GY 111: Physical Geology

Total Page:16

File Type:pdf, Size:1020Kb

GY 111: Physical Geology UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 9: Extrusive Igneous Rocks Instructor: Dr. Douglas W. Haywick Last Time 1) The chemical composition of the crust 2) Crystallization of molten rock 3) Bowen's Reaction Series Web notes 8 Chemical Composition of the Crust Element Wt% % of atoms Oxygen 46.6 60.5 Silicon 27.7 20.5 Aluminum 8.1 6.2 Iron 5.0 1.9 Calcium 3.6 1.9 Sodium 2.8 2.5 Potassium 2.6 1.8 Magnesium 2.1 1.4 All other elements 1.5 3.3 Crystallization of Magma http://myweb.cwpost.liu.edu/vdivener/notes/igneous.htm Bowen’s Reaction Series Source http://www.ltcconline.net/julian Igneous Rock Composition Source: http://hyperphysics.phy-astr.gsu.edu Composition Formation Dominant Silica content Temperature Minerals Ultramafic Very high Olivine, pyroxene Very low (<45%) Mafic High Olivine, pyroxene, low Ca-plagioclase Intermediate Medium Na-Plagioclase, moderate amphibole, biotite Felsic Medium-low Orthoclase, quartz, high (>65%) muscovite, biotite Igneous Rock Texture Extrusive Rocks (Rapid Cooling; non visible* crystals) Intrusive Rocks (slow cooling; 100 % visible crystals) *with a hand lens Igneous Rock Texture Igneous Rock Texture Today’s Agenda 1) Pyro-what? (air fall volcanic rocks) 2) Felsic and Intermediate Extrusive Rocks 3) Mafic Extrusive Rocks Web notes 9 Pyroclastic Igneous Rocks Pyroclastic Igneous Rocks Pyroclastic: Pyro means “fire”. Clastic means particles; both are of Greek origin. Pyroclastic Igneous Rocks Pyroclastic: Pyro means “fire”. Clastic means particles; both are of Greek origin. Pyroclastic rocks are usually erupted from composite volcanoes (e.g., they are produced via explosive eruptions from viscous, “cool” lavas) Pyroclastic Igneous Rocks Pyroclastic: Pyro means “fire”. Clastic means particles; both are of Greek origin. Pyroclastic rocks are usually erupted from composite volcanoes (e.g., they are produced via explosive eruptions from viscous, “cool” lavas) The eruptions that produce pyroclastic rocks include phreatic, plinian and ultraplinian. Pyroclastic Igneous Rocks Pyroclastic: Pyro means “fire”. Clastic means particles; both are of Greek origin. Pyroclastic rocks are usually erupted from composite volcanoes (e.g., they are produced via explosive eruptions from viscous, “cool” lavas) The eruptions that produce pyroclastic rocks include phreatic, plinian and ultraplinian. These rocks cool extremely rapidly. Textures are glassy to aphanitic. Pyroclastic Igneous Rocks Pyroclastic Igneous Rocks Volcanic ash Pyroclastic Igneous Rocks Volcanic ash Pumice Pyroclastic Igneous Rocks Volcanic ash Obsidian Pyroclastic Igneous Rocks Nuee ardents and pyroclastic flows may deposit volcanic breccias or ignimbrites http://ougseurope.org/trips/santorini/santorini/Picture04.jpg Ignimbrite Pyroclastic Igneous Rocks During pyroclastic eruptions, “volcanic gas” is produced in copious quantities (more so than ash and rock). •water vapor (H20) •carbon dioxide (CO2) •hydrogen chloride (HCl) •sulfur dioxide (SO2) •nitrogen oxide (N2O) •Hydrogen cyanide (HCN) •argon (Ar) •helium (He) Other “pyroclastic” rocks Volcanic Bombs Tuff Rhyolite Chalk board Felsic/Intermediate Extrusive Igneous Rocks Felsic/Intermediate Extrusive Igneous Rocks Rhyolite Mt. St. Helens Lava dome Felsic and intermediate rocks are classified by the amount of SiO2 in their bulk chemistry (they have relatively high SiO2 content). We can distinguish them on the basis of mineral composition and color. Andesite Mafic Extrusive Igneous Rocks Mafic Extrusive Igneous Rocks Basalt http://z.about.com/d/geology/1/0/F/W/scoria.jpg Mafic extrusive igneous rocks have relatively low SiO2 contents in their bulk chemistry. Ultramafic extrusive igneous rocks are relatively rare today. Scoria Mafic Extrusive Igneous Rocks Mafic extrusive igneous rocks erupted under water produce a unique structure called “pillows”. Pillow Basalt Pillow basalt forms at divergent plate boundaries like the Mid- Atlantic Ridge Today’s Homework 1. Study; Lecture test 1 next Tuesday Next Time 1. Quiz 5; fill in the blanks 2. Intrusive igneous rocks GY 111: Physical Geology Lecture 9: Extrusive Igneous Rocks Instructor: Dr. Doug Haywick [email protected] This is a free open access lecture, but not for commercial purposes. For personal use only. .
