Revised Regional Correlations and Tectonic Implications Of
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Prehistoric Trackways National Monument Recreation Area Management Plan
October 2020 Prehistoric Trackways National Monument Recreation Area Management Plan Environmental Assessment DOI-BLM-NM-L0000-2021-0004-EA Las Cruces District Office 1800 Marquess Street Las Cruces, New Mexico 88005 575-525-4300 TABLE OF CONTENTS CHAPTER 1. INTRODUCTION .................................................................................................. 1 1.1. Purpose and Need ........................................................................................................... 1 1.2. Decision to Be Made ....................................................................................................... 1 1.3. RAMP Planning Process ................................................................................................ 3 1.4. Plan Conformance and Relationship to Statutes and Regulations ............................ 3 1.4.1. Plan Conformance ..................................................................................................... 3 1.4.2. Relationship to Statutes and Regulations .................................................................. 5 1.5. Scoping and Issues .......................................................................................................... 6 1.5.1. Internal Scoping ........................................................................................................ 6 1.5.2. Internal and External Scoping ................................................................................... 7 1.5.3. Issues ........................................................................................................................ -
Precise Age and Biostratigraphic Significance of the Kinney Brick Quarry Lagerstätte, Pennsylvanian of New Mexico, USA
Precise age and biostratigraphic significance of the Kinney Brick Quarry Lagerstätte, Pennsylvanian of New Mexico, USA Spencer G. Lucas1, Bruce D. Allen2, Karl Krainer3, James Barrick4, Daniel Vachard5, Joerg W. Schneider6, William A. DiMichele7 and Arden R. Bashforth8 1New Mexico Museum of Natural History, 1801 Mountain Road N.W., Albuquerque, New Mexico, 87104, USA email: [email protected] 2New Mexico Bureau of Geology and Mineral Resources, 801 Leroy Place, Socorro, New Mexico, 87801, USA email: [email protected] 3Institute of Geology and Paleontology, University of Innsbruck, Innsbruck, A-6020, Austria email: [email protected] 4Department of Geosciences, Texas Tech University, Box 41053, Lubbock, Texas, 79409, USA email: [email protected] 5Université des Sciences et Technologies de Lille, UFR des Sciences de la Terre, UPRESA 8014 du CNRS, Laboratoire LP3, Bâtiment SN 5, F-59655 Villeneuve d’Ascq, Cédex, France email: [email protected] 6TU Bergakademie Freiberg, Cottastasse 2, D-09596 Freiberg, Germany email:[email protected] 7Department of Paleobiology, NMNH Smithsonian Institution, Washington, DC 20560 email: [email protected] 8Geological Museum, Natural History Museum of Denmark, University of Copenhagen, Øster Voldgade 5-7, 1350 Copenhagen K, Denmark email: [email protected] ABSTRACT: The Kinney Brick Quarry is a world famous Late Pennsylvanian fossil Lagerstätte in central New Mexico, USA. The age assigned to the Kinney Brick Quarry (early-middle Virgilian) has long been based more on its inferred lithostratigraphic position than on biostratigraphic indicators at the quarry. We have developed three datasets —-stratigraphic position, fusulinids and conodonts— that in- dicate the Kinney Brick Quarry is older, of middle Missourian (Kasimovian) age. -
The Lower Permian Abo Formation in the Fra Cristobal and Caballo Mountains, Sierra County, New Mexico Spencer G
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/63 The Lower Permian Abo Formation in the Fra Cristobal and Caballo Mountains, Sierra County, New Mexico Spencer G. Lucas, Karl Krainer, Dan S. Chaney, William A. DiMichele, Sebastian Voigt, David S. Berman, and Amy C. Henrici, 2012, pp. 345-376 in: Geology of the Warm Springs Region, Lucas, Spencer G.; McLemore, Virginia T.; Lueth, Virgil W.; Spielmann, Justin A.; Krainer, Karl, New Mexico Geological Society 63rd Annual Fall Field Conference Guidebook, 580 p. This is one of many related papers that were included in the 2012 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. -
Hydrogeologic Investigation of the Southern Taos Valley, Taos County, New Mexico
