Scenic Trips to the Geologic Past No. 13: Espanola
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Plant Diversity and Composition Changes Along an Altitudinal Gradient in the Isolated Volcano Sumaco in the Ecuadorian Amazon
diversity Article Plant Diversity and Composition Changes along an Altitudinal Gradient in the Isolated Volcano Sumaco in the Ecuadorian Amazon Pablo Lozano 1,*, Omar Cabrera 2 , Gwendolyn Peyre 3 , Antoine Cleef 4 and Theofilos Toulkeridis 5 1 1 Herbario ECUAMZ, Universidad Estatal Amazónica, Km 2 2 vía Puyo Tena, Paso Lateral, 160-150 Puyo, Ecuador 2 Dpto. de Ciencias Biológicas, Universidad Técnica Particular de Loja, San Cayetano Alto s/n, 110-104 Loja, Ecuador; [email protected] 3 Dpto. de Ingeniería Civil y Ambiental, Universidad de los Andes, Cra. 1E No. 19a-40, 111711 Bogotá, Colombia; [email protected] 4 IBED, Paleoecology & Landscape ecology, University of Amsterdam, Science Park 904, 1098 HX Amsterdam, The Netherlands; [email protected] 5 Universidad de las Fuerzas Armadas ESPE, Av. General Rumiñahui s/n, P.O.Box, 171-5-231B Sangolquí, Ecuador; [email protected] * Correspondence: [email protected]; Tel.: +593-961-162-250 Received: 29 April 2020; Accepted: 29 May 2020; Published: 8 June 2020 Abstract: The paramo is a unique and severely threatened ecosystem scattered in the high northern Andes of South America. However, several further, extra-Andean paramos exist, of which a particular case is situated on the active volcano Sumaco, in the northwestern Amazon Basin of Ecuador. We have set an elevational gradient of 600 m (3200–3800 m a.s.l.) and sampled a total of 21 vegetation plots, using the phytosociological method. All vascular plants encountered were typified by their taxonomy, life form and phytogeographic origin. In order to determine if plots may be ensembled into vegetation units and understand what the main environmental factors shaping this pattern are, a non-metric multidimensional scaling (NMDS) analysis was performed. -
University of Oklahoma Graduate College
UNIVERSITY OF OKLAHOMA GRADUATE COLLEGE POTENTIAL FIELD STUDIES OF THE CENTRAL SAN LUIS BASIN AND SAN JUAN MOUNTAINS, COLORADO AND NEW MEXICO, AND SOUTHERN AND WESTERN AFGHANISTAN A DISSERTATION SUBMITTED TO THE GRADUATE FACULTY in partial fulfillment of the requirements for the Degree of DOCTOR OF PHILOSOPHY By BENJAMIN JOHN DRENTH Norman, Oklahoma 2009 POTENTIAL FIELD STUDIES OF THE CENTRAL SAN LUIS BASIN AND SAN JUAN MOUNTAINS, COLORADO AND NEW MEXICO, AND SOUTHERN AND WESTERN AFGHANISTAN A DISSERTATION APPROVED FOR THE CONOCOPHILLIPS SCHOOL OF GEOLOGY AND GEOPHYSICS BY _______________________________ Dr. G. Randy Keller, Chair _______________________________ Dr. V.J.S. Grauch _______________________________ Dr. Carol Finn _______________________________ Dr. R. Douglas Elmore _______________________________ Dr. Ze’ev Reches _______________________________ Dr. Carl Sondergeld © Copyright by BENJAMIN JOHN DRENTH 2009 All Rights Reserved. TABLE OF CONTENTS Introduction…………………………………………………………………………..……1 Chapter A: Geophysical Constraints on Rio Grande Rift Structure in the Central San Luis Basin, Colorado and New Mexico………………………………………………………...2 Chapter B: A Geophysical Study of the San Juan Mountains Batholith, southwestern Colorado………………………………………………………………………………….61 Chapter C: Geophysical Expression of Intrusions and Tectonic Blocks of Southern and Western Afghanistan…………………………………………………………………....110 Conclusions……………………………………………………………………………..154 iv LIST OF TABLES Chapter A: Geophysical Constraints on Rio Grande Rift Structure in the Central -
Summary of the Paleontology of the Santa Fe Group (Mio-Pliocene), North-Central New Mexico Barry S