Recommended publications
  • Volcanic Gases and Aerosols Guidelines Introduction
    IVHHN Gas Guidelines www.ivhhn.org/gas/guidelines.html Volcanic Gases and Aerosols Guidelines The following pages contain information relating to the health hazards of gases and aerosols typically emitted during volcanic activity. Each section outlines the properties of the emission; its impacts on health; international guidelines for concentrations; and examples of concentrations and effects in volcanic contexts, including casualties. Before looking at the emissions data, we recommend that you read the general introduction to volcanic gases and aerosols first. A glossary to some of the terms used in the explanations and guidelines is also provided at the end of this document. Introduction An introduction to the aims and purpose of the Gas and Aerosol Guidelines is given here, as well as further information on international guideline levels and the units used in the website. A brief review of safety procedures currently implemented by volcanologists and volcano observatories is also provided. General Introduction Gas and aerosol hazards are associated with all volcanic activity, from diffuse soil gas emissions to 2- plinian eruptions. The volcanic emissions of most concern are SO2, HF, sulphate (SO4 ), CO2, HCl and H2S, although, there are other volcanic volatile species that may have human health implications, including mercury and other metals. Since 1900, there have been at least 62 serious volcanic-gas related incidents. Of these, the gas-outburst at Lake Nyos in 1986 was the most disastrous, causing 1746 deaths, >845 injuries and the evacuation of 4430 people. Other volcanic-gas related incidents have been responsible for more than 280 deaths and 1120 injuries, and contributed to the evacuation or ill health of >53,700 people (Witham, in review).
    [Show full text]
  • Full-Text PDF (Final Published Version)
    Pritchard, M. E., de Silva, S. L., Michelfelder, G., Zandt, G., McNutt, S. R., Gottsmann, J., West, M. E., Blundy, J., Christensen, D. H., Finnegan, N. J., Minaya, E., Sparks, R. S. J., Sunagua, M., Unsworth, M. J., Alvizuri, C., Comeau, M. J., del Potro, R., Díaz, D., Diez, M., ... Ward, K. M. (2018). Synthesis: PLUTONS: Investigating the relationship between pluton growth and volcanism in the Central Andes. Geosphere, 14(3), 954-982. https://doi.org/10.1130/GES01578.1 Publisher's PDF, also known as Version of record License (if available): CC BY-NC Link to published version (if available): 10.1130/GES01578.1 Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via Geo Science World at https://doi.org/10.1130/GES01578.1 . Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Research Paper THEMED ISSUE: PLUTONS: Investigating the Relationship between Pluton Growth and Volcanism in the Central Andes GEOSPHERE Synthesis: PLUTONS: Investigating the relationship between pluton growth and volcanism in the Central Andes GEOSPHERE; v. 14, no. 3 M.E. Pritchard1,2, S.L. de Silva3, G. Michelfelder4, G. Zandt5, S.R. McNutt6, J. Gottsmann2, M.E. West7, J. Blundy2, D.H.
