Valles Caldera National Preserve Foundation Document Overview
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Passive Monitoring of Ambient Reactive Gaseous Mercury in The
Passive Monitoring of Ambient Reactive Gaseous Mercury ihFin the Four Corners Area, Eastern OklhOklahoma, an d Central/East Texas: Important Method Evaluation and Baseline Work Presented at the National Air Toxics Monitoring and Data Analysis Workshop, Dallas, Texas, April 7, 2011. • Mark Sather, U.S. EPA Region 6, Air Quality Analysis Section • (214) 665-8353, [email protected] 1 Introduction • This presentation will summarize the first year of a two year monitoring project estimating reactive gaseous mercury (RGM, a.k.a. gaseous oxidized mercury, GOM) dry deposition in the Four Corners area and eastern Oklahoma, and preview a similar study to be done in Texas. • RGM of interest because of its chemical reactivity/water solubility; RGM readily deposits to water , soils and vegetation by both dry and wet processes; atmospheric lifetime = 0.5-2 days versus 0.5-2 years for elemental mercury which is mildly reactive and sparingly soluble in water. • Four Corners/Eastern Oklahoma project is a two year effort funded by U.S. EPA ORD Regional Applied Research Effort (RARE) program; the upcoming Texas study will also be funded by RARE . • Project Collaborators: U.S. EPA Region 6, U.S. EPA ORD, Frontier Geosci/lbliiences/Global Sciences, Ali on, NMED, NPS, USFS/ BLM, Jemez Pueblo/Valles Caldera Trust, Cherokee Nation. • Ambient monitoring began in August, 2009, and will run through the first part of August, 2011. 2 Project Objectives • To gather first-time RGM dry deposition estimates for 24 consecutive months at six sites in the Four Corners area to set a valuable ambient RGM dry deposition estimate baseline with proper assessment of: (a) the effectiveness of the Frontier Atmospheric Dry Deposition (FADD) surrogate surface devices in providing reliable RGM dry deposition estimates and (b) the inter-annual RGM dry deposition estimate variability. -
Stratigraphic Nomenclature of ' Volcanic Rocks in the Jemez Mountains, New Mexico
-» Stratigraphic Nomenclature of ' Volcanic Rocks in the Jemez Mountains, New Mexico By R. A. BAILEY, R. L. SMITH, and C. S. ROSS CONTRIBUTIONS TO STRATIGRAPHY » GEOLOGICAL SURVEY BULLETIN 1274-P New Stratigraphic names and revisions in nomenclature of upper Tertiary and , Quaternary volcanic rocks in the Jemez Mountains UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director U.S. GOVERNMENT PRINTING OFFICE WASHINGTON : 1969 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 15 cents (paper cover) CONTENTS Page Abstract.._..._________-...______.._-.._._____.. PI Introduction. -_-________.._.____-_------___-_______------_-_---_-_ 1 General relations._____-___________--_--___-__--_-___-----___---__. 2 Keres Group..__________________--------_-___-_------------_------ 2 Canovas Canyon Rhyolite..__-__-_---_________---___-____-_--__ 5 Paliza Canyon Formation.___-_________-__-_-__-__-_-_______--- 6 Bearhead Rhyolite-___________________________________________ 8 Cochiti Formation.._______________________________________________ 8 Polvadera Group..______________-__-_------________--_-______---__ 10 Lobato Basalt______________________________________________ 10 Tschicoma Formation_______-__-_-____---_-__-______-______-- 11 El Rechuelos Rhyolite--_____---------_--------------_-_------- 11 Puye Formation_________________------___________-_--______-.__- 12 Tewa Group__._...._.______........___._.___.____......___...__ 12 Bandelier Tuff.______________.______________... 13 Tsankawi Pumice Bed._____________________________________ 14 Valles Rhyolite______.__-___---_____________.________..__ 15 Deer Canyon Member.______-_____-__.____--_--___-__-____ 15 Redondo Creek Member.__________________________________ 15 Valle Grande Member____-__-_--___-___--_-____-___-._-.__ 16 Battleship Rock Member...______________________________ 17 El Cajete Member____..._____________________ 17 Banco Bonito Member.___-_--_---_-_----_---_----._____--- 18 References . -
Geothermal Hydrology of Valles Caldera and the Southwestern Jemez Mountains, New Mexico
