Geohydrology of the San Agustin Basin, Alamosa Creek Basin

Total Page:16

File Type:pdf, Size:1020Kb

Geohydrology of the San Agustin Basin, Alamosa Creek Basin Geohydrology of the San Agustin Basin, Alamosa Creek Basin upstream from Monticello Box, and upper Gila Basin in parts of Catron, Socorro, and Sierra Counties, New Mexico By R.G. Myers, J.T. Everheart, and C.A. Wilson U.S. GEOLOGICAL SURVEY WATER-RESOURCES INVESTIGATIONS REPORT 94-4125 Prepared in cooperation with the NEW MEXICO STATE ENGINEER OFFICE Albuquerque, New Mexico 1994 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director For additional information Copies of this report can write to: be purchased from: U.S. Geological Survey District Chief Earth Science Information Center U.S. Geological Survey Open-File Reports Section Water Resources Division Box 25286, MS 517 4501 Indian School Rd. NE, Suite 200 Denver Federal Center Albuquerque, New Mexico 87110 Denver, Colorado 80225 CONTENTS Page Abstract.................................................................................................................................................. 1 Introduction........................................................................................................................................... 1 Purpose and scope...................................................................................................................... 3 Location and extent.................................................................................................................... 3 Ctimate....................................^ 3 Previous hydrologic investigations.......................................................................................... 4 Well- and spring-numbering system....................................................................................... 4 Acknowledgments...................................................................................................................... 5 Geohydrology........................................................................................................................................ 5 Regional setting and geologic history...................................................................................... 5 Geologic units and water-yielding characteristics................................................................. 9 Quaternary Period ........................................................................................................... 9 Quaternary and Tertiary Period...................................................................................... 10 Tertiary Period................................................................................................................... 10 Cretaceous Period............................................................................................................. 11 Triassic Period.................................................................................................................... 11 Permian Period.................................................................................................................. 11 Pennsylvanian Period....................................................................................................... 12 Soils........................................................................................................................... 12 Aquifer characteristics determined from geophysical studies............................................. 12 Surface electrical-resistivity soundings.......................................................................... 12 Gravity anomalies............................................................................................................. 14 Ground-water hydrology........................................................................................................... 17 San Agustin bolson-fill aquifer....................................................................................... 18 Datil aquifer....................................................................................................................... 24 Shallow upland aquifers.................................................................................................. 24 Alamosa Creek shallow aquifer...................................................................................... 26 Geothermal potential.................................................................................................................. 26 Summary................................................................................................................................................ 29 References.............................................................................................................................................. 30 111 PLATES (In pocket) Plate 1. Map showing location of wells, springs, vertical electrical-resistivity soundings/ and geohydrologic sections in the San Agustin Basin/ Alamosa Creek Basin upstream from Monticello Box/ and upper Gila Basin in parts of Catron, Socorro/ and Sierra Counties/ New Mexico. 2. Geohydrologic sections of the Plains of San Agustin. FIGURES Page Figure 1. Map showing location and physiographic features of the study area........................ 2 2. Diagram showing system of numbering wells and springs in New Mexico.............. 5 3. Map showing structural features of the study area and vicinity.................................. 6 4. Map showing surh'cial geology......................................................................................... 7 5. Map showing soil types...................................................................................................... 13 6. Map showing altitude of the bedrock surface in the Plains of San Agustin.............. 15 7. Complete Bouguer anomaly map..................................................................................... 16 8. Map showing approximate altitude of the water table in the San Agustin bolson-fill aquifer within the Plains of San Agustin................................................. 19 9. Map showing approximate saturated thickness of San Agustin bolson-fill aquifer containing freshwater in the Plains of San Agustin.................................................. 22 10. Map showing approximate altitude of the saline/freshwater interface in the Plains of San Agustin................................................................................................................ 23 11. Map showing approximate altitude of the water table in the Datil aquifer............... 25 12. Map showing approximate altitude of the water table in the Alamosa Creek shallow aquifer............................................................................................................... 27 13. Map showing wells and springs with a point-of-discharge temperature equal to or greater than 21 degrees Celsius............................................................... 28 IV TABLES Page Table 1. Soil types in the San Agustin study area............................................................................ 33 2. Records of selected wells in the San Agustin study area................................................. 34 3. Records of selected springs in the San Agustin study area............................................. 49 4. On-site specific-conductance and temperature measurements of water from selected wells and springs in the San Agustin study area.......................................... 55 5. Water-quality analyses for selected wells and springs in the San Agustin study area........................................................................................................................... 62 6. Trace elements in water from selected wells and springs in the San Agustin study area........................................................................................................................... 66 7. Radiochemical analyses of water from selected wells and springs in the San Agustin study area............................................................................................................ 69 CONVERSION FACTORS AND VERTICAL DATUM Multiply By To obtain acre 4,047 square meter acre 0.4047 hectare acre-foot 1,233 cubic meter cubic foot per second 0.02832 cubic meter per second foot 0.3048 meter foot per mile 0.1894 meter per kilometer foot per day 0.3048 meter per day foot squared per day 0.0929 meter squared per day gallon per minute per foot 0.2070 liter per second per meter gallon 3.785 liter gallon per minute 0.06309 liter per second inch 25.4 millimeter mile 1.609 kilometer square mile 2.590 square kilometer Temperature in degrees Fahrenheit ( °F) or degrees Celsius (°C) can be converted as follows: °C = 5/9(°F-32) °F = 9/5(°C) + 32 Sea level: In this report "sea level" refers to the National Geodetic Vertical Datum of 1929 a geodetic datum derived from a general adjustment of the first-order level nets of the United States and Canada, formerly called Sea Level Datum of 1929. GEOHYDROLOGY OF THE SAN AGUSTIN BASIN, ALAMOSA CREEK BASIN UPSTREAM FROM MONTICELLO BOX, AND UPPER GILA BASIN IN PARTS OF CATRON, SOCORRO, AND SIERRA COUNTIES, NEW MEXICO By R.G. Myers, J.T. Everheart, and C.A. Wttson ABSTRACT The San Agustin Basin, the Alamosa Creek Basin upstream from Monticello Box, and the upper Gila Basin are located in parts of Catron, Socorro, and Sierra Counties in west-central New Mexico. Four major aquifers are within the study area: (1) the San Agustin bolson-fill aquifer; (2) the Datil aquifer; (3) the shallow upland aquifers; and (4) the Alamosa
Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Petrology, Diagenesis, and Genetic Stratigraphy of the Eocene Baca Formation, Alamo Navajo Reservation and Vicinity, Socorro County, New Mexico
    OPEN FILE REPORT 125 PETROLOGY, DIAGENESIS, AND GENETIC STRATIGRAPHY OF THE EOCENE BACA FORMATION, ALAMO NAVAJO RESERVATION AND VICINITY, SOCORRO COUNTY, NEW MEXICO APPROVED : PETROLOGY, DIAGENESIS, AND GENETIC STRATIGRAPHYOF THE EOCENE BACA FORMATION, ALAMO NAVAJO RESERVATION AND VICINITY, SOCORRO COUNTY, NEW MEXICO by STEVEN MARTIN CATHER,B.S. THESIS Presented to the Facultyof the Graduate School of The Universityof Texas at Austin in Partial Fulfillment of the Requirements for the Degreeof MASTER OF ARTS THE UNIVERSITYOF TEXAS AT AUSTIN August 1980 ACKNOWLEDGMENTS I wish to sincerelythank Drs. R. L. Folkand C. E. Chapin fortheir enthusiasmtoward this study and theirpatience in tutoring a novicegeologist in their respectivefields of expertise. Dr. A. J. Scott provided many helpful comments concerning lacustrinesedimentation and thesisillustrations. Discussions with BruceJohnson contributedgreatly to my understanding of thedistribution of facies and paleoenvironments within the Baca-Eagar basin. I would also like to thank my colleaguesin Austin and e Socorrofor their helpful comments and criticisms. Bob Blodgettserved as studenteditor. Finally, I would like to acknowledge JerryGarcia, who providedunending inspiration and motivation throughout the course of this study. Financialsupport for field work and the writing of this manuscript wa-s generously provided by the New Mexico Bureau of Mines andMineral Resources. The University of TexasGeology Foundationalso provided funds for travel expenses and field work. This thesis was submitted tothe committee in June, 1980. iii PETROLOGY, DIAGENESIS, AND GENETIC STRATIGRAPHY OF THE EOCENE BACA FORMATION, AIAMO NAVAJO RESERVATION AND VICINITY, SOCORRO COUNTY, NEW MEXICO by Steven M. Cather ABSTRACT The Eocene Baca Formation of New Mexico and. correlative EagarFormation and Mogollon Rim gravels of Arizonacomprise a redbedsequence conglomerate,of sandstone, mudstone,and claystone which cropsout from near Socorro, New Mexico, to the Mogollon Rim of Arizona.
