The status of the Mt. Meager Volcanic Complex. Glyn Williams-Jones Department of Earth Sciences Simon Fraser University
|
|
- Beatrice Goodman
- 5 years ago
- Views:
Transcription
1 The status of the Mt. Meager Volcanic Complex Glyn Williams-Jones Department of Earth Sciences Simon Fraser University
2 Location 60 km NW of Pemberton, BC Canadian segment of Cascades
3 Location 60 km NW of Pemberton, BC Canadian segment of Cascades Andrews et al.
4 Mt. Meager Perkin s Pillar Capricorn Mtn. Mt. Job Plinth Peak
5 Long-lived volcanic history & complex geology 2.2 Ma to present Multiple eroded summit lava domes and volcanic necks Extensive hydrothermal system cgenarchive.or g
6 Initial explosive phase of eruption Pyroclasitc flows down into Lillooet valley Widespread pumice deposits Eruption plume height: > km Kirstie Simpson Total erupted volume: 0.8 km 3 Mt. St. Helens: ~ 1 km 3
7 Bridge River fall out pumice tephra < 80 m think deposits on Mt Meager Fine grained ash deposited ~ 530 km E in Alberta Iceland (2010)
8 Eruption transitioned to lava flow & pyroclastic flows Formation of ~110 m high dam of welded block and ash flows capped by unwelded block and ash flows, avalanche deposits blocked the Lillooet River and formed temporary lake (> 0.55 km 3 ) Kirstie Simpson
9 >40-65 days to overtop dam Catastrophic failure of dam generated outburst flood & lahar Peak deluge for ~ 8 h eroded 2.5-km long canyon traceable >65 km downstream Andrews et al. (2014) Kirstie Simpson
10 At least 10 significant historic rock avalanche, landslide events Very weak rock mass of altered volcanics sitting on granitic basement Lillooet River altered volcanic rock Tim Gage (2010)
11 Vol.: ~49 million m 3 Largest historic slide in Canada Frank slide: 30 Mm 3 Hope slide: 47 Mm 3 Velocity: m/s Temporarily dammed Lillooet River, Meager Creek Seismicity (M2.6) detected 2800 km away m run-up on opposite valley wall backsplash temporary lake Melanie Kelman (2010)
12 First reported sulphur smells in February 2016
13 Mt. Meager Perkin s Pillar Capricorn Mtn. Mt. Job Plinth Peak
14 Jan Feb. 2016: 92 M1-2 EQs recorded in vicinity Small swarm S of Mt. Meager in Mt Meager No close seismic station difficult to constrain EQ depths many focal depths of km But seismologists thought much shallower
15 Hannibal Preto (July 20, 2016)
16 1 st Reconnaissance survey FLIR survey Max 23 C Megan Dewit, SFU (Aug 20, 2016) Digital photogrammetry Opening diameters 30 x 30 m ~25-30 m deep
17 SPOT images - June 2015 Cracks but not fumarole openings Artifact of snowfall? N N July 2016 June 2015 ~1 km
18 2 nd Survey Gio Roberti, SFU (Sept 11, 2016)
19 2 nd Survey MultiGAS sensor (H 2 O/CO 2 /SO 2 /CO/H 2 S) Max: 280 ppm H 2 S, 2700 ppm CO 2 FM2 FM1 Low T fumarole field Subsequent reports suggest presences since at least 1930s Gio Roberti, SFU (Sept 11, 2016)
20 Stratovolcanoes are unstable composites of varying material that is spatially heterogeneous USGS
21 Mt. St. Helens (1980) Introduction History Status Hazards Monitoring Proximal hazards (< ~5 km) Ballistics Gas hazards Pyroclastic flows Lava flows Mt. St. Helens (1980) Medial to Distal hazards (> ~5 km) Lahars (mudflow) Landslides Ash
22 Yakima WA (1980) Introduction History Status Hazards Monitoring Why worry? Direct human impact Urban Centres Distance Population Pemberton 60 km ~ 2400 Whistler 67 km > 10,000 Metro Vancouver 160 km > 2.5 million Clague & Turner (2003)