    [Show full text]
  • Compositional Zoning of the Bishop Tuff
    JOURNAL OF PETROLOGY VOLUME 48 NUMBER 5 PAGES 951^999 2007 doi:10.1093/petrology/egm007 Compositional Zoning of the Bishop Tuff WES HILDRETH1* AND COLIN J. N. WILSON2 1US GEOLOGICAL SURVEY, MS-910, MENLO PARK, CA 94025, USA 2SCHOOL OF GEOGRAPHY, GEOLOGY AND ENVIRONMENTAL SCIENCE, UNIVERSITY OF AUCKLAND, PB 92019 AUCKLAND MAIL CENTRE, AUCKLAND 1142, NEW ZEALAND Downloaded from https://academic.oup.com/petrology/article/48/5/951/1472295 by guest on 29 September 2021 RECEIVED JANUARY 7, 2006; ACCEPTED FEBRUARY 13, 2007 ADVANCE ACCESS PUBLICATION MARCH 29, 2007 Compositional data for 4400 pumice clasts, organized according to and the roofward decline in liquidus temperature of the zoned melt, eruptive sequence, crystal content, and texture, provide new perspec- prevented significant crystallization against the roof, consistent with tives on eruption and pre-eruptive evolution of the4600 km3 of zoned dominance of crystal-poor magma early in the eruption and lack of rhyolitic magma ejected as the BishopTuff during formation of Long any roof-rind fragments among the Bishop ejecta, before or after onset Valley caldera. Proportions and compositions of different pumice of caldera collapse. A model of secular incremental zoning is types are given for each ignimbrite package and for the intercalated advanced wherein numerous batches of crystal-poor melt were plinian pumice-fall layers that erupted synchronously. Although released from a mush zone (many kilometers thick) that floored the withdrawal of the zoned magma was less systematic than previously accumulating rhyolitic melt-rich body. Each batch rose to its own realized, the overall sequence displays trends toward greater propor- appropriate level in the melt-buoyancy gradient, which was self- tions of less evolved pumice, more crystals (0Á5^24 wt %), and sustaining against wholesale convective re-homogenization, while higher FeTi-oxide temperatures (714^8188C).
    [Show full text]
  • Deep Carbon Emissions from Volcanoes Michael R
    Reviews in Mineralogy & Geochemistry Vol. 75 pp. 323-354, 2013 11 Copyright © Mineralogical Society of America Deep Carbon Emissions from Volcanoes Michael R. Burton Istituto Nazionale di Geofisica e Vulcanologia Via della Faggiola, 32 56123 Pisa, Italy [email protected] Georgina M. Sawyer Laboratoire Magmas et Volcans, Université Blaise Pascal 5 rue Kessler, 63038 Clermont Ferrand, France and Istituto Nazionale di Geofisica e Vulcanologia Via della Faggiola, 32 56123 Pisa, Italy Domenico Granieri Istituto Nazionale di Geofisica e Vulcanologia Via della Faggiola, 32 56123 Pisa, Italy INTRODUCTION: VOLCANIC CO2 EMISSIONS IN THE GEOLOGICAL CARBON CYCLE Over long periods of time (~Ma), we may consider the oceans, atmosphere and biosphere as a single exospheric reservoir for CO2. The geological carbon cycle describes the inputs to this exosphere from mantle degassing, metamorphism of subducted carbonates and outputs from weathering of aluminosilicate rocks (Walker et al. 1981). A feedback mechanism relates the weathering rate with the amount of CO2 in the atmosphere via the greenhouse effect (e.g., Wang et al. 1976). An increase in atmospheric CO2 concentrations induces higher temperatures, leading to higher rates of weathering, which draw down atmospheric CO2 concentrations (Ber- ner 1991). Atmospheric CO2 concentrations are therefore stabilized over long timescales by this feedback mechanism (Zeebe and Caldeira 2008). This process may have played a role (Feulner et al. 2012) in stabilizing temperatures on Earth while solar radiation steadily increased due to stellar evolution (Bahcall et al. 2001). In this context the role of CO2 degassing from the Earth is clearly fundamental to the stability of the climate, and therefore to life on Earth.
