GEORGE W. BERGANTZ Curriculum Vitae

Total Page:16

File Type:pdf, Size:1020Kb

GEORGE W. BERGANTZ Curriculum Vitae GEORGE W. BERGANTZ Curriculum Vitae Dept. of Earth and Space Sciences, Box 351310 7336 38th Ave., N.E. The University of Washington Seattle, WA 98115-5939 Seattle, WA 98195 (206) 525-1457 (206) 685-4972 Education: Ph.D. in Earth and Planetary Sciences, July, 1988 The Johns Hopkins University Dissertation Title: Convection and Solidification in Tall Magma Chambers M.S. in Geophysical Sciences, May, 1985 Georgia Institute of Technology, Thesis title, “Double-diffusive Boundary Layer Convection in a Porous Medium: Implications for Fractionation in Magma Chambers” B.Sc. (Cum Laude) in Geological Engineering, May, 1983 Minor in Mathematics Mackay School of Mines, University of Nevada, Reno Academic and Professional Experience: Professor Dept. of Earth and Space Sciences, University of Washington, Sept. 2000 to present. Associate Professor Dept. of Geological Sciences, University ofWashington, Sept. 1993 to Sept. 2000. Adjunct Associate Professor in Geophysics. Assistant Professor Dept. of Geological Sciences, University of Washington, Sept. 1988 to Sept. 1993. Appointed Member of Graduate Faculty. Geologist, Geological Engineer Lawrence Livermore National Laboratory, Summers 1983-1985. Geologist U.S.Geological Survey, field geologist, summers 1979-1981. Geologist Woodward-Clyde and Consultant Dr. D. B. Slemmons, 1980-1983. University Service Faculty Senate Executive Council Faculty Senate (nominated for Vice Chair, nomination refused) Dean’s Summer Program Committee Faculty Appeal Board Burke Museum Site-planning Committee Ad hoc President’s Roadmap Committee Diversity in the Curriculum Committee (Graduate School) Department Service Executive Committee Undergraduate Advisor Graduate Admissions Committee Awards Committee (three times) Curriculum Committee Colloquium Organizer (four times) Technical Staff Evaluation Library Liaison Department newsletter (twice) 9 search committees for tenure-track faculty positions Geological Sciences Chair Search committee White Paper Committee Curriculum Committee PEC Committee Student Numbers and Quality Committee Grants, Fellowships & Contracts: Single PI: Univ. Washington Graduate School Research Fund: "Thermal Mechanical Constraints on Granite Melt Dynamics and Crystallization" $ 8,333. Dates: July 1, 1989 – June 15, 1990. Univ. of Washington Royalty Research Fund: “Interplay between crustal growth, mantle magmatism and chemical diversity” $19,921. Dates: Jan. 15, 1995 – April 15, 1996. Battelle, Pacific Northwest Labs: "Feasibility Study of ISV" $8,500. Dates: Oct. 1, 1989 – Oct. 1, 1990. NSF-OSE: "Magmatic Processes at Oceanic Spreading Centers" $ 60,401. Dates: July, 1, 1990 – July 1, 1993. NSF-EAR: "Underplating and Partial Melting: Implications for Magma Generation" $63,922. Dates: Jan. 15, 1991 – June 30, 1993. NSF-EAR: “The Generation and Mobilization of Dehydration Melts, Formation of Migmatites, Plutons and Mixed Magmas ” $100,390. Dates: July 1, 1995 – Jan. 1, 1998. NSF-EAR: “Multiphase Modeling of Solidification and the Dynamics of Magma Chambers” $81,000. Dates: July 1, 1998 - June 30, 2000. NSF-EAR: “Using Spatial Coherency to Determine Mechanics of Mixing”, $198,093. Dates: July 1, 2001-June 30, 2004 NSF-EAR, “Support for Penrose Conference” $10,000. Dates Feb. 1, 2001-Jan. 31, 2002 NASA , “Graduate student fellowship for eruption modeling” $72,000, Sept. 1, 2004-Sept. 14, 2007 NSF-EAR, “Integrating computational volcanology with natural deposits: an investigation of over-water and over-land volcanic transport of the Kos Plateau Tuff” $265,085. Dates: Jan.1 2005 – Dec. 31, 2008 NSF-EAR, “Dynamics and timescales of magmatic processes in the crust: A collaborative study of Volcán