATER AND NATURAL RESOURCES COMMITTEE 2012 INTERIM FINAL REPORT to the FIFTIETH LEGISLATURE SECOND SESSION New Mexico Legislative Council Service Santa Fe, New Mexico December 2012 WATER AND NATURAL RESOURCES COMMITTEE 2012 REPORT Santa Fe, New Mexico December 2012 2012 LEGISLATIVE INTERIM WATER AND NATURAL RESOURCES COMMITTEE SUMMARY OF WORK The committee scheduled five meetings during the 2012 interim that were held in Las Cruces, Truth or Consequences, Ruidoso, Albuquerque and Santa Fe. Continued drought and major wildfires again dominated the news in 2012. Through November 2012, the average precipitation for New Mexico was near the record lowest value, ranking as the second driest since 1895, as severe to exceptional drought continued across New Mexico, and the average temperature for the state for the year was the highest on record. It was also the second consecutive year during which record-breaking wildfires burned across the state. The lightning-sparked Whitewater-Baldy Complex Fire in the Gila Wilderness burned more than 297,845 acres, which surpassed the area burned by the Las Conchas Fire of 2011, making it the largest wildfire in New Mexico state history. The Little Bear Fire was also started by a lightning strike; it burned 44,330 acres and 254 buildings in Lincoln County after quickly growing out of control due to dry, windy conditions. The city of Ruidoso and the surrounding area will need more than $14 million in the coming years to address the effects of that fire on their drinking water supplies alone. At the committee's joint meeting in August with the Courts, Corrections and Justice Committee, the committees reviewed several legal issues of concern to both committees, including the state's suit against the federal Bureau of Reclamation on its administration of Rio Grande Project water, implementation of the Pecos River Settlement, the status of ongoing adjudications and the need for spaceport liability legislation. -
Butch Cassidy Roamed Incognito in Southwest New Mexico
Nancy Coggeshall I For The New Mexican Hideout in the Gila Butch Cassidy roamed incognito in southwest New Mexico. Hideout in the Gila utch Cassidy’s presence in southwestern New Mexico is barely noted today. Notorious for his successful bank Butch Cassidy roamed and train robberies at the turn of the 20th century, incognito in southwest Cassidy was idealized and idolized as a “gentleman out- New Mexico wilderness Blaw” and leader of the Wild Bunch. He and various members of the • gang worked incognito at the WS Ranch — set between Arizona’s Blue Range and San Carlos Apache Reservation to the west and the Nancy Coggeshall rugged Mogollon Mountains to the east — from February 1899 For The New Mexican until May 1900. Descendants of pioneers and ranchers acquainted with Cassidy tell stories about the man their ancestors knew as “Jim Lowe.” Nancy Thomas grew up hearing from her grandfather Clarence Tipton and others that Cassidy was a “man of his word.” Tipton was the foreman at the WS immediately before Cassidy’s arrival. The ranch sits at the southern end of the Outlaw Trail, a string of accommodating ranches and Wild Bunch hideouts stretching from Montana and the Canadian border into Mexico. The country surrounding the WS Ranch is forbidding; volcanic terrain cleft with precipitously angled, crenelated canyon walls defies access. A “pretty hard layout,” local old-timer Robert Bell told Lou Blachly, whose collection of interviews with pioneers — conducted PROMIENT PLACES - between 1942 and 1953 — are housed at the University of New OUTLAW TRAIL Mexico. What better place to dodge the law? 1. -
By Douglas P. Klein with Plates by G.A. Abrams and P.L. Hill U.S. Geological Survey, Denver, Colorado
U.S DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY STRUCTURE OF THE BASINS AND RANGES, SOUTHWEST NEW MEXICO, AN INTERPRETATION OF SEISMIC VELOCITY SECTIONS by Douglas P. Klein with plates by G.A. Abrams and P.L. Hill U.S. Geological Survey, Denver, Colorado Open-file Report 95-506 1995 This report is preliminary and has not been edited or reviewed for conformity with U.S. Geological Survey editorial standards. The use of trade, product, or firm names in this papers is for descriptive purposes only, and does not imply endorsement by the U.S. Government. STRUCTURE OF THE BASINS AND RANGES, SOUTHWEST NEW MEXICO, AN INTERPRETATION OF SEISMIC VELOCITY SECTIONS by Douglas P. Klein CONTENTS INTRODUCTION .................................................. 1 DEEP SEISMIC CRUSTAL STUDIES .................................. 