Index. Assimilant, 178 hypothetical, 179 Assimilation, 84, 156, 159, 175, 181, 203 bulk, 182 Atlas fracture, 25, 250 Avalanche breccia, 66
|
|
- Tyler Paul
- 6 years ago
- Views:
Transcription
1 Author Biographies Juan Carlos Carracedo: A prestigious research professor of the Spanish Research Council (CSIC) and director of the Estación Volcanológica de Canarias (EVC) until 2011 is now an emeritus research associate at the University of Las Palmas de Gran Canaria (GEOVOL GROUP). Prof. Carracedo has worked in the Canary Islands over 40 years and published over 200 scientific articles on the geology, palaeomagnetism and geomorphology of the Canaries. jcarracedo@proyinves.ulpgc.es. Valentin R. Troll: Lectured in volcanology and petrology at Trinity College Dublin for seven years before taking up the Chair in Petrology and Geochemistry at Uppsala University, Sweden in Prof. Troll has worked on the volcanic phenomena of the Canary Islands since the late 1990s and has published over 25 scientific articles on the geology, petrology and geochemical characteristics of the archipelago. valentin. Troll@geo.uu.se. J. C. Carracedo and V. R. Troll (eds.), Teide Volcano, Active Volcanoes of the World, DOI: / , Ó Springer-Verlag Berlin Heidelberg
2 Index A A a lava, 5, 44, 45, 199, 215 Accretionary lava balls, 217 Aeolian landforms, 48 Aeromagnetic studies, 238 African craton, 26 African plate, 23, 58 Alkali magma series, 83 Alluvial fans, 50 Anaga massif, 78 Anaga, 30, See also Shield volcano Analogue experiments, 63 Ankaramite, 83, Ar/ 39 Ar, 30. See also Radiometric dating Assimilant, 178 hypothetical, 179 Assimilation, 84, 156, 159, 175, 181, 203 bulk, 182 Atlas fracture, 25, 250 Avalanche breccia, 66 B Background noise, 243 Basanite, 83, 160, 195 isotopic composition, 198 Bimodality of lava compositions, 69, 106, 130, 149, 158, 159. See also Bunsen-Daly Gap Boca Cangrejo volcano, 132 Boca de Tauce volcano, 237 Borehole, 236 Bottom breccia, 194 Bouguer anomaly, 237 Bouguer anomaly map, 237 Bunsen-Daly Gap, 158 C Caldera, 5 Calvas del Teide, 222 Canarian archipelago, 234 Canary Islands, 76 age progression, 25, 26 paleocanaries, 24 Central shield, 30. See also Shield volcano Central volcano, 110 Chahorra eruption, 138 Charcoal, 94, 109, 132 Chilled margin, 195, 199, 203 Chinyero, 17, 138 Chinyero volcano, 132 Christopher Columbus, 131 Cinder cones, 217 Climate, 48 Collapse embayment, 96, 107, 109 Collapse unloading, 124 Conjugate graben, 63 Coulées, 115 Craters of elevation, 11 Creeping sector, 62 Crustal contamination, 83 Crustal melting, 183, 186, 187 Crustal recycling, 159, 167, 187 Cryptodomes, 115 Cuevas Negras, 149, 210 D Debris avalanche deposits, 38, 39 Debris flows deposits, 52 Decompression fracturing, 25 Density filter, 111 Density filtering, 187 Diego Hernández Formation, 41. See also Las Cañadas volcano Diffusive gradient, 199 Digital elevation model (DEM), 40 Dyke complex, 58, 63 Dyke intrusion, 252 Dyke petrography, 80 ankaramite group, 80 aphyric group, 80 feldspar-and pyroxene-rich group, 80 feldspar-rich group, 80 J. C. Carracedo and V. R. Troll (eds.), Teide Volcano, Active Volcanoes of the World, DOI: / , Ó Springer-Verlag Berlin Heidelberg
3 276 Index D (cont.) olivine-and pyroxene-rich group, 80 pyroxene-rich group, 80 E EC-AFC model, 183 Echeide, 6 Effusive eruptions, 214, 215 El Hierro, 29 End-member, 175 Erosion rate, 41 Eruption frequency, 167 Eruption rates, 47, 96, 98, 110, 258 Eruption style, 214 Hawaiian, 214 phreatic explosion, 45 phreatoplinian, 214 plinian, 214 strombolian, 214 surtseyan, 214 vulcanian, 214 Eruption volume, 47, 215 Evapotranspiration, 48 Explosion breccia, 225 Explosive volcanism, 156 Eye-witness accounts, 105 F Fault, 70 Felsic lavas, 47, 164 isotopic composition, 176, 181 Felsic volcanism, 33 Fissure eruption, 33, 119 Flank collapse, 38, 57, 81, 124 Güímar, 41, 66, 78 Icod, 70, 97, 106 La Orotava, 78 Micheque, 66, 78 Orotava, 41, 67 Forced intrusion, 206 Fractional crystallisation, 83, 156, 174, 181, 186 Fuel-coolant interaction, 214 Fumarolic activity, 234 G Galería, 39, 58, 63, 78, 96, 107, 161 Garachico eruption, 129, 135 Gas geochemistry, 235 Gelifluction lobes, 50 Geochronology, 93 Geological hazards, 250 Geological map, 263 Geomagnetic excursions, 94, 99 Mono Lake, 100 