    [Show full text]
  • Receiver Function Analyses of Uturuncu Volcano, Bolivia and Vicinity
    University of South Florida Scholar Commons School of Geosciences Faculty and Staff Publications School of Geosciences 11-2017 Receiver Function Analyses of Uturuncu Volcano, Bolivia and Vicinity Heather McFarlin University of South Florida Douglas Christensen University of Alaska, Fairbanks Stephen R. McNutt University of South Florida, [email protected] Kevin M. Ward University of Utah Jamie Ryan University of Arizona See next page for additional authors Follow this and additional works at: https://scholarcommons.usf.edu/geo_facpub Part of the Earth Sciences Commons Scholar Commons Citation McFarlin, Heather; Christensen, Douglas; McNutt, Stephen R.; Ward, Kevin M.; Ryan, Jamie; Zandt, George; and Thompson, Glenn, "Receiver Function Analyses of Uturuncu Volcano, Bolivia and Vicinity" (2017). School of Geosciences Faculty and Staff Publications. 1430. https://scholarcommons.usf.edu/geo_facpub/1430 This Article is brought to you for free and open access by the School of Geosciences at Scholar Commons. It has been accepted for inclusion in School of Geosciences Faculty and Staff Publications by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. Authors Heather McFarlin, Douglas Christensen, Stephen R. McNutt, Kevin M. Ward, Jamie Ryan, George Zandt, and Glenn Thompson This article is available at Scholar Commons: https://scholarcommons.usf.edu/geo_facpub/1430 Research Paper THEMED ISSUE: PLUTONS: Investigating the Relationship between Pluton Growth and Volcanism in the Central Andes GEOSPHERE Receiver function analyses of Uturuncu volcano, Bolivia and vicinity Heather McFarlin1, Douglas Christensen2, Stephen R. McNutt1, Kevin M. Ward3, Jamie Ryan4, George Zandt4, and Glenn Thompson1 1University of South Florida School of Geosciences, 4202 E. Fowler Avenue, NES 107, Tampa, Florida 33620, USA GEOSPHERE; v.
    [Show full text]
  • Insights Into the Recurrent Energetic Eruptions That Drive Awu Among the Deadliest Volcanoes on Earth
    Insights into the recurrent energetic eruptions that drive Awu among the deadliest volcanoes on earth Philipson Bani1, Kristianto2, Syegi Kunrat2, Devy Kamil Syahbana2 5 1- Laboratoire Magmas et Volcans, Université Blaise Pascal - CNRS -IRD, OPGC, Aubière, France. 2- Center for Volcanology and Geological Hazard Mitigation (CVGHM), Jl. Diponegoro No. 57, Bandung, Indonesia Correspondence to: Philipson Bani ([email protected]) 10 Abstract The little known Awu volcano (Sangihe island, Indonesia) is among the deadliest with a cumulative death toll of 11048. In less than 4 centuries, 18 eruptions were recorded, including two VEI-4 and three VEI-3 eruptions with worldwide impacts. The regional geodynamic setting is controlled by a divergent-double-subduction and an arc-arc collision. In that context, the slab stalls in the mantle, undergoes an increase of temperature and becomes prone to 15 melting, a process that sustained the magmatic supply. Awu also has the particularity to host alternatively and simultaneously a lava dome and a crater lake throughout its activity. The lava dome passively erupted through the crater lake and induced strong water evaporation from the crater. A conduit plug associated with this dome emplacement subsequently channeled the gas emission to the crater wall. However, with the lava dome cooling, the high annual rainfall eventually reconstituted the crater lake and created a hazardous situation on Awu. Indeed with a new magma 20 injection, rapid pressure buildup may pulverize the conduit plug and the lava dome, allowing lake water injection and subsequent explosive water-magma interaction. The past vigorous eruptions are likely induced by these phenomena, a possible scenario for the future events.