4 SEISMIC REFRACTION DATA ....................................... 7 RELIABILITY OF VELOCITY STRUCTURE ............................. 9 CHARACTER OF THE SEISMIC VELOCITY SECTION ..................... 13 DRILL HOLE DATA ............................................... 16 BASIN DEPOSITS AND BEDROCK STRUCTURE .......................... 20 Line 1 - Playas Valley ................................... 21 Cowboy Rim caldera .................................. 23 Valley floor ........................................ 24 Line 2 - San Luis Valley through the Alamo Hueco Mountains ....................................... 25 San Luis Valley ..................................... 26 San Luis and Whitewater Mountains ................... 26 Southern -
A Proposed Low Distortion Projection for the City of Las Cruces and Dona Ana County Scott Farnham, PE, PS City Surveyor, City of Las Cruces NM October 2020
A Proposed Low Distortion Projection for the City of Las Cruces and Dona Ana County Scott Farnham, PE, PS City Surveyor, City of Las Cruces NM October 2020 Introduction As part of the ongoing modernization of the U.S. National Spatial Reference System (NSRS), the National Geodetic Survey (NGS) will replace our horizontal and vertical datums (NAD83 and NAVD88) with new geometric datums assigned in the North American Terrestrial Reference Frame of 2022 (NATRF2022). The City of Las Cruces / Dona Ana County and the City of Albuquerque / Bernalillo County submitted proposals to NGS to incorporate Low Distortion Projections (LDP) as part of the New Mexico State Plane Coordinate Systems. Approval by NGS was obtained on June 17, 2019 for the proposed systems (see approval notice). Design of the LDP is the responsibility of the submitting agencies and must be submitted to NGS on or prior to March 31, 2021. Mark Marrujo1 with NMDOT is submitting final LDP design forms to NGS for the State of New Mexico. The City of Las Cruces (City) is designing a new Low Distortion Projection for Public Works Department, Engineering and Architecture projects to NGS criteria. To meet NGS LDP minimum size and shape criterion, the LDP area extends to Dona Ana County (County) boundary lines. This report presents design analysis and conclusions of the proposed City / County local NGS LDP system for stakeholders’ review prior to NGS final design submittal. NGS NM SPCS2022 Zones and Stakeholder Organizations NGS is designing new State Plane Coordinate Systems (SPCS2022) for New Mexico. The default SPCS2022 designs for the State are a statewide single zone and the three State Plane Zones: West, Central, and East. -
Some Effects of Fire on Shrubs and Succulents in a Chihuahuan Desert Community in the Franklin Mountains, El Paso County, Texas Richard D
No. 3 January 1987 Contributed Papers of the SECOND SYMPOSIUM ON RESOURCES OF THE CHIHUAHUAN DESERT REGION United States and Mexico —BOTANICAL BIOLOGY— A. Michael Powell, Editor Some Effects of Fire on Shrubs and Succulents in a Chihuahuan Desert Community in the Franklin Mountains, El Paso County, Texas Richard D. Worthington and Rafael D. Corral THE CHIHUAHUAN DESERT RESEARCH INSTITUTE (CDRI) is a nonprofit scientific and educational organization. Its purpose is the collection and dissemination of information pertaining to the Chihuahuan Desert Region of the United States and Mexico. Memberships are available. Annual dues: Individual, $15; Student, $10; Family and Institutional, $25. The Chihuahuan Desert Research Institute publishes the semiannual magazine Chihuahuan Desert Discovery, which is free to members. Nonmembers and members receive our semiannual bulletin Chihuahuan Desert NewsBriefs. Papers in this series were presented during the Second Symposium on the Resources of the Chihuahuan Desert: United States and Mexico, at Sul Ross State University, Alpine, Texas, on October 20—21, 1983, and have been subjected to peer review. Contributed Papers of the SECOND SYMPOSIUM ON RESOURCES OF THE CHIHUAHUAN DESERT: United States and Mexico is a series by the Chihuahuan Desert Research Institute, Box 1334, Alpine,; Texas 79831; 915—837-8370. Copyright © 1986 by the Chihuahuan Desert Research Institute SOME EFFECTS OF FIRE ON SHRUBS AND SUCCULENTS IN A CHIHUAHUAN DESERT COMMUNITY IN THE FRANKLIN MOUNTAINS, EL PASO COUNTY, TEXAS RICHARD D. WORTHINGTON AND RAFAEL D. CORRAL, DEPARTMENT OF BIOLOGICAL SCIENCES, THE UNIVERSITY OF TEXAS AT EL PASO, EL PASO, TEXAS 79968 ABSTRACT.--On 15 July 1981, a fire burned about 30 ha of Chihua— huan desertscrub community in the Franklin Mountains, El Paso County, Texas. -
