After the Flow: Landscape Response to the Emplacement Of

Total Page:16

File Type:pdf, Size:1020Kb

After the Flow: Landscape Response to the Emplacement Of AFTER THE FLOW: LANDSCAPE RESPONSE TO THE EMPLACEMENT OF HOLOCENE LAVA FLOWS, CENTRAL OREGON CASCADES, USA by NATALIA IRMA DELIGNE A DISSERTATION Presented to the Department of Geological Sciences and the Graduate School of the University of Oregon in partial fulfillment of the requirements for the degree of Doctor of Philosophy September 2012 DISSERTATION APPROVAL PAGE Student: Natalia Irma Deligne Title: After the Flow: Landscape Response to the Emplacement of Holocene Lava Flows, Central Oregon Cascades, USA This dissertation has been accepted and approved in partial fulfillment of the requirements for the Doctor of Philosophy degree in the Department of Geological Sciences by: Katharine V. Cashman Chairperson Gordon E. Grant Member Alan W. Rempel Member Joshua J. Roering Member Daniel G. Gavin Outside Member and Kimberly Andrews Espy Vice President for Research & Innovation/Dean of the Graduate School Original approval signatures are on file with the University of Oregon Graduate School. Degree awarded September 2012 ii © 2012 Natalia Irma Deligne iii DISSERTATION ABSTRACT Natalia Irma Deligne Doctor of Philosophy Department of Geological Sciences September 2012 Title: After the Flow: Landscape Response to the Emplacement of Holocene Lava Flows, Central Oregon Cascades, USA Effusive volcanic eruptions repave landscapes rapidly with lava flows, resetting the underlying landscape and ecosystem. The unique physical properties of lava pose interesting challenges for recovery, as lava flows can be highly permeable while lava itself is dense, sterile, and generally inhospitable towards life. This dissertation examines two aspects of landscape recovery following lava flow emplacement: (1) hydrologic adaptation of surface and groundwater to recent volcanism and (2) plant colonization of young lava flows. I examine two sites in the central Oregon Cascades: the c. 3 ka Sand Mountain volcanic field (SMVF), located in the headwaters of the McKenzie River, a critical water resource for the state of Oregon, and the c. 1.5 ka Collier Cone lava flow, originating on the north flanks of North Sister volcano. My investigation of the SMVF and upper McKenzie River watershed reveals a complex volcanic history with profound impacts on the configuration and short-term discharge of the McKenzie River: lava flows from the SMVF and other Holocene vents have buried, dammed, and altered the path of the McKenzie River. Moreover, given the large groundwater contribution from the SMVF to the McKenzie River, I estimate that SMVF activity caused McKenzie River discharge in present-day Eugene, Oregon to iv decrease by up to 20% for days to months at a time; future regional mafic volcanic activity could have a similar impact. The SMVF and the Collier Cone lava flow are notable for the juxtaposition of barren exposed lava and mature forests on the same or similarly aged lava flows. I use a combination of LiDAR analysis, field observations, and soil characterization to examine soil and vegetation at these two sites and find that the presence of an external soil source greatly facilitates plant establishment, growth, and survival. Here, external soil sources are syn- or post-eruptive tephra (SMVF) or flood-borne deposits (Collier Cone lava flow). External soil appears to provide a substrate for plants to grow in along with key nutrients and sufficient moisture; overall, external soil sources are key for the initial recovery following an effusive volcanic disturbance. This dissertation includes co-authored material submitted for publication. v CURRICULUM VITAE NAME OF AUTHOR: Natalia Irma Deligne GRADUATE AND UNDERGRADUATE SCHOOLS ATTENDED: University of Oregon, Eugene University of Bristol, Bristol, United Kingdom