The Geology of Jarilla Mountains, Otero County, New Mexico

Total Page:16

File Type:pdf, Size:1020Kb

The Geology of Jarilla Mountains, Otero County, New Mexico BULLETIN 82 The Geology of the Jarilla Mountains, Otero County, New Mexico By Paul G. Schmidt and Campbell Craddock 1 9 6 4 STATE BUREAU OF MINES AND MINERAL RESOURCES NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY CAMPUS STATION SOCORRO, NEW MEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Alvin J. Thompson, Director THE REGENTS MEMBERS Ex OFFICIO The Honorable Jack M. Campbell ....................... Governor of New Mexico Leonard DeLayo ...................................... Superintendent of Public Instruction APPOINTED MEMBERS William G. Abbott ............................................................................. Hobbs Eugene L. Coulson, M.D. .............................................................. Socorro Thomas M. Cramer ........................................................................ Carlsbad Eva M. Larrazolo (Mrs. Paul F.) ........................................... Albuquerque Richard M. Zimmerly ...................................................................... Socorro For sale by the New Mexico Bureau of Mines and Mineral Resources Campus Station, Socorro, N. Mex.—Price $1.50 Contents Page ABSTRACT ............................................................................................................ 1 INTRODUCTION ............................................................................................... 2 Previous work .................................................................................................... 3 Acknowledgments ............................................................................................. 3 Physiography ...................................................................................................... 3 Climate and vegetation ..................................................................................... 4 Culture ................................................................................................................ 4 SEDIMENTARY ROCKS .................................................................................. 6 Pennsylvanian System ...................................................................................... 6 Lithology ......................................................................................................... 6 Fossils .............................................................................................................. 7 Correlations .................................................................................................... 8 Measured section of Pennsylvanian strata ............................................... 10 Permian System ............................................................................................... 12 Lithology ....................................................................................................... 13 Fossils ............................................................................................................ 14 Correlations ................................................................................................... 16 Measured section of Laborcita and Hueco formations ......................... 18 IGNEOUS ROCKS ........................................................................................... 22 Biotite syenodiorite ......................................................................................... 22 Leucorhyolite ................................................................................................... 22 Monzonite-adamellite ..................................................................................... 23 Orthoclase adamellite ..................................................................................... 26 Dikes ................................................................................................................. 27 Origin of the intrusive rocks ......................................................................... 28 Extrusive igneous rocks ................................................................................. 29 METAMORPHIC ROCKS .............................................................................. 31 Northern area .................................................................................................. 31 Southern area ................................................................................................... 35 STRUCTURAL GEOLOGY ............................................................................. 38 Emplacement of igneous rocks .................................................................... 38 Dikes ................................................................................................................. 40 Folds and faults in sedimentary rocks ........................................................... 40 Mechanics of deformation .............................................................................. 41 GEOMORPHOLOGY ...................................................................................... 43 ECONOMIC GEOLOGY ............................................................................... 43 Nonferrous metals, lode mines ...................................................................... 44 Iron mines .......................................................................................................... 46 Placer operations ............................................................................................... 47 Other ores .......................................................................................................... 48 Future of mining ............................................................................................... 48 Ground water .................................................................................................... 49 GEOLOGIC HISTORY ................................................................................... 51 Precambrian .................................................................................................. 51 Early Paleozoic ............................................................................................. 51 Late Paleozoic ............................................................................................... 52 Mesozoic ........................................................................................................ 52 Cenozoic ........................................................................................................ 53 REFERENCES ................................................................................................... 