Museum of New Mexico
MUSEUM OF NEW MEXICO OFFICE OF ARCHAEOLOGICAL STUDIES ARCHAEOLOGY OF THE MOGOLLON HIGHLANDS: SETTLEMENT SYSTEMS AND ADAPTATIONS edited by Yvonne R. Oakes and Dorothy A. Zamora VOLUME 6. SYNTHESIS AND CONCLUSIONS Yvonne R. Oakes Submitted by Timothy D. Maxwell Principal Investigator ARCHAEOLOGY NOTES 232 SANTA FE 1999 NEW MEXICO TABLE OF CONTENTS Figures............................................................................iii Tables............................................................................. iv VOLUME 6. SYNTHESIS AND CONCLUSIONS ARCHITECTURAL VARIATION IN MOGOLLON STRUCTURES .......................... 1 Structural Variation through Time ................................................ 1 Communal Structures......................................................... 19 CHANGING SETTLEMENT PATTERNS IN THE MOGOLLON HIGHLANDS ................ 27 Research Orientation .......................................................... 27 Methodology ................................................................ 27 Examination of Settlement Patterns .............................................. 29 Population Movements ........................................................ 35 Conclusions................................................................. 41 REGIONAL ABANDONMENT PROCESSES IN THE MOGOLLON HIGHLANDS ............ 43 Background for Studying Abandonment Processes .................................. 43 Causes of Regional Abandonment ............................................... 44 Abandonment Patterns in the Mogollon Highlands -
Southwest Area 2015 Aviation Contacts and Communications Guide
Southwest Area 2015 Aviation Contacts and Communications Guide “Safety First” Printed on recycled paper. May 2015 Contents Dispatch Centers .................................................................... 3-4 Air-to-Ground Radio Frequencies Map .....................................5 Air-to-Air Radio Frequencies Map ............................................6 Tones and Frequencies ...............................................................7 New Mexico Frequencies Alamogordo Interagency Dispatch Center .................... 8-9 Albuquerque Interagency Dispatch Center ....................... 10-11 Silver City Interagency Dispatch Center .................. 12-13 Santa Fe Interagency Dispatch Center ...................... 14-15 Taos Interagency Dispatch Center ............................ 16-17 Arizona Frequencies Arizona Interagency Dispatch Center ....................... 18-19 Flagstaff Interagency Dispatch Center ...................... 20-21 Phoenix Interagency Dispatch Center ....................... 22-23 Prescott Interagency Dispatch Center ....................... 24-27 Show Low Interagency Dispatch Center .................. 28-31 Tucson Interagency Dispatch Center ........................ 32-33 Williams Interagency Dispatch Center ..................... 34-35 Southwest Aviation Phone Contact List R3 Regional Office .........................................................36 Bureau of Indian Affairs .................................................37 Bureau of Land Management..........................................37 National -
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. -
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 -
Wilderness Study Areas
I ___- .-ll..l .“..l..““l.--..- I. _.^.___” _^.__.._._ - ._____.-.-.. ------ FEDERAL LAND M.ANAGEMENT Status and Uses of Wilderness Study Areas I 150156 RESTRICTED--Not to be released outside the General Accounting Wice unless specifically approved by the Office of Congressional Relations. ssBO4’8 RELEASED ---- ---. - (;Ao/li:( ‘I:I)-!L~-l~~lL - United States General Accounting OfTice GAO Washington, D.C. 20548 Resources, Community, and Economic Development Division B-262989 September 23,1993 The Honorable Bruce F. Vento Chairman, Subcommittee on National Parks, Forests, and Public Lands Committee on Natural Resources House of Representatives Dear Mr. Chairman: Concerned about alleged degradation of areas being considered for possible inclusion in the National Wilderness Preservation System (wilderness study areas), you requested that we provide you with information on the types and effects of activities in these study areas. As agreed with your office, we gathered information on areas managed by two agencies: the Department of the Interior’s Bureau of Land Management (BLN) and the Department of Agriculture’s Forest Service. Specifically, this report provides information on (1) legislative guidance and the agency policies governing wilderness study area management, (2) the various activities and uses occurring in the agencies’ study areas, (3) the ways these activities and uses affect the areas, and (4) agency actions to monitor and restrict these uses and to repair damage resulting from them. Appendixes I and II provide data on the number, acreage, and locations of wilderness study areas managed by BLM and the Forest Service, as well as data on the types of uses occurring in the areas. -