Geomagnetic field, 101 Geomagnetic reversals, 94, 97 G (cont.) Geothermal gradient, 187 Geothermobarometry, 181 Giant landslide, 65. See also Flank collapse Gravitational sinking, 266 Gravity model, 237 Gregory Rift valley, 158 Ground deformation, 244, 266 Growth rate, 65 Güímar, 78. See also Flank collapse Güímar valley, 16 Guyot, 27 H Half-life, 174 Hazard map, 259 Hazards, 257 Hemipelagic sedimentation, 41 Hiatus stage, 38. See aslo Tenerife evolution Hijo de Tenerife, 254 Historic eruptions, 47, 105, 119, 131 Hornitos, 45, 136, 217 Hotspot model, 26 trail, 25 Hybridisation, 205 Hydraulic fracturing, 252 Hydrothermal alteration, 97, 234 I Icod landslide, 39, 70, 106, 160, 187, 237. See also Flank collapse Inclusions, 195, 203 Inflation, 252 Instituto Geográfico Nacional (IGN), 256 Intraplate earthquakes, 251 Ionic radius, 182 Isopach maps, 147, 220 Isopleth maps, 220 Isotope analysis oxygen, 84, 175 Sr Nd Pb, 78, 175, 195 Isotopic composition of gases, 236 Isotopic fingerprinting, 175, 180, 203 K K/Ar age, 30 K Ar, 109. See also Radiometric dating Katmai, Alaska, 207 L La Gomera, 29 La Palma, 29, 59 Landslide deposits, 39 Lanthanide contraction, 182
4 Index 277 Lars seamount, 25. See also Seamounts Las Cañadas Caldera, 10, 38, 39, 44, 48, 107, 109, 110 origin, 70 Las Cañadas volcano, 17, 39, 63, 64, 78, 106, 158, 159, 215 abrigo ignimbrite, 160 Diego Hernández Formation, 47, 159, 179, 187. See also Las Cañadas volcano granadilla ignimbrite, 160, 179 lower group, 159 poris member, 159 upper group, 179 Las Lenguas, 147 Lava channels, 45 Lava flow paths, 264 Lava inundation, 264 Lavas Negras, 110, 142 Lava tubes, 45, 217 Levées, 45 Lithic blocks, 160 Lithospheric faults, 25 Lithospheric loading, 251 Low temperature alteration, 84 Low velocity zone, 142 M Macaronesia, 5, 26 Madeira Volcanic Province, 25. See also Macaronesia Mafic enclaves, 164, 195. See also Inclusions Mafic foam, 203 Mafic lavas, 46, 160 Magma co-genetic batches, 203 evolved, 30 filaments, 204 isotope ratios, 174 mechanisms of, 192 residence time of, 156, 187 silica content of, 156 Magma bulging, 115 Magma chamber, 142 Magma mingling, 199, 205 Magma mixing, 119, 158, 164, 192, 200 active region, 204 coherent region, 204 timescales of, 192 Magma reservoir, 267 Magmatic differentiation, 156, 175 degree of, 156 silica content of, 156 Magmatic eruptions, 214 Magmatic plumbing system, 177 Magmatic series, 20 Mafic lavas isotopic composition, 176 Magnetic anomaly lineations, 234 Magnetic anomaly map, 239 Magnetotelluric profiles, 234 Major and trace element analysis, 78 Malpaís, 5, 215 Mantle plume, 25 Mantle signal, 177 Mantle source, 85 May 2004, 254 Micheque, 78. See also Flank collapse Microseismic activity, 257 Microseismicity, 242 Mixing hyperbola, 180 Moho, 241 Montaña Abejera, 42 Montaña Amarilla, 227 Montaña Arenas Negras, 122 Montaña Bilma, 139 Montaña Blanca, 6, 18, 42, 108, 145, 168, 220, 242, 265 Montaña Cerrillar, 122 Montaña de Enmedio, 122 Montaña Escachada, 227 Montaña Guamasa, 122 Montaña Los Erales, 227 Montaña Mostaza, 122 Montaña Negra, 135 Montaña Reventada, 119, 147, 192, 194 stratigraphy, 193 Morphological evolution, 38, 40 N Nepheline syenite, 179 oxygen isotope composition, 181 Neptunists, 2 Northeast rift zone (NERZ), 38, 43, 119. See also Rift zone Northwest rift zone (NWRZ), 118., See also Rift zone O Oceanic crust, 28, 157, 177, 234 Ocean island, 76 evolution, 58 Ogives, 145 Open-system processes, 177, 181 Orotava valley, 6, 41 Orotava, 78. See also Flank collapse Oxygen isotope analysis, 78 Oxygen isotope ratios, 181 P Pāhoehoe lava, 5, 46, 161 Paleocliff, 48 Paleomagnetic analysis, 81, 98 Bruhnes chron, 82 Matuyama chron, 82 Partial melting, 182 Batch, 182 Periglacial processes, 49 Phase equilibrium experiments, 142