NEW MEXICO BUREAU OF GEOLOGY AND MINERAL RESOURCES Hydrogeologic Investigation of the Southern Taos Valley, Taos County, New Mexico Peggy S. Johnson Paul W. Bauer Brigitte Felix Final Technical Report August 2016 (updated November 2016) Open-File Report 581 New Mexico Bureau of Geology and Mineral Resources A division of New Mexico Institute of Mining and Technology Socorro, NM 87801 (575) 835 5490 Fax (575) 835 6333 geoinfo.nmt.edu Hydrogeologic Investigation of the Southern Taos Valley, Taos County, New Mexico Peggy S. Johnson Paul W. Bauer Brigitte Felix Final Technical Report August 2016 (updated November 2016) Open-File Report 581 New Mexico Bureau of Geology and Mineral Resources PROJECT FUNDING Taos County New Mexico Bureau of Geology and Mineral Resources, Aquifer Mapping Program Healy Foundation The views and conclusions are those of the authors, and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the State of New Mexico. Cover photograph: View north down the Picuris piedmont in an area where Quaternary sand and gravel depos- its cover a complex system of buried Embudo faults and Picuris-Pecos faults. Proterozoic rocks of the Sangre de Cristo Mountains are on the right horizon, and isolated volcanoes of the Taos Plateau volcanic field in the Rio Grande rift are on the left horizon. The water well being drilled in the fall of 2015 penetrated 1200 feet of Santa Fe Group and Picuris Formation sedimentary rocks. Photograph by Paul Bauer NEW MEXICO BUREAU OF GEOLOGY AND MINERAL RESOURCES SOUTH TAOS VALLEY, TAOS COUNTY CONTENTS Proterozoic rocks ....................................................31 Executive Summary ............................................................ -
The Geology of New Mexico As Understood in 1912: an Essay for the Centennial of New Mexico Statehood Part 2 Barry S
Celebrating New Mexico's Centennial The geology of New Mexico as understood in 1912: an essay for the centennial of New Mexico statehood Part 2 Barry S. Kues, Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico, [email protected] Introduction he first part of this contribution, presented in the February Here I first discuss contemporary ideas on two fundamental areas 2012 issue of New Mexico Geology, laid the groundwork for an of geologic thought—the accurate dating of rocks and the move- exploration of what geologists knew or surmised about the ment of continents through time—that were at the beginning of Tgeology of New Mexico as the territory transitioned into statehood paradigm shifts around 1912. Then I explore research trends and in 1912. Part 1 included an overview of the demographic, economic, the developing state of knowledge in stratigraphy and paleontol- social, cultural, and technological attributes of New Mexico and its ogy, two disciplines of geology that were essential in understand- people a century ago, and a discussion of important individuals, ing New Mexico’s rock record (some 84% of New Mexico’s surface institutions, and areas and methods of research—the geologic envi- area is covered by sediments or sedimentary rocks) and which were ronment, so to speak—that existed in the new state at that time. advancing rapidly through the first decade of the 20th century. The geologic time scale and age of rocks The geologic time scale familiar to geologists working in New The USGS did not adopt the Paleocene as the earliest epoch of the Mexico in 1912 was not greatly different from that used by modern Cenozoic until 1939. -
Unm-ER FIRE! "We Are Simply Askirig That the Department Implement a Defensible Recovery Plan Based on the Best Available Science in Order to Bring Back Bighorn Sheep
NE"" MEXICO COUGARS UNm-ER FIRE! "We are simply askirig that the Department implement a defensible recovery plan based on the best available science in order to bring back bighorn sheep. Persecuting predators like cougars will not save New Mexico's bighorn. Deliberate and serious recovery efforts will," said Lisa Jennings, Executive Director, APNM. "Cougars and bighorn sheep have historically coexisted. By examining and altering other limiting factors such as habitat degrada tion and disease transmission from domestic livestock,. we can ensure the continued abundant presence of both these species in our state," ANIMAL PROTECTION OF NEW MEXICO, INC. Non-Profit Org. U.S. Postage URGENT ACTION ALERT! PAID Albuquerque, N.M. Permit No. 1130 Animal Protection ''If hi ew Mexico, Inc. P.O. Box 11395 Albuquerque, NM 87192-0395 Return Service Requested www.APNM.org WILDLIFE IN JEOPARDY: New Mexico's Faulty Cougar Policies At JUly's New Mexico Game Commission meeting, all six in three Wilderness Study Commissioners present (Commissioner Emery was absent) voted Areas NVSA's). to approve a controversial cougar killing program promoted by the Department: of Game and Fish (Department) in order to While there is no question ostensibly protect New Mexico's endangered bighorn sheep that the state's bighorn pop population. The approved regulations will allow for the killing of ulations are in dire straits, up to 34 cougars per year, for five years, in fOUf bighorn sheep killing cougars is unHkely to territories, whether or not cougars have killed bighorn sheep. In solve the problem of dwin essence, any cougar in bighorn sheep territory is a dead cougar. -
Seismic Investigation of the Yavapai-Mazatzal Transition Zone and the Jemez Lineament in Northeastern New Mexico
Seismic Investigation of the Yavapai-Mazatzal Transition Zone and the Jemez Lineament in Northeastern New Mexico Maria Beatrice Magnani and Alan Levander Department of Earth Science, Rice University, Houston, Texas Kate C. Miller and Tefera Eshete Department of Geological Sciences, University of Texas at El Paso, El Paso, Texas Karl E. Karlstrom Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico A new seismic reflection profile of the Precambrian lithosphere under the Jemez Lineament (JL) (northeastern New Mexico, USA) shows impressive reflectivity throughout the crust. The upper crust is characterized by a 2 km thick undeformed Paleozoic and Mesozoic sedimen- tary sequence above the Precambrian basement. At a depth of 5–8 km, undulating reflec- tions image a Proterozoic nappe cropping out in the nearby Rincon Range. To the south the upper crust is seismically transparent except for south dipping reflections at 2–10 km depth. The middle-lower crust, from 10–45 km depth, shows oppositely dipping reflections that converge in the deep crust (35–37 km) roughly at the center of the profile. To the north the reflectivity dips southward at 25° to a depth of 33 km before fading in the lower crust. In the southern part of the profile a crustal-scale duplex structure extends horizontally for more than 60 km. We interpret the oppositely dipping reflections as the elements of a doubly ver- gent suture zone that resulted from the accretion of the Mazatzal island arc to the southern margin of the Yavapai proto-craton at ~1.65–1.68 Ga. -
Petroglyph National Monument: Geologic Resources Inventory Report
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Petroglyph National Monument Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2017/1547 ON THE COVER Photograph of Albuquerque volcanoes. Three spatter cones, known as the Sisters, form a distinctive skyline west of Albuquerque, New Mexico. These small volcanoes are part of the Albuquerque volcanic field and occur in the Volcanoes area of Petroglyph National Monument. The volcanic field was active about 156,000 years ago. NPS photograph by Chanteil Walter (Petroglyph National Monument). THIS PAGE Photograph of the West Mesa escarpment along the Rinconada Canyon Trail. Erosion of the Santa Fe Group sediments that underlie a basaltic cap rock has caused large blocks of rock to tumble down the eastern escarpment of the mesa. Most of the petroglyphs were chiseled into the dark patina of desert varnish on these large boulders, exposing the lighter colored basaltic rock beneath. NPS photograph by Dale Pate (Geologic Resources Division). Petroglyph National Monument Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2017/1547 Katie KellerLynn Colorado State University Research Associate National Park Service Geologic Resources Division Geologic Resources Inventory PO Box 25287 Denver, CO 80225 November 2017 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. -
Stratigraphic Nomenclature of Proterozoic Rocks, Northern New
Stratigraphicnomenclature ol proterozoic rocks, northern NewMexico-revisions, redefinitions, andformalization byPaul W' Bauer, New MexicoBureau ol Minesancl Mineral Resources, Socono, NM 87801 , and Michaet L. Wiltiams,Department of Geology and Geography, Universityof Massachusetts, Amherst, MA 01003 Abstract lithotectonic nomenclature for the supra- Much of the exposed Proterozoic rock in crustal Precambrianrocks exposed in north- This paper proposes formal northern New Mexico can be assignedto one revisions of ern New Mexico. the lithostratigraphicnomenclature for some of four major lithologic assemblages:1) se- Early Proterozoic rocks in northern New quencesdominated by metamorphosedmafic volcanicrocks, ca 1,755-I,720 Ma in age;2) sequencesdominated by metamorphosed felsic volcanic rocks and immature clastic sedimentaryrocks, ca 1,700Ma and ca 1,500- tains, the Truchas Peaksarea, the Rio Mora- 1,650Ma in age;3)massive clean quartzite(s) and sequencesof interlayered pelitic schist and quartzite, 