23 Why worry? Direct economic impact airport closure, re-routing / cancellation, grounding of airplanes & repairs Eyjafjallajökull, Iceland (Mar. - Oct. 2010) 7 million passengers US$200 million/day Total loss ~US$ 1.7 billion Mt Kelud, Indonesia (2014) Eyjafjallajökull, Iceland (2010)
24 Recall - At least 10 significant historic rock avalanche / landslide events N N Plinth Peak km Gio Roberti,
25 NW flank of Plinth Peak (~ 2 km E of fumaroles) 5 to 30 mm/yr of deformation from 1992 to 2001 Potentially 5 times greater than the 2010 Capricorn Creek slide N Plinth Peak Gio Roberti, 2.5 Mm 2 unstable area 1 km vertical drop 250 Mm 3 unstable volume Gio Roberti,
26 INNERGEX Run of river projects Upper Lillooet (54 MW), Boulder Creek (17 MW); Miller Creek (33 MW) Costs of 2010 landslide estimated at > $10 million Miller Creek Powerhouse Pemberton Meadows (2010) The Canadian Press m
27 Deformation monitoring InSAR (Radarsat 2, Sentinel) for 15 volcanoes in Canada Infill of Meager InSAR history Radarsat 2 targets InSAR image revealing the 10 cm uplift near South Sister volcano, Oregon ( ); USGS
28 NRCan installed a temporary seismic station (MGMB) Second higher altitude site located To be installed Spring 2017 Mt Meager 3-component Broadband system earthquakescanada.nrcan.gc.ca/
29 Visual surveys Helicopter pilot conducting regular avalanche control for Innergex will make visual observations of fumarole field throughout winter Geochemical surveys Repeat geochemical survey of fumaroles in Summer 2017 to look for changes in gas ratios Important sign of reactivation is an increase in SO 2 emissions and decrease in C/S ratio
30 Debris flows a major hazard at Mt. Meager At least 3 large debris flows in drill core All reached inhabited areas Lahar inundation zone modeling LAHARZ (GIS tool) use lahar volume and DEM to model down valley impacts Melanie Kelman after Simpson et al. (2006)
31 Integrated & comprehensive Volcanic hazard map needed Possible M.Sc. project Collection of baseline time series data (e.g., seismic, deformation, etc.) Comprehensive Volcanic & Landslide database under development
32 Long lived volcanic complex Fumarolic activity since at least 1930s Significant past volcanic & landslide events Seismic data do not suggest magmatic unrest Deformation at Plinth Peak likely not magmatic Possible landslide hazard Increasing population & economic resources at risk Monitoring & mapping needed for effective management & mitigation of any future crisis
33 Hannibal Preto & Dante Canil (UVic) Canadian Hazards Information Service David McCormack, Reid Van Brabant Geological Survey of Canada Melanie Kelman, Rick Hall Canada Centre for Mapping & Earth Observation Sergey Samsanov, Ian Olthof, Geneviève Marquis Department of Earth Sciences Gioachino Roberti, Megan Dewit, Carie-Ann Lau, Swetha Venugopal, Brent Ward Department of Earth, Ocean & Atmospheric Sciences Alex Wilson, Kelly Russell
LECTURE #11: Volcanoes: Monitoring & Mitigation
GEOL 0820 Ramsey Natural Disasters Spring, 2018 LECTURE #11: Volcanoes: Monitoring & Mitigation Date: 15 February 2018 I. What is volcanic monitoring? the continuous collection of one or more data sources
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 informationDebris Avalanches. Debris avalanche deposits on a volcano in Chile. All of the area in the foreground is buried by a thick debris avalanche.
