Falk Amelung. Sang-Ho Yun. Thomas Walter. Asta Miklius. now at GFZ Potsdam. Hawaii Volcano Observatory. Stanford University

Similar documents
Constraints on Magma Chamber Geometry at. Sierra Negra Volcano, Galápagos Islands, based on InSAR Observations

What is the Relationship between Pressure & Volume Change in a Magma Chamber and Surface Deformation at Active Volcanoes?

Supporting the response to the 2018 lower East Rift Zone and summit collapse at Kīlauea Volcano, Hawaiʻi

Magma Migration, Storage and Evolution in the Galápagos Region John Sinton University of Hawai i

The Geohazard Supersites and Natural Laboratories (GSNL).

Earthquake and Volcano Deformation

Effects of magma compressibility on volcano deformation and seismicity. Eleonora Rivalta

GSNL - Geohazard Supersites and Natural Laboratories. Biennial report for Candidate/Permanent Supersite. Hawaiʻi Supersite. Annex to report

Volcano Seismicity and Tremor. Geodetic + Seismic

ASAR IMAGES A DIVERSE SET OF DEFORMATION PATTERNS AT KĪLAUEA VOLCANO, HAWAI`I

The 12 September 1999 Upper East Rift Zone dike intrusion at Kilauea Volcano, Hawaii

McGill: What is the nature of fluid flow in the clastic apron surrounding ocean islands, and what are the implications for instability?

Hawai i Volcanoes Data

Activity Flour box volcano deformation model

Magma degassing triggered by static decompression at K lauea Volcano, Hawai i

Introduction to Volcanic Seismology

High-resolution temporal imaging of. Howard Zebker

Detecting the Source Location of Recent Summit Inflation via Three-Dimensional InSAR Observation of Kīlauea Volcano

The role of viscous magma mush spreading in volcanic flank motion at Kīlauea Volcano, Hawai i

When Mount St. Helens erupted, trapped gases caused the north side of the mountain to explode. Volcanic ash was ejected high into the atmosphere.

Lecture 19: Volcanoes II. GEOS 655 Tectonic Geodesy Jeff Freymueller

Earthquake and Volcano Clustering at Mono Basin (California)

REVIEW: The Setting - Climatology of the Hawaiian Archipelago

The Removal of Lava Flow Subsidence Signals from deformation interferograms at Nyamuragira Volcano, D.R. Congo

NC Earth Science Essential Standards

Aftershock decay, productivity, and stress rates in Hawaii: Indicators of temperature and stress from magma sources

Objectives: Describe how volcanoes can affect people. Describe conditions that cause volcanoes. Describe the relationship between volcanoes and Earth

Evolution of the 2007 earthquake swarm, Tanzania: Envisat and ALOS interferometry, ground observations and elastic modeling

Volcano Monitoring on a Regional Scale:

Goal 2.1 Forces in the Lithosphere. Volcanic Activity

About Volcanoes Volcanology IMPORTANT TERMS

Effects of Eruptions. Most active in the world Kilauea, Hawaii.

Determining the relationship between the summit and Pu u Ō ō on Kilauea

4D gravity changes associated with the 2005 eruption of Sierra Negra volcano, Galápagos

Magma. Objectives. Describe factors that affect the formation of magma. Compare and contrast the different types of magma. Vocabulary.

Monitoring Volcanoes & Predicting Eruptions. I.G Kenyon

Geohazard Supersites and Natural Laboratories

Slow Deformation of Mt. Baekdu Stratovolcano Observed by Satellite Radar Interferometry

FINAL EXAM December 20 th, here at 1:00 3:00 pm

Determining the rate of magma supply to a volcano requires

Evolution of dike opening during the March 2011 Kamoamoa fissure eruption, Kīlauea Volcano, Hawai`i