5 278 Index P (cont.) Phonolite, 160, 162, 195 isotopic composition, 178, 198 Phonotephrite, 162 Phreatic explosion, 45. See also Eruption style Phreatomagmatic eruptions, 110, 214, 221 Phreatomagmatic explosions, 214 Pico Cabras, 42 Pico Viejo. See also Teide-Pico Viejo, 42 Pinatubo, Philipines, 206 Pipkrake, 50 Plagioclase basalt, 161 Plinian eruption, 33 Plutonic complex, 237 Plutonists, 2 Posterosional stage, 34 Pre-Hispanic period, 6 Pre-historic eruptions, 130 Primary magma, 156 Pumice, 220 Pyroclastic fall deposit, 33 Pyroclastic flow deposit, 33 R Radioactive decay, 174 Radiocarbon age, 6, 94, 109, 132 Radiogenic isotope ratios, 174 variability, 177 Radiometric age, 8, 93, 94, 98 Radiometric dating, 18, Ar/ 39 Ar, 30, 93 K Ar, 30, 93 unspiked K/Ar, 96 Rare earth elements (REE), 182 modelling, 182 Rb Sr isotope system, 175 Reawakening, 268 Rejuvenated stage, 33. See also Tenerife evolution Resurfacing map, 257 Retrograde erosion, 42 Rift zone, 43, 57, 58, 76, 106, 160, 187, 257 development, 60 Northeast rift zone (NERZ), 30, 38, 41, 43, 45, 64, 69, 77, 78, 98, 119, 167 Northwest rift zone (NWRZ), 45, 48, 64, 77, 118, 167 organization, 81 triple junction, 61 Roque Del Conde, 30. See also Shield volcano Roque Nublo, 28 Roques Blancos, 42, 118, 144 Roques de Garcia, 39 Rosette structure, 146 Run out length, 218 S Sea water, 227 Seafloor sediment, pre-island, 175, 177 S (cont.) Seamounts, 24 Lars seamount, 25 Sediment contamination, 87 Seismic profiles, 240 Seismic tomography, 242 Seismicity, 254 Shadow zone, 167 Shield-building stage, 30 Shield stage, 30. See also Tenerife evolution Shield volcano, 30, 38, 159 Anaga, 30, 64, 159 central shield, 30 Roque Del Conde, 30, 159 Teno, 30, 119, 159 Siete Fuentes volcano, 133 Sieve texture, 204 Single-line chain, 29 Spatter cone, 45 Sr/Nd ratio, 180 Strombolian. See also Eruption style, 214, 215, 220, 227, 229 Submarine volcanoes, 254 Subsidence, 27 Summit crater, 110, 234 Swath batymetry side-scan sonar, 237 T Taburiente, Caldera de, 16, 59 TAS diagram, 164, 198 Teide Pico Viejo, 2, 106, 109 altitude, 9 central complex, 42 Echeide, 130 future activity, 168 geothermal gradient, 183 morphology, 42 national park, 18, 38 old Teide, 110, 222 parasitic vents, 42 peak, 8, 42 petrogenesis, 187 petrology, 160 Pico Viejo, 42, 111 volcanic complex, 18 Teide s headdress, 7, 130 Tenerife, 29 Tenerife evolution, 38 hiatus stage, 38 rejuvenated stage, 33, 38 shield stage, 30 Tenerife unrest, 256 Teno, 30. See also Shield volcano Tephriphonolite, 162 Tephrite, 160 Timanfaya, 138 Top breccia, 195 Trace element patterns, 164, 182
6 Index 279 Trachybasalt, 162 Transitional lavas, 164, 167 isotopic composition, 176 Tsunami risk, 250 U Underplating, 167, 169, 187 Uphill diffusion, 202 V Vent distribution, 217 Vertical-axis rotation, 82 Vesiculation, 199 Viscosity, 205 Viscosity contrast, 205 Viscous coupling, 206 Volatile contents, 215 Volcán de Arafo, 134 Volcán de Fasnia, 134 Volcán del Portillo, 122 Volcanic cones, 44 Volcaniclastic deposits, 220 Volcanic rift zones, 76
Visualizing Earth Science. Chapter Overview. Volcanoes and Eruption Types. By Z. Merali and B. F. Skinner. Chapter 9 Volcanism and Other
Visualizing Earth Science By Z. Merali and B. F. Skinner Chapter 9 Volcanism and Other Igneous Processes Volcanoes types and effects of eruption Chapter Overview Melting and cooling of rocks Geological
More informationEruptive and structural history of Teide Volcano and rift zones of Tenerife, Canary Islands
Eruptive and structural history of Teide Volcano and rift zones of Tenerife, Canary Islands J.C. Carracedo Estación Volcanológica de Canarias, Consejo Superior de Investigaciones Cientifi cas, La Laguna,
More informationJ. Mangas and F.J. Perez-Torrado. Departamento de Física. Universidad de Las Palmas de Gran Canaria Las Palmas de Gran Canaria.
Magmatic processes in the oceanic lithosphere: characterization of the ultramafic and mafic materials from the Holocene volcanic centers of Bandama and La Caldera de Pinos de Gáldar (Gran Canaria, Canary
More informationJournal of Volcanology and Geothermal Research
Journal of Volcanology and Geothermal Research 178 (2008) 529 542 Contents lists available at ScienceDirect Journal of Volcanology and Geothermal Research journal homepage: www.elsevier.com/locate/jvolgeores
More informationOverview of Ch. 4. I. The nature of volcanic eruptions 9/19/2011. Volcanoes and Other Igneous Activity Chapter 4 or 5
Overview of Ch. 4 Volcanoes and Other Igneous Activity Chapter 4 or 5 I. Nature of Volcanic Eruptions II. Materials Extruded from a Volcano III.Types of Volcanoes IV.Volcanic Landforms V. Plutonic (intrusive)
More informationCalc-alkaline Volcanic Rocks. Calc-alkali Volcanics. Fabric. Petrography. Compositional Classification. Petrography. Processes.