California Institute of Technology, Pasadena DEGREES AWARDED: Doctor of Philosophy, Geology, 2012, University of Oregon Master of Science by Research, Natural Hazards, 2006, University of Bristol Bachelor of Science, Geology, 2004, California Institute of Technology AREAS OF SPECIAL INTEREST: Physical volcanology Landscape evolution PROFESSIONAL EXPERIENCE: Graduate Teaching and Research Fellow, Department of Geological Sciences, University of Oregon, 2007 - 2012 Seismic Data Analyst, Seismological Laboratory, California Institute of Technology, 2005 - 2007 Teaching Assistant, Division of Geological and Planetary Sciences, California Institute of Technology, 2004 Laboratory Assistant, Division of Geological and Planetary Sciences, California Institute of Technology, 2001 - 2004 GRANTS, AWARDS, AND HONORS: Good Citizen Award, Department of Geological Sciences, University of Oregon, 2011 and 2012 Graduate Student Research Grant, Mazamas, 2010 vi Thayer Scholarship, Department of Geological Sciences, University of Oregon, 2008 and 2009 Kleinman Grant for Volcano Research, US Geological Survey, 2008 Conference Support, IAVCEI General Assembly, 2008 Howard Reynolds Memorial Prize in Geology, Division of Geological and Planetary Sciences, California Institute of Technology, 2004 Summer Undergraduate Research Fellowship, California Institute of Technology, 2001 and 2002 PUBLICATIONS: Riddick, S., Schmidt, D.A. & Deligne, N.I. in press. An analysis of terrain properties and the location of surface scatterers from persistent scatterer interferometry. ISPRS Journal of Photogrammetry and Remote Sensing. Cashman, K.V., Soule, S.A., Mackey, B.H., Deligne, N.I., Deardorff, N.D. & Dietterich, H.R. in press. How lava flows: New insights from applications of lidar technologies to lava flow studies. Geosphere. Deligne, N.I., Coles, S.G. & Sparks, R.S.J. 2010. Recurrence rates of large explosive volcanic eruptions. Journal of Geophysical Research – Solid Earth 115: B06203. Cashman K.V., Deligne, N.I., Gannett, M.W., Grant, G.E. & Jefferson, A. 2009. Fire and water: Volcanology, geomorphology, and hydrogeology of the Cascades Range, central Oregon. In: O’Connor, J.E., Dorsey, R.I. & Madin, I.P. (eds.) Volcanoes to Vineyards: Geologic Field Trips through the Dynamic Landscape of the Pacific Northwest: Field Guide 15, pp. 539-582. Geological Society of America, Boulder, CO, US. Mosenfelder, J.L., Deligne, N.I., Asimow, P.D. & Rossman, G.R. 2006. Hydrogen incorporation in olivine from 2 – 12 GPa. American Mineralogist 91: 285-294. vii ACKNOWLEDGMENTS I thank my advisor, Kathy Cashman, for being incredibly supportive as I followed my curiosity into uncharted territory, and for expecting rigor and clarity in scientific thought, execution, and communication. Kathy has profoundly shaped the scientist I am today. I have also been fortunate to have a fantastic committee – Dan Gavin, Gordon Grant, Josh Roering, and Alan Rempel – who have been very generous with their ideas, energy, resources, and time. Thank you. I also thank Qusheng Jin, Andrew Marcus, and David Schmidt who served on earlier versions of my committee. Many people went above and beyond what could be reasonably expected to help me over the course of my PhD. I am deeply indebted to Rick Conrey, who taught me how to approach volcanic mapping, freely shared his extensive geochemical database, and analyzed over 100 XRF samples for me on his own dime. I am constantly humbled by his generosity, knowledge, and enthusiasm. I also thank the following people for sharing their data with me: Nick Deardorff (LiDAR data for the Collier Cone lava flow, acquired through a 2006 NCALM graduate student grant), and Duane Champion (paleomagnetic data for the Sand Mountain volcanic field). Karl Morgenstern (Eugene Water and Electric Board) and Ian Madin (Oregon’s Department of Geology and Mineral Industries) made acquisition of the upper McKenzie River LiDAR possible. I am lucky to have had great field assistants: Kathy Cashman (rower extraordinaire!), Jim Cleavenger, Nick Deardorff, Brent Deyo, Ariana Everson, Ali Furmall, Emily Gottesfeld, Kyle House, Daniele Mckay, Win McLaughlin, Leland O’Driscoll, Nick Tanushev, Robin Tuohy, Lucy Walsh, Brian Webb and Josh Roering’s river mechanics class. For the days I was alone in the field, Corina Cerovski-Darriau, Scott viii Maguffin, Kristin Sweeney, and Nick Tanushev provided me with a safety net – thank you for participating in Operation Staying Alive. Linn County Parks and Recreation provided me with free rowboat rental in exchange for a map. Chad Everson and Brian Cochran from the Eugene Dive Club worked hard to collected a sample from a 40 m deep tree at altitude in frigid water. I have also enjoyed wonderful days in the field exploring, talking with, and learning from the Cashman and Roering groups and associates, Jim O’Connor and the Collier glacier photomatching crew, and the Kleinman grant and Yeehow teams. In the lab, Willy Amidon guided me through 3He sample preparation from afar and then ran my samples at Caltech the weekend prior to his move to Middlebury College. The Bridgham and Gavin labs provided me with space and resources to conduct my soil analyses; I am particularly grateful to Lorien Reynolds and Erin Herring for always having the time for me despite their packed schedules. The Wallace lab let me monopolize the picking scope for weeks, and Kathryn Watts helped me with sample preparation. The Cashman lab, in particular Daniele Mckay and Hannah Dietterich, kept me sane and happy. I am grateful to have been part of a great department – many thanks to the faculty, office staff, and grad students who make it the special place that it is. Finally, I thank my parents for instilling in me a sense of wonder towards the world and determination for figuring things out, and
Recommended publications
  • Geologic Studies of Union County, New Mexico
    Bulletin 63 New Mexico Bureau of Mines & Mineral Resources A DIVISION OF NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY Geologic Studies of Union County, New Mexico by Brewster Baldwin and William R. Muehlberger SOCORRO 1959 NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY KENNETH W. FORD, President NEW MEXICO BUREAU OF MINES & MINERAL RESOURCES FRANK E. KOTTLOWSKI, Director GEORGE S. Austin, Deputy Director BOARD OF REGENTS Ex Officio Bruce King, Governor of New Mexico Leonard DeLayo, Superintendent of Public Instruction Appointed William G. Abbott, Secretary-Treasurer, 1961-1985, Hobbs Judy Floyd, President, 1977-1981, Las Cruces Owen Lopez, 1977-1983, Santa Fe Dave Rice, 1972-1983, Carlsbad Steve Torres, 1967-1985, Socorro BUREAU STAFF Full Time MARLA D. ADKINS, Assistant Editor LYNNE MCNEIL, Staff Secretary ORIN J. ANDERSON, Geologist NORMA J. MEEKS, Department Secretary RUBEN ARCHULETA, Technician I ARLEEN MONTOYA, Librarian/Typist WILLIAM E. ARNOLD, Scientific Illustrator SUE NESS, Receptionist ROBERT A. BIEBERMAN, Senior Petrol. Geologist ROBERT M. NORTH, Mineralogist LYNN A. BRANDVOLD, Chemist JOANNE C. OSBURN, Geologist CORALE BRIEBLEY, Chemical Microbiologist GLENN R. OSBURN, Volcanologist BRENDA R. BROADWELL, Assoc. Lab Geoscientist LINDA PADILLA, Staff Secretary FRANK CAMPBELL, Coal Geologist JOAN C. PENDLETON, Associate Editor RICHARD CHAMBERLIN, Economic Geologist JUDY PERALTA, Executive Secretary CHARLES E. CHAPIN, Senior Geologist BARBARA R. Popp, Lab. Biotechnologist JEANETTE CHAVEZ, Admin. Secretary I ROBERT QUICK, Driller's Helper/Driller RICHARD R. CHAVEZ, Assistant Head, Petroleum MARSHALL A. REITER, Senior Geophyicist RUBEN A. CRESPIN, Laboratory Technician II JACQUES R. RENAULT, Senior Geologist Lois M. DEVLIN, Director, Bus.-Pub. Office JAMES M. ROBERTSON, Mining Geologist KATHY C. EDEN, Editorial Technician GRETCHEN H.
    [Show full text]
  • Source to Surface Model of Monogenetic Volcanism: a Critical Review
    Downloaded from http://sp.lyellcollection.org/ by guest on September 28, 2021 Source to surface model of monogenetic volcanism: a critical review I. E. M. SMITH1 &K.NE´ METH2* 1School of Environment, University of Auckland, Auckland, New Zealand 2Volcanic Risk Solutions, Massey University, Palmerston North 4442, New Zealand *Correspondence: [email protected] Abstract: Small-scale volcanic systems are the most widespread type of volcanism on Earth and occur in all of the main tectonic settings. Most commonly, these systems erupt basaltic magmas within a wide compositional range from strongly silica undersaturated to saturated and oversatu- rated; less commonly, the spectrum includes more siliceous compositions. Small-scale volcanic systems are commonly monogenetic in the sense that they are represented at the Earth’s surface by fields of small volcanoes, each the product of a temporally restricted eruption of a composition- ally distinct batch of magma, and this is in contrast to polygenetic systems characterized by rela- tively large edifices built by multiple eruptions over longer periods of time involving magmas with diverse origins. Eruption styles of small-scale volcanoes range from pyroclastic to effusive, and are strongly controlled by the relative influence of the characteristics of the magmatic system and the surface environment. Gold Open Access: This article is published under the terms of the CC-BY 3.0 license. Small-scale basaltic magmatic systems characteris- hazards associated with eruptions, and this is tically occur at the Earth’s surface as fields of small particularly true where volcanic fields are in close monogenetic volcanoes. These volcanoes are the proximity to population centres.
    [Show full text]
  • Natural Phenomena Around the World
    What are some of the best rare natural phenomena that occur on Earth? What is a phenomenon? It is an interesting fact or even that happens and is typically difficult to understand or explain fully. Below we will learn about some of Mother Nature’s most amazing phoneomena, from Australia’s bubblegum-pink lake and a blood-red waterfall in Antarctica and a US valley where stones eerily move. Let’s find out more about Mother Nature’s natural phenomena. Frozen methane bubbles, Canada They look like flying saucers that dropped into the water and froze, or like jellyfish captured in ice. In fact, these icy circles are frozen methane bubbles – pockets of gas that, when trapped underwater and frozen, form a spectacular landscape. Found in winter in high northern latitude lakes like Lake Abraham in Alberta, Canada, these gas bubbles are created when dead leaves, grass and animals fall into the water, sink and are eaten by bacteria that excrete methane. The gas (methane) is released as bubbles that transform into tens of thousands of icy white disks when they come into contact with frozen water. This potent greenhouse gas not only warms the planet, but also is highly flammable – so the frozen bubbles are in fact quite dangerous. Come spring, when the ice melts, the methane bubbles pop and fizz in a spectacular release – but if anyone happens to light a match nearby, the masses of methane will ignite into a giant explosion! Sailing Stones, US The dry lake of Racetrack Playa in California’s Death Valley, US, is famous for its sailing stones.
    [Show full text]
  • Further Details of Martinique Horror
    FURTHER DETAILS OF MARTINIQUE HORROR Captain of the Steamer “Roddam” Describes the Terrible Scenes Through Which He Passed —Tale Perhaps Never Had a Parallel in Stories of the Sea passed First of all the ships that watch I found that we had been about to everybody to stand clear. An In- Lucia, the brave man refused all medi- . culminates in the vast crater of Morne through the shower of ashes of Mont an hour reaching daylight. stant later the air was filled with flame cal treatment until the others were y Garou, which in 1812 was the scene Pelee and reached the American main- "Our decks were covered two inches and falling batches of fire. The ship cared for. He will live, the doctors of a tremendous eruption. Billions of land to tell about It, the British Etona, with this matter.” and the captain ex- was immediately ablaze from end to tell me.” tonH of rock and earth were hurled bound to New York from Montevideo hibited a box of volcanic dust, which end, and the crew and laborers aboard air—part, BEAUTIFUL ISLE OF ST. VINCENT high into the aa molten and St. Lucia, has arrived at New had been saved by his crew. “You began to rush about, frantic with pain. lava, flowed down Into the sea; part, York. Her captain, John Cantell, and can see the marks of it yet about the “Capt. Freeman ran Into tin.' chart- Wm an Earth!? rara ll««- lleforr tha shivered into thin dust, was carried her passengers brought woodwork, with them a marts and our polished room, but was driven out again by Rat ant Awful IMuaa'er.