Peter Shearer 1, Robin Matoza 1, Cecily Wolfe 2, Guoqing Lin 3, & Paul Okubo 4

J. Foster, 1 B. Brooks, 1 T. Cherubini, 1 C. Shacat, 1 S. Businger, 1 and C. L. Werner Introduction

Chapter 7 Lecture Outline. Volcanoes and Other Igneous Activity

3.2 Notes: Volcanoes Form as Molten Rock Erupts

A Volcano is An opening in Earth s crust through

Chapter 7 Lecture Outline. Volcanoes and Other Igneous Activity

Locating the Epicenter

Feedback processes between magmatic events and flank movement at Mount Etna (Italy) during the eruption

Chapter 18. Volcanism

Evolution of dike opening during the March 2011 Kamoamoa fissure eruption, Kīlauea Volcano, Hawai'i

Visualizing Earth Science. Chapter Overview. Volcanoes and Eruption Types. By Z. Merali and B. F. Skinner. Chapter 9 Volcanism and Other

Diverse deformation patterns of Aleutian volcanoes from InSAR

3D temporal evolution of displacements recorded on Mt. Etna from the 2007 to 2010 through the SISTEM method

M 7.2 Earthquake along Iraq Iran border Sunday, November 12, Close to boundary of the Arabian and Eurasian Plates

Magma 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.

Volcanoes. What is a volcano

GEOLOGY MEDIA SUITE Chapter 12

OIKOS > volcano > mechanism >types of volcanoes

Topics. Magma Ascent and Emplacement. Magma Generation. Magma Rise. Energy Sources. Instabilities. How does magma ascend? How do dikes form?

Magma. Objectives. Describe factors that affect the formation of magma. Compare and contrast the different types of magma. Vocabulary.

NAME IGNEOUS & METAMORPHIC PETROLOGY INTRUSION OF MAGMA

Geohazard Supersites and Natural Laboratories

Volcano-Tectonic Interactions as Triggers of Volcanic Eruptions

Dynamic Planet PUT ALL YOUR ANSWERS ON THE ANSWER SHEET. c) low temperature d) high volatile content

CALDERAS: STRUCTURE, UNREST, MAGMA TRANSFER

Plate Tectonics Lab II: Background Information

NC Earth Science Essential Standards

Plate Boundaries & Resulting Landforms

New insights into Kilauea s volcano dynamics brought by large-scale relative relocation of microearthquakes

Systematic relocation of seismicity on Hawaii Island from 1992 to 2009 using waveform cross correlation and cluster analysis

MIGRATING SWARMS OF BRITTLE-FAILURE EARTHQUAKES IN THE LOWER CRUST BENEATH MAMMOTH MOUNTAIN, CALIFORNIA

608 CHAPTER 20 Earthquakes and Volcanoes Spencer Grant/PhotoEdit, Inc.

Overview of Ch. 4. I. The nature of volcanic eruptions 9/19/2011. Volcanoes and Other Igneous Activity Chapter 4 or 5

Geology of the Hawaiian Islands

EAS 116 Earthquakes and Volcanoes

Earth s Changing Surface

"Dynamics and structural evolution of collapse calderas: A comparison between field evidence, analogue and mathematical models"

Chapter 18 - Volcanic Activity. Aka Volcano Under the City

Kilauea Volcano in Eruption on Postals

Volcanoes. Table of Contents Volcanoes and Plate Tectonics Volcanic Eruptions Volcanic Landforms

Prentice Hall EARTH SCIENCE

INTRODUCTION TO VOLCANIC SEISMOLOGY

GEOL 10: Environmental Geology Mid Term II Study Guide

The Santorini Inflation Episode, Monitored by InSAR and GPS

Focusing of Eruptions by Fracture Wall Erosion

Hawaiian Islands. Lesson 13

A MICROANALYTICAL APPROACH TO UNDERSTANDING THE ORIGIN OF CUMULATE XENOLITHS FROM MAUNA KEA, HAWAII

The 2005 eruption of Sierra Negra volcano, Galápagos, Ecuador

180 points. 1. Lava erupts through an opening in Earth s crust called a. 2. A bowl-shaped depression that forms around the vent of a volcano is a

THE FEBRUARY 1993 KILAUEA EAST RIFT ZONE DIKE INTRUSION REVEALED THROUGH INSAR

3-Dimension Deformation Mapping from InSAR & Multiaperture. Hyung-Sup Jung The Univ. of Seoul, Korea Zhong Lu U.S. Geological Survey, U.S.A.