GEOTHERMAL HYDROLOGY OF VALLES CALDERA AND THE SOUTHWESTERN JEMEZ MOUNTAINS, NEW MEXICO U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 00-4067 Prepared in cooperation with the OFFICE OF THE STATE ENGINEER GEOTHERMAL HYDROLOGY OF VALLES CALDERA AND THE SOUTHWESTERN JEMEZ MOUNTAINS, NEW MEXICO By Frank W. Trainer, Robert J. Rogers, and Michael L. Sorey U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 00-4067 Prepared in cooperation with the OFFICE OF THE STATE ENGINEER Albuquerque, New Mexico 2000 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director The use of firm, trade, and brand names in this report is for identification purposes only and does not constitute endorsement by the U.S. Geological Survey. For additional information write to: Copies of this report can be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Information Services Water Resources Division Box 25286 5338 Montgomery NE, Suite 400 Denver, CO 80225-0286 Albuquerque, NM 87109-1311 Information regarding research and data-collection programs of the U.S. Geological Survey is available on the Internet via the World Wide Web. You may connect to the Home Page for the New Mexico District Office using the URL: http://nm.water.usgs.gov CONTENTS Page Abstract............................................................. 1 Introduction ........................................ 2 Purpose and scope........................................................................................................................ -
A Vegetation Map of the Valles Caldera National Preserve, New
______________________________________________________________________________ A Vegetation Map of the Valles Caldera National Preserve, New Mexico ______________________________________________________________________________ A Vegetation Map of Valles Caldera National Preserve, New Mexico 1 Esteban Muldavin, Paul Neville, Charlie Jackson, and Teri Neville2 2006 ______________________________________________________________________________ SUMMARY To support the management and sustainability of the ecosystems of the Valles Caldera National Preserve (VCNP), a map of current vegetation was developed. The map was based on aerial photography from 2000 and Landsat satellite imagery from 1999 and 2001, and was designed to serve natural resources management planning activities at an operational scale of 1:24,000. There are 20 map units distributed among forest, shrubland, grassland, and wetland ecosystems. Each map unit is defined in terms of a vegetation classification that was developed for the preserve based on 348 ground plots. An annotated legend is provided with details of vegetation composition, environment, and distribution of each unit in the preserve. Map sheets at 1:32,000 scale were produced, and a stand-alone geographic information system was constructed to house the digital version of the map. In addition, all supporting field data was compiled into a relational database for use by preserve managers. Cerro La Jarra in Valle Grande of the Valles Caldera National Preserve (Photo: E. Muldavin) 1 Final report submitted in April 4, 2006 in partial fulfillment of National Prak Service Award No. 1443-CA-1248- 01-001 and Valles Caldrea Trust Contract No. VCT-TO 0401. 2 Esteban Muldavin (Senior Ecologist), Charlie Jackson (Mapping Specialist), and Teri Neville (GIS Specialist) are with Natural Heritage New Mexico of the Museum of Southwestern Biology at the University of New Mexico (UNM); Paul Neville is with the Earth Data Analysis Center (EDAC) at UNM. -
Bailey-1976.Pdf
VOL. 81, NO. 5 JOURNAL OF GEOPHYSICAL RESEARCH FEBRUARY 10, 1976 Volcanism, Structure,and Geochronologyof Long Valley Caldera, Mono County, California RoY A. BAILEY U.S. GeologicalSurvey, Reston, Virginia 22092 G. BRENT DALRYMPLE AND MARVIN A. LANPHERE U.S. GeologicalSurvey, Menlo Park, California 94025 Long Valley caldera, a 17- by 32-km elliptical depressionon the east front of the Sierra Nevada, formed 0.7 m.y. ago during eruption of the Bishoptuff. Subsequentintracaldera volcanism included eruption of (1) aphyric rhyolite 0.68-0.64 m.y. ago during resurgentdoming of the caldera floor, (2) porphyritic hornblende-biotiterhyolite from centersperipheral to the resurgentdome at 0.5, 0.3, and 0.1 m.y. ago, and (3) porphyritic hornblende-biotiterhyodacite from outer ring fractures0.2 m.y. ago to 50,000 yr ago, a sequencethat apparently records progressivecrystallization of a subjacentchemically zoned magma chamber. Holocene rhyolitic and phreatic eruptions suggestthat residual magma was present in the chamber as recentlyas 450 yr ago. Intracaldera hydrothermalactivity beganat least0.3 m.y. ago and was widespreadin the caldera moat; it has sincedeclined due to self-sealingof near-surfacecaldera sediments by zeolitization, argillization, and silicificationand has becomelocalized on recentlyreactivated north- west-trendingSierra Nevada frontal faults that tap hot water at depth. INTRODUCTION concentrates were treated with a dilute HF solution to remove small bits of attached glassand fragments of other mineral In the westernUnited States,only three calderasare known grains. Obsidian used for dating was totally unhydrated and to be large enoughand young enoughto possiblystill contain not devitrified. Small blocks sawed from many of the hand residual magma in their chambers:the Vailes caldera (•1.1 specimenswere used for dating. -