Debris Avalanches Volcanoes are not very stable structures. From time to time, they collapse producing large rock and ash avalanches that travel at high speeds down valleys. Collapse maybe caused by an
More informationThe Orting Community College of Vulcanology
The Orting Community College of Vulcanology A Recommendation For His Honourable Mayor A. Young By DAG (Doom-and-Gloom), LLP (Michael, Chris, Bryan, Lauren, Dave) Agenda 1. 2. 3. 4. 5. 6. Description of
More informationEarthquakes, volcanic eruptions, tsunamis (why do we live here?) Tectonic plates. Tectonic plates: Juan de Fuca. Volcanism the past 37 million years
Earthquakes, volcanic eruptions, tsunamis (why do we live here?) Tectonic plates Tectonic plates: Juan de Fuca Volcanism the past 37 million years Tectonic plates: Juan de Fuca Volcanism the past 37 million
More informationMount St. Helens changed the way we look at things!
Mount St. Helens, a turning point in studies of, and perceptions about explosive volcanoes Mount St. Helens changed the way we look at things! Plinian column during the cataclysmic eruption of May 18,
More informationGEOLOGY 285: INTRO. PETROLOGY
Dr. Helen Lang Dept. of Geology & Geography West Virginia University FALL 2005 GEOLOGY 285: INTRO. PETROLOGY Mount St. Helens 1980 Eruption Small earthquakes Small steam and ash eruptions in March and
More informationUGRC 144 Science and Technology in Our Lives/Geohazards
UGRC 144 Science and Technology in Our Lives/Geohazards Session 6 Volcanic Hazards Lecturer: Dr. Patrick Asamoah Sakyi Department of Earth Science, UG Contact Information: pasakyi@ug.edu.gh College of
More informationOrting Community College Proposal
Orting Community College Proposal Cedric, Celina, Francine, Sarah, Samuel GEO CORP Located in Washington, 42 miles south of Seattle. Situated between two rivers on fertile plains. Built on lahar deposits.
More informationCase History: Mt. St. Helens
Case History: Mt. St. Helens EAS 458 Volcanology Introduction 1980 eruption of Mt. St. Helens was particularly interesting and violent eruption with an unusual lateral blast. In the 1970 s, the USGS (Crandell(
More informationWhy was this eruption important?
Mount St. Helens Mount St. Helens has a long geological history (>3,000 yrs) of explosive eruptions. The 1980 Events: Initial relatively mild steam and ash (Vulcanian) eruptions. Sustained plinian eruption
More informationA New College in Orting?
A New College in Orting? Risk Report and Recommendation by: Safe Schools Kause Everyone Deserves (SSKED) 2017 Geographic location and physical site of Orting The city of Orting is located in Pierce county,
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 informationGEOLOGY 285: INTRO. PETROLOGY
Dr. Helen Lang Dept. of Geology & Geography West Virginia University SPRING 2015 GEOLOGY 285: INTRO. PETROLOGY The Cascade Volcanoes are a good example of the Circum- Pacific ring of fire of subductionrelated
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 informationMount St. Helens. Copyright 2010 LessonSnips
Mount St. Helens Washington State is home to the Cascade Mountains, a range of mountains that extends from the Canadian province of British Columbia to northern California. Many of these mountains are
More informationVisualizing 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 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 informationSylvain Charbonnier. PASI Workshop About 60% of Indonesians live around 16 active volcanoes on the island of Java
Numerical modelling of pyroclastic flows: a case study from the recent activity of Merapi Volcano, Central Java, Indonesia Sylvain Charbonnier PASI Workshop 2011 Case study: Merapi Volcano! About 60% of
More informationReleased Science Inquiry Task Encounter with an Active Volcano Grade 11
Date: Your Name: Released Science Inquiry Task Encounter with an Active Volcano 2016 Grade 11 Directions: Science You will be reading a story and analyzing the data provided to answer a set of questions.