Volcanoes. Presented by Kesler Science

INSAR TIME SERIES ANALYSIS OF SUBTLE TRANSIENT CRUSTAL DEFORMATION SIGNALS ASSOCIATED WITH THE 2010 SLOW SLIP EVENT AT KILAUEA, HAWAII

Volcano: a weak spot in the crust where molten material or magma comes to the surface

CALDERA VOLCANISM: ANALYSIS, MODELLING AND RESPONSE

How do Volcanoes change the Earth s surface?

This is a repository copy of How caldera collapse shapes the shallow emplacement and transfer of magma in active volcanoes.

Section 10.1 The Nature of Volcanic Eruptions This section discusses volcanic eruptions, types of volcanoes, and other volcanic landforms.

Maka u Pele: A Learning Game for

Transcription:

Falk Amelung RSMAS - University of Miami Thomas Walter now at GFZ Potsdam Sang-Ho Yun Stanford University Asta Miklius Hawaii Volcano Observatory

Pinatubo 1991 Bautista et al., 98 Mount Pinatubo erupted 9 months after earthquake Luzon M7.8 earthquake 100 km Did the earthquake trigger the eruption, and how?

Karymksy 1996 Karymsky erupted 2 days after earthquake M7.2 1996 earthquake 50 km

Karymksy 1996 Static stress changes due to earthquake Static stress changes may explain the eruption!

Galapagos Islands Fernandina 1992-1998 ERS interferog 1995 radial dike Fernandina 2005 circumferential dike Jonsson et al., Isabela Island Eruptions in 1995, 13 May 2005 Fernandina

Galapagos Islands Fernandina 1992-1998 ERS interferog 1995 radial dike Fernandina 2005 circumferential dike Jonsson et al., Isabela Island

Static stress changes Fernandina 1992-1998 ERS interferog 1995 radial dike Modelling of changes in the stress field along calderabounding rift zone 2005 circumferential dike

3D view Static stress changes Fernandina 1992-1998 ERS interferog 1995 radial dike Normal stress 2005 circumferential dike clamping unclamping

3D view Static stress changes Fernandina 1992-1998 ERS interferog 1995 radial dike unclamping Normal stress clamping unclamping 2005 circumferential dike Conclusion: 2005 dike intruded in area unclamped by the 1995 dike!

Fernandina 1992-1998 ERS interferog 1995 radial dike unclamping 2005 circumferential dike clamping unclamping

Sierra Negra volcano Fernandina and Isabela Islands - Ground Deformation Sierra Negra volcano trapdoor faulting in 1998 ERS interferograms Sill at 2 km depth 0

Sierra Negra volcano Fernandina and Isabela Islands - Ground Deformation trapdoor faulting in spring 200 Envisat interferograms 0

Sierra Negra volcano eruption 22 Oct 2005 trapdoor faulting in spring 20 eruptions 1979, 2005?, 1998, 2005 Envisat interferograms Simulation: Sang-ho Yun sill propagation model 0 north-south cross-section Conclusion: 2005 eruption site consistent with propagating sill model

Mauna Loa volcano, Hawaii The Hawaiian Volcanoes Mauna Loa: eruptions in 1950, 1984 Kilauea: continuous eruption since 1983 Photos: HVO

Mauna Loa volcano, Hawaii 2002-2003 Radarsat A3 interferogram ALEP ELEP Inflation since May 2002 ~ 7 cm/yr extension across caldera

Mauna Loa volcano, Hawaