United States Geological Survey a Comparison of Paleozoic Sections in Southern New Mexico

Total Page:16

File Type:pdf, Size:1020Kb

United States Geological Survey a Comparison of Paleozoic Sections in Southern New Mexico V- DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director PROFESSIONAL PAPER 108 C A COMPARISON OF PALEOZOIC SECTIONS IN SOUTHERN NEW MEXICO BY N. H. DARTON Published May 29,1917 Shorter contributions to general geology, 1917 (Pages 31-55) WASHINGTON GOVERNMENT PRINTING OFFICE 1917 DEPARTMENT OF THE INTERIOR FRANKLIN K. LANE, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Professional Paper 108 C A COMPARISON OF PALEOZOIC SECTIONS IN SOUTHERN NEW MEXICO BY N. H. DARTON Published May 29,1917 Shorter contributions to general geology, 1917 (Pages 31-55) WASHINGTON GOVERNMENT PRINTING OFFICE 1917 CONTENTS. Page. Page. Introduction..................................... 31 Silurian system Continued, Cambrian system................................ 32 Fusselman limestone Continued. General features............................ 32 41 Bliss sandstone............................... 32 41 Franklin Mountains....................... 32 Caballos Mountains. ................... 41 Florida Mountains and Cooks Range...... 32 42 Silver City region.... + .................... 32 42 Caballos Mountains.. .j................... 33 42 San Andres Mountains..................... 33 42 Sacramento Mountains.................... 33 43 Mimbres Mountains..................... 33 43 Ordovician system................................ 34 44 General features............................ 34 44 El Paso limestone............................ 34 44 Franklin Mountains....................... 34 44 Florida Mountains........................ 34 44 Cooks Range............................. 34 Florida Mountains .................... 44 Snake Hills.............................. 35 Silver City. ........................... 44 Victorio Mountains........................ qc 44 Klondike Hills............................ 35 45 Silver City region......................... qc 45 Caballos Mountains...................... qc San Andres Mountains. ................ 45 Lake Valley district..................... 35 45 Mimbres Mountains....................... qc Age and correlation ................... 46 San Andres Mountains................... 35 46 Sacramento Mountains.................... 36 46 Fossils................................... q« 47 Age and correlation........................ q« 47 Montoya limestone............................ q7 Orvnlra "RdTiom 48 General relations...........:.............. q7 48 Franklin Mountains....................... q7 48 Luna County............................. q7 48 Silver City region......................... qo 48 Caballos Mountains and adjoining regions. qc 49 Lake Valley............................... qc 49 Mimbres Mountains...................... qa 50 San Andres Mountains................... qq 50 Sacramento Mountains.................... qq Magdalena group ............................ 53 Fossils................................... qq Cooks Range. .......................... 53 Age and correlation....................... 40 Silver City region....................... 53 Silurian system.................................... 41 53 Fusselman limestone......................... 41 53 Franklin Mountains and eastward........ 41 Gym limestone ............................. 53 Cooks Range............................. 41 Hueco limestone. f ..................... 55 Florida Mountains........................ 41 Geologic history. .............................. 55 ni ILLUSTRATIONS. PLATE XIII. Map of part of New Mexico and adjoin­ FIGURE 2. Columnar sections showing atratigraphic ing regions, showing relations of relations of Paleozoic rocks in southern lower Paleozoic rocks.............. 32 New Mexico........................ 