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. -
Fire History in the Taos Valley Watersheds, New Mexico, USA
fire Article Surface Fire to Crown Fire: Fire History in the Taos Valley Watersheds, New Mexico, USA Lane B. Johnson 1 and Ellis Q. Margolis 2,* 1 University of Minnesota, Cloquet Forestry Center, 175 University Drive, Cloquet, MN 55720, USA; [email protected] 2 U. S. Geological Survey, Fort Collins Science Center, New Mexico Landscapes Field Station, 301 Dinosaur Trail, Santa Fe, NM 87508, USA * Correspondence: [email protected]; Tel.: +1-505-954-2251 Received: 9 February 2019; Accepted: 8 March 2019; Published: 14 March 2019 Abstract: Tree-ring fire scars, tree ages, historical photographs, and historical surveys indicate that, for centuries, fire played different ecological roles across gradients of elevation, forest, and fire regimes in the Taos Valley Watersheds. Historical fire regimes collapsed across the three watersheds by 1899, leaving all sites without fire for at least 119 years. Historical photographs and quaking aspen (Populus tremuloides Michx.) ages indicate that a high-severity fire historically burned at multiple high-elevation subalpine plots in today’s Village of Taos Ski Valley, with large high-severity patches (>640 ha). Low-severity, frequent (9–29-year median interval) surface fires burned on the south aspects in nearby lower elevation dry conifer forests in all watersheds. Fires were associated with drought during the fire year. Widespread fires commonly burned synchronously in multiple watersheds during more severe drought years, preceded by wet years, including fire in all three watersheds in 1664, 1715, and 1842. In contrast, recent local “large” wildfires have only burned within single watersheds and may not be considered large in a historical context. -
Canadian Volcanoes, Based on Recent Seismic Activity; There Are Over 200 Geological Young Volcanic Centres
Volcanoes of Canada 1 V4 C.J. Hickson and M. Ulmi, Jan. 3, 2006 • Global Volcanism and Plate tectonics Where do volcanoes occur? Driving forces • Volcano chemistry and eruption types • Volcanic Hazards Pyroclastic flows and surges Lava flows Ash fall (tephra) Lahars/Debris Flows Debris Avalanches Volcanic Gases • Anatomy of an Eruption – Mt. St. Helens • Volcanoes of Canada Stikine volcanic belt Presentation Outline Anahim volcanic belt Wells Gray – Clearwater volcanic field 2 Garibaldi volcanic belt • USA volcanoes – Cascade Magmatic Arc V4 Volcanoes in Our Backyard Global Volcanism and Plate tectonics In Canada, British Columbia and Yukon are the host to a vast wealth of volcanic 3 landforms. V4 How many active volcanoes are there on Earth? • Erupting now about 20 • Each year 50-70 • Each decade about 160 • Historical eruptions about 550 Global Volcanism and Plate tectonics • Holocene eruptions (last 10,000 years) about 1500 Although none of Canada’s volcanoes are erupting now, they have been active as recently as a couple of 4 hundred years ago. V4 The Earth’s Beginning Global Volcanism and Plate tectonics 5 V4 The Earth’s Beginning These global forces have created, mountain Global Volcanism and Plate tectonics ranges, continents and oceans. 6 V4 continental crust ic ocean crust mantle Where do volcanoes occur? Global Volcanism and Plate tectonics 7 V4 Driving Forces: Moving Plates Global Volcanism and Plate tectonics 8 V4 Driving Forces: Subduction Global Volcanism and Plate tectonics 9 V4 Driving Forces: Hot Spots Global Volcanism and Plate tectonics 10 V4 Driving Forces: Rifting Global Volcanism and Plate tectonics Ocean plates moving apart create new crust. -
July 13, 2015 Cons: # 02ENNM00
New Mexico Ecological Services Field Office 2105 Osuna NE Albuquerque, New Mexico 87113 Phone: (505) 346-2525 Fax: (505) 346-2542 July 13, 2015 Cons: # 02ENNM00-2014-F-0266 Maria T. Garcia, Forest Supervisor Santa Fe National Forest 11 Forest Lane Santa Fe, New Mexico 87508 Dear Ms. Garcia: Thank you for your request for formal consultation and conferencing with the U.S. Fish and Wildlife Service (USFWS) pursuant to section 7 of the Endangered Species Act of 1973 (16 U.S.C. § 1531 et seq.), as amended (Act). We began early coordination with you and received a Biological Assessment (BA) (dated June 6, 2014) and supplemental information, which evaluate the impacts of the Southwest Jemez Mountains Restoration Project Santa Fe National Forest Jemez Ranger District Sandoval County, New Mexico (Restoration Project). At issue are potential impacts from the proposed action on the Mexican spotted owl (Strix occidentalis lucida) (MSO) and its critical habitat, the Jemez Mountains salamander (Plethodon neomexicanus) (salamander) and its critical habitat, the New Mexico meadow jumping mouse (Zapus hudsonius luteus) and its proposed critical habitat, and the Rio Grande Cutthroat trout (Oncorhynchus clarki virginalis) (cutthroat trout). You determined that the proposed action “may affect, is likely to adversely affect” the MSO and its designated critical habitat, the salamander and its designated critical habitat, the jumping mouse and its proposed critical habitat. This biological opinion does not rely on the regulatory definition of “destruction or adverse modification” of critical habitat at 50 CFR 402.02. Instead, we have relied upon the statute and the August 6, 2004, Ninth Circuit Court of Appeals decision in Gifford Pinchot Task Force v. -
Geology of the Northern Jemez Mountains, North-Central New Mexico Kirt A
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/58 Geology of the northern Jemez Mountains, north-central New Mexico Kirt A. Kempter, Shari A. Kelley, and John R. Lawrence, 2007, pp. 155-168 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. -
New Mexico Forest and Watershed Restoration Institute Annual Report 2013-2014
New Mexico Forest and Watershed Restoration Institute Annual Report 2013-2014 The New Mexico Forest and Watershed Restoration Institute (FWRI) exists to promote practices that reduce the risk of catastrophic wildfire and enhance ecosystem function. We have pursued this through four program areas: the biology of restoration treatments, or which tree to cut and which to leave, with an emphasis on the need to burn treated areas; the mechanics of treatments, or how to operate safely and efficiently, a program area that was most active 2008-2010 but currently is dormant; support from geographic information systems (GIS) to field work by FWRI and our partners, which usually involves maps; and monitoring, or how to determine if treatments are effective, and is the subject which accounts for most of our partner’s requests for technical assistance. This report is organized into three broad areas: technical assistance and monitoring, restoration- based economic development, and watershed restoration partnerships. These areas are further subivided as needed. This report focuses on the period 1 October 2013 through 30 September 2014, with activities outside of that period mentioned as needed for context. This period was one of transition for FWRI. First, the previous Director, Andy Egan, left in May 2013 to become Dean of Science at a university in Canada, and the FWRI forester stepped in as Interim Director. Second, an employee resigned unexpectedly at the end of September 2013. We took this opportunity to restructure two positions as program directors for restoration monitoring and for collaboration. These positions were advertised in July 2014. In addition, our Administrative Associate missed six months due to a serious illness. -
Campi Flegrei Caldera, Somma–Vesuvius Volcano, and Ischia Island) from 20 Years of Continuous GPS Observations (2000–2019)
remote sensing Technical Note The Ground Deformation History of the Neapolitan Volcanic Area (Campi Flegrei Caldera, Somma–Vesuvius Volcano, and Ischia Island) from 20 Years of Continuous GPS Observations (2000–2019) Prospero De Martino 1,2,* , Mario Dolce 1, Giuseppe Brandi 1, Giovanni Scarpato 1 and Umberto Tammaro 1 1 Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Napoli Osservatorio Vesuviano, via Diocleziano 328, 80124 Napoli, Italy; [email protected] (M.D.); [email protected] (G.B.); [email protected] (G.S.); [email protected] (U.T.) 2 Istituto per il Rilevamento Elettromagnetico dell’Ambiente, Consiglio Nazionale delle Ricerche, via Diocleziano 328, 80124 Napoli, Italy * Correspondence: [email protected] Abstract: The Neapolitan volcanic area includes three active and high-risk volcanoes: Campi Flegrei caldera, Somma–Vesuvius, and Ischia island. The Campi Flegrei volcanic area is a typical exam- ple of a resurgent caldera, characterized by intense uplift periods followed by subsidence phases (bradyseism). After about 21 years of subsidence following the 1982–1984 unrest, a new inflation period started in 2005 and, with increasing rates over time, is ongoing. The overall uplift from 2005 to December 2019 is about 65 cm. This paper provides the history of the recent Campi Flegrei caldera Citation: De Martino, P.; Dolce, M.; unrest and an overview of the ground deformation patterns of the Somma–Vesuvius and Ischia vol- Brandi, G.; Scarpato, G.; Tammaro, U. canoes from continuous GPS observations. In the 2000–2019 time span, the GPS time series allowed The Ground Deformation History of the continuous and accurate tracking of ground and seafloor deformation of the whole volcanic area.