Quizapu” $230,693. Dates: July 1 2007 – June 30, 2010 NSF-EAR, “Dynamics of Large Silicic Magma Reservoirs: Combining Geochemical Data and Physical Models on Voluminous Ignimbrites From the San Juan Volcanic Field, Colorado” $305,000. Dates July 1, 2008-June 30 2011. NSF-EAR, “Establishing the Time and Length Scales of Initial Arc Construction: The Mantle-crust Connection” $322,545. Dates March 1, 2011 – Feb. 28, 2014. NSF-EAR, “Life Cycles of Basaltic Magma Mushes: The Dynamic Controls on Unlocking and Mixing” $325, 142. Dates April 1, 2015-March 31, 2018. Associated Western Universities Fellowship to Battelle, Pacific Northwest Labs, Summer 1994. Multiple PI: NSF-EAR: "A Re-evaluation of the Ballooning Pluton Hypothesis", $ 8,000, sub-contract from Prof. Scott Paterson at U.S.C. Dates: Sept. 1, 1989 – Sept. 1, 1990. NSF-EAR: “Integration of Advanced Computer Workstations into Undergraduate Geological Sciences Curriculum”, $29,000. Dates July 15, 1993-Dec. 31, 1995. NSF-VPW: Women in Science Program, joint with Prof. Anita Grunder, Oregon State University. Funded sabbatical leave and research costs for visiting woman scientist at UW, $79,166. Sept. 1, 1993-Feb. 28, 1995. NSF-SAT: Science and Technology Center in Volcanology. Joint with University of Hawaii, total 5 year budget: $19,271,925. Proposal passed highly competitive initial reviews but not list of final five. Associate Editor: Journal of Petrology Journal of Volcanology and Geothermal Research Conferences and Symposium Organized: Penrose Conference on Arc Magmatism and Origin of Tonalites, Chelan, WA, 1992 Keynote Symposium GSA National Meeting, Seattle, 1995 Penrose Conference on Melt Generation and Migration, Verbania, Italy 1997 Penrose Conference on Longevity of Silicic Systems, Mammoth Lakes, California 2001 Pardee Symposium on Melt in the Crust and Mantle, GSA National Meeting, 2001 Special Session AGU-EUG-EGU meeting, Nice, 2003 Special Session AGU meeting Spring 2004 Special Sessipn AGU meeting Fall 2005 Modeling Explosive Volcanism Workshop, Spring 2007 Special session AGU meeting Fall 2012 Keynote and Invited Talks: EGU Spring meeting 2016 “Re-awakening magmatic systems” SOTA “State of the Arc” Conference 2015 AGU Session Fall 2014 “Physical Petrology” IAVCEI meeting Japan, 2013 AGU Session Fall 2012, “Space, Time, and Transport in Petrology and Geochemistry” AGU Session Fall 2012 The Mush Model: Paradigm or Straitjacket? PIRE Workshop on Environmental and extreme multiphase flows 2012, “Grain-scale processes in dense and transitional granular flows” AGU Session on Crustal Systematics 2011 MARGINS Planning Workshop 2011 Society of Mathematical Geology, Pisa Italy 2010 Penrose on Yellowstone and SRP rhyolites 2009 Mineralogical Society Short Course: “Magma Dynamics” 2008 IAVCEI Cities on Volcanoes “Probing the emergent structures and mechanics of pyroclastic flows: Integrating thedynamics and deposits of volcanic eruptions" 2007 AGU Session “Will the Real PhenoCryst Please Stand Up?” Fall 2005 AGU Session “Experimental and Numerical Exploration of Volcanic Phenomena” Fall 2005 Conference on Mechanics of Turbidites, Santa Barbara, keynote, 2005 American Physical Society, Fluid Dynamics Div., keynote for annual meeting 2004 AGU Session “Birth, Growth, and Death of Magmatic Arcs: Comparisons Among Arcs in Different Settings,” AGU Fall 2003 SOTA ‘State of the Arc’ Conference, 2003 SOTA ‘State of the Arc’ Conference, 2007 Eruption Modeling Workshop, 2002 Penrose Conference on Silicic Systems, 2001 German Conference: “Orogenic processes - quantification and simulation in the mid-European Variscides" Penrose Conference on Melt Generation and Migration Chapman Conference on Ocean Island Magmatism Hutton Conference on the Origin of Granites Reviews of Mineralogy Short Course on Contact Metamorphism Penrose Conference on Arc Magmatism and Origin of Tonalites Reviews of Mineralogy Short Course on Modern Methods of Igneous Petrology Conference on Chaotic Systems and Geology IAVCEI meeting on Continental Magmatism Penrose Conference of the Mechanisms of Emplacement of Magmas NATO Conference on Structure and Dynamics of Partially Solidified Systems Other Invited Talks: Cal Tech, U.C.S.C., U.C. Berkeley, Univ. Oregon, U.S.C., Univ. of Chicago, Penn. State., U.C.L.A. (twice), Stanford, Cascade Volcano Observatory, Univ. Mass., Oregon State Univ., Hampshire College, Univ. New Mexico, Univ. Nevada, Mich. State, Univ. North Carolina, Univ. of Iowa, Western Washington, Univ. of Georgia, Univ. of Alaska, U.C. Davis, Univ. British Columbia, Univ. Utah Student Supervision (detailed elsewhere): Committee chair: 5 Ph.D., 5 M.S. Committee member: 18 Ph.D., 5 M.S. Competitive and Outside Offers Offered Macdonald Chair (at full Professor rank) in Volcanology and position of State Volcanologist, University and State of Hawaii, 1998. UW retention offer accepted. Other Fellow of the Geological Society of America Fulbright Scholar evaluation committee Evaluation letters for: promotion to full rank, UCLA; tenure at WSU, Univ. Wyoming, Univ. of Minnesota, Univ. of Illionis, Univ. of Missiouri, Pamona College, Rice Univ., Brown Univ., Univ. British Columbia; Habilitation for German University System. Membership: American Geophysical Union, Geological Society of America, Sigma Xi, Tau Beta Pi (engineering honor society) Member ARCUS, Arctic Research review panel Member of the AAAS Review Committee for the USGS Volcano Hazards Program U.S. DOE Multiphase Flow & Multiscale Simulations and Optimization Merit Review Google Scholar Profile http://scholar.google.com/citations?user=BeHnnFIAAAAJ&hl=en Publications (* invited papers) all are peer or editor reviewed: Schleicher, J.M., Bergantz, G.W., Breidenthal, R.E., Burgisser, A., 2016, “Time scales of mixing in magma mushes”, Geophysical Research Letters, v. 43(4), p. 1543-1550. Bergantz, G.W., Schleicher, J.M., Burgisser,
Recommended publications
  • A Pictorial Summary of the Life and Work of George Patrick Leonard Walker
    A pictorial summary of the life and work of George Patrick Leonard Walker SCOTT K. ROWLAND1* & R. S. J. SPARKS2 1Department of Geology and Geophysics, University of Hawaii at Manoa, 1680 East–West Road, Honolulu, Hawaii, USA 2Department of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK *Corresponding author (e-mail: [email protected]) Abstract: George Patrick Leonard Walker was one of the fathers of modern volcanology. He worked in many parts of the world and contributed to the understanding of a huge range of volca- nological processes. He was a field geologist at heart, and one of his greatest skills was the ability to quantify volcanological ideas – not with obscure statistical treatments or complex numerical models, but with clear graphical relationships supported by tremendous amounts of carefully col- lected field data. Here we present some glimpses of his life and work in photographs and diagrams. George Walker was born on 2 March 1926 in Iceland, as well as to India, Italy, the Azores and London. In 1939, when he was 13, the family Africa, among other locations. In 1978 George moved to Northern Ireland. In 1948 and 1949, moved to the University of Auckland and in 1982 respectively, George received his Bachelors and he moved to the University of Hawaii. Over the Masters degrees from Queen’s University, Belfast. span of his career he visited almost every volcanic In 1956 he completed his PhD at the University of region in the world, including Australia, the Azores, Leeds with a dissertation on secondary minerals in the Canary Islands, Chile, China, Costa Rica, igneous rocks of Northern Iceland.
    [Show full text]
  • Mars Field Geology, Biology, and Paleontology Workshop, Summary
    MARS FIELD GEOLOGY, BIOLOGY, AND PALEONTOLOGY WORKSHOP: SUMMARY AND RECOMMENDATIONS November 18–19, 1998 Space Center Houston, Houston, Texas LPI Contribution No. 968 MARS FIELD GEOLOGY, BIOLOGY, AND PALEONTOLOGY WORKSHOP: SUMMARY AND RECOMMENDATIONS November 18–19, 1998 Space Center Houston Edited by Nancy Ann Budden Lunar and Planetary Institute Sponsored by Lunar and Planetary Institute National Aeronautics and Space Administration Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 LPI Contribution No. 968 Compiled in 1999 by LUNAR AND PLANETARY INSTITUTE The Institute is operated by the Universities Space Research Association under Contract No. NASW-4574 with the National Aeronautcis and Space Administration. Material in this volume may be copied without restraint for library, abstract service, education, or personal research purposes; however, republication of any paper or portion thereof requires the written permission of the authors as well as the appropriate acknowledgment of this publication. This volume may be cited as Budden N. A., ed. (1999) Mars Field Geology, Biology, and Paleontology Workshop: Summary and Recommendations. LPI Contribution No. 968, Lunar and Planetary Institute, Houston. 80 pp. This volume is distributed by ORDER DEPARTMENT Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 Phone: 281-486-2172 Fax: 281-486-2186 E-mail: [email protected] Mail order requestors will be invoiced for the cost of shipping and handling. _________________ Cover: Mars test suit subject and field geologist Dean Eppler overlooking Meteor Crater, Arizona, in Mark III Mars EVA suit. PREFACE In November 1998 the Lunar and Planetary Institute, under the sponsorship of the NASA/HEDS (Human Exploration and Development of Space) Enterprise, held a workshop to explore the objectives, desired capabilities, and operational requirements for the first human exploration of Mars.
    [Show full text]
  • Educators Guide
    EDUCATORS GUIDE 02 | Supervolcanoes Volcanism is one of the most creative and destructive processes on our planet. It can build huge mountain ranges, create islands rising from the ocean, and produce some of the most fertile soil on the planet. It can also destroy forests, obliterate buildings, and cause mass extinctions on a global scale. To understand volcanoes one must first understand the theory of plate tectonics. Plate tectonics, while generally accepted by the geologic community, is a relatively new theory devised in the late 1960’s. Plate tectonics and seafloor spreading are what geologists use to interpret the features and movements of Earth’s surface. According to plate tectonics, Earth’s surface, or crust, is made up of a patchwork of about a dozen large plates and many smaller plates that move relative to one another at speeds ranging from less than one to ten centimeters per year. These plates can move away from each other, collide into each other, slide past each other, or even be forced beneath each other. These “subduction zones” are generally where the most earthquakes and volcanoes occur. Yellowstone Magma Plume (left) and Toba Eruption (cover page) from Supervolcanoes. 01 | Supervolcanoes National Next Generation Science Standards Content Standards - Middle School Content Standards - High School MS-ESS2-a. Use plate tectonic models to support the HS-ESS2-a explanation that, due to convection, matter Use Earth system models to support cycles between Earth’s surface and deep explanations of how Earth’s internal and mantle. surface processes operate concurrently at different spatial and temporal scales to MS-ESS2-e form landscapes and seafloor features.
    [Show full text]
  • GSA TODAY December Vol
    Vol. 5, No. 12 December 1995 INSIDE • New Members, Fellows, Student Associates, p. 247 GSA TODAY South-Central Section Meeting, p. 250 • A Publication of the Geological Society of America • Northeastern Section Meeting, p. 253 Seismic Images of the A B Core-Mantle Boundary Michael E. Wysession, Department of Earth and Planetary Sciences, Washington University, St. Louis, MO 63130 C D ABSTRACT INTRODUCTION Seismology presents several ways While most geologists, including of providing images of the geologic specialists in the field of seismology, structures that exist in the lowermost study rocks at Earth’s surface, more mantle just above the core-mantle attention also is being paid to the boundary (CMB). An understanding planet’s other major boundary, that of the possibly complex geophysical between the core and mantle. With a E F processes occurring at this major density jump of 4.3 kg/m3 between discontinuity requires the combined the silicate lower mantle and the liquid efforts of many fields, but it is the iron outer core, as well as a tempera- role of seismology to geographically ture increase of possibly 1500 °C map out this largely uncharted terri- between the lower mantle adiabat and tory. Seismic phases that reflect, outer core, the core-mantle boundary diffract, and refract across the CMB (CMB) may well be Earth’s most signifi- can all be used to provide different cant and dramatic discontinuity. Our Figure 1. Images from a motion picture showing the propagation of seismic shear energy information in different ways. increasing knowledge of this highly through the mantle (Wysession and Shore, 1994).
    [Show full text]
  • Sharon R. Allen Is a Physical Volcanologist Who Has Worked On
    Sharon R. Allen is a physical volcanologist who Timothy H. Druitt is a volcanologist who works has worked on the processes and products of felsic on the processes and products of explosive volca­ effusive and explosive volcanism in both subaerial nism. His approaches include the field study of and submarine environments from a range of tec­ volcanic products, laboratory analogue experi­ tonic settings. She has been researching the South ments, and the petrology and chemistry of magmas. Aegean volcanic arc since 1993, first as a PhD He has used Santorini Volcano (Greece) as a natural student at Monash University (Australia), later as a laboratory for identifying fundamental questions post­doc at the University of Tasmania (UTAS) (Australia), and currently related to volcanism and for testing hypotheses. He obtained his PhD as a university associate at UTAS. Her scientific interests include subae­ at the University of Cambridge (UK) and is currently Professor of rial caldera forming eruptions, the dynamics of pyroclastic currents Volcanology at Clermont­Auvergne University (France). He was Editor­ on land and when interacting with water, submarine pyroclastic erup­ in­Chief of the Bulletin of Volcanology for four years and received the tions and mechanisms for the formation of pumice in submarine set­ 2018 Norman L. Bowen Award of the American Geophysical Union. tings. Her approach includes field studies of volcanic products and laboratory analogue experimentation. Lorella Francalanci is a geochemist and volcano­ logist who investigates active volcanoes to reveal Olivier Bachmann is a professor of volcanology the pre­eruptive processes that are relevant to the and magmatic petrology at the Eidgenössische dynamics of volcanic eruptions.
    [Show full text]
  • Earthsciencesnews Issue No 05 2014
    Department of earth Sciences Magazine EarthScienceSNEWS iSSue no 05 2014 P4 Fundamental Fieldtrips P8 From Himalayas to Marcellus P10 Mineralogy in Myanmar P12 earthquake Risk in Turkey P16 London Volcano 1 modern process, underpins climate science. In diverse and subtle ways, earth sciences weLcoMe influence the discussion of windmills and carbon taxes at the present Lima climate conference or next year’s major Paris by Professor Gideon Henderson meeting. Head of Department Climate science is also important, along with many other branches of the earth sciences, in the help and guidance it provides to developing nations. Oxford earth scientists work all over the world; climate events help to initiate a burst Does the study of climate literally from Abu Dhabi to Zambia. Many of evolution? Geological understanding nations have significant natural resources, belong in an earth-sciences of climate is also important for more fascinating geology, and are threatened applied questions. Past warm periods of department? by geological hazards and environmental ocean anoxia led to the preservation of change, but lack modern geological tools Sometimes, amongst the swirl of debate hydrocarbons, still critical to global energy and the understanding to benefit from their about wind-farms, carbon taxes, and the production. And it is the winds, sun, tides resources or assess their risks. Universities policy response to warming, it is possible and waves of the earth system that offer such as Oxford have a huge amount to offer to wonder what climate has to do with the alternatives we must rapidly adopt for such nations, as evident in the department’s geology.