Calc-alkaline Volcanic Rocks Calc-alkali Volcanics Winter Chapters 16 & 17 Petrography Processes Field relations Volcanic arcs Petrogenesis Petrography Fabric Classification Alteration Fabric Aphanitic
More informationGEOLOGY MEDIA SUITE Chapter 12
UNDERSTANDING EARTH, SIXTH EDITION GROTZINGER JORDAN GEOLOGY MEDIA SUITE Chapter 12 Volcanoes 2010 W.H. Freeman and Company Plate tectonics explains the global pattern of volcanism. Key Figure 12.20 (page
More informationA REGIONAL SCALE RADON MONITORING NETWORK IN THE VOLCANIC ISLAND OF TENERIFE, CANARY ISLANDS (SPAIN)
A REGIONAL SCALE RADON MONITORING NETWORK IN THE VOLCANIC ISLAND OF TENERIFE, CANARY ISLANDS (SPAIN) Ronaldo Viñas Departamento de Edafología y Geología, Universidad de La Laguna, Spain ronaldovinas@gmail.com
More information1/31/2013 BASALTIC BASALTIC ANDESITIC RHYOLITIC
Can you predict the location of volcanoes? What is causing this eruption? What factors influence its character? A volcano is any landform from which lava, gas, or ashes, escape from underground or have
More informationDynamic Planet PUT ALL YOUR ANSWERS ON THE ANSWER SHEET. c) low temperature d) high volatile content
School Name: Team #: Students Names: Dynamic Planet 2016 Science Olympiad Invitational University of Texas at Austin PUT ALL YOUR ANSWERS ON THE ANSWER SHEET 1) Low viscosity magmas have: a) high silica
More informationCOMPOSITION and PHYSICAL PROPERTIES GENERAL SUBJECTS. GEODESY and GRAVITY
COMPOSITION and PHYSICAL PROPERTIES Composition and structure of the continental crust Composition and structure of the core Composition and structure of the mantle Composition and structure of the oceanic
More informationIgneous Rocks. Magma molten rock material consisting of liquid rock and crystals. A variety exists, but here are the end members:
Igneous Rocks Magma molten rock material consisting of liquid rock and crystals. A variety exists, but here are the end members: Types of Magma Basaltic, Basic or Mafic very hot (900-1200 C) very fluid
More informationIntroduction to Earth s s Spheres The Benchmark
Introduction to Earth s s Spheres The Benchmark Volcanism Volcanic eruptions Effusive: lavas (e.g., Kilauea) Volcanism Volcanic eruptions Explosive: pyroclastic rocks (e.g., Krakatau) Factors Governing
More informationThe Nature of Igneous Rocks
The Nature of Igneous Rocks Form from Magma Hot, partially molten mixture of solid liquid and gas Mineral crystals form in the magma making a crystal slush Gases - H 2 O, CO 2, etc. - are dissolved in
More informationChapter 18 - Volcanic Activity. Aka Volcano Under the City
Chapter 18 - Volcanic Activity Aka Volcano Under the City 18.1 Magma Describe factors that affect the formation of magma. Compare and contrast the different types of magma. Temperature and pressure increase
More informationEngineering Geology ECIV 2204
Engineering Geology ECIV 2204 2017-2016 Chapter (4) Volcanoes Chapter 4: Volcanoes and Other Igneous Activity cataclysmic relating to or denoting a violent natural even Eventually the entire
More informationIgneous and Metamorphic Rock Forming Minerals. Department of Geology Mr. Victor Tibane SGM 210_2013
Igneous and Metamorphic Rock Forming Minerals Department of Geology Mr. Victor Tibane 1 SGM 210_2013 Intrusive and Effusive Rocks Effusive rocks: rapid cooling small crystalls or glas Lava & ash Magmatic
More informationVulcanicity. Objectives to identify the basic structure of volcanoes and understand how they form.
Vulcanicity Objectives to identify the basic structure of volcanoes and understand how they form. Some key terms to start.. Viscosity how well a substance (lava) flows. Acid lavas have a high viscosity,
More informationPart A GEOLOGY 12 CHAPTER 4 WORKSHEET VOLCANOES. Name
GEOLOGY 12 CHAPTER 4 WORKSHEET VOLCANOES Name Part A 1. The rough, jumbled blocky or jagged surface of a lava flow is called a. pahoehoe b. lahar c. aa d. phreatic 2. The Cascade volcanoes like Mt. St.
More informationFoundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa
Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa Fires Within: Igneous Activity Foundations, 6e - Chapter 7 Stan Hatfield Southwestern Illinois College The nature of volcanic eruptions Characteristics
More informationGEOL1 Physical Geology Laboratory Manual College of the Redwoods Lesson Five: Volcanoes Background Reading: Volcanoes Volcanic Terms: Silca:
Name: Date: GEOL1 Physical Geology Laboratory Manual College of the Redwoods Lesson Five: Volcanoes Background Reading: Volcanoes Volcanic Terms: Silca: SiO 2 silicon dioxide. This is quartz when it crystallizes.
More informationStudy guide chapter 9
Study guide chapter 9 1. What are the three ways solid mantle material can change phase to a liquid? Associate a boundary/hot spot to each way mantle material changes phase. 1. A decrease in pressure which
More informationNew evidence about the structure and growth of ocean island volcanoes from aeromagnetic data: The case of Tenerife, Canary Islands
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 116,, doi:10.1029/2010jb007646, 2011 New evidence about the structure and growth of ocean island volcanoes from aeromagnetic data: The case of Tenerife, Canary Islands
More informationDirected Reading. Section: Volcanic Eruptions. light in color is called a. felsic. b. oceanic. c. mantle. d. mafic. dark in color is called
Skills Worksheet Directed Reading Section: Volcanic Eruptions 1. Lava provides an opportunity for scientists to study a. the nature of Earth s inner core. b. the nature of Earth s tectonic plates. c. temperatures
More informationPrentice Hall EARTH SCIENCE
Prentice Hall EARTH SCIENCE Tarbuck Lutgens Chapter 10 Volcanoes and Other Igneous Activity 10.1 The Nature of Volcanic Eruptions Factors Affecting Eruptions Factors that determine the violence of an eruption
More informationImagine the first rock and the cycles that it has been through.