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/30 Summary of the paleontology of the Santa Fe Group (Mio-Pliocene), north-central New Mexico Barry S. Kues and Spencer G. Lucas, 1979, pp. 237-241 in: Santa Fe Country, Ingersoll, R. V. ; Woodward, L. A.; James, H. L.; [eds.], New Mexico Geological Society 30th Annual Fall Field Conference Guidebook, 310 p. This is one of many related papers that were included in the 1979 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. -
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. -
Geologic Map of the Central San Juan Caldera Cluster, Southwestern Colorado by Peter W
Geologic Map of the Central San Juan Caldera Cluster, Southwestern Colorado By Peter W. Lipman Pamphlet to accompany Geologic Investigations Series I–2799 dacite Ceobolla Creek Tuff Nelson Mountain Tuff, rhyolite Rat Creek Tuff, dacite Cebolla Creek Tuff Rat Creek Tuff, rhyolite Wheeler Geologic Monument (Half Moon Pass quadrangle) provides exceptional exposures of three outflow tuff sheets erupted from the San Luis caldera complex. Lowest sheet is Rat Creek Tuff, which is nonwelded throughout but grades upward from light-tan rhyolite (~74% SiO2) into pale brown dacite (~66% SiO2) that contains sparse dark-brown andesitic scoria. Distinctive hornblende-rich middle Cebolla Creek Tuff contains basal surge beds, overlain by vitrophyre of uniform mafic dacite that becomes less welded upward. Uppermost Nelson Mountain Tuff consists of nonwelded to weakly welded, crystal-poor rhyolite, which grades upward to a densely welded caprock of crystal-rich dacite (~68% SiO2). White arrows show contacts between outflow units. 2006 U.S. Department of the Interior U.S. Geological Survey CONTENTS Geologic setting . 1 Volcanism . 1 Structure . 2 Methods of study . 3 Description of map units . 4 Surficial deposits . 4 Glacial deposits . 4 Postcaldera volcanic rocks . 4 Hinsdale Formation . 4 Los Pinos Formation . 5 Oligocene volcanic rocks . 5 Rocks of the Creede Caldera cycle . 5 Creede Formation . 5 Fisher Dacite . 5 Snowshoe Mountain Tuff . 6 Rocks of the San Luis caldera complex . 7 Rocks of the Nelson Mountain caldera cycle . 7 Rocks of the Cebolla Creek caldera cycle . 9 Rocks of the Rat Creek caldera cycle . 10 Lava flows premonitory(?) to San Luis caldera complex . .11 Rocks of the South River caldera cycle . -
Muon Tomography Sites for Colombian Volcanoes
Muon Tomography sites for Colombian volcanoes A. Vesga-Ramírez Centro Internacional para Estudios de la Tierra, Comisión Nacional de Energía Atómica Buenos Aires-Argentina. D. Sierra-Porta1 Escuela de Física, Universidad Industrial de Santander, Bucaramanga-Colombia and Centro de Modelado Científico, Universidad del Zulia, Maracaibo-Venezuela, J. Peña-Rodríguez, J.D. Sanabria-Gómez, M. Valencia-Otero Escuela de Física, Universidad Industrial de Santander, Bucaramanga-Colombia. C. Sarmiento-Cano Instituto de Tecnologías en Detección y Astropartículas, 1650, Buenos Aires-Argentina. , M. Suárez-Durán Departamento de Física y Geología, Universidad de Pamplona, Pamplona-Colombia H. Asorey Laboratorio Detección de Partículas y Radiación, Instituto Balseiro Centro Atómico Bariloche, Comisión Nacional de Energía Atómica, Bariloche-Argentina; Universidad Nacional de Río Negro, 8400, Bariloche-Argentina and Instituto de Tecnologías en Detección y Astropartículas, 1650, Buenos Aires-Argentina. L. A. Núñez Escuela de Física, Universidad Industrial de Santander, Bucaramanga-Colombia and Departamento de Física, Universidad de Los Andes, Mérida-Venezuela. December 30, 2019 arXiv:1705.09884v2 [physics.geo-ph] 27 Dec 2019 1Corresponding author Abstract By using a very detailed simulation scheme, we have calculated the cosmic ray background flux at 13 active Colombian volcanoes and developed a methodology to identify the most convenient places for a muon telescope to study their inner structure. Our simulation scheme considers three critical factors with different spatial and time scales: the geo- magnetic effects, the development of extensive air showers in the atmosphere, and the detector response at ground level. The muon energy dissipation along the path crossing the geological structure is mod- eled considering the losses due to ionization, and also contributions from radiative Bremßtrahlung, nuclear interactions, and pair production. -
