Geology of Organ Mountains and Southern San Andres Mountains, New Mexico

Total Page:16

File Type:pdf, Size:1020Kb

Geology of Organ Mountains and Southern San Andres Mountains, New Mexico Geology of Organ Mountains and southern San Andres Mountains, New Mexico COVER—"THE SIERRA DE LOS ORGANOS' OR ORGAN MOUNTAINS are so named from their pinnacled summits and sides which resemble the pipes of an organ. They are of a light gray granite, and rise to the height of 3,000 feet above the river. The defiles are filled with large pines and the more open valley, with live oaks. From the place where we halted and lunched, I took a sketch of these mountains and of the defile through which I had passed." (from Bartlett, 1854) FRONTISPIECE: ORGAN MOUNTAINS AND SOUTHERN JORNADA DEL MUERTO; view to east-southeast (photo courtesy of Rollag and Associates, El Paso, Texas). Memoir 36 New Mexico Bureau of Mines & Mineral Resources A DIVISION OF NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY Geology of Organ Mountains and southern San Andres Mountains, New Mexico by William R. Seager SOCORRO 1981 iv NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY KENNETH W. FORD, President NEW MEXICO BUREAU OF MINES & MINERAL RESOURCES FRANK E. KOTTLOWSKI, Director GEORGE S. AUSTIN, Deputy Director BOARD OF REGENTS Ex Officio Bruce King, Governor of New Mexico Leonard DeLayo, Superintendent of Public Instruction Appointed William G. Abbott, President, 1961-1985, Hobbs Judy Floyd, 1977-1987, Las Cruces Owen Lopez, 1977-1983, Santa Fe Dave Rice, 1972-1983, Carlsbad Steve Torres, Secretary-Treasurer, 1967-1985, Socorro BUREAU STAFF Full Time MARLA D. ADKINS, Assistant Editor DAVID W. LOVE, Environmental Geologist ORIN J. ANDERSON, Geologist WESS MAULDIN, Driller's Helper RUBEN ARCHULETA, Technician I VIRGINIA McLEMORE, Geologist KEVIN C. BAKER, Field Researcher LYNNE McNEIL, Staff Secretary ROBERT A. BIEBERMAN, Senior Petrol. Geologist NORMA J. MEEKS, Department Secretary STEVE BLODGETT, Assistant Editor DAVID MENZIE, Geologist LYNN A. BRANDVOLD, Chemist ARLEEN MONTOYA, Librarian/Typist JAMES C. BRANNAN, Draftsperson TERESA A. MUELLER, Draftsperson CORALE BRIERLEY, Chemical Microbiologist SUE NESS, Receptionist BRENDA R. BROADWELL, Assoc. Lab Geoscientist ROBERT M. NORTH, Mineralogist FRANK CAMPBELL, Coal Geologist KEITH O'BRIEN, Hydrologist RICHARD CHAMBERLIN, Economic Geologist JOANNE C. OSBURN, Coal Geologist CHARLES E. CHAPIN, Senior Geologist GLENN R. OSBURN, Volcanologist JEANETTE CHAVEZ, Admin. Secretary I JOAN C. PENDLETON, Associate Editor RICHARD R. CHAVEZ, Assistant Head, Petroleum BARBARA R. POPP, Lab. Biotechnologist RUBEN A. CRESPIN, Laboratory Technician II ROBERT QUICK, Driller LOIS M. DEVLIN, Director, Bus.—Pub. Office MARSHALL A. REITER, Senior Geophysicist KATHY C. EDEN, Editorial Technician JACQUES R. RENAULT, Senior Geologist ROBERT W. EVELETH, Mining Engineer JAMES M. ROBERTSON, Mining Geologist K. BABETTE FARIS, X-ray Lab. Manager GRETCHEN H. ROYBAL, Coal Geologist ROUSSEAU H. FLOWER, Sr. Emeritus Paleontologist AMY SHACKLETT, Asst. Lab Biotechnologist STEPHEN J. FROST, Coal Geologist JACKIE H. SMITH, Laboratory Technician IV JOHN W. HAWLEY, Environmental Geologist DALE STALEY, Driller's Helper DANA M. HELJESON, Editorial Technician WILLIAM J. STONE, Hydrogeologist STEPHEN C. HOOK, Paleontologist SAMUEL THOMPSON III, Petroleum Geologist MELVIN JENNINGS, Metallurgist JUDY M. VAIZA, Executive Secretary BARBARA J. JOHNSON, Staff Secretary DEBRA VETTERMAN, Draftsperson ROBERT W. KELLEY, Editor & Geologist ROBERT H. WEBER, Senior Geologist SHERRY A. KRUKOWSKI, Record Manager DONALD WOLBERG, Vertebrate Paleontologist MARK LOGSDON, Economic Geologist MICHAEL W. WOOLDRIDGE, Scientific Illustrator ANNABELLE LOPEZ, Clerk Typist Part Time CHRISTINA L. BALK, Geologist BEVERLY OHLINE, Newswriter, Information Services HOWARD B. NICKELSON, Coal Geologist THOMAS E. ZIMMERMAN, Chief Security Officer Graduate Students BRUCE W. BAKER ROBERTA EGGLESTON TOM MCANULTY INDIRA BALKISSOON TED EGGLESTON LAWRENCE NELSON GERRY W. CLARKSON ADRIAN HUNT JOHN YOUNG Plus about 50 undergraduate assistants First Printing, 1981 Published by Authority of State of New Mexico, NMSA 1953 Sec. 63-1-4 Printed by University of New Mexico Printing Plant, May, 1981 Available from New Mexico Bureau of Mines & Mineral Resources, Socorro, NM 87801 Price $20.00 v Preface Forty-five years have passed since Sir Kingsley Charles swarms of gnats and small flies infest every bush and rocky crevice along the higher peaks. They can be set into motion just by a Dunham wrote Geology of the Organ Mountains, yet his account ' of the geology of the range is as timely