A rock is a naturally formed, consolidated material usually composed of grains of one or more minerals The rock cycle shows how one type of rocky material gets transformed into another The Rock Cycle Representation
More informationLecture 6 - Igneous Rocks and Volcanoes
Lecture 6 - Igneous Rocks and Volcanoes Learning objectives Understand and be able to predict where and why magma will be forming at different tectonic settings Understand the factors controlling magma
More informationErupted and killed approximately 15,000 people 200 years ago
1 2 3 4 5 6 7 8 Introduction to Environmental Geology, 5e Chapter 8 Volcanic Activity Volcanoes: summary in haiku form A volcano forms. Magma comes to the surface - explodes, if felsic. Case History: Mt.
More informationVolcano - A Volcano is an opening in the Earth s surface through which molten material or volcanic gases are erupted.
What is a Volcano? Volcano - A Volcano is an opening in the Earth s surface through which molten material or volcanic gases are erupted. A volcano can either be a classic volcanic cone.. Mt. St. Helens,
More informationDirected Reading. Section: Volcanic Eruptions
Skills Worksheet Directed Reading Section: Volcanic Eruptions 1. Lava provides an opportunity for scientists to study a. the nature of Earth s inner core. b. the nature of Earth s tectonic plates. c. temperatures
More informationHawaiian Volcanism Evolution of Hawaiian Volcanoes. Link to Video of Dive to Lo ihi
Hawaiian Volcanism Evolution of Hawaiian Volcanoes Link to Video of Dive to Lo ihi Review of Regional Patterns Isostasy: equilibrium of lithosphere and asthenosphere, whereby tectonic plates float at an
More informationEAS 116 Earthquakes and Volcanoes
EAS 116 Earthquakes and Volcanoes J. Haase Forecasting Volcanic Eruptions Assessment of Volcanic Hazard Is that volcano active? Mount Lassen: 12000 BP and 1915 Santorini, IT: 180,000 BP, 70,000 BP, 21000
More informationBimodality of Lavas in the Teide^Pico Viejo Succession intenerifeçthe Role of Crustal Melting in the Origin of Recent Phonolites
JOURNAL OF PETROLOGY VOLUME 53 NUMBER12 PAGES 2465^2495 2012 doi:10.1093/petrology/egs056 Bimodality of Lavas in the Teide^Pico Viejo Succession intenerifeçthe Role of Crustal Melting in the Origin of
More informationEarthquakes. Earthquakes are caused by a sudden release of energy
Earthquakes Earthquakes are caused by a sudden release of energy The amount of energy released determines the magnitude of the earthquake Seismic waves carry the energy away from its origin Fig. 18.1 Origin
More informationVolcanic Landforms, Volcanoes and Plate Tectonics
Page 1 of 12 EENS 3050 Tulane University Natural Disasters Prof. Stephen A. Nelson Volcanic Landforms, Volcanoes and Plate Tectonics This page last updated on 26-Aug-2017 Volcanic Landforms Volcanic landforms
More informationChapter 7 Lecture Outline. Volcanoes and Other Igneous Activity
Chapter 7 Lecture Outline Volcanoes and Other Igneous Activity Focus Question 7.1 How were the eruptions of Mount St. Helens and Hawaii s Kilauea volcano different? Mount St. Helens eruption (May 18,1980)
More informationMagma. Objectives. Describe factors that affect the formation of magma. Compare and contrast the different types of magma. Vocabulary.
Magma Objectives Describe factors that affect the formation of magma. Compare and contrast the different types of magma. Vocabulary viscosity Magma Magma The ash that spews from some volcanoes can form
More informationUnit 4 Lesson 4 Volcanoes. Copyright Houghton Mifflin Harcourt Publishing Company
Magma Magic What is a volcano? A volcano is any place where gas, ash, or melted rock come out of the ground. Many volcanoes are dormant, meaning an eruption has not occurred in a long period of time. What
More informationGlobal Tectonics. Kearey, Philip. Table of Contents ISBN-13: Historical perspective. 2. The interior of the Earth.
Global Tectonics Kearey, Philip ISBN-13: 9781405107778 Table of Contents Preface. Acknowledgments. 1. Historical perspective. 1.1 Continental drift. 1.2 Sea floor spreading and the birth of plate tectonics.
More informationGeology Brad Paisley 5/10/2014
Geology Brad Paisley 5/10/2014 Midterm #2 Info Midterm info: Midterm exam on Thursday, October 29th 50 multiple choice/true-false questions Covers material from Lectures 9-17 1 hand-written page cheat
More informationSection 10.1 The Nature of Volcanic Eruptions This section discusses volcanic eruptions, types of volcanoes, and other volcanic landforms.
Chapter 10 Section 10.1 The Nature of Volcanic Eruptions This section discusses volcanic eruptions, types of volcanoes, and other volcanic landforms. Reading Strategy Previewing Before you read the section,
More informationChapter 7 Lecture Outline. Volcanoes and Other Igneous Activity
Chapter 7 Lecture Outline Volcanoes and Other Igneous Activity Mount St. Helens eruption (May 18,1980) Largest historic eruption in North America Lowered peak by more than 400 m Destroyed all trees in
More informationPlease be sure to look over the study guides for the midterms, and your review questions and the keys for those (from the course webpages).
Earth Science 104 Study Guide Final Exam Please be sure to look over the study guides for the midterms, and your review questions and the keys for those (from the course webpages). Vocabulary A a Accretionary
More information2/25/2013. Volcanoes: summary in haiku form A volcano forms. Magma comes to the surface - explodes, if felsic.