    [Show full text]
  • Lightning Bolt
    THE LIGHTNING BOLT CRAWFORD LEADS THE CHARGE MARIO GAME AND MOVIE REVIEWS COVID COVERAGE-THEATRE, SPORTS, TEACHERS,PROCEDURES VOLUME 33 iSSUE 1 CHANCELLOR HIGH SCHOOL 6300 HARRISON ROAD, FREDERICKSBURG, VA 22407 1 Sep/Oct 2020 RETIREMENT, RETURN TO SCHOOL, MRS. GATTIE AND CRAWFORD ADVISOR FAITH REMICK Left Mrs. Bass-Fortune is at her retirement parade on June EDITOR-IN-CHIEF 24 that was held to honor her many years at Chancellor High School. For more than three CARA SEELY hours decorated cars drove by the school, honking at Mrs. NEWS EDITOR Bass-Fortune, giving her gifts and well wishes. CARA HADDEN FEATURES EDITOR KAITLYN GARVEY SPORTS EDITOR STEPHANIE MARTINEZ & EMMA PURCELL OP-ED EDITORS Above and Left: Chancellor gets a facelift of decorated doors throughout the school. MIKAH NELSON Front Cover:New Principal Mrs. Cassandra Crawford & Back Cover: Newly Retired HAILEY PATTEN Mrs. Bass-Fortune CHARGING CORNER CHARGER FUR BABIES CONTEST MATCH THE NAME OF THE PET TO THE PICTURE AND TAKE YOUR ANSWERS TO ROOM A113 OR EMAIL LGATTIE@SPOT- SYLVANIA.K12.VA.US FOR A CHANCE TO WIN A PRIZE. HAVE A PHOTO OF YOUR FURRY FRIEND YOU WANT TO SUBMIT? EMAIL SUBMISSIONS TO [email protected]. Charger 1 Charger 2 Charger 3 Charger 4 Names to choose from. Note: There are more names than pictures! Banks, Sadie, Fenway, Bently, Spot, Bear, Prince, Thor, Sunshine, Lady Sep/Oct 2020 2 IS THERE REWARD TO THIS RISK? By Faith Remick school even for two days a many students with height- money to get our kids back Editor-In-Chief week is dangerous, and the ened behavioral needs that to school safely.” I agree.
    [Show full text]
  • A History of Beaver County, Utah Centennial County History Series
    A HISTORY OF 'Beaver County Martha Sonntag Bradley UTAH CENTENNIAL COUNTY HISTORY SERIES A HISTORY OF 'Beaver County Martha Sonntag Bradley The settlement of Beaver County began in February 1856 when fifteen families from Parowan moved by wagon thirty miles north to Beaver Valley. The county was created by the Utah legislature on 31 January 1856, a week before the Parowan group set out to make their new home. However, centuries before, prehistoric peoples lived in the area, obtaining obsidian for arrow and spear points from the Mineral Mountains. Later, the area became home to Paiute Indians. Franciscan Friars Dominguez and Escalante passed through the area in October 1776. The Mormon settlement of Beaver devel­ oped at the foot of the Tushar Mountains. In 1859 the community of Minersville was es­ tablished, and residents farmed, raised live­ stock, and mined the lead deposits there. In the last quarter of the nineteenth century the Mineral Mountains and other locations in the county saw extensive mining develop­ ment, particularly in the towns of Frisco and Newhouse. Mining activities were given a boost with the completion of the Utah South­ ern Railroad to Milford in 1880. The birth­ place of both famous western outlaw Butch Cassidy and inventor of television Philo T. Farnsworth, Beaver County is rich in history, historic buildings, and mineral treasures. ISBN: 0-913738-17-4 A HISTORY OF 'Beaver County A HISTORY OF Beaver County Martha Sonntag Bradley 1999 Utah State Historical Society Beaver County Commission Copyright © 1999 by Beaver County Commission All rights reserved ISBN 0-913738-17-4 Library of Congress Catalog Card Number 98-61325 Map by Automated Geographic Reference Center—State of Utah Printed in the United States of America Utah State Historical Society 300 Rio Grande Salt Lake City, Utah 84101-1182 Contents ACKNOWLEDGMENTS vii GENERAL INTRODUCTION ix CHAPTER 1 Beaver County: The Places That Shape Us .
    [Show full text]
  • Lunar Crater Volcanic Field (Reveille and Pancake Ranges, Basin and Range Province, Nevada, USA)
    Research Paper GEOSPHERE Lunar Crater volcanic field (Reveille and Pancake Ranges, Basin and Range Province, Nevada, USA) 1 2,3 4 5 4 5 1 GEOSPHERE; v. 13, no. 2 Greg A. Valentine , Joaquín A. Cortés , Elisabeth Widom , Eugene I. Smith , Christine Rasoazanamparany , Racheal Johnsen , Jason P. Briner , Andrew G. Harp1, and Brent Turrin6 doi:10.1130/GES01428.1 1Department of Geology, 126 Cooke Hall, University at Buffalo, Buffalo, New York 14260, USA 2School of Geosciences, The Grant Institute, The Kings Buildings, James Hutton Road, University of Edinburgh, Edinburgh, EH 3FE, UK 3School of Civil Engineering and Geosciences, Newcastle University, Newcastle, NE1 7RU, UK 31 figures; 3 tables; 3 supplemental files 4Department of Geology and Environmental Earth Science, Shideler Hall, Miami University, Oxford, Ohio 45056, USA 5Department of Geoscience, 4505 S. Maryland Parkway, University of Nevada Las Vegas, Las Vegas, Nevada 89154, USA CORRESPONDENCE: gav4@ buffalo .edu 6Department of Earth and Planetary Sciences, 610 Taylor Road, Rutgers University, Piscataway, New Jersey 08854-8066, USA CITATION: Valentine, G.A., Cortés, J.A., Widom, ABSTRACT some of the erupted magmas. The LCVF exhibits clustering in the form of E., Smith, E.I., Rasoazanamparany, C., Johnsen, R., Briner, J.P., Harp, A.G., and Turrin, B., 2017, overlapping and colocated monogenetic volcanoes that were separated by Lunar Crater volcanic field (Reveille and Pancake The Lunar Crater volcanic field (LCVF) in central Nevada (USA) is domi­ variable amounts of time to as much as several hundred thousand years, but Ranges, Basin and Range Province, Nevada, USA): nated by monogenetic mafic volcanoes spanning the late Miocene to Pleisto­ without sustained crustal reservoirs between the episodes.
    [Show full text]
  • PDF Linkchapter
    Index [Italic page numbers indicate major references] Abajo Mountains, 382, 388 Amargosa River, 285, 309, 311, 322, Arkansas River, 443, 456, 461, 515, Abort Lake, 283 337, 341, 342 516, 521, 540, 541, 550, 556, Abies, 21, 25 Amarillo, Texas, 482 559, 560, 561 Abra, 587 Amarillo-Wichita uplift, 504, 507, Arkansas River valley, 512, 531, 540 Absaroka Range, 409 508 Arlington volcanic field, 358 Acer, 21, 23, 24 Amasas Back, 387 Aromas dune field, 181 Acoma-Zuni scction, 374, 379, 391 Ambrose tenace, 522, 523 Aromas Red Sand, 180 stream evolution patterns, 391 Ambrosia, 21, 24 Arroyo Colorado, 395 Aden Crater, 368 American Falls Lava Beds, 275, 276 Arroyo Seco unit, 176 Afton Canyon, 334, 341 American Falls Reservoir, 275, 276 Artemisia, 21, 24 Afton interglacial age, 29 American River, 36, 165, 173 Ascension Parish, Louisana, 567 aggradation, 167, 176, 182, 226, 237, amino acid ash, 81, 118, 134, 244, 430 323, 336, 355, 357, 390, 413, geochronology, 65, 68 basaltic, 85 443, 451, 552, 613 ratios, 65 beds, 127,129 glaciofluvial, 423 aminostratigraphy, 66 clays, 451 Piedmont, 345 Amity area, 162 clouds, 95 aggregate, 181 Anadara, 587 flows, 75, 121 discharge, 277 Anastasia Formation, 602, 642, 647 layer, 10, 117 Agua Fria Peak area, 489 Anastasia Island, 602 rhyolitic, 170 Agua Fria River, 357 Anchor Silt, 188, 198, 199 volcanic, 54, 85, 98, 117, 129, Airport bench, 421, 423 Anderson coal, 448 243, 276, 295, 396, 409, 412, Alabama coastal plain, 594 Anderson Pond, 617, 618 509, 520 Alamosa Basin, 366 andesite, 75, 80, 489 Ash Flat, 364 Alamosa
    [Show full text]
  • Geomorphological Evolution and Chronology of the Eruptive Activity of the Columba and Cuevas Volcanoes (Campo De Calatrava Volcanic Field, Ciudad Real, Central Spain)
    Accepted Manuscript Geomorphological evolution and chronology of the eruptive activity of the Columba and Cuevas volcanoes (Campo de Calatrava Volcanic Field, Ciudad Real, Central Spain) Miguel Ángel Poblete Piedrabuena, Joan Martí Molist, Salvador Beato Bergua, José Luis Marino Alfonso PII: S0169-555X(19)30125-4 DOI: https://doi.org/10.1016/j.geomorph.2019.03.026 Reference: GEOMOR 6720 To appear in: Geomorphology Received date: 4 December 2018 Revised date: 14 March 2019 Accepted date: 25 March 2019 Please cite this article as: M.Á.P. Piedrabuena, J.M. Molist, S.B. Bergua, et al., Geomorphological evolution and chronology of the eruptive activity of the Columba and Cuevas volcanoes (Campo de Calatrava Volcanic Field, Ciudad Real, Central Spain), Geomorphology, https://doi.org/10.1016/j.geomorph.2019.03.026 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. ACCEPTED MANUSCRIPT Geomorphological evolution and chronology of the eruptive activity of the Columba and Cuevas volcanoes (Campo de Calatrava Volcanic Field, Ciudad Real, Central Spain) Miguel Ángel Poblete Piedrabuena1*, Joan Martí Molist2, Salvador Beato Bergua1, José Luis Marino Alfonso1 Department of Geography, University of Oviedo, Campus de El Milán, C/Amparo Pedregal, 5, Oviedo-33011, Spain.
    [Show full text]
  • The Lathrop Wells Volcanic Center: Status of Field and Geochronology
    THE LATHROP WELLS VOLCANIC CENTERi;,? - t, ,„ . STATUS OF HELD AND GEOCHRONOLOOy STUDIES ° WJ o B. Crowe and R. Morley, Los Alamos Naiional Laboratory. Las VegasSr, Nevad/ a S. Wells, University of California, Riverside, Riverside, California 3. Geissroan, E. McDonald, L. McFaddcn, and. F. Perry, University of New Mesaco. Albuquerque, New Mexico M. Murrell and J. Poths, Los Alamos National Laboratory, Los AJamos, New Mexico S. Forman, Ohio State University, Columbus, Ohio INTRODUCTION passible age assignments for the Lalhrop Wells center.10-" The affects of Ihe different age assignments The Lathrop Wells volcanic center is located 20 km wer*. evaluated for calculations of the recurrence of south of the poienusl Yucca Mountain site, at the south vdcanjc events for *-he Yucca Mountain region. The end of the Yucca Mountain range, [t has long been impact of a possible Late pleistocene or Holocenc age recognized AS the youngesi basalt center is the region.1 for all or parts of the center can be examined in terns However, determination of the age and eruptive history of two hypotheses. If we assume the Lathrop Wells of the center has proven problematic The Lathrop center is young (< 50 ka) and (hat hypothesis is Wells center was interpreted originally as a incorrect, we have erred toward overesUmai ing volcanic monogenetk basalt center," Its age was inferred to be risk. Conversely if the hypothesis e tint the center is about 300 lea/-5 However, during the earliest stages of older (> 100 ka), and that ts incorrect, we have erred study of the Yucca Mountain area (1980-1985), two toward underestimating volcanic risk.