today as it was in 1935 and persons presence and they seem indifferent to insect repellent. his writing style is as much a pleasure to read now as then. His They come at you in clouds, and shortly your ears, eyes, nose, and description of the ore deposits and his petrographic work with the mouth are full. Retreat from the ridge top is the only effective igneous and metamorphic rocks are not likely to be improved upon antidote. At least once in each summer swarms of ladybugs also for many years. Besides being of interest for the local geology, the take over the highest peaks, rendering the rocks orange by their book is also of general value because Dunham carefully martials numbers. evidence from the Organs on such topics as the emplacement of Satisfying experiences far outweigh the disagreeable ones, batholiths, structural and lithologic controls of orebodies, however. Reaching the summit of the range and looking out over metamorphic mineral equilibrium assemblages, and alteration the vast stretches of canyons and ridges below to the broad desert processes. Geology of the Organ Mountains has justly become a beyond is always exhilarating. To come upon unexpected springs classic in the geology of New Mexico. or groves of aspen or Douglas fir is a pleasant surprise and a walk The quality of Dunham's work is such that few additional through a flattish stretch of canyon floor shaded by high Ponderosa geologic studies in the Organ district were published between 1935 pines or ancient juniper trees is a pleasure. Golden eagles and 1980, although many individuals and mining companies used swooping up a canyon toward you, bighorn rams or huge deer Dunham's report as a basis for mineral exploration during the same clashing and locking horns in front of you, newly born, unafraid period. The present study was undertaken partly to integrate the fawns motionless beneath a bush at your side—these are all results of recent exploration activity, geophysical studies, and occasional rewards which more than compensate for the bugs and radiometric dating into Dunham's geologic framework and partly to for the spells of disagreeable weather. Of course, over the long run, show geologic details on greatly improved 7½-min topographic the daily variety for a geologist working in the Organ or San base maps. Additional objectives were: 1) to map previously Andres Mountains is provided by the geology itself. Even if there unmapped portions of the northern Organ and southern San Andres were nothing else to make field work a pleasure, the geologic Mountains that contain features of structural significance, 2) to relations among rocks and structures are sufficiently challenging describe sections of Paleozoic rocks that had not been described in and revealing to insure boredom as an impossibility. Putting detail or subdivided into up-to-date stratigraphic units, and finally together a picture of the geologic relationships and history of the 3) to investigate relationships between the Organ batholith and range can be likened to assembling a huge, complex puzzle with volcanic rocks in the southern Organ range, which recently were half (or more?) of the pieces missing. For a geologist the best part shown to be of the same age. During the course of mapping and of the field experience—aspen, eagles, and fawns from many discussions with John Hawley, I realized that there notwithstanding—is putting that puzzle together. were many kinds and ages of alluvial deposits mantling the edge of ACKNOWLEDGMENTS-Many people have directly or indi- the mountains and that they were related to the general geomorphic rectly contributed to this effort through their advice, critical evolution of the range and to repeated movements on the boundary readings of the text, or with other kinds of help and cooperation. I fault along its eastern margin. Another objective in this study was thank Sam Thompson III, Pete Lipman, Dick Chamberlin, Jerry to distinguish among these deposits and relate them to the Mueller, John Hawley, Tom Giordano, Charles Chapin, Glenn R. Quaternary erosional and faulting history of the range. Osburn, and D. D. Seager for reviewing various chapters of the Field work was done between 1975 and 1978, mostly during the book, Charles B. Hunt for reviewing an early version of the summer months. Working in the summer in the Organ Mountains manuscript and for his help with fig. 83, and especially Vincent C. can be exhilarating, discouraging, rewarding, frightening, or Kelley for reviewing the manuscript in its entirety. The New satisfying, and is always different from day to day. Aside from the Mexico Bureau of Mines and Mineral Resources funded chemical steep slopes, rocky precipices, and occasional rattlesnakes (mostly analyses, and I thank Lynn Brandvold for running those analyses. black-tailed rattlers), nature uses other ways to insure that geologic The University of Arizona geochronology laboratory also provided information does not come easily from the mountains. Many of the some chemical analyses, a radiometric date, and computer analysis higher slopes are covered