    [Show full text]
  • Evolution Stages and Petrology of the Kekuknai Volcanic Massif As Reflecting the Magmatism in Backarc Zone of Kuril–Kamchatka Island Arc System
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Institute of Volcanology and Seismology FEB RAS Repository ISSN 07420463, Journal of Volcanology and Seismology, 2011, Vol. 5, No. 5, pp. 312–334. © Pleiades Publishing, Ltd., 2011. Original Russian Text © A.V. Koloskov, G.B. Flerov, A.B. Perepelov, I.V. Melekestsev, M.Yu. Puzankov, T.M. Filosofova, 2011, published in Vulkanologiya i Seismologiya, 2011, No. 5, pp. 17–41. Evolution Stages and Petrology of the Kekuknai Volcanic Massif as Reflecting the Magmatism in Backarc Zone of Kuril–Kamchatka Island Arc System. Part 1. Geological Position and Geochemistry of Volcanic Rocks A. V. Koloskova, G. B. Flerova, A. B. Perepelovb, I. V. Melekestseva, M. Yu. Puzankova, and T. M. Filosofovaa a Institute of Volcanology and Seismology, Far East Branch, Russian Academy of Sciences, Piipa boulevard, 9, PetropavlovskKamchatskii, 683006 Russia email: [email protected] b A. P. Vinogradov Institute of Geochemistry, Siberian Branch, Russian Academy of Sciences, ul. Favorskogo, 1A, Irkutsk, 664033 Russia email: [email protected] Received October 25, 2010 Abstract—The evolution of the Quaternary Kekuknai volcanic massif (the western flank of the Sredinnyi Range in Kamchatka) has been subdivided into five stages: (1) the precaldera trachybasalt– basaltic andes ite, (2) the extrusive trachyandesite–trachydacite, (3) the early trachybasalt, (4) the middle hawaiite– mugearite (with occasional occurrences of basaltic andesites), and (5) the late trachybasalt–hawaiite– mugearite (with occasional andesites) of areal volcanism. On the basis of petrologic data we identified the island arc and the intraplate geochemical types of rocks in the massif.
    [Show full text]
  • Prospects and Pitfalls in Integrating Volcanology and Archaeology: Areview
    Journal of Volcanology and Geothermal Research 401 (2020) 106977 Contents lists available at ScienceDirect Journal of Volcanology and Geothermal Research journal homepage: www.elsevier.com/locate/jvolgeores Invited review article Prospects and pitfalls in integrating volcanology and archaeology: Areview Felix Riede a,⁎, Gina L. Barnes b, Mark D. Elson c, Gerald A. Oetelaar d, Karen G. Holmberg e, Payson Sheets f a Laboratory for Past Disaster Science, Department of Archaeology and Heritage Studies, Aarhus University, Denmark b Department of Earth Sciences, Durham University, United Kingdom c School of Anthropology, University of Arizona, United States of America d Department of Anthropology and Archaeology, University of Calgary, Canada e Gallatin School of Individualized Study, New York University, United States of America f Department of Anthropology, University of Colorado, Boulder, United States of America article info abstract Article history: Volcanic eruptions and interactions with the landforms and products these yield, are a constant feature of human Received 28 February 2020 life in many parts of the world. Seen over long timespans, human–volcano interactions become stratified in sed- Received in revised form 15 June 2020 imentary archives containing eruptive products and archaeological remains. This review is concerned with Accepted 15 June 2020 charting the overlapping territory of volcanology and archaeology and attempts to plot productive routes for fur- Available online 17 June 2020 ther conjoined research. We define archaeological volcanology as a field of study that brings together incentives, insights, and methods from both volcanology and from archaeology in an effort to better understand both past Keywords: Social volcanology volcanism as well as past cultural change, and to improve risk management practices as well as the contemporary Geoarcheology engagement with volcanism and its products.