31 XIV. A, Bliss sandstone in Bennett Can­ 3. Section across the Franklin Mountain? yon, 18 miles northeast of Las 3 miles north of El Paso, Tex......... 32 Cruces, N. Mex.; B, West face of 4. Section across Cooks Range at Cooks, Sandia Mountains at Bernalillo, N.Mex............................. 35 N. Mex.......................... 32 5. Section through the Klondike Hills, XV. Views on east side of San Andres Luna County, N. Mex................ 36 Mountains, west of Alamogordo, 6. Section through the Snake Hills, south­ N. Mex.: A, View looking east out west of Deming, N. Mex............. 37 of mouth of Hembrillo Canyon; B, 7. Cross section showing relations of Paleo­ View looking northeast in Good- zoic rocks in the Silver City region, fortune Canyon................... 33 N.Mex............................. 38 XVI. A, West face of Caballos Mountains 8. Section across the Caballos Mountains, near Apache Canyon, Sierra County, southwest of Engle, N. Mex......... 39 N. Mex.; B, Paleozoic rocks on 9. Sections across the San Andres Moun­ granite at Capitol Dome, Florida tains, Socorro and Dona Ana counties, Mountains, Luna County, N. Mex.. 34 N. Mex............................ 42 XVII. A, Sierra Cuchillo west of Palomas 10. Section through the Lake Valley mining- Springs, N. Mex.; B, Fault in lime­ district, Sierra County, N. Mex...... 44 stone at Palomas Gap, Caballos 11. Columnar sections showing stratigraphic Mountains, Sierra County, N. Mex.. 35 variations in lower Paleozoic rocks in XVIII. A, Limestones from Ordovician to the San Andres Mountains, Dona Ana Pennsylvanian on granite, Sheep and Socorro counties,N.Mex......... 45 Mountain, San Andres Mountains, 12. Section from the Mimbres Mountainr Socorro County, N. Mex.; B, East eastward through Kingston and Hilla- face of San Andres Mountains at boro. N. Mex....................... 48 Rhodes Canyon, Socorro County, 13. Section of the west front of the Sacra­ N.Mex.......................... 36 mento Mountains, 12 miles southeast XIX. A, North side of entrance to Alamo of Alamogordo, N. Mex.............. 50 Canyon, 3 miles southeast of Alamo­ 14. Section along western slope of the gordo, N. Mex.; B, Kelly limestone Sacramento Mountains east of Alamo­ at Graphic mine, near Magdalena, gordo, N. Mex., from La Luz Canyor N.Mex.......................... 37 to Grapevine Canyon............... 51 XX. View looking southeast along weat 15. Section across the southern part of the front of Sacramento Mountains Florida Mountains, Luna County, from Alamogordo, Otero County, N.Mex............................. 54 N.Mex.......................... 50 XXI. View along west front of Sacramento Mountains at Agua Chiquita Can­ yon, Otero County, N. Mex........ 51 COS I.:; *-JIJ NVS Mxr»o*iD j,siocno3") HO A COMPARISON OF PALEOZOIC SECTIONS IN SOUTHERN NEW MEXICO. By N. H. DABTON. INTRODUCTION. in publications by Gordon and Graton, Lee, In studying the geology oi different parts Herrick, and others. of southern New Mexico the writer has ob­ It has been known for some time that in tained many new data on the distribution southern New Mexico there are representa­ and relations of the sedimentary rocks. The tives of portions of later Cambrian, Ordovi- stratigraphy of the Pennsylvanian series was cian, Silurian, Devonian, earlier Mississippian, investigated in detail, and in Luna County all and Pennsylvanian time, and that the lower the formations were studied.1 A recently formations thin out to the north, so that in Frankli n F lorid 3 ( :ooks Silver C aballc s Lake K hgst 3n- SanAnd res Sac rame nto Mts MtS. F City Mts. Valley H llsbo TO Mts Mts. TERTIARY *~t**tf; TERTIARY _i— 1_ agglom­ jK Red beds \ erate erate 2,000 (Abo) 10 soo/ o 1 !_!_ FCoJpfSab' £00+ a i 1 Colorado 1 //|r l,000± 1,800 + Hueco 300 "-- o 1 1 ' $ ^ m Gap ~"~ — -i?~ Red beds . cc • ' Gym \ S 1 1 i i 1 1 i i / . 1 1 i i / I,IOO± 1 1 Gym / limestone i i Fierro i / * — i— i- / 600 \\ \ -U-L- 800 \ \ • 650 i ' i ' / •z. 1,200,' ^ \ 1 1 i i i i •> Lake i ' i 1 CL i i _J_ L _• Valley --t^r i i 300 JD;50 •i i fe---_ i i :75^ to _,- ^r- i i 500 ,' i i 163-—- - —— JTjf i i 300 i — r i i i i . 