    [Show full text]
  • 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
    [Show full text]
  • 2013 NMGS Spring Meeting: Abstract-67
    TOWARD STANDARDIZATION OF PHANEROZOIC STRATIGRAPHIC NOMENCLATURE IN NEW MEXICO Steven M. Cather1, Kate E. Zeigler2, Greg H. Mack3 and Shari A. Kelley1 1New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, 801 Leroy Pl., Socorro, NM, 87801, [email protected] 2Department of Natural Resources Management, New Mexico Highlands University, Las Vegas, NM, 87701 3Department of Geological Sciences, New Mexico State University, Las Cruces, NM, 88003 Recent decades have seen an unprecedented rate of change in the Phanerozoic stratigraphic nomenclature of New Mexico. At the same time, the state has experienced a dramatic resurgence of geologic quadrangle mapping, primarily facilitated by the National Geologic Mapping Act of 1992, which enabled the STATEMAP and EDMAP programs. The utility of the new stratigraphic nomenclature has not yet been adequately tested, and in some cases has been opposed by other researchers. Despite a lack of consensus among stratigraphers, it is desirable to have an agreed-upon nomenclature for the purpose of ongoing geologic mapping. We present here, from our perspective as geologic mappers, revisions to the Phanerozoic stratigraphic nomenclature of New Mexico. We hope our discussion will eventually lead to adoption of a standardized nomenclature, for the purposes of mapping, by the New Mexico Bureau of Geology and Mineral Resources, which administers the STATEMAP and EDMAP programs in New Mexico. Here we criticize, and suggest alternatives to, aspects of recent nomenclatural
    [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]
  • Stratigraphy, Age, and Rates of Deposition of the Datil Group (Upper
    Stratigraphy,age, and rates of deposition ol the Datil Group (Upper Eocene-Lower0ligocene), west-central New Mexico bySteren M. Cather,Willian C. Mclntosh, and Charles E. Chapin,New Mexico Bureau of Minesand Mineral Resources, Socorro, NM 87801 Introduction Stratigraphyand contacts The Datil Group, formerly called the SpearsFormation, comprises The term Datil Formation was coined by Winchester(1920), but a seriesof volcaniclasticrocks, lava flows, and ash-flow tuffs that its usagehas since evolved considerably(see, for example,Elston, crops out in a broad, west-trending swath of discontinuous expo- 1976;Cather, 1986).In this report, we employ the nomenclatureof suresin west-centralNew Mexico.The Datil Group is the oldestunit Osburn and Chapin (1983),who restrict usage of the Datil Group in the_northern Mogollon-Datil volcanic field, and ranges in thick- to the volcanic and volcaniclastic rocks that occur belowHells Mesa ness from more than 1 km to about 300 m where it onlaps late Tuff. In addition, we divide the Datil Group into two informal units, Laramideuplifts. This report summarizespart of a doctoral disser- the lower Datil and the upper Datil (Fig. 2). tation on the Datil Group (Cathea 1986)and incorporates15 new The lower Datil is dominatedby andesiticvolcaniclastic rocks that {rdiometric datesby Mclntosh et al. (1986),Mclntosh (in progress), are characterizedby phenocrystic plagioclase,amphibole, and ti- C. E. Chapin (unpublished),and Cather (1986).To facilitatediscus- tanomagnetite(+ biotite). Silicacontent in Datil andesitestypically sion of various Datil Group exposureswithin the study area, we rangesfrom 58 Io 64 wt. percent.Throughout most of the northern have divided the outcrop belt into geographicsegments'(Fig 1).