    [Show full text]
  • This Dynamic Earth in January of 1992
    View of the planet Earth from the Apollo spacecraft. The Red Sea, which separates Saudi Arabia from the continent of Africa, is clearly visible at the top. (Photograph courtesy of NASA.) Contents Preface Historical perspective Developing the theory Understanding plate motions "Hotspots": Mantle Some unanswered questions Plate tectonics and people Endnotes thermal plumes 1 of 77 2002-01-01 11:52 This pdf-version was edited by Peter Lindeberg in December 2001. Any deviation from the original text is non-intentional. This book was originally published in paper form in February 1996 (design and coordination by Martha Kiger; illustrations and production by Jane Russell). It is for sale for $7 from: U.S. Government Printing Office Superintendent of Documents, Mail Stop SSOP Washington, DC 20402-9328 or it can be ordered directly from the U.S. Geological Survey: Call toll-free 1-888-ASK-USGS Or write to USGS Information Services Box 25286, Building 810 Denver Federal Center Denver, CO 80225 303-202-4700; Fax 303-202-4693 ISBN 0-16-048220-8 Version 1.08 The online edition contains all text from the original book in its entirety. Some figures have been modified to enhance legibility at screen resolutions. Many of the images in this book are available in high resolution from the USGS Media for Science page. USGS Home Page URL: http://pubs.usgs.gov/publications/text/dynamic.html Last updated: 01.29.01 Contact: [email protected] 2 of 77 2002-01-01 11:52 In the early 1960s, the emergence of the theory of plate tectonics started a revolution in the earth sciences.
    [Show full text]
  • Short Curriculum Vitae BRUCE FRANK HOUGHTON (A) Education University of Auckland N.Z
    Short Curriculum Vitae BRUCE FRANK HOUGHTON (a) Education University of Auckland N.Z. Geology BSc (Hons) 1972 University of Otago N.Z. Volcanology PhD 1977 Ruhr Universitat Germany Volcanology Postdoctoral Fellow 1983-1984 (b) Appointments 2009-present Science Director National Disaster Preparedness Training Center. 1999-present Professor University of Hawaii, Manoa 1994-1999 Program Leader Institute of Geological & Nuclear Sciences 1992-1994 Group Manager Institute of Geological & Nuclear Sciences 1991-1992 Program Leader DSIR Geology & Geophysics 1976-1990 Volcanologist N.Z. Geological Survey (c) Awards, Honours 2021 Board of Regents Excellence in Research Award (University of Hawaii) 2021 NSF Research News Highlight 2018 Fellow of the American Geophysical Union 2018- New Zealand National Science Challenges International Advisory Group 2017 Thorarinsson Medallist, International Association of Volcanology and Chemistry of the Earth’s Interior 2014- Editorial Board, Frontiers in Earth Science. 2014-15 Editor “Encyclopaedia of Volcanoes Edition 2” (Elsevier). 2013-15 Distinguished Academic Visitor, Queens’ College, University of Cambridge. 2010-13 Editorial Board, Geology. 2010-16 Editorial Board, Journal of Applied Volcanology. 2009-13 Coordinating Scientist, Hawaiian Volcano Observatory. 2004 Fellow of the Geological Society of America. 2000 Fellow of the Royal Society of New Zealand. 2000- Hawaiian State Volcanologist. 2000- Gordon A. Macdonald Professor of Volcanology. 2000 Editor “Encyclopaedia of Volcanoes” (Academic Press). 1996-98 British Council High Education Links Award. 1996 Marsden Advisory Panel Earth Science-Astronomy. 1992 Hochstetter Lecturer, Geological Society of New Zealand. 1989 Department of Scientific & Industrial Research Prestige Award. 1989-94 Editor, Bulletin of Volcanology. 1987-07 Associate Editor, Journal of Volcanology & Geothermal Research. 1983-84 Alexander von Humboldt Fellowship.