Geology and Mineral Resources of Sierra Nacimiento and Vicinity, New
iv Contents ABSTRACT 7 TERTIARY-QUATERNARY 47 INTRODUCTION 7 QUATERNARY 48 LOCATION 7 Bandelier Tuff 48 PHYSIOGRAPHY 9 Surficial deposits 48 PREVIOUS WORK 9 PALEOTECTONIC SETTING 48 ROCKS AND FORMATIONS 9 REGIONAL TECTONIC SETTING 49 PRECAMBRIAN 9 STRUCTURE 49 Northern Nacimiento area 9 NACIMIENTO UPLIFT 49 Southern Nacimiento area 15 Nacimiento fault 51 CAMBRIAN-ORDOVICIAN (?) 20 Pajarito fault 52 MISSISSIPPIAN 20 Synthetic reverse faults 52 Arroyo Peñasco Formation 20 Eastward-trending faults 53 Log Springs Formation 21 Trail Creek fault 53 PENNSYLVANIAN 21 Antithetic reverse faults 53 Osha Canyon Formation 23 Normal faults 53 Sandia Formation 23 Folds 54 Madera Formation 23 SAN JUAN BASIN 55 Paleotectonic interpretation 25 En echelon folds 55 PERMIAN 25 Northeast-trending faults 55 Abo Formation 25 Synclinal bend 56 Yeso Formation 27 Northerly trending normal faults 56 Glorieta Sandstone 30 Antithetic reverse faults 56 Bernal Formation 30 GALLINA-ARCHULETA ARCH 56 TRIASSIC 30 CHAMA BASIN 57 Chinle Formation 30 RIΟ GRANDE RIFT 57 JURASSIC 34 JEMEZ VOLCANIC FIELD 59 Entrada Sandstone 34 TECTONIC EVOLUTION 60 Todilto Formation 34 MINERAL AND ENERGY RESOURCES 63 Morrison Formation 34 COPPER 63 Depositional environments 37 Mineralization 63 CRETACEOUS 37 Origin 67 Dakota Formation 37 AGGREGATE 69 Mancos Shale 39 TRAVERTINE 70 Mesaverde Group 40 GYPSUM 70 Lewis Shale 41 COAL 70 Pictured Cliffs Sandstone 41 ΗUMΑTE 70 Fruitland Formation and Kirtland Shale URANIUM 70 undivided 42 GEOTHERMAL ENERGY 72 TERTIARY 42 OIL AND GAS 72 Ojo Alamo Sandstone -
Army Regulars on the Western Frontier, 1848-1861 / Dunvood Ball
Amy Regulars on the WestmFrontieq r 848-1 861 This page intentionally left blank Army Regulars on the Western Frontier DURWOOD BALL University of Oklahoma Press :Norman Library of Congress Cataloging-in-Publication Data Ball, Dunvood, 1960- Army regulars on the western frontier, 1848-1861 / Dunvood Ball. p. cm. Includes bibliographical references (p. ) and index. ISBN 0-8061-3312-0 I. West (U.S.)-History, Military-I 9th century. 2. United States. Army-History- 19th century. 3. United States-Military policy-19th century. 4. Frontier and pioneer life-West (U.S.) 5. West (US.)-Race relations. 6. Indians of North Arnerica- Government relations-1789-1869. 7. Indians of North America-West (U.S.)- History-19th century. 8. Civil-military relations-West (U.S.)-History-19th century. 9. Violence-West (U.S.)-History-I 9th century. I. Title. F593 .B18 2001 3 5~'.00978'09034-dcz I 00-047669 CIP The paper in this book meets the guidelines for permanence and durability of the Committee on Production Guidelines for Book Longevity of the Council on Library Resources, Inc. m Copyright O 2001 by the University of Oklahoma Press, Norman, Publishing Division of the University. All rights reserved. Manufactured in the U.S.A. 12345678910 For Mom, Dad, and Kristina This page intentionally left blank CONTENTS List of Illustrations and Maps IX Preface XI Acknowledgments xv INT R o D U C T I o N : Organize, Deploy, and Multiply XIX Prologue 3 PART I. DEFENSE, WAR, AND POLITICS I Ambivalent Duty: Soldiers, Indians, and Frontiersmen I 3 2 All Front, No Rear: Soldiers, Desert, and War 24 3 Chastise Them: Campaigns, Combat, and Killing 3 8 4 Internal Fissures: Soldiers, Politics, and Sectionalism 56 PART 11. -