54 Illustrations FIGURES View of Jarilla Mountains .................................................................. Frontispiece 1. Index map showing location of Jarilla Mountains ................................ 2 2. Nodule of Chaetetes eximius? ....................................................................... 8 3. Thinsections of Chaetetes eximius? ............................................................. 9 4. Isopach map for Pennsylvanian ............................................................. 11 5. Specimens of limestone-pebble conglomerates ................................... 14 6. Silicified log of Dadoxylon in limestone .................................................. 15 7. Thinsection of biotite syenodiorite ........................................................ 23 8. Thinsection of monzonite-adamellite .................................................... 25 9. Thinsection of orthoclase adamellite ..................................................... 27 10. Thinsection of unmetamorphosed limestone ...................................... 32 11. Thinsection of metamorphosed limestone ........................................... 33 12. Reaction of chert nodule with limestone .............................................. 34 13. "Intrusive skarn" ....................................................................................... 37 PLATES 1. Geologic map of the Jarilla Mountains ....................................... In pocket 2. Tabulation of Igneous and Metamorphic Thin Section Data ..................................................................... In pocket Abstract The Jarilla Mountains are a small range of hills in southern New Mexico. The oldest exposed rocks are of Desmoinesian (Pennsylvanian) age; they consist of cherty gray limestone with minor sandstone and shale and are correlated with the Bug Scuffle Member of the Gobbler Formation. This unit is incompletely exposed but is 822 feet thick. Rocks of early to middle Wolfcampian (Permian) and probably latest Pennsylvanian age crop out in the northern and eastern parts of the range. This section is also incompletely exposed but consists of 1200 feet of interbedded thin limestone, siltstone, shale, and conglomerate correlated with the Laborcita Formation, and 1000 feet of gray lime- stone correlated with the Hueco Formation. The Laborcita Formation and possibly the Bug Scuffle Member and the Hueco Formation were deposited in the Orogrande basin, a local subsiding element on the marine shelf of late Pennsylvanian and early Permian time. Igneous stocks, dikes, and sills of probable Tertiary age were in- truded into the Paleozoic rocks. Three main stages of injection are recognized: a massive syenodiorite, followed by monzonite-adamellite of somewhat variable composition, then by adamellite with large ortho- clase phenocrysts. The monzonite-adamellite has in places undergone severe
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]
  • 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
    [Show full text]
  • A Preliminary Assessment of the Geologic Setting, Hydrology, and Geochemistry of the Hueco Tanks Geothermal Area, Texas and New Mexico
    Geological Circular 81-1 APreliminaryAssessmentoftheGeologicSetting,Hydrology,andGeochemistyoftheHuecoTanksGeothermalArea,TexasandNewMexico Christopher D.Henry and James K.Gluck jointly published by Bureau of Economic Geology The University of Texas at Austin Austin, Texas 78712 W. L.Fisher,Director and Texas Energy and Natural Resources Advisory Council Executive Office Building 411 West 13th Street, Suite 800 Austin, Texas 78701 Milton L. Holloway, Executive Director prime funding provided by Texas Energy and Natural Resources Advisory Council throughInteragency Cooperation Contract No.IAC(80-81)-0899 1981 Contents Abstract 1 Introduction 2 Regional geologic setting 2 Origin and locationof geothermal waters 5 Hot wells 5 Source of heat and ground-water flow paths 5 Faults in geothermal area 9 Implications of geophysical data 15 Hydrology 16 Data availability 16 Water-table elevation 17 Substrate permeability 19 Geochemistry 22 Geothermometry 27 Summary 32 Acknowledgments 32 References 33 Appendix A. Well data 35 Appendix B. Chemical analyses Wl Appendix C. Well designations WJ Figures 1. Tectonic map of Hueco Bolson near El Paso, Texas 3 2. Wells in Hueco Tanks geothermal area 6 3. Measured andreported temperatures ( C) of thermal and nonthermal wells 7 4. Depth to bedrock, absolute elevation of bedrock, and inferred normal faults . 10 5. Generalized west-east cross sections in Hueco Tanks geothermal area . .11 6. Depth to water table, absolute elevation of water table, and water- table elevation contours 18 111 7. Percentages of gravel, sand, clay, and bedrock from driller's logs 21 8. Trilinear diagram of thermal and nonthermal waters 24 9. Total dissolved solids and chloride concentrations 25 Tables 1. Saturation indices 28 2.
    [Show full text]
  • 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.
    [Show full text]
  • Santa Fe New Mexican, 09-28-1904 New Mexican Printing Company
    University of New Mexico UNM Digital Repository Santa Fe New Mexican, 1883-1913 New Mexico Historical Newspapers 9-28-1904 Santa Fe New Mexican, 09-28-1904 New Mexican Printing Company Follow this and additional works at: https://digitalrepository.unm.edu/sfnm_news Recommended Citation New Mexican Printing Company. "Santa Fe New Mexican, 09-28-1904." (1904). https://digitalrepository.unm.edu/sfnm_news/2075 This Newspaper is brought to you for free and open access by the New Mexico Historical Newspapers at UNM Digital Repository. It has been accepted for inclusion in Santa Fe New Mexican, 1883-1913 by an authorized administrator of UNM Digital Repository. For more information, please contact [email protected]. h In InI SANTA .J New m.EXICAN VOL. 41. SANTA jpfe; N. M., WEDNESDAY, SEPTEMBER 28, 1904. NO. 188. LETTER WAS SANDOVAL IS BIG TIME NOT FOR RODEY ScenSc New Mexico, A FORGERY IS PROMISED Prominent Citizen of That County Says His Section is For - ;...".!:. President Roosevelt Never Wrote 'Andrews.' Those Who Attend New Mexico to President Donnelly of "Sandoval County will support the Annual Fair in October at Butchers' Union. regular Republican nominee for dele- gate to Congress, whether or not Mr. Albuquerque. Rodey runs on an Independent ticket," said Alejandro Sandoval, a member MANY COPIED AND PRINTED of the Territorial Board of Equaliza- n ATTRACTIONS tion, to a representative of the New Mexican. Mr. Sandoval is a member Have Been In Miner's at Denver Per Com- is Secured for the Occasion' Magazine of the Sandoval County ..Central w' petrator Will Be Prosecuted If mittee and is ina position to known Indian Sacred Fire Dance his will do in the - Apprehended.