Recommended publications
  • An Interpretation of the Structural Geology of the Franklin Mountains, Texas Earl M
    New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/26 An interpretation of the structural geology of the Franklin Mountains, Texas Earl M. P. Lovejoy, 1975, pp. 261-268 in: Las Cruces Country, Seager, W. R.; Clemons, R. E.; Callender, J. F.; [eds.], New Mexico Geological Society 26th Annual Fall Field Conference Guidebook, 376 p. This is one of many related papers that were included in the 1975 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States.
    [Show full text]
  • Prehistoric Trackways National Monument Recreation Area Management Plan
    October 2020 Prehistoric Trackways National Monument Recreation Area Management Plan Environmental Assessment DOI-BLM-NM-L0000-2021-0004-EA Las Cruces District Office 1800 Marquess Street Las Cruces, New Mexico 88005 575-525-4300 TABLE OF CONTENTS CHAPTER 1. INTRODUCTION .................................................................................................. 1 1.1. Purpose and Need ........................................................................................................... 1 1.2. Decision to Be Made ....................................................................................................... 1 1.3. RAMP Planning Process ................................................................................................ 3 1.4. Plan Conformance and Relationship to Statutes and Regulations ............................ 3 1.4.1. Plan Conformance ..................................................................................................... 3 1.4.2. Relationship to Statutes and Regulations .................................................................. 5 1.5. Scoping and Issues .......................................................................................................... 6 1.5.1. Internal Scoping ........................................................................................................ 6 1.5.2. Internal and External Scoping ................................................................................... 7 1.5.3. Issues ........................................................................................................................
    [Show full text]
  • An Environmental History of the Middle Rio Grande Basin
    United States Department of From the Rio to the Sierra: Agriculture Forest Service An Environmental History of Rocky Mountain Research Station the Middle Rio Grande Basin Fort Collins, Colorado 80526 General Technical Report RMRS-GTR-5 Dan Scurlock i Scurlock, Dan. 1998. From the rio to the sierra: An environmental history of the Middle Rio Grande Basin. General Technical Report RMRS-GTR-5. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 440 p. Abstract Various human groups have greatly affected the processes and evolution of Middle Rio Grande Basin ecosystems, especially riparian zones, from A.D. 1540 to the present. Overgrazing, clear-cutting, irrigation farming, fire suppression, intensive hunting, and introduction of exotic plants have combined with droughts and floods to bring about environmental and associated cultural changes in the Basin. As a result of these changes, public laws were passed and agencies created to rectify or mitigate various environmental problems in the region. Although restoration and remedial programs have improved the overall “health” of Basin ecosystems, most old and new environmental problems persist. Keywords: environmental impact, environmental history, historic climate, historic fauna, historic flora, Rio Grande Publisher’s Note The opinions and recommendations expressed in this report are those of the author and do not necessarily reflect the views of the USDA Forest Service. Mention of trade names does not constitute endorsement or recommendation for use by the Federal Government. The author withheld diacritical marks from the Spanish words in text for consistency with English punctuation. Publisher Rocky Mountain Research Station Fort Collins, Colorado May 1998 You may order additional copies of this publication by sending your mailing information in label form through one of the following media.