    [Show full text]
  • Using Google Earth to Study the Basic Characteristics of Volcanoes
    USING GOOGLE EARTH TO STUDY THE BASIC CHARACTERISTICS OF VOLCANOES by Stacia Schipper and Stephen Mattox 28 SCIENCE SCOPE USING GOOGLE EARTH TO STUDY THE BASIC CHARACTERISTICS OF VOLCANOES andforms, natural hazards, and the change canocams.html) provides links to numerous live in the Earth over time are common material webcams. in state and national standards. Volcanoes exemplify these standards and readily cap- Getting started with Google Earth Lture the interest and imagination of students. With a Google Earth is a program that allows you to explore minimum of training, students can recognize erupted the Earth in great detail. This virtual globe allows materials and types of volcanoes; in turn, students can you to visit any location on Earth and observe a 3-D relate these characteristics to eruption violence and view of Earth’s surface and gather other data. Google potential risk to both nearby and distant populations. Earth can be downloaded for free from http://earth. With the advent of Google Earth and the database of google.com . volcanoes supplied by the Smithsonian Institutions’ To allow students to be able to view the 3-D relief Global Volcanism of volcanoes, the “terrain” feature should be selected. Program (www.volcano.si.edu), students can de- This can be achieved by going to the “Layers” pull- scribe almost any volcano on Earth. Although about down menu and checking the box labeled “terrain.” 60 volcanoes erupt in an average year, there are 15 to To ensure that metric units of measurement are being 20 that have been continuously active for many years, used, go to the “Tools” tab and select “Options.” Click and will probably continue to erupt for decades.
    [Show full text]
  • 1 TRACY K.P. GREGG Department of Geology 126 Cooke Hall University
    TRACY K.P. GREGG Department of Geology Tel.: (716) 645-4328 126 Cooke Hall Fax: (716) 645-3999 University at Buffalo E-mail: [email protected] The State University of New York Buffalo, NY 14260-3050 EDUCATION Sc.B. (honors), Geological Sciences, Brown University, Providence, RI, 1990. Thesis: Rhyolitic ridges on martian basalts, Peter H. Schultz, advisor. Ph.D., Geology, Arizona State University, Tempe, AZ, 1995. Dissertation: Quantification of lava flow morphologies through analog experiments, Jonathan H. Fink, advisor. RESEARCH INTERESTS Volcanic eruptions in extreme environments (mid-ocean ridges and extraterrestrial surfaces); lava flow eruption and emplacement on Earth and other planets; constraining physics of eruptions from resulting volcanic morphologies. PROFESSIONAL EXPERIENCE 2004 to present: Associate Professor, Department of Geology, University at Buffalo. Supervision of graduate and undergraduate students; instruction of volcanology, planetary geology, magma petrogenesis and ascent, and supervision of introductory laboratories. 1998 to 2004: Assistant Professor, Department of Geology, University at Buffalo. Supervision of graduate and undergraduate students; instruction of volcanology, introductory geology, planetary geology and marine geology. 1998 to present: Adjunct Assistant Scientist, Woods Hole Oceanographic Institution. Constraining volcanic and hydrothermal processes in submarine volcanic zones. 1997 to 2002: Consultant, Proxemy Research, Bowie, Maryland. 1997-1998: Assistant Scientist, Woods Hole Oceanographic Institution. Quantification of submarine and extraterrestrial eruption dynamics through numerical, physical, and analytical modeling. 1997: Adjunct Laboratory Instructor, Dept. of Geology, Bridgewater State College, Bridgewater, MA. Taught 1 section of undergraduate introductory geology laboratory. 1995 – 1997: RIDGE post-doctoral Fellow (funded through NSF Ocean Sciences), Dept. of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA; Dr.
    [Show full text]