    [Show full text]
  • Promise Beheld and the Limits of Place
    Promise Beheld and the Limits of Place A Historic Resource Study of Carlsbad Caverns and Guadalupe Mountains National Parks and the Surrounding Areas By Hal K. Rothman Daniel Holder, Research Associate National Park Service, Southwest Regional Office Series Number Acknowledgments This book would not be possible without the full cooperation of the men and women working for the National Park Service, starting with the superintendents of the two parks, Frank Deckert at Carlsbad Caverns National Park and Larry Henderson at Guadalupe Mountains National Park. One of the true joys of writing about the park system is meeting the professionals who interpret, protect and preserve the nation’s treasures. Just as important are the librarians, archivists and researchers who assisted us at libraries in several states. There are too many to mention individuals, so all we can say is thank you to all those people who guided us through the catalogs, pulled books and documents for us, and filed them back away after we left. One individual who deserves special mention is Jed Howard of Carlsbad, who provided local insight into the area’s national parks. Through his position with the Southeastern New Mexico Historical Society, he supplied many of the photographs in this book. We sincerely appreciate all of his help. And finally, this book is the product of many sacrifices on the part of our families. This book is dedicated to LauraLee and Lucille, who gave us the time to write it, and Talia, Brent, and Megan, who provide the reasons for writing. Hal Rothman Dan Holder September 1998 i Executive Summary Located on the great Permian Uplift, the Guadalupe Mountains and Carlsbad Caverns national parks area is rich in prehistory and history.
    [Show full text]
  • 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.
    [Show full text]
  • Silver and Gold Occurrences in New Mexico by Robert M
    New Mexico Bureau of Mines & Mineral Resources Resource Map 15 March 1986 Silver and gold occurrences in New Mexico by Robert M. North and Virginia T. Mclemore New Mexico Bureau of Mines and Mineral Resources, Socorro, New Mexico 87801 Abstract Anomalous amounts of silver and/or gold have been identified in 153 mining districts or prospect areas of New Mexico. Production from most of these occurrences has been small; figures or estimates are given when known. Thirty-five districts have produced in excess of 10,000 troy ounces of gold or 200,000 ounces of silver. Silver and gold in New Mexico occur in 14 distinct types of deposits ranging in age from Precam­ brian (Proterozoic) to Recent. Mid-Tertiary to Recent deposits include the placer, volcanic-epithermal, supergene copper-uranium (silver), and Great Plains Margin types. Late Cretaceous to mid-Tertiary deposits include the sedimentary-hydrothermal barite-fluorite-galena, carbonate-hosted silver (lead­ manganese ), lead-zinc and copper skarn, Laramide vein, and prophyry-copper types. Late Paleozoic to early Mesozoic deposits include the sedimentary-copper type and possibly some of the Permian Mississippi Valley type. Precambrian deposits include the vein and replacement and Precambrian massive-sulfide types. Deposits that have produced significant silver and/or gold as the primary product are the placer, volcanic-epithermal, Great Plains Margin, carbonate-hosted silver, and Lar­ amide vein types. Deposits that have produced significant precious metals as a byproduct of base­ metal mining include the carbonate-hosted lead-zinc, copper skarn, and porphyry-copper types. Introduction Precious metals in varying degrees of importance or 14 ppm (0.41 oz/ton) silver.
    [Show full text]
  • Burned the Crucifixes and Other Religious Objects That Had Been Scattered in and Around the Pueblo. Otermin's Army Repeated This
    burned the crucifixes and other religious objects not successful in reestablishing Spanish rule of that had been scattered in and around the the Pueblos, the interviews and explorations pueblo. Otermin's army repeated this ritual at Otermin and Mendoza conducted give the most Alamillo and Sevilleta. A short distance from complete picture of the effects of the revolt Sevilleta the army found deep pits where the among the pueblos. The Spanish presidio at El Indians had cached corn and protected it with a Paso sent two more punitive expeditions to New shrine of herbs. feathers and a clay vessel Mexico in 1688 and 1689 but it was not until the modeled with a human face and the body of a toad term of Governor Don Diego de Vargas (1690-1696) (Hackett and Shelby 1942:I:cxxix). On the march that New Mexico was reclaimed by Spain. from Socorro to Isleta. the army passed through the burned remains of four estancias. The The Aftermath of the Revolt estancia of Las Barrancas, located 23 leagues beyond Senecu and ten leagues downstream from Documentation of the 12-year period following the Isleta, was the only estancia that had not been Pueblo Revolt is scarce but speculation and greatly vandalized and burned (Hackett and Shelby conjecture abound. The more dramatic recon­ 1942:cxxx). structions of life among the Pueblos after the revolt show the Pueblos having destroyed every Otermin staged a surprise attack, taking Isleta vestige of Hispanic culture, including household Pueblo on December 6, 1681. About 500 Isleta and and religious objects, domesticated animals and Piro Indians were living in the village at the cereal crops.