    [Show full text]
  • Geologic Map of the Indian Spring Quadrangle, San Bernardino County, California
    U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Geologic Map of the Indian Spring Quadrangle, San Bernardino County, California by H.G. Wilshire 1 Open-File Report 92-181 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. *345 Middlefield Road MS/975, Menlo Park, CA 94025 GEOLOGIC MAP OF THE INDIAN SPRING QUADRANGLE, SAN BERNARDINO COUNTY, CALIFORNIA INTRODUCTION Eruptive rocks of the Cima volcanic field occur almost entirely within six 7.5 minute quadrangles, Indian Spring, Marl Mountains, Granite Spring, Cow Cove, Solomons Knob, and Valley Wells. The following description applies to all six quadrangles. The Cima volcanic field is a small (-300 km^) Tertiary-Quaternary alkaline basalt field in the Ivanpah highlands (Hewett, 1956), in east-central Mojave Desert (Fig. 1). The basaltic rocks, which range from late Miocene to Holocene, were erupted from at least 71 vents. The younger vents are well-formed cinder cones, whereas older vents are marked by degraded cinder cones, plugs, and crater-fill lava flows. The volcanic rocks were described in a general geologic study by Hewett (1956). The southern part of the field was mapped by Barca (1966), and fie northern part by DeWitt (1980). Topical studies of the volcanic field include the geomorphology of pediment domes (Sharp, 1957; Dohrenwend and others, 1984a,b), geomorphic and soil evolution of the lava flows (Wells and others, 1984; McFadden and others, 1984), paleontology and stratigraphy of Tertiary and Quaternary deposits of the Shadow Valley Basin (Reynolds and Nance, 1988), structural studies (Hewett, 1956; Dunne, 1977; Reynolds, 1990; Skirvin and Wells, 1990), polycyclic volcanism (Renault and Wells, 1990), and evolution of the upper mantle and lower crust beneath Cima based on xenoliths in the basalts (Wilshire, 1990; Wilshire and others, 1991).
    [Show full text]
  • PHOTOVOLTAIC SYSTEM for BUILDING 300 at DIAMOND HEAD OAHU, HAWAII Job No. CA–1105-C TECHNICAL SPECIFICATIONS
    PHOTOVOLTAIC SYSTEM FOR BUILDING 300 AT DIAMOND HEAD OAHU, HAWAII Job No. CA–1105-C PREPARED FOR Hawaii Army National Guard Department of Defense State of Hawaii TECHNICAL SPECIFICATIONS FINAL DESIGN June 2012 828 Fort Street Mall, Suite 500 y Honolulu, Hawaii 96813 Tel: 808 521-3773 TABLE OF CONTENTS DIVISION 1 – GENERAL REQUIREMENTS Section 01100 Project Requirements..................................................................... 1-4 Section 01105 Special Project Procedures ............................................................ 1-2 Section 01310 Project Management and Coordination .......................................... 1-5 Section 01320 Construction Progress Documentation........................................... 1-7 Section 01330 Submittal Procedures..................................................................... 1-5 Section 01500 Temporary Facilities and Controls................................................ 1-14 Section 01575 Temporary Controls – Air Quality ................................................... 1-4 Section 01700 Execution Requirements ................................................................ 1-5 Section 01715 Existing Conditions – Hazardous Material Survey (see attached report).......................................................................1-3 (Attachment: Targeted Hazardous Material Survey Report for Building 300, Solar Photovoltaic Installation, Hawai’I Army National Guard Armory, 3949 Diamond Head Road, Honolulu, Hawaii, dated September 5, 2011, prepared by Myounghee Noh & Assoc.,
    [Show full text]