More informationImages from: Boston.com
Images from: Boston.com Ireland in the shadow of a volcano: Understanding the 2010 eruption at Eyjafjallajökull, Iceland. Chris Bean, School of Geological Sciences, UCD. World Quakes and Volcanoes 1960-2010
More informationHAZARD IDENTIFICATION AND VULNERABILITY ANALYSIS (HIVA) Walla Walla County, Washington VOLCANO ASH FALL
HAZARD IDENTIFICATION AND VULNERABILITY ANALYSIS (HIVA) Walla Walla County, Washington VOLCANO ASH FALL Hazard Overview A volcano is a vent in the earth's crust through which magma (molten rock), rock
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 MONITORING PRACTICAL. Hazard alert levels established for communication at Mt. Pinatubo
VOLCANO MONITORING PRACTICAL Predicting volcanic eruptions is a hazardous and stressful business. If an eruption has occurred and was not predicted then the volcanologists get the blame for not giving
More informationLiving on the Edge: Unit 5: Convergent Plate Boundaries
Living on the Edge: Unit 5: Convergent Plate Boundaries Because of its eleva.on (4,392 m), relief, hydrothermal altera.on, ice cap, glacier- fed radial valleys, and proximity to suburbs of the SeaBle-
More information3/7/17. #16 - Case Studies of Volcanoes II. Announcements Monday 2/27
Announcements Monday 2/27 Exam #1: Monday Feb. 27 th, 7:15-8:15 (see web site) Last Names A - N Loomis 141 Last Names O - Z Loomis 151 Bring your student ID An old exam is posted in Compass If you are
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 informationAlso, when Cascade volcanoes do erupt, high-speed avalanches of pyroclastic flows
INTRODUCTION A volcano is a vent through which molten rock escapes to the Earth s surface. Unlike other mountains, which are pushed up from below, volcanoes are built by surface accumulation of their eruptive
More informationNSF-MARGINS Expedition to Anatahan Volcano March 2005
1 NSF-MARGINS Expedition to Anatahan Volcano March 2005 According to the Emergency Management Office (EMO) report distributed in February 2005, the third historical eruption of Anatahan began on January
More informationJulie Fero NRS 509. Mapping Volcanic Risk with GIS
Julie Fero NRS 509 Mapping Volcanic Risk with GIS Introduction Volcanoes are present throughout the world, generally occurring along plate margins, making the entire world prone to volcanic influence,
More informationVolcanoes and Urban Planning
Background Reading & Lesson Plan Document ID: 10_04_04_1 Date Received: 2004-10-04 Date Revised: 2004-11-16 Date Accepted: 2004-11-23 Curriculum Topic Benchmarks: M1.3.5, M3.3.17, M5.3.3, M9.3.2, S12.3.7,
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 informationWhat mainly controls eruptive style?
Introduction to volcanoes, volcanic eruptions, and volcanic landforms Previous: Magmatic differentiation, Bowens Reaction series (mineral melting points), mafic vs. felsic (fluid vs. sticky) Video: Lava
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 informationVolcanoes. Introduction
Volcanoes Introduction Display Slide V-0 Explain that a volcano is a vent through which molten rock escapes to the Earth s surface. Unlike other mountains, which are pushed up from below, volcanoes are
More informationInterpretive Map Series 24
Oregon Department of Geology and Mineral Industries Interpretive Map Series 24 Geologic Hazards, and Hazard Maps, and Future Damage Estimates for Six Counties in the Mid/Southern Willamette Valley Including
More informationLand-use planning and volcanic hazards: Opportunities for New Zealand
Land-use planning and volcanic hazards: Opportunities for New Zealand Julia Becker, Wendy Saunders, Graham Leonard, David Johnston, Lower Hutt Clare Robertson, Massey University, Palmerston North Presentation
More informationVolcanic Mass Flow Processes and Deposits
Volcanic Mass Flow Processes and Deposits Smith and Lowe, 1991 Lahars=hyperconcentrated (flood) flow (HFF) and debris flow Note ideal HFF deposit has normal grading, parallel bedding, better sorting Ideal
More informationVolcanism (Chapter 5)
GEOLOGY 306 Laboratory Instructor: TERRY J. BOROUGHS NAME: Volcanism (Chapter 5) For this assignment, you will require: a calculator, colored pencils, string, protractor, stereoscopes (provided). Objectives
More informationMonitoring Cascade Volcanoes
Cascades Volcano Observatory Cascade Volcanoes http://volcanoes.usgs.gov/observatories/cvo/cvo_monitoring.html Cascade Volcanoes Volcano eruption forecasting relies on several disciplines of volcanology.