    [Show full text]
  • Mineral and Energy Resources of the BLM Roswell Resource Area, East-Central New Mexico
    U. S. DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY Mineral and Energy Resources of the BLM Roswell Resource Area, East-central New Mexico by Susan Bartsch-Winkleri, editor Open-File Report 92-0261 1992 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1 Denver, Colorado iMail Stop 937 Federal Center P.O. Box 25046 Denver, Colorado 80225 MINERAL AND ENERGY RESOURCES OF THE BLM ROSWELL RESOURCE AREA, EAST-CENTRAL NEW MEXICO Summary.......................................................................................... 1 Introduction.................................................................................... 1 Location and geography of study area...................................... 1 Purpose and methodology........................................................ 3 Acknowledgements......................................................................... 4 Geology of east-central New Mexico, by Susan Bartsch-Winkler, with a section on Intrusive and extrusive alkaline rocks of the Lincoln County porphyry belt by Theodore J. Armbrustmacher 4 General..................................................................................... 4 Structure................................................................................. 5 Uplifts........................................................................
    [Show full text]
  • Bulletin 39: the Metal Resources of New Mexico and Their Economic
    BULLETIN 3 9 The Metal Resources of New Mexico and Their Economic Features Through 1954 A revision of Bulletin 7, by Lasky and Wootton, with detailed information for the years 1932-1954 BY EUGENE CARTER ANDERSON 1957 STATE BUREAU OF MINES AND MINERAL RESOURCES NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY CAMPUS STATION SOCORRO, NEW MEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Alvin J. Thompson, Director THE REGENTS MEMBERS EX OFFICIO THE HONORABLE EDWIN L. MECHEM………...Governor of New Mexico MRS. GEORGIA L. LUSK ......................Superintendent of Public Instruction APPOINTED MEMBERS ROBERT W. BOTTS ....................................................................Albuquerque HOLM O. BURSUM, JR. .....................................................................Socorro THOMAS M. CRAMER .................................................................... Carlsbad JOHN N. MATHEWS, JR. ...................................................................Socorro RICHARD A. MATUSZESKI ......................................................Albuquerque Contents Page INTRODUCTION .......................................................................................................... 1 Purpose and Scope of Bulletin ..................................................................................... 1 Other Reports Dealing With the Geology and Mineral Resources of New Mexico ......................................................................................................
    [Show full text]
  • Features of the Tularosa Basin Place Names in New Mexico, As You Might Imagine, Often Derive from Native American, Spanish, and Anglo Words and Family Names
    National Park Service White Sands Department of the Interior White Sands National Monument Features of the Tularosa Basin Place names in New Mexico, as you might imagine, often derive from Native American, Spanish, and Anglo words and family names. The Tularosa Basin is no exception—the word “tularosa” is Spanish for “reddish reeds.” Like much of the American Southwest, the basin is full of such colorful place names. Below you’ll find a description of the most significant features, arranged to correspond with the accompanying map. The Chupadera Mesa is an upland rising at the north end of the Tularosa Basin. Chupadera probably refers to “sinkholes”—although geographer T. M. Pearce says that it could also refer to “sucking insects.” Chupadero The Oscura Mountains form the northwest border of the Tularosa Mesa basin. Oscura means “dark” in Spanish, and with their piñon and juniper forested tops, the Oscura Mountains can appear darker than the neighboring San Andres Mountain range to the south. The highest elevation in the range is Oscura Peak at 8,732 feet high. The San Andres Mountains border the Tularosa Basin on the west. The range extends approximately 75 miles north to south. The highest Oscura point is Salinas Peak, with an elevation just under 9,000 feet. The Mountains southern San Andres Mountains are home to a wildlife refuge of the same name. However, the San Andres National Wildlife Refuge and the San Andres Mountains are within the boundaries of the White * Carrizozo Sands Missile Range and therefore closed to public access. The Oscura Mountains to the north are separated from the San Andres range at Mockingbird Gap, while the Organ Mountains to the south are separated from the San Andres by San Augustin Pass.
    [Show full text]