Introduction to Environmental Geology, 5e Edward A. Keller Chapter 8 Volcanic Activity Volcanoes: summary in haiku form A volcano forms. Magma comes to the surface - explodes, if felsic. Lecture Presentation
More informationREVIEW: The Setting - Climatology of the Hawaiian Archipelago
REVIEW: The Setting - Climatology of the Hawaiian Archipelago Atmosphere and Ocean 5 facts: NE trade-winds tropical water subtropical gyre Seasonality N S gradients Four dominant swell regimes: north Pacific
More informationInteractive comment on Long-term volcanic hazard assessment on El Hierro (Canary Islands) by L. Becerril et al.
Interactive comment on Long-term volcanic hazard assessment on El Hierro (Canary Islands) by L. Becerril et al. J. Lindsay (Referee) General comments 1. The use of susceptibility map requires further explanation
More informationVolcanoes. Volcanic eruptions can be more powerful than the explosion of an atomic bomb.
Ch. 13 Volcanoes Volcanoes Volcanic eruptions can be more powerful than the explosion of an atomic bomb. Many of these eruptions are caused by the movement of tectonic plates. Volcanism Volcanism-any activity
More informationGLY July Ms. Nelda Breedt. Plates move slowly and eventually.
GLY 162 Tectonic Processes: Volcanism Ms. Nelda Breedt GLY 162 Environmental Geology Plate Tectonics Plates move slowly and eventually. 2 Spread apart (divergent plates) Dive beneath one another (converging
More informationWhen Mount St. Helens erupted, trapped gases caused the north side of the mountain to explode. Volcanic ash was ejected high into the atmosphere.
When Mount St. Helens erupted, trapped gases caused the north side of the mountain to explode. Volcanic ash was ejected high into the atmosphere. A volcano is a mountain that forms when magma reaches the
More informationApr 20 2:26 PM. the opening in Earth's crust through which molten rock, gases, and ash erupt. the landform that develops around this opening
Volcanoes Cleveland Volcano, Alaska, May 2006 Taken from the ISS Apr 20 2:26 PM The term volcano can refer to two things: 1. the opening in Earth's crust through which molten rock, gases, and ash erupt
More informationChapter 10: Volcanoes and Other Igneous Activity Section 1: The Nature of Volcanic Eruptions I. Factors Affecting Eruptions Group # Main Idea:
Chapter 10: Volcanoes and Other Igneous Activity Section 1: The Nature of Volcanic Eruptions I. Factors Affecting Eruptions Group # A. Viscosity Group # B. Dissolved Gases Group # II. Volcanic Material
More informationChapter 5 9/10/2011. Introduction. Volcanoes and Volcanism. Volcanism. Introduction. Introduction. Introduction
Introduction Chapter 5 Volcanism is the eruption of magma, and associated gases at the surface. Some magma erupts explosively as pyroclastic (fire-broken) rock and other erupts as lava flows. Volcanoes
More informationPhysical Geology, 15/e
Lecture Outlines Physical Geology, 15/e Plummer, Carlson & Hammersley Copyright McGraw-Hill Education, Inc. Permission required for reproduction or display. Volcanism and Extrusive Rocks Physical Geology
More informationA Volcano is An opening in Earth s crust through
Volcanoes A Volcano is An opening in Earth s crust through which molten rock, gases, and ash erupt. Also, the landform that develops around this opening. Kinds of Eruptions Geologists classify volcanic
More informationThe Chilwa Alkaline Province, Malawi Geochemistry, Isotope Geology, and Petrogenesis
The Chilwa Alkaline Province, Malawi Geochemistry, Isotope Geology, and Petrogenesis G. N. Eby, University Massachusetts Lowell, USA A. R. Woolley, Natural History Museum, UK K. Collerson, University of
More informationMultiple Choice Identify the letter of the choice that best completes the statement or answers the question.
volcano sample test Multiple Choice Identify the letter of the choice that best completes the statement or answers the question. 1. Volcanic belts form along a. islands in the Pacific Ocean. b. North American
More informationGeology 1 st Semester Exam YSBAT
1. What is the role of a geologist? Geology 1 st Semester Exam YSBAT 2016-2017 2. Earth is subdivided into three main layers based on what? 3. What features do you find at divergent boundaries? 4. Rock
More informationMt St Helens was know to have entered into active periods that lasted from years once every years over the last 500 years, (Figure 5).
Lecture #8 notes; Geology 3950, Spring 2006; CR Stern May 1980 eruption of Mt St Helens volcano (text pages 183-192 in the 4 th edition and 206-222 in the 5 th edition) Mt St Helens in southwest Washington
More informationCh12&13 Test. 3. Where does the first motion of an earthquake occur? a. fault c. epicenter b. focus d. locus
Ch12&13 Test Multiple Choice Identify the choice that best completes the statement or answers the question. 1. What is the epicenter of an earthquake? a. the location along a fault where the first motion
More informationRegional and local variations in geochemistry and tectonics along and across Central America
Regional and local variations in geochemistry and tectonics along and across Central America Michael J. Carr, Department of Geological Sciences, Wright Lab Rutgers University, 610 Taylor Rd., Piscataway
More informationHawaiian Submarine Volcanism. Stages of Hawaiian Volcanoes:
Hawaiian Submarine Volcanism November 1, 2011 Mary Tardona GG 711 Stages of Hawaiian Volcanoes: Typically, three main stages: Pre shield Shield Post shield Sometimes followed by: Rejuvenation Stage GG
More informationChapter Introduction Lesson 1 Earthquakes Lesson 2 Volcanoes Chapter Wrap-Up
Chapter Introduction Lesson 1 Earthquakes Lesson 2 Volcanoes Chapter Wrap-Up What causes earthquakes and volcanic eruptions? What do you think? Before you begin, decide if you agree or disagree with each
More informationMagma. Objectives. Describe factors that affect the formation of magma. Compare and contrast the different types of magma. Vocabulary.