    [Show full text]
  • Volcano Hazards at Newberry Volcano, Oregon
    Volcano Hazards at Newberry Volcano, Oregon By David R. Sherrod1, Larry G. Mastin2, William E. Scott2, and Steven P. Schilling2 1 U.S. Geological Survey, Hawaii National Park, HI 96718 2 U.S. Geological Survey, Vancouver, WA 98661 OPEN-FILE REPORT 97-513 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, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1997 U.S. Department of the Interior U.S. Geological Survey CONTENTS Introduction 1 Hazardous volcanic phenomena 2 Newberry's volcanic history is a guide to future eruptions 2 Flank eruptions would most likely be basaltic 3 The caldera would be the site of most rhyolitic eruptions—and other types of dangerously explosive eruptions 3 The presence of lakes may add to the danger of eruptions in the caldera 5 The most damaging lahars and floods at Newberry volcano would be limited to the Paulina Creek area 5 Small to moderate-size earthquakes are commonly associated with volcanic activity 6 Volcano hazard zonation 7 Hazard zone for pyroclastic eruptions 7 Regional tephra hazards 8 Hazard zone for lahars or floods on Paulina Creek 8 Hazard zone for volcanic gases 10 Hazard zones for lava flows 10 Large-magnitude explosive eruptions of low probability 11 Monitoring and warnings 12 Suggestions for further reading 12 Endnotes 13 ILLUSTRATIONS Plate 1. Volcano hazards at Newberry volcano, Oregon in pocket Figure 1. Index map showing Newberry volcano and vicinity 1 Figure 2.
    [Show full text]
  • Origins of High-Temperature Fluids in the Goshogake Mud Volcano Field, Tohoku, Northern Japan: Chemical and Isotopic Studies of Gas and Water
    49th Lunar and Planetary Science Conference 2018 (LPI Contrib. No. 2083) 1210.pdf ORIGINS OF HIGH-TEMPERATURE FLUIDS IN THE GOSHOGAKE MUD VOLCANO FIELD, TOHOKU, NORTHERN JAPAN: CHEMICAL AND ISOTOPIC STUDIES OF GAS AND WATER. R. Ishimaru1, N. Miyake1, G. Komatsu2, K. Kawai3, M. Kobayashi4, H. Sakuma5, T. Matsui1 1Planetary Exploration Research Center (PERC), Chiba Institute of Technology (Chitech) (2-17-1 Tsudanuma, Narashino, Chiba 275-0016, Japan; [email protected]), 2International Research School of Planetary Sciences, Università d'Annunzio (Viale Pindaro 42, 65127 Pescara, Italy), 3Department of Earth and Planetary Science, School of Science, University of Tokyo (Hongo 7-3-1, Bunkyo, Tokyo 113-0033, Japan), 4Department of Earth and Planetary Environmental Sci- ence, School of Science, University of Tokyo (Hongo 7-3-1, Bunkyo, Tokyo 113-0033, Japan), 5Reseach Center for Functional Materials, National Institute for Materials Science (1-1 Namiki, Tsukuba, 305-0044 Japan). Introduction: Mud volcanoes occur everywhere Gas sampling and laboratory analysis. Gases were in various geological settings on the Earth [e.g., 1] and, collected with a custom-made sampling device for possibly, on other planetary bodies, such as Mars [e.g., laboratory measurement of the gas species. The com- 2] and Enceladus ocean floor. Their surface terrains position analysis of the gas samples in the chamber are formed by mud ascending and erupting, together was conducted using Gas Chromatography (GS) in the with water and gas, from depths. Therefore, mud vol- laboratory. The GC analyses are made in two ways: cano is one of the most suitable landforms for explor- qualitative and quantitative analyses.