50 IS ^-aoo — 7 —— —— - i i = !<=!= 200 -~? 350 ZOO ORDOVICIANSIU.CAMBRIANORDOVICIAN Montoya 300 250 350 / 1 1 to 350 150 -i- i i 400 j —i — n75--~ 200 tt &£ U^- 300 ^&? 300 600 to i^ PRE-LATEEARLYLATE 800 900- 400 v s' 1,000+ i El Paso -100+ —— ^s / 20ti\ / / 180' . L _., L, 200,--^ "Oto f Bliss 2OO ____- Scale 500 0 5CX3 1 000 Feet Granite,etc. P i 'S-^T? mf Mississippian fossi s m Magdalena fossils FIGURE 2. Columnar sections showing stratigraphic relations of Paleozoic rocks in southern New Mexico. published folio 2 gives many new facts for the central New Mexico the strata of the Penn­ stratigraphy of the Silver City region, some of sylvanian series lie directly on the pre-Cam- which are utilized in the present paper. Rich­ brian crystalline rocks, as shown in Plate ardson's work in the El Paso region 3 estab­ XIV, B. There are also numerous irregulari­ lished the succession in the southeastern part ties in the overlap relations of the formations. of New Mexico. There are also many details The broader features of the stratigraphy of this region are here presented. The principal 1 Darton, N. H., Geology and underground waters of Luna County, N. Mex.: U. S. Geol. Survey Bull. 618, 188 pp., 13 pi., 1916. Paleozoic formations in southern New Mexico- 2 Paige, Sidney, U. S. Geol. Survey Geol. Atlas, Silver City folio (No. are shown in the columnar sections (fig. 2), 199), 1916. s Richardson, G. B., U. S. Geol. Survey Geol. Atlas, El Paso folio and some conditions of the distribution of the (No. 166), 1909. formations are indicated on the map (PI. XIII). 31 32 SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY, 1917. CAMBRIAN SYSTEM. beds comprise Lingulepis acuminata, Obolus matinalis ?, and fragments of Lingulella. Some
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]
  • 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 Carboniferous Bryozoans from La Hermida, Spain
    Late Carboniferous bryozoans from La Hermida, Spain Andrej Ernst and Elke Minwegen Acta Palaeontologica Polonica 51 (3), 2006: 569-588 Fifteen bryozoan species belonging to thirteen genera have been identified from an outcrop of the Picos de Europa Formation (Moscovian, Upper Carboniferous) at La Hermida in northern Spain. Three species and one genus are new Coscinium hermidensis sp. nov., Cystodictya pustulosa sp. nov., and Cystocladia hispanica gen. et sp. nov. Rhabdomesid bryozoans are the most diverse order with seven species, followed by cystoporids (four species), fenestellids (three species) and trepostomids (one species). Bryozoans with erect branched or reticulate colonies dominate in the studied assemblage; only two species possess encrusting colonies. Together with associated crinoids, the bryozoan assemblage indicates a subtidal environment below the zone of vigorous water movement. The La Hermida bryozoan fauna confirms the Upper Carboniferous age of the Picos de Europa Formation and allows various biogeographical interpretations. All previously known species of the genus Coscinium were reported from the Lower Permian of Russia. Clausotrypa monticola is known from the Lower Permian of Russia and Arctic as well as from the Upper Carboniferous of Carnic Alps (Austria). Rhabdomeson cf. propatulissimum and Penniretepora pseudotrilineata are known from the same level of Italian Carnic Alps. Streblotrypa (Streblascopora ) nikiforovae and Rhombocladia punctata are known from the Upper Carboniferous (Moscovian) of Ukraine. Fistulipora petaloida is known from Kasimovian Stage of Russian Plate. Several other species show connections with North America. Key words: Bryozoa, Cystoporida, Fenestellida, Carboniferous, Picos de Europa Formation, Spain. Andrej Ernst [email protected], Institut für Geowissenschaften, Christian-Albrechts-Universität zu Kiel, Ludewig-Meyn-Str.