    [Show full text]
  • Subsurface Geologic Plates of Eastern Arizona and Western New Mexico
    Implications of Live Oil Shows in an Eastern Arizona Geothermal Test (1 Alpine-Federal) by Steven L. Rauzi Oil and Gas Program Administrator Arizona Geological Survey Open-File Report 94-1 Version 2.0 June, 2009 Arizona Geological Survey 416 W. Congress St., #100, Tucson, Arizona 85701 INTRODUCTION The 1 Alpine-Federal geothermal test, at an elevation of 8,556 feet in eastern Arizona, was drilled by the Arizona Department of Commerce and U.S. Department of Energy to obtain information about the hot-dry-rock potential of Precambrian rocks in the Alpine-Nutrioso area, a region of extensive basaltic volcanism in southern Apache County. The hole reached total depth of 4,505 feet in August 1993. Temperature measurements were taken through October 1993 when final temperature, gamma ray, and neutron logs were run. The Alpine-Federal hole is located just east of U.S. Highway 180/191 (old 180/666) at the divide between Alpine and Nutrioso, in sec. 23, T. 6 N., R. 30 E., in the Apache-Sitgreaves National Forest (Fig. 1). The town of Alpine is about 6 miles south of the wellsite and the Arizona-New Mexico state line is about 6 miles east. The basaltic Springerville volcanic field is just north of the wellsite (Crumpler, L.S., Aubele, J.C., and Condit, C.D., 1994). Although volcanic rocks of middle Miocene to Oligocene age (Reynolds, 1988) are widespread in the region, erosion has removed them from the main valleys between Alpine and Nutrioso. As a result, the 1 Alpine-Federal was spudded in sedimentary strata of Oligocene to Eocene age (Reynolds, 1988).
    [Show full text]
  • Mother Hubbard
    Gila National Forest Plan Revision Evaluation Report of Lands Inventoried for Potential Wilderness Characteristics Final Report, December 2019 Cover Photo by Eric Flood: Gila River, Gila Wilderness In accordance with Federal civil rights law and U.S. Department of Agriculture (USDA) civil rights regulations and policies, the USDA, its Agencies, offices, and employees, and institutions participating in or administering USDA programs are prohibited from discriminating based on race, color, national origin, religion, sex, gender identity (including gender expression), sexual orientation, disability, age, marital status, family/parental status, income derived from a public assistance program, political beliefs, or reprisal or retaliation for prior civil rights activity, in any program or activity conducted or funded by USDA (not all bases apply to all programs). Remedies and complaint filing deadlines vary by program or incident. Persons with disabilities who require alternative means of communication for program information (e.g., Braille, large print, audiotape, American Sign Language, etc.) should contact the responsible Agency or USDA’s TARGET Center at (202) 720-2600 (voice and TTY) or contact USDA through the Federal Relay Service at (800) 877-8339. Additionally, program information may be made available in languages other than English. To file a program discrimination complaint, complete the USDA Program Discrimination Complaint Form, AD-3027, found online at http://www.ascr.usda.gov/complaint_filing_cust.html and at any USDA office or write a letter addressed to USDA and provide in the letter all of the information requested in the form. To request a copy of the complaint form, call (866) 632-9992. Submit your completed form or letter to USDA by: (1) mail: U.S.
    [Show full text]
  • Jaguar Critical Habitat Comments in Response to 71 FR 50214-50242 (Aug
    October 19, 2012 Submitted on-line via www.regulations.gov, Docket No. FWS-R2-ES-2012-0042. Re: Jaguar critical habitat comments in response to 71 FR 50214-50242 (Aug. 20, 2012). To Whom it May Concern, The Center for Biological Diversity supports the designation of the entirety of the areas that the Fish and Wildlife Service proposes as critical habitat. However, these areas are not sufficient to conserve the jaguar in the United States. Nor does the Service’s itemization of threats to critical habitat areas cover the array of actions that would in fact destroy or adversely modify them. As we explain in detail in the comments below and through evidence presented in our appended letter of 10/1/2012 on the Recovery Outline for the Jaguar, we request seven principal changes in the final critical habitat designation rule, as follows: 1. The following additional mountain ranges within the current boundary of the Northwestern Recovery Unit (as described in the April 2012 Recovery Outline for the Jaguar) should be designated as critical habitat: in Arizona, the Chiricahua, Dos Cabezas, Dragoon and Mule mountains, and in New Mexico the Animas and adjoining Pyramid mountains. 2. The following additional “sky island” mountain ranges outside of the current boundaries of the Northwestern Recovery Unit should be designated as critical habitat: In New Mexico, the Alama Hueco, Big Hatchet, Little Hatchet, Florida, West and East Potrillo, Cedar and Big Burro mountains; in Arizona, the Galiuro, Santa Teresa, Pinaleno, Whitlock, Santa Catalina and Rincon mountains. Straddling both states, the Peloncillo Mountains north of the current boundaries of the Northwestern Recovery Unit should also be designated 3.