    [Show full text]
  • 1998 Volcanic Activity in Alaska and Kamchatka: Summary of Events and Response of the Alaska Volcano Observatory by Robert G
    1998 Volcanic Activity in Alaska and Kamchatka: Summary of Events and Response of the Alaska Volcano Observatory by Robert G. McGimsey, Christina A. Neal, and Olga Girina Open-File Report 03-423 U.S. Department of the Interior U.S. Geological Survey 1998 Volcanic Activity in Alaska and Kamchatka: Summary of Events and Response of the Alaska Volcano Observatory By Robert G. McGimsey1, Christina A. Neal1, and Olga Girina2 1Alaska Volcano Observatory, 4200 University Dr., Anchorage, AK 99508-4664 2Kamchatka Volcanic eruptions Response Team, Institute of Volcanic Geology and Geochemistry, Piip Blvd., 9 Petropavlovsk-Kam- chatsky, 683006, Russia AVO is a cooperative program of the U.S. Geological Survey, University of Alaska Fairbanks Geophysical Institute, and the Alaska Division of Geological and Geophysical Surveys. AVO is funded by the U.S. Geological Survey Volcano Hazards Program and the State of Alaska Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government Open-File Report 03-423 U.S. Department of the Interior U.S. Geological Survey TABLE OF CONTENTS Introduction. 1 Reports of volcanic activity, northeast to southwest along Aleutian arc . 4 Shrub Mud Volcano . 4 Augustine Volcano . 6 Becharof Lake Area . 8 Chiginagak Volcano . 10 Shishaldin Volcano. 12 Akutan Volcano . 12 Korovin Volcano . 13 Reports of Volcanic activity, Kamchatka, Russia, North to South . 15 Sheveluch Volcano . 17 Klyuchevskoy Volcano. 19 Bezymianny Volcano . 21 Karymsky Volcano . 23 References. 24 Acknowledgments . 26 Figures 1 A. Map location of historically active volcanoes in Alaska and place names used in this summary .
    [Show full text]
  • Mineralogical and Geochemical Indicators of Subaerial Weathering in the Pozzolane Rosse Ignimbrite (Alban Hills Volcanic District, Italy)
    Georgia State University ScholarWorks @ Georgia State University Geosciences Theses Department of Geosciences 4-27-2010 Mineralogical and Geochemical Indicators of Subaerial Weathering in the Pozzolane Rosse Ignimbrite (Alban Hills Volcanic District, Italy) Jennifer M. Dickie Georgia State University Follow this and additional works at: https://scholarworks.gsu.edu/geosciences_theses Part of the Geography Commons, and the Geology Commons Recommended Citation Dickie, Jennifer M., "Mineralogical and Geochemical Indicators of Subaerial Weathering in the Pozzolane Rosse Ignimbrite (Alban Hills Volcanic District, Italy)." Thesis, Georgia State University, 2010. https://scholarworks.gsu.edu/geosciences_theses/23 This Thesis is brought to you for free and open access by the Department of Geosciences at ScholarWorks @ Georgia State University. It has been accepted for inclusion in Geosciences Theses by an authorized administrator of ScholarWorks @ Georgia State University. For more information, please contact [email protected]. MINERALOGICAL AND GEOCHEMICAL INDICATORS OF SUBAERIAL WEATHERING IN THE POZZOLANE ROSSE IGNIMBRITE (ALBAN HILLS VOLCANIC DISTRICT, ITALY) by JENNIFER M. DICKIE Under the direction of Dr. Daniel Deocampo ABSTRACT The Pozzolane Rosse ignimbrite [PR] (457±4 ka) in the Alban Hills Volcanic District, Rome, Italy was exposed ~ 40 ka prior to a subsequent volcanic event which coverd it entirely. XRF, XRD, and clay separation results from PR samples from INGV and CA1 boreholes and Castel di Leva quarry show evidence of paleopedogenesis. All locations display loss of base cations, loss of K is consistent with XRD datat showing dissolution or alteration of leucite to analcime. Accumulation of Al and high L.O.I. support XRD evidence of 1:1 clay species at upper depth.