    [Show full text]
  • Field Guide to the Sandia Mountains, Edited by Robert Julyan & Mary
    Volume 45 Issue 4 Fall 2005 Fall 2005 Field Guide to the Sandia Mountains, edited by Robert Julyan & Mary Stuever Nancy Harbert Recommended Citation Nancy Harbert, Field Guide to the Sandia Mountains, edited by Robert Julyan & Mary Stuever, 45 Nat. Resources J. 1120 (2005). Available at: https://digitalrepository.unm.edu/nrj/vol45/iss4/11 This Book Review is brought to you for free and open access by the Law Journals at UNM Digital Repository. It has been accepted for inclusion in Natural Resources Journal by an authorized editor of UNM Digital Repository. For more information, please contact [email protected], [email protected], [email protected]. 1120 NATURAL RESOURCES JOURNAL [Vol. 45 Field Guide to the Sandia Mountains. Edited by Robert Julyan & Mary Stuever: Albuquerque: University of New Mexico Press, 2005. Pp. 255. $19.95 spiral-bound paperback. This easy-to-absorb handbook does not pretend to be an exhaustive manual to the Sandia Mountains. Early on, editor Robert Julyan, who is best known for his book The Place Names of New Mexico, makes it clear that the intention among the guide's many contributors is to provide an introduction to the various elements that combine to make up the Sandia Mountains, a compact mountain range that provides the eastern backdrop for Albuquerque. With hundreds of plants and animals, not to mention microbes and soil types, Julyan points out that it would be impossible to represent them all in a guidebook. Therefore, the book focuses on the species and features that visitors are most likely to encounter. Because of the range's proximity to Albuquerque, a city of nearly 500,000 people, it is probably trampled on more than any other mountains in the state.
    [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]
  • 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 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]
  • 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]
  • Mosaic of New Mexico's Scenery, Rocks, and History
    Mosaic of New Mexico's Scenery, Rocks, and History SCENIC TRIPS TO THE GEOLOGIC PAST NO. 8 Scenic Trips to the Geologic Past Series: No. 1—SANTA FE, NEW MEXICO No. 2—TAOS—RED RIVER—EAGLE NEST, NEW MEXICO, CIRCLE DRIVE No. 3—ROSWELL—CAPITAN—RUIDOSO AND BOTTOMLESS LAKES STATE PARK, NEW MEXICO No. 4—SOUTHERN ZUNI MOUNTAINS, NEW MEXICO No. 5—SILVER CITY—SANTA RITA—HURLEY, NEW MEXICO No. 6—TRAIL GUIDE TO THE UPPER PECOS, NEW MEXICO No. 7—HIGH PLAINS NORTHEASTERN NEW MEXICO, RATON- CAPULIN MOUNTAIN—CLAYTON No. 8—MOSlAC OF NEW MEXICO'S SCENERY, ROCKS, AND HISTORY No. 9—ALBUQUERQUE—ITS MOUNTAINS, VALLEYS, WATER, AND VOLCANOES No. 10—SOUTHWESTERN NEW MEXICO No. 11—CUMBRE,S AND TOLTEC SCENIC RAILROAD C O V E R : REDONDO PEAK, FROM JEMEZ CANYON (Forest Service, U.S.D.A., by John Whiteside) Mosaic of New Mexico's Scenery, Rocks, and History (Forest Service, U.S.D.A., by Robert W . Talbott) WHITEWATER CANYON NEAR GLENWOOD SCENIC TRIPS TO THE GEOLOGIC PAST NO. 8 Mosaic of New Mexico's Scenery, Rocks, a n d History edited by PAIGE W. CHRISTIANSEN and FRANK E. KOTTLOWSKI NEW MEXICO BUREAU OF MINES AND MINERAL RESOURCES 1972 NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY STIRLING A. COLGATE, President NEW MEXICO BUREAU OF MINES & MINERAL RESOURCES FRANK E. KOTTLOWSKI, Director BOARD OF REGENTS Ex Officio Bruce King, Governor of New Mexico Leonard DeLayo, Superintendent of Public Instruction Appointed William G. Abbott, President, 1961-1979, Hobbs George A. Cowan, 1972-1975, Los Alamos Dave Rice, 1972-1977, Carlsbad Steve Torres, 1967-1979, Socorro James R.
    [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]
  • 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]