Magma Objectives Describe factors that affect the formation of magma. Compare and contrast the different types of magma. Vocabulary viscosity Magma Magma The ash that spews from some volcanoes can form
More informationDirected Reading. Section: Volcanoes and Plate Tectonics
Skills Worksheet Directed Reading Section: Volcanoes and Plate Tectonics 1. Some volcanic eruptions can be more powerful than a(n) a. hand grenade. b. earthquake. c. geyser. d. atomic bomb. 2. The cause
More informationVolcanoes. 11/25/2013. Geology 15 Lecture 27 VOLCANO!
Hazard Update Surprise POP Review Tsunami Activity 10 B Today s Material Volcanoes Volcanic Hazards Geology 15 Lecture 27 VOLCANO! http://motherboard.vice.com/blog/watch an erupting volcano create a newisland
More informationIntroduction. Volcano a vent where molten rock comes out of Earth
Introduction Volcano a vent where molten rock comes out of Earth Example: Kilauea Volcano, Hawaii Hot (~1,200 o C) lava pools around the volcanic vent. Hot, syrupy lava runs downhill as a lava flow. The
More informationWET EXPLOSIVE ERUPTIONS. Hawaii Photograph: Dorian Weisel
WET EXPLOSIVE ERUPTIONS Hawaii Photograph: Dorian Weisel WET EXPLOSIVE ERUPTIONS mechanisms hot magma/ hot rock + water pyroclasts + steam rapid expansion of gas fragmentation of magma + wall rock external
More informationVolcanic Plumes. JOHN WILEY & SONS Chichester New York Weinheim Brisbane Singapore Toronto
Volcanic Plumes R. S. J. SPARKS University of Bristol, UK M. I. BURSIK State University of New York, USA S. N. CAREY University of Rhode Island, USA J. S. GILBERT Lancaster University, UK L. S. GLAZE NASA/Goddard
More informationA bowl shaped depression formed by the collapse of a volcano is called a. Magma that has left the vent of a volcano is known as. Lava.
Magma that has left the vent of a volcano is known as Lava A bowl shaped depression formed by the collapse of a volcano is called a Caldera This can form in a caldera when magma starts to come back up
More informationVolcanoes. I Types of Volcanoes II Plutonic Activity III Plate Tectonics and Igneous Activity IV Magma and Lava V Types of Lava Flows
Volcanoes I Types of Volcanoes II Plutonic Activity III Plate Tectonics and Igneous Activity IV Magma and Lava V Types of Lava Flows 1 Some Definitions Igneous refers to processes and rocks involving or
More informationOpen-system processes in the differentiation of mafic magma in the Teide Pico Viejo succession, Tenerife
213 research-articlethematic Set ArticleXXX1.1144/jgs212-16S. Wiesmaier et al.differentiation of Teide Mafic Lavas Journal of the Geological Society, London, Vol. 17, 213, pp. 557 57.
More informationVolcano: a weak spot in the crust where molten material or magma comes to the surface
Chapter 7 Volcano: a weak spot in the crust where molten material or magma comes to the surface Magma: a molten mixture of rock forming substances, gases and H 2 O from the mantle Volcanic Belts: Form
More informationPage One. GEOL 1030 Pre test S15. Please enter your rst and last name.
GEOL 1030 Pre test S15 Page One Please enter your rst and last name. First Name: Last Name: 1. The most common elements in the Earth's crust, in order of decreasing abundance, are: a. feldspar, quartz,
More informationV o l c a n o es. Part I Composition. Types of deposits. Types of volcanoes Distribution
V o l c a n o es Part I Composition Types of deposits Types of volcanoes Distribution Volcano: A mound of material that is extruded to the Earth s surface from a vent that is connected to a magma chamber
More informationNC Earth Science Essential Standards
NC Earth Science Essential Standards EEn. 2.1 Explain how processes and forces affect the Lithosphere. EEn. 2.1.1 Explain how the rock cycle, plate tectonics, volcanoes, and earthquakes impact the Lithosphere.
More informationChapter 18. Volcanism
Chapter 18 Volcanism Ring of fire contains 66% of world s active volcanoes Convergent : Divergent: Icelandic Eruption Mount Etna Different Kinds of eruptions: Volcanic activity is controlled by plate tectonics,
More informationSubject Classification
Istituto Nazionale di Geofisica e Vulcanologia earth-prints home page roma library bologna library catania library milano library napoli library palerm Subject Classification Earth-prints organize its
More informationCritical Thinking 1. Contrast How could you tell the difference between a mafic rock and a felsic rock by looking at them?
CHAPTER 13 2 SECTION Volcanoes Volcanic Eruptions KEY IDEAS As you read this section, keep these questions in mind: How does the composition of magma affect volcanic eruptions and lava flow? What are the
More informationPyroclastic Deposits I: Pyroclastic Fall Deposits
Pyroclastic Deposits I: Pyroclastic Fall Deposits EAS 458 Volcanology Introduction We have seen that physics is useful in understanding volcanic processes, but physical models must be constrained by and
More informationBryson Extra Credit Reading
VOLCANOES New homework due next Tuesday, Nov 23 Extra Credit Chapter 14 The Fire Below due next Tuesday, Nov 23 Bryson Extra Credit Reading A Short History of Nearly Everything Chapter 14: The Fire Below
More informationMagma Migration, Storage and Evolution in the Galápagos Region John Sinton University of Hawai i
Magma Migration, Storage and Evolution in the Galápagos Region John Sinton University of Hawai i The Importance of Magma Supply and its relationship to mantle melting Magma Chamber Processes as deduced
More informationUGRC 144 Science and Technology in Our Lives/Geohazards
UGRC 144 Science and Technology in Our Lives/Geohazards Session 5 Magma and Volcanism Lecturer: Dr. Patrick Asamoah Sakyi Department of Earth Science, UG Contact Information: pasakyi@ug.edu.gh College
More informationAbstract...ii. Acknowledgements.iii. List of Figures and Tables...iv. Introduction 1. Geologic Setting and Background...2. Methods..
T ABLE OF C ONTENTS Abstract...ii Acknowledgements.iii List of Figures and Tables...iv Introduction 1 Geologic Setting and Background...2 Methods..7 Results and Discussion...8 Conclusions and Recommendations
More informationFrom Punchbowl to Panum: Long Valley Volcanism and the Mono-Inyo Crater Chain
From Punchbowl to Panum: Leslie Schaffer E105 2002 Final Paper Long Valley Volcanism and the Mono-Inyo Crater Chain Figure 1. After a sequence of earthquakes during the late 1970 s to the early 1980 s
More informationPlate Tectonics. entirely rock both and rock
Plate Tectonics I. Tectonics A. Tectonic Forces are forces generated from within Earth causing rock to become. B. 1. The study of the origin and arrangement of Earth surface including mountain belts, continents,
More informationSubaerial Felsic Lava Flows and Domes
Subaerial Felsic Lava Flows and Domes Occurrence Alone or in linear and arcuate chains up to 20 km long Margins of calderas or volcanic depressions. Feeder occupies synvolcanic fault (ring fracture). Extrusion
More informationLECTURE #11: Volcanic Disasters: Lava Properties & Eruption Types
GEOL 0820 Ramsey Natural Disasters Spring, 2018 LECTURE #11: Volcanic Disasters: Lava Properties & Eruption Types Date: 13 February 2018 I. Exam I grades are posted on the class website (link at the bottom
More informationGeology Example Midterm Exam #1
Geology 100 - Example Midterm Exam #1 1. A naturally occurring, inorganic, crystalline substance having a definite chemical composition is. a) an igneous rock b) a mineral c) an atom d) an electron 2.
More informationVolcanic Eruptions and Hydrovolcanism
Find the Face Volcanic Eruptions and Hydrovolcanism Ocean Ridges Continental Rifts Subduction Zones: Continental Oceanic Back Arc Basins Hot Spots Plumes Cinder Cones Composite Volcanoes Shield VolcanoesCinder
More informationGLY 155 Introduction to Physical Geology, W. Altermann. Grotzinger Jordan. Understanding Earth. Sixth Edition
Grotzinger Jordan Understanding Earth Sixth Edition Chapter 4: IGNEOUS ROCKS Solids from Melts 2011 by W. H. Freeman and Company Chapter 4: Igneous Rocks: Solids from Melts 1 About Igneous Rocks Igneous
More informationTypes of Volcanoes. Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries.
Types of Volcanoes Key Concept: Tectonic plate motions can result in volcanic activity at plate boundaries. Volcanoes How do volcanoes work? How do volcanoes work? Magma is forced onto Earth s surface.
More informationEssentials of Geology, 11e
Essentials of Geology, 11e Igneous Rocks and Intrusive Activity Chapter 3 Instructor Jennifer Barson Spokane Falls Community College Geology 101 Stanley Hatfield Southwestern Illinois College Characteristics
More informationTypes of Volcanoes KEY CONCEPT: TECTONIC PLATE MOTIONS CAN RESULT IN VOLCANIC ACTIVITY AT PLATE BOUNDARIES.
Types of Volcanoes KEY CONCEPT: TECTONIC PLATE MOTIONS CAN RESULT IN VOLCANIC ACTIVITY AT PLATE BOUNDARIES. Volcanoes How do volcanoes work? How do volcanoes work? Magma is forced onto Earth s surface.
More informationQuestions and Topics
Plate Tectonics and Continental Drift Questions and Topics 1. What are the theories of Plate Tectonics and Continental Drift? 2. What is the evidence that Continents move? 3. What are the forces that
More informationEARTH SCIENCE KESSEL
EARTH SCIENCE KESSEL Bell Ringer List everything you KNOW about a volcano (at least 3 things). Then list everything you WANT to know about volcanoes (at least 2 things). Bell Ringer What evidence might
More informationMagma vs. Lava. Molten rock below Earth s surface is called magma. The magma that reaches the surface and erupts out of a volcano is called lava.
CH. 10.1 Be able to Explain the factors that determine the type of volcanic eruption. List the 3 types of volcanoes Describe the features of a volcano. What is a Volcano? Volcanoes are sites where molten
More informationTAKE HOME EXAM 8R - Geology
Name Period Date TAKE HOME EXAM 8R - Geology PART 1 - Multiple Choice 1. A volcanic cone made up of alternating layers of lava and rock particles is a cone. a. cinder b. lava c. shield d. composite 2.
More informationBefore Plate Tectonics: Theory of Continental Drift
Before Plate Tectonics: Theory of Continental Drift Predecessor to modern plate tectonics Shape and fit of the continents was the initial evidence Snider-Pelligrini (1858) Taylor (1908) Wegner (1915) Fig.
More informationWHAT IS A MAGMA. Magma is a mixture of molten rock, volatiles and solids that is found beneath the surface of the Earth.
UNIT - 8 VOLCANOES WHAT IS A MAGMA Magma is a mixture of molten rock, volatiles and solids that is found beneath the surface of the Earth. In some instances, it solidifies within the crust to form plutonic
More informationDYNAMIC PLANET. Name: School:
DYNAMIC PLANET November 4 th Scrimmage Name: School: Directions: DO NOT open the packet until prompted to. The test will be a 50 minute test and answer each question to the best of your abilities. Total:
More information