Geology of the Cebolla Quadrangle, Rio Arriba County, New Mexico
BULLETIN 92 Geology of the Cebolla Quadrangle Rio Arriba County, New Mexico by HUGH H. DONEY 1 9 6 8 STATE BUREAU OF MINES AND MINERAL RESOURCES NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY CAMPUS STATION SOCORRO, NEW MEXICO NEW MEXICO INSTITUTE OF MINING AND TECHNOLOGY STIRLING A. COLGATE, President STATE BUREAU OF MINES AND MINERAL RESOURCES FRANK E. KOTTLOWSKI, Acting Director THE REGENTS MEMBERS Ex OFFICIO The Honorable David F. Cargo ...................................... Governor of New Mexico Leonard DeLayo ................................................. Superintendent of Public Instruction APPOINTED MEMBERS William G. Abbott .........................................................................................Hobbs Henry S. Birdseye ............................................................................... Albuquerque Thomas M. Cramer ................................................................................... Carlsbad Steve S. Torres, Jr. ....................................................................................... Socorro Richard M. Zimmerly .................................................................................... Socorro For sale by the New Mexico Bureau of Mines and Mineral Resources Campus Station, Socorro, N. Mex. 87801—Price $3.00 Abstract The Cebolla quadrangle overlaps two physiographic provinces, the San Juan Basin and the Tusas Mountains. Westward-dipping Mesozoic rocks, Quaternary cinder cones and flow rock, and Quaternary gravel terraces occur in the Chama Basin of the San Juan -
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 ............................................................ -
Geologic Summary of the Abiquiu Quadrangle, North-Central New Mexico Florian Maldonado and Daniel P
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/58 Geologic summary of the Abiquiu quadrangle, north-central New Mexico Florian Maldonado and Daniel P. Miggins, 2007, pp. 182-187 in: Geology of the Jemez Region II, Kues, Barry S., Kelley, Shari A., Lueth, Virgil W.; [eds.], New Mexico Geological Society 58th Annual Fall Field Conference Guidebook, 499 p. This is one of many related papers that were included in the 2007 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. -
Frontier Defense in the Territory of New Mexico, 1853–1861
New Mexico Historical Review Volume 9 Number 4 Article 2 10-1-1934 Frontier Defense in the Territory of New Mexico, 1853–1861 A. B. Bender Follow this and additional works at: https://digitalrepository.unm.edu/nmhr Recommended Citation Bender, A. B.. "Frontier Defense in the Territory of New Mexico, 1853–1861." New Mexico Historical Review 9, 4 (1934). https://digitalrepository.unm.edu/nmhr/vol9/iss4/2 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]. I NEW MEXICO HISTORICAL \. \ REVIEW '\ ~ VOL. IX OCTOBER, 1934 No.4 FRONTIER DEFENSE IN THE TERRITORY OF NEW MEXICO, 1853-1861 1 By A. B. BENDER EFFERSON DAVIS became secretary of war on M;arch 7, , 1853.2 Taking up the problem' of fr~ntier defense, he ) Jdeclared that he was not in sympathy with the plan of his predecessor." In his annual report of December 1, 1853, Davis characterized Conrad's defense program-that of lo cating a long line of military posts among the Indians-lis expensive and ineffective. He contended that such a plan would injure discipline and deaden the efficiency of the troops. Furthermore, the division of forces would be in terpreted by the Indians as an exhibition of weakness. To attempt to guard the entire' frontier was utterly imprac tical. He lea~ed, therefore, to the frontier policy of Quar termaster General Thomas S.