    [Show full text]
  • Summary of the Geology and Resources of Uranium in the San Juan Basin and Adjacent Region
    u~c..~ OFR :J8- 'JtgLJ all''1 I. i \ "' ! .SUHMARY OF THE GEOLOGY .ANp RESOURCES OF ,URANIUM IN THE SAN JUAN BASIN AND ADJACENT 'REGION, NEW MEXICO, ARIZONA, UTAH & COLORADO I , J.L. Ridgley, et. al. 1978 US. 6EOL~ SURVEY ~RD, US'RARY 505 MARQU51"1"5 NW, RM 72e I .1\LB'U·QuERQ~, N.M. 87'102 i I UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY SUMMARY OF THE GEOLOGY AND RESOURCES OF URANIUM IN THE SAN JUAN BASIN AND ADJACENT REGION, NEW MEXICO, A~IZONA, UTAH, AND COLORADO 'V'R.0 t ~.-4~ . GICAL SURVEY p.· ..... P• 0 . .:.;J .. _. ·5 ALBU~U~~QUE, N. By Jennie L. Ridgley, Morris W. Green, Charles T. Pierson, • Warren I. Finch, and Robert D. Lupe Open-file Report 78-964 1978 Contents • Page Abstract Introduction 3 General geologic setting 3 Stratigraphy and depositional environments 4 Rocks of Precambrian age 5 .. Rocks of Cambrian age 5 < 'I Ignacio Quartzite 6 Rocks of Devonian age 6... i Aneth Formation 6 Elbert Formation 7 Ouray Limestone 7 Rocks of Mississippian age 8 Redwall Limestone 8 Leadville Limestone 8 Kelly Limestone 9 Arroyo Penasco Group 10 Log Springs Formation 10 Rocks of Pennsylvanian age 11 Molas Formation 11 ~ermosa Formation 12 .' . Ric9 Formation'· 13 .. •;,. Sandia Fotfuatto~ 13 Madera Limestone 14 Unnamed Pennsylvanian rocks 15 • ii • Rocks of Permian age 15 Bursum Formation 16 Abo Formation 16 Cutler Formation 17. Yeso Formation 18 Glorieta Sandstone 19 San Andres Limestone 19 Rocks of Triassic age 20 Moenkopi(?) Formation 21 Chinle Formation 21 Shinarump Member 21 Monitor Butte Member 22 Petrified Forest
    [Show full text]
  • Brave Christian Soldiers: the New Mexico Territorial Militia in the Civil War
    New Mexico Historical Review Volume 89 Number 3 Article 2 7-1-2014 Brave Christian Soldiers: The New Mexico Territorial Militia in the Civil War Jerry D. Thompson Follow this and additional works at: https://digitalrepository.unm.edu/nmhr Recommended Citation Thompson, Jerry D.. "Brave Christian Soldiers: The New Mexico Territorial Militia in the Civil War." New Mexico Historical Review 89, 3 (2014). https://digitalrepository.unm.edu/nmhr/vol89/iss3/2 This Article is brought to you for free and open access by UNM Digital Repository. It has been accepted for inclusion in New Mexico Historical Review by an authorized editor of UNM Digital Repository. For more information, please contact [email protected], [email protected], [email protected]. • Brave Christian Soldiers • The New Mexico Territorial Militia in the Civil War JERRY D. THOMPSON he mood in the capital was one of confusion and great anxiety on the cold wintry morning of 1 February 1862. New York–born Surveyor Gen. TJohn Anderson Clark watched the arrival of several militia companies, all scurrying south to meet a large Confederate Army that was reported to be moving out of the Mesilla Valley. “Today was the arrival in the town of two or three small companies of yeomanry on their way to war,” Clark recorded. “They leave tomorrow for the South—of course these undisciplined troops will not be taken to meet the enemy in the open field, but will be used as guerrillas and to garrison posts.”1 The next day, after the militia marched to St. Francis Church and lined up in formation, Bishop Jean-Baptiste Lamy appeared in full regalia on the steps of the adobe edifice.
    [Show full text]