More informationVOLCANOES. Homework due Wed./Thurs. I have a few copies left, or get by moodle or webpage
VOLCANOES Homework due Wed./Thurs. I have a few copies left, or get by moodle or webpage Bowen s Reaction Series Oceanic basin tectonics http://my.execpc.com/~acmelasr/mountains/geogramsnf.html Icelandic
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 informationLiving on the Edge: Unit3: Convergent Plate Boundaries
Living on the Edge: Unit3: Convergent Plate Boundaries Because of its eleva.on (4,392 m), relief, hydrothermal altera.on, ice cap, glacier- fed radial valleys, and proximity to suburbs of the SeaBle- Tacoma
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 informationFire and Ice. Overview. Grade Level 6 8. Students will be able to: Objectives
Fire and Ice Overview Students use a power point presentation to compare and contrast the geologic history and environment of Mount Rainier and Mount Fuji, the Sister Mountains. Grade Level 6 8 Students
More informationVolcanoes. Environmental Geology, Mr. Paul Lowrey Stacey Singleton, Cassandra Combs, Dwight Stephenson, Matt Smithyman
Volcanoes Environmental Geology, Mr. Paul Lowrey Stacey Singleton, Cassandra Combs, Dwight Stephenson, Matt Smithyman EMPACTS Project, Spring 2017 Northwest Arkansas Community College, Bentonville, AR
More informationSEISMIC DATA SET 2 (THROUGH JUNE 12)
Living on the Edge: Unit 6 Prework, Hazards and Risks at Convergent Plate Boundaries SEISMIC DATA SET 2 (THROUGH JUNE 12) Note: you only need to examine/describe the same type of data you used during the
More informationCATACLYSMIC ERUPTIONS
CATACLYSMIC ERUPTIONS The really big ones! This figure compares the size of some recent, well-known eruptions. Note how small the eruptions of Mount St. Helens and even Vesuvius are compared to Katmai,
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 informationTectonic Processes and Hazards Enquiry Question 1: Why are some locations more at risk from tectonic hazards?
Tectonic Processes and Hazards Enquiry Question 1: Why are some locations more at risk from tectonic hazards? Key words Basalt Andesite Rhyolite Benioff Zone Subduction zone Crustal fracturing Definition
More informationEHaz 26 April 2007 Questions. The following questions are arranged by topic. Risk assessment & management MTU
EHaz 26 April 2007 Questions The following questions are arranged by topic. Risk assessment & management Slide 17 (very good slide, by the way!): In the case of the Merapi and Mt. St. Helens crises, how
More informationVolcanism Activity. Choose one of the options below to complete for tomorrow. You may work with a partner on this activity. Be creative and realistic!
Volcanism Activity Choose one of the options below to complete for tomorrow. You may work with a partner on this activity. Be creative and realistic! Option 1 Option 2 Option 3 Create a comic strip or
More informationFigure 8-21 Distribution of Lava Flow for the Model
Figure 8-21 Distribution of Lava Flow for the Model 2) Pyroclastic Flow The energy cone model was used for the simulation. a. The angle of inclination of Energy Line, φ, from the summit was 5.3 degrees
More informationThe Cascading Hazards from Cascadia s Earthquakes
Tsunamis The Cascading Hazards from Cascadia s Earthquakes Earthquakes (Nisqually earthquake, Seattle, WA) Volcanoes (Mt St Helens eruption, WA) Joan Gomberg gomberg@usgs.gov Landslides (Oso landslide,
More informationProgress Report: Sentinel Asia Success Story in the Philippines
Progress Report: Sentinel Asia Success Story in the Philippines 3 rd Joint Project Team Meeting on the Sentinel Asia STEP-2 July 6-8, 2010 Hyatt Hotel, Manila, Philippines Renato U. Solidum Jr. Director
More informationStudy Guide: Unit 1. 1) Take careful notes in class during the lectures as well as the information given in the slides presented during class
Geology 101 Study Guide: Unit 1 The purpose of this study guide is to help you prepare for the first unit exam by focusing your studying and providing example essay questions. You will not be asked to
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 informationWelcome back. During last lecture, we were talking about eruption which took place along St Mount Helens so that during 1980.
Earth Sciences for Civil Engineering Professor Javed N Malik Department of Earth Sciences Indian Institute of Technology Kanpur Module 2 Lecture No 8 Rock types and their Properties (Part-2) Welcome back.
More informationEarth Structures and Processes Teacher Notes
Aleutian Islands String of islands resulting from volcanic activity Part of the Pacific Ring of Fire Coast is very jagged and rocky with steep cliffs and mountains Underwater eruptions form new landforms
More informationName: Page 1. 2) What do increases and decreases in RSAM data indicate about magma movement inside the volcano?
Name: Page 1 Living on the Edge Unit 5: SEISMOLOGISTS A report on the seismic activity must be prepared in order to assess and forecast future activity. Complete the following components of the seismology
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 informationDetection from Space of Active Volcanism on Earth and, Potentially, on Venus and Rocky Exoplanets
Detection from Space of Active Volcanism on Earth and, Potentially, on Venus and Rocky Exoplanets Pete Mouginis Mark Hawaii Institute Geophysics and Planetology University of Hawaii Overview Styles of
More informationVolcanic Deformation and Evolution.
Volcanic Deformation and Evolution of Mt. Saint SitHelens http://pubs.usgs.gov/sim/3008/ B. A. Digital perspective view derived from USGS Digital Elevation Model (DEM) of Mount St. Helens as seen from
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 informationActivity 4: volcanic Hazards: Airborne Debris!
Activity 4: volcanic Hazards: Airborne Debris! Create an entry in your table of contents with this name Write the name of the activity in BIG LETTERS on the next open page of your notebook. Find your new
More informationHomework III. Volcanological Exercises
Page 1 of 5 EENS 3050 Tulane University Natural Disasters Prof. Stephen A. Nelson Homework III. Volcanological Exercises This page last updated on 16-Feb-2018 1. In your work as an insurance company executive
More informationVolcanoes: Help or Hindrance?
Volcanoes: Help or Hindrance? Volcanic eruptions can range from violent to mild. All kinds of eruptions have effects that can be both harmful and beneficial to people and the environment. Volcanoes Can
More informationSIO15 Midterm 1, Monday Oct. 30, 2017 TEST VARIATION: 2
SIO15 Midterm 1, Monday Oct. 30, 2017 TEST VARIATION: 2 1) Over the last 20 years, which of these natural disasters killed the most people in the U.S.? a) heat waves b) hurricanes c) lightning strikes
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 informationand their risks A look at volcano risk for young students. Produced by the MED-SUV project.
and their risks A look at volcano risk for young students. Produced by the MED-SUV project. Volcano Shapes: A volcano is a place (on Earth and OTHER PLANETS) where magma comes to the surface. This event
More information3.12 Geology and Topography Affected Environment
3 Affected Environment and Environmental Consequences 3.12 Geology and Topography 3.12.1 Affected Environment 3.12.1.1 Earthquakes Sterling Highway MP 45 60 Project Draft SEIS The Kenai Peninsula is predisposed
More informationGeography. Key facts. Volcanoes and volcanic eruptions
Geography Volcanoes and volcanic eruptions Volcanoes form when magma reaches the Earth's surface, causing eruptions of lava and ash. They occur at destructive (compressional) and constructive (tensional)
More informationGuidance for GEOGRAPHY End of Year Examination 2016
Guidance for GEOGRAPHY End of Year Examination 2016 The End of Year Examination takes place in Week 4 of the Summer Term. The Geography Examination will last 50 minutes. The Examination will include questions
More informationThe Quaternary and Pliocene Yellowstone Plateau Volcanic Field of Wyoming, Idaho and Montana Robert L. Christenson, USGS PP 729-G
The Quaternary and Pliocene Yellowstone Plateau Volcanic Field of Wyoming, Idaho and Montana Robert L. Christenson, USGS PP 729-G Three Volcanic Cycles of Yellowstone Three extraordinarily large explosive
More informationVolcanoes. volcanic hazards. Image courtesy of USGS.
Volcanoes volcanic hazards Volcanic hazards Pyroclastic flows and surges Pyroclastic flows and surges PYROCLAST: all solid fragments ejected from volcanoes PYROCLASTIC FLOW: A flow of hot gas and volcanic
More informationTectonics of Magma. From partial melting of mantle Occurs at oceanic ridges and mantle plumes More dense: makes oceanic crust
VOLCANOES Tectonics of Magma Basaltic magma From partial melting of mantle Occurs at oceanic ridges and mantle plumes More dense: makes oceanic crust Granitic magma From melting of crust, with water as
More informationSurname 1. Name: Instructor s Name: Course Number: Date: Geological Significance
Surname 1 Name: Instructor s Name: Course Number: Date: Geological Significance Eruption of Mt. St. Helens in 1980 Eruption of Mt.St. Helens in the 1980s availed a significant learning experience in geology.
More informationAlOS-PALSAR data for Landslide Monitoring and Geological Mapping
AlOS-PALSAR data for Landslide Monitoring and Geological Mapping Vern Singhroy, P-J Alasset, G Pavlic Canada Centre for Remote Sensing Ottawa, Canada vern.singhroy@ccrs.nrcan.gc.ca Objectives InSAR monitoring
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 informationNew A-Level Physical Geography
Half Term 1 3.1 Physical Geography: 3.1.5 Hazards: Plate Tectonics This optional section of our specification focuses on the lithosphere and the atmosphere, which intermittently but regularly present natural
More informationMulti Hazard Evaluation of a High Voltage Transmission Network. John Eidinger 1 and Leon Kempner 2
Multi Hazard Evaluation of a High Voltage Transmission Network John Eidinger 1 and Leon Kempner 2 1 G&E Engineering Systems Inc., P. O. Box 3592 Olympic Valley, CA 96146-3592; eidinger@earthlink.net. 2
More information3/24/2016. Geology 12 Mr. M. Gauthier 24 March 2016
Geology 12 Mr. M. Gauthier 24 March 2016 Introduction: Mt. St. Helens Before 1980 Mt. St Helens, in Southern Washington State, had not erupted since 1857 On March 27,1980 minor ashand eruptions were due
More informationUSGS Volcano Hazards Program
USGS Volcano Hazards Program NAS Board on Earth Sciences and Resources May 12, 2014 Charlie Mandeville USGS Program Coordinator cmandeville@usgs.gov www.volcanoes.usgs.gov Volcano Hazards Program Mission:
More informationNeed of Proper Development in Hilly Urban Areas to Avoid
Need of Proper Development in Hilly Urban Areas to Avoid Landslide Hazard Dr. Arvind Phukan, P.E. Cosultant/Former Professor of Civil Engineering University of Alaska, Anchorage, USA RI District Governor
More informationStudy Guide: Unit 3. Density and Pressure: You should be able to answer the types of questions given in the end of module questions.
IDS 102 Study Guide: Unit 3 The purpose of this study guide is to help you prepare for the third exam by focusing your studying and providing example essay questions. In the Focus On section you will find
More informationEarthquakes and volcanoes in Iceland
Jenny Jenkins Daði Harðarson Explosive Earth Earthquakes and volcanoes in Iceland The eruption of Bárðarbunga volcano in Iceland, July 2014 Key words volcano earthquake seismology prediction Bárðarbunga
More informationDegassing processes and recent activity at Volcán de Colima. Universidad de Colima, Mexico Corresponding author
Degassing processes and recent activity at Volcán de Colima Nick Varley * & Gabriel Reyes Dávila Universidad de Colima, Mexico Corresponding author email: nick@ucol.mx Volcán de Colima is currently in
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 informationMajor External Processes Driven by energy from the sun and from gravity. Also create hazards and resources.
Geologic Processes and Hazards Definition of Geology External and Internal Processes: examples of each Fundamentals of Plate Tectonics: definition, types of boundaries, general geography, hazards & resources
More informationVolcanic Hazards & Prediction of Volcanic Eruptions
Page 1 of 11 EENS 3050 Tulane University Natural Disasters Prof. Stephen A. Nelson Volcanic Hazards & Prediction of Volcanic Eruptions This page last updated on 04-Oct-2016 Volcanic Hazards This lecture
More informationGEO 305: LIVING WITH ACTIVE CASCADE VOLCANOES SUMMER 2002 (7/22 8/15) COURSE SYLLABUS. Faculty Contact: Instructor, Summer 2002:
GEO 305: LIVING WITH ACTIVE CASCADE VOLCANOES SUMMER 2002 (7/22 8/15) COURSE SYLLABUS Faculty Contact: Instructor, Summer 2002: Roger Nielsen Heather Petcovic Geology Program Director Office Dawes 21 Dept.
More informationVolcanology. The study of volcanoes
Volcanology The study of volcanoes Magma forms wherever temperature and pressure are high enough to melt rock. Some magma forms at the aesthenosphere Magma also forms at plate boundaries, where intense
More informationMass Wasting: The Work of Gravity
Chapter 15 Lecture Earth: An Introduction to Physical Geology Twelfth Edition Mass Wasting: The Work of Gravity Tarbuck and Lutgens Chapter 15 Mass Wasting The Importance of Mass Wasting Slopes are the
More informationFIRST GRADE HAZARDS 1 WEEK LESSON PLANS AND ACTIVITIES
FIRST GRADE HAZARDS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF FIRST GRADE VOLCANOES WEEK 1. PRE: Learning the shapes of volcanoes. LAB: Experimenting with "lava." POST: Comparing
More informationPavlof. Alaska Peninsula N, W; summit elev. 2,519 m. All times are local (= UTC - 9 hours)
Pavlof Alaska Peninsula 55.42 N, 161.887 W; summit elev. 2,519 m All times are local (= UTC - 9 hours) Eruption in May-June 2013 with lava flows and ash emissions to ~8.5 km a.s.l. Pavlof, the most active
More informationGLG Ch 6: Volcanoes & Volcanic Hazards. 3. Name, describe (DSC) and draw the three types of volcanoes from smallest to largest.
GLG 101 - Ch 6: Volcanoes & Volcanic Hazards Name 6.1 What Is and and Is Not a Volcano? 1. Three common characteristics of a volcano include A B C 2. How did the Hopi Buttes (figure 06 01.b1) form? 3.
More informationVolcanoes. Table of Contents Volcanoes and Plate Tectonics Volcanic Eruptions Volcanic Landforms
Volcanoes Table of Contents Volcanoes and Plate Tectonics Volcanic Eruptions Volcanic Landforms What is a volcano? cone Conduit Or Pipe vent Side vent Central vent Crater A volcano is a vent or 'chimney'
More informationVolcanism. Dr. Dan Britt Department of Physics
Volcanism Dr. Dan Britt Department of Physics Pompeii and Herculaneum Buried in a AD 79 eruption of Mt. Vesuvius. Pompeii was under ~20 feet of ash and pumice Herculaneum was under ~80 feet of welded tuff.
More informationOIKOS > landslide > mechanism >predisposing causes
predisposing causes and trigger OIKOS > landslide > mechanism >predisposing causes Landslides are events that occur in space and time. As such, it is usually possible to identify both one or more landslide
More informationES 104 Lab Quiz Name: _ Sample _KEY DO NOT WRITE ON THIS SHEET. USE THE SCANTRON FORM!
ES 104 Lab Quiz Name: _ Sample _KEY DO NOT WRITE ON THIS SHEET. USE THE SCANTRON FORM! 1.1 Color in the shadowed side of Moon. This side is in shadow this side is lighted This diagram shows the moon in
More information