    [Show full text]
  • Erosion, Transport and Segregation of Pumice and Lithic Clasts in Pyroclastic ¯Ows Inferred from Ignimbrite at Lascar Volcano, Chile
    Journal of Volcanology and Geothermal Research 104 (2000) 201±235 www.elsevier.nl/locate/jvolgeores Erosion, transport and segregation of pumice and lithic clasts in pyroclastic ¯ows inferred from ignimbrite at Lascar Volcano, Chile E.S. Caldera,*, R.S.J. Sparksa, M.C. Gardewegb aDepartment of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK bServicio Nacional de Geologia y Mineria, Avenida Santa Maria 0104, Casilla 10465, Santiago, Chile Received 4 November 1998; revised and accepted 4 May 2000 Abstract Investigations have been made on the distribution of pumice and lithic clasts in the lithic rich Soncor ignimbrite (26.5 ka) and the 1993 pumice ¯ow deposits of Lascar Volcano, Chile. The Soncor ignimbrite shows three main lithofacies which grade into one another. Coarse lithic breccias range from matrix poor strati®ed varieties, irregular shaped sheets and elongate hummocks in proximal environments, to breccia lenses with pumiceous ignimbrite matrix. Massive, lithic rich facies comprise the bulk of the ignimbrite. Pumice rich facies are bimodal with abundant large pumice clasts (often with reverse grading), rare lithic clasts and occur distally and on high ground adjacent to deep proximal valleys. In the 1993 pyroclastic ¯ow deposits lithic rich facies are deposited on slopes up to 148 whereas pumice rich facies are deposited only on slopes ,48. Lithic rich parts show a thin pumice rich corrugated surface which can be traced into the pumice rich facies. The high lithic content in the Soncor ignimbrite is attributed to the destruction of a pre-existing dome complex, deep explosive cratering into the interior of the volcano and erosion during pyroclastic ¯ow emplacement.
    [Show full text]
  • One Hundred Volatile Years of Volcanic Gas Studies at the Hawaiian Volcano Observatory
    Characteristics of Hawaiian Volcanoes Editors: Michael P. Poland, Taeko Jane Takahashi, and Claire M. Landowski U.S. Geological Survey Professional Paper 1801, 2014 Chapter 7 One Hundred Volatile Years of Volcanic Gas Studies at the Hawaiian Volcano Observatory By A. Jeff Sutton1 and Tamar Elias1 The smell of sulphur is strong, but not unpleasant to Kīlauea’s summit, together with surface-deformation and a sinner. other data, detected an increase in deep magma supply more than a year before a corresponding surge in effusive activity. —Mark Twain, Letters from Hawaii, 1866 Correspondingly, HVO routinely uses SO2 emissions to study shallow eruptive processes and effusion rates. HVO gas studies and Kīlauea’s long-running East Rift Zone eruption also demonstrate that volatile emissions can be a substantial Abstract volcanic hazard in Hawai‘i. From its humble beginning, trying to determine the chemical composition of volcanic The first volcanic gas studies in Hawai‘i, beginning gases over a century ago, HVO has evolved to routinely use in 1912, established that volatile emissions from Kīlauea real-time gas chemistry to track eruptive processes, as well Volcano contained mostly water vapor, in addition to as hazards. carbon dioxide and sulfur dioxide. This straightforward discovery overturned a popular volatile theory of the day and, in the same action, helped affirm Thomas A. Jaggar, Introduction Jr.’s, vision of the Hawaiian Volcano Observatory (HVO) as a preeminent place to study volcanic processes. Decades later, the environmental movement produced a watershed Volcanic gases are a dominating force in eruptive of quantitative analytical tools that, after being tested activity.
    [Show full text]