Reconstruction of Mid Wisconsin Environments in Southern New Mexico
Articles Arthur H. Harris Reconstruction of Mid Wisconsin Environments in Southern New Mexico Abundant vertebrate remains from two mid-Wisconsin cave deposits in New Mexico allow reconstruction of paleoenvironments. Dry Cave lies in southeastern New Mexico, U-Bar Cave in the extreme southwest (Figure 1). Both sites are in the ecotone between woodland and Chihuahuan Desert vegetations. During the mid Wisconsin, both had vertebrate species indicative of woodland, but otherwise differed greatly. Dry Cave had winter temperatures milder than those at the site today, but otherwise the climate was similar to that now found some 450 km to the north. Except for taxa allowed into the area by mild winters, extralimital forms occur in nearby highland woodlands or in northeastern New Mexico. U-Bar Cave probably lacked winter freezes, had cool summers, and had precipitation more evenly distributed than now. Taxa now as distant as the Great Basin occurred together with species from the nearer highlands. Relatively warm summers and retention of seasonal patterns of precipitation at Dry Cave in contrast to cool summers and decreased seasonality of precipitation at U-Bar Cave produced more extreme biotic differences between the sites than is the case now. Whether this was due to different contemporaneous climatic regimes or to chronological differences between the faunas is uncertain. The last major subdivision of the Pleistocene Epoch is the Wisconsin Age. Between ice advances in the early Wisconsin, terminating around 60 000 B.P., and a major renewal of glacial activity in the late Wisconsin, commencing around 32 000 to 27 000 B. P., there was a long span of less severe climatic conditions, the mid Wisconsin (see Bradley 1985 for age estimates). -
Cenozoic Thermal, Mechanical and Tectonic Evolution of the Rio Grande Rift
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 91, NO. B6, PAGES 6263-6276, MAY 10, 1986 Cenozoic Thermal, Mechanical and Tectonic Evolution of the Rio Grande Rift PAUL MORGAN1 Departmentof Geosciences,Purdue University,West Lafayette, Indiana WILLIAM R. SEAGER Departmentof Earth Sciences,New Mexico State University,Las Cruces MATTHEW P. GOLOMBEK Jet PropulsionLaboratory, CaliforniaInstitute of Technology,Pasadena Careful documentationof the Cenozoicgeologic history of the Rio Grande rift in New Mexico reveals a complexsequence of events.At least two phasesof extensionhave been identified.An early phase of extensionbegan in the mid-Oligocene(about 30 Ma) and may have continuedto the early Miocene (about 18 Ma). This phaseof extensionwas characterizedby local high-strainextension events (locally, 50-100%,regionally, 30-50%), low-anglefaulting, and the developmentof broad, relativelyshallow basins, all indicatingan approximatelyNE-SW •-25ø extensiondirection, consistent with the regionalstress field at that time.Extension events were not synchronousduring early phase extension and were often temporally and spatiallyassociated with major magmatism.A late phaseof extensionoccurred primarily in the late Miocene(10-5 Ma) with minor extensioncontinuing to the present.It was characterizedby apparently synchronous,high-angle faulting givinglarge verticalstrains with relativelyminor lateral strain (5-20%) whichproduced the moderuRio Granderift morphology.Extension direction was approximatelyE-W, consistentwith the contemporaryregional stress field. Late phasegraben or half-grabenbasins cut and often obscureearly phasebroad basins.Early phase extensionalstyle and basin formation indicate a ductilelithosphere, and this extensionoccurred during the climax of Paleogenemagmatic activity in this zone.Late phaseextensional style indicates a more brittle lithosphere,and this extensionfollowed a middle Miocenelull in volcanism.Regional uplift of about1 km appearsto haveaccompanied late phase extension, andrelatively minor volcanism has continued to thepresent.