    [Show full text]
  • Late Paleozoic Tectonic and Sedimentologic History of the Penasco Uplift, North-Central New Mexico
    RICE UNIVERSITY LATE PALEOZOIC TECTONIC AND SEDIMENTOLOGIC HISTORY OF THE PENASCO UPLIFT, NORTH-CENTRAL NEW MEXICO by ROY DONALD ADAMS A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE MASTER OF ARTS APPROVED, THESIS COMMITTEE: 0^ (3- /jtd&i obfe B. Anderson, Chairman Assistant Professor pf Geology KT Rudy R. Schwarzer, Adjunct Assistant Professor of GSology John /E. Warme Professor of Geology Donald R. Baker Professor of Geology Houston, Texas May, 1980 ABSTRACT LATE PALEOZOIC TECTONIC AND SEDIMENTOLOGIC HISTORY OF THE PENASCO UPLIFT, NORTH-CENTRAL NEW MEXICO Roy Donald Adams The Paleozoic Peiiasco Uplift, located on the site of the present Nacimiento Mountains of north-central New Mexico, acted as a sediment source and modifier of regional sedimentation patterns from Middle Pennsylvanian to Early Permian time. The earliest history of the uplift is still poorly defined. Orogenic activity may have started as early as the Late Mississippian, or there may have been quiescence until after deposition of the Morrow-age Osha Canyon Formation and prior to deposition of the Atoka-age Sandia Formation. Coarse, arkosic siliciclastic sediments inter- bedded with fossilferious carbonates in the Madera Formation indicate that by early Desmoinesian time the Peiiasco Uplift had risen sufficiently to expose and erode Precambrian rocks. Paleotransport indicators in the arkosic sediments show transport away from the uplift. Throughout the remainder of the Pennsylvanian, the Peiiasco Uplift was a sediment source. The siliciclastic sediments derived from the Peiiasco Uplift formed a wedge that prograded out onto and interfingered with carbonate sediments of a shallow normal marine shelf. A change in paleotransport directions from northeasterly to southwesterly occurs on the east side of the Peiiasco Uplift and is due to the arrival of a flood of siliciclastic sediments derived from the Uncompahgre-San Luis Uplift to the northeast.
    [Show full text]
  • Porphyry and Other Molybdenum Deposits of Idaho and Montana
    Porphyry and Other Molybdenum Deposits of Idaho and Montana Joseph E. Worthington Idaho Geological Survey University of Idaho Technical Report 07-3 Moscow, Idaho ISBN 1-55765-515-4 CONTENTS Introduction ................................................................................................ 1 Molybdenum Vein Deposits ...................................................................... 2 Tertiary Molybdenum Deposits ................................................................. 2 Little Falls—1 ............................................................................. 3 CUMO—2 .................................................................................. 3 Red Mountain Prospect—45 ...................................................... 3 Rocky Bar District—43 .............................................................. 3 West Eight Mile—37 .................................................................. 3 Devil’s Creek Prospect—46 ....................................................... 3 Walton—8 .................................................................................. 4 Ima—3 ........................................................................................ 4 Liver Peak (a.k.a. Goat Creek)—4 ............................................. 4 Bald Butte—5 ............................................................................. 5 Big Ben—6 ................................................................................. 6 Emigrant Gulch—7 ...................................................................