1,700-1,650Ma; and 4) intru- sive rocks that range widely in age and com- position (Robertsonet al., in press).Each of these is discussed separately.Table L sum- marizes both existing and proposed new no- Kiowa Mountain in the Tusas Mountains. menclature for stratified units. Several distinctive units are designated as of northern and central New Mexico, and formations: Big Rock Formation, Burned perhaps in parts of Arizona and southern Mafic metavolcanic sequences Mountain Formation, Marquenas Forma- Colorado (Burns and Wobus, 1.983;Wobus, tion, Clenwoody Formation. Extensive terrains dominated by amphi- The metase- 1985;Bauer and Williams, 1985;Grambling dimentary sequencepreviously bolite and mafic schist of igneous parenfage called the and Williams, 1985;Williams, Ortega Group is,renamedthe Hondo 1987). -
Challenges and Opportunities for Brackish
CHALLENGES AND OPPORTUNITIES FOR BRACKISH GROUNDWATER- RESOURCE DEVELOPMENT IN NEW MEXICO—PREDICTION HYDRO-SCIENCE FROM AN OCTOGENARIAN HYDROGEOLOGIST’S PERSPECTIVE Introduction to Part-2 of Invited Presentations on Desalination Science/Technology (Mike Hightower, SNL) and New Mexico’s Brackish Groundwater Resources to the Urban Land Institute-New Mexico Section, April 28, 2016 John W. Hawley, Ph.D., Emeritus Senior Environmental Geologist, N.M. Bureau of Geology & Mineral Resources, NMIMT Visiting Senior Hydrogeologist, N.M. Water Resources Research Institute, NMSU dba HAWLEY GEOMATTERS [email protected] P.O. Box 4370, Albuquerque, NM 87196-4370; Phone (o) 505-255-4847, (c) 505-263-6921 PREFACE This informal “white paper” introduces a pptx presentation on “Challenges and Opportunities for Brackish Groundwater-Resource Development in New Mexico,” and includes representative slides and an expanded list of background references. Most illustrations with a GoogleTMearth base have been designed by Baird Swanson of Swanson Geoscience, LLC; and all hydrogeologic maps and cross sections were initially created by HAWLEY GEOMATTERS for the N.M. Water Resources Research Institute Transboundary Aquifer Assessment Project (TAAP). Since exposure to water-based realities in our dryland-culture can be a bit depressing, I’ll try to keep my remarks as optimistic and moist as possible. Also, since bad-news bearers have often met bad ends throughout history, it’s prudent to avoid doom and gloom scenarios whenever I can. So, emphasis here will be on places where de-watered aquifer spaces can be replenished through timely application of state-of-the-art Aquifer Storage & Recovery (ASR) technology. Professional observations and opinions on the interlinkage of land, water, and energy resources reflects an early career in the New Mexico-West Texas region as a research geologist for the Soil Survey Investigations Division of the USDA Soil Conservation Service (SCS-now NRCS), with field headquarters at NMSU-Las Cruces (1962-1971), Texas Tech University-Lubbock (1971- 1974), N.M. -
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. -
Do Proterozoic Metamorphic Rocks in Northern New Mexico Record One
Bucknell University Bucknell Digital Commons Honors Theses Student Theses 2016 Do Proterozoic Metamorphic Rocks in Northern New Mexico Record One Metamorphic Event At 1.4 Ga, or Two Overprinting Events At 1.65 GA and 1.4 GA Sara Vivienne Stotter Bucknell University, [email protected] Follow this and additional works at: https://digitalcommons.bucknell.edu/honors_theses Recommended Citation Stotter, Sara Vivienne, "Do Proterozoic Metamorphic Rocks in Northern New Mexico Record One Metamorphic Event At 1.4 Ga, or Two Overprinting Events At 1.65 GA and 1.4 GA" (2016). Honors Theses. 355. https://digitalcommons.bucknell.edu/honors_theses/355 This Honors Thesis is brought to you for free and open access by the Student Theses at Bucknell Digital Commons. It has been accepted for inclusion in Honors Theses by an authorized administrator of Bucknell Digital Commons. For more information, please contact [email protected]. iv ACKNOWLEDGEMENTS I would first like to thank my thesis advisor, Dr. Chris Daniel, for his unwavering guidance, encouragement, patience, and support throughout the course of my research project. Sophomore year, when I first started doing work with Dr. Daniel, I never imagined that I would accomplish and learn so much, and I am truly grateful for his insight and mentoring. He always pushed me to do my best, and continually challenged me to think critically which allowed me to reach my goals and excel beyond them. I would also like to thank Dr. Mary Beth Gray for her kind words and endless motivation that kept me going even in the most stressful of times.