    [Show full text]
  • Preprint 15-084
    SME Annual Meeting Feb. 15 - 18, 2015, Denver, CO Preprint 15-084 MINERAL DEPOSITS ASSOCIATED WITH TERTIARY ALKALINE IGNEOUS ROCKS IN NEW MEXICO V. T. McLemore, New Mexico Bureau of Geology and Mineral Resources, Socorro, NM ABSTRACT related mineral deposits in New Mexico, (2) discuss the age and formation of these deposits, and (3) comment on the future economic Lindgren (1933) defined a belt of alkaline-igneous rocks associated potential of mineral deposits in New Mexico. This work is part of with large quantities of gold and rare earth elements (REE) that extends ongoing studies of mineral deposits in New Mexico and includes from Alaska and British Columbia southward into New Mexico, Texas and updates and revisions of prior work by North and McLemore (1986, eastern Mexico. The North American Cordilleran alkaline-igneous belt 1988) and McLemore (1996, 2001). Some of the data referred to in this since has been exploited for numerous types of mineral deposits. In New paper is unpublished but available upon request. Mexico, Mid-Tertiary alkaline to calc-alkaline rocks are found with seven types of deposits in these districts: (1) polymetallic epithermal/mesothermal veins, (2) gold-bearing breccias/quartz veins, (3) Cu-Au, Au and Mo porphyry deposits, (4) skarns and carbonate- hosted deposits, (5) iron skarns and replacement bodies (with some gold), (6) gold placers, and (7) Th-REE (with some U, Nb) epithermal veins. Some of New Mexico’s largest gold and REE deposits are found within this belt. Their origin is not well understood, but a compilation of new data (age dates, isotopic and chemical analyses) allows for a better understanding.
    [Show full text]
  • Mule Deer and Antelope Staff Specialist Peregrine Wolff, Wildlife Health Specialist
    STATE OF NEVADA Steve Sisolak, Governor DEPARTMENT OF WILDLIFE Tony Wasley, Director GAME DIVISION Brian F. Wakeling, Chief Mike Cox, Bighorn Sheep and Mountain Goat Staff Specialist Pat Jackson, Predator Management Staff Specialist Cody McKee, Elk Staff Biologist Cody Schroeder, Mule Deer and Antelope Staff Specialist Peregrine Wolff, Wildlife Health Specialist Western Region Southern Region Eastern Region Regional Supervisors Mike Scott Steve Kimble Tom Donham Big Game Biologists Chris Hampson Joe Bennett Travis Allen Carl Lackey Pat Cummings Clint Garrett Kyle Neill Cooper Munson Sarah Hale Ed Partee Kari Huebner Jason Salisbury Matt Jeffress Kody Menghini Tyler Nall Scott Roberts This publication will be made available in an alternative format upon request. Nevada Department of Wildlife receives funding through the Federal Aid in Wildlife Restoration. Federal Laws prohibit discrimination on the basis of race, color, national origin, age, sex, or disability. If you believe you’ve been discriminated against in any NDOW program, activity, or facility, please write to the following: Diversity Program Manager or Director U.S. Fish and Wildlife Service Nevada Department of Wildlife 4401 North Fairfax Drive, Mailstop: 7072-43 6980 Sierra Center Parkway, Suite 120 Arlington, VA 22203 Reno, Nevada 8911-2237 Individuals with hearing impairments may contact the Department via telecommunications device at our Headquarters at 775-688-1500 via a text telephone (TTY) telecommunications device by first calling the State of Nevada Relay Operator at 1-800-326-6868. NEVADA DEPARTMENT OF WILDLIFE 2018-2019 BIG GAME STATUS This program is supported by Federal financial assistance titled “Statewide Game Management” submitted to the U.S.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • The Lower Permian Abo Formation in the Fra Cristobal and Caballo Mountains, Sierra County, New Mexico Spencer G
    New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/63 The Lower Permian Abo Formation in the Fra Cristobal and Caballo Mountains, Sierra County, New Mexico Spencer G. Lucas, Karl Krainer, Dan S. Chaney, William A. DiMichele, Sebastian Voigt, David S. Berman, and Amy C. Henrici, 2012, pp. 345-376 in: Geology of the Warm Springs Region, Lucas, Spencer G.; McLemore, Virginia T.; Lueth, Virgil W.; Spielmann, Justin A.; Krainer, Karl, New Mexico Geological Society 63rd Annual Fall Field Conference Guidebook, 580 p. This is one of many related papers that were included in the 2012 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download.
    [Show full text]
  • 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.
    [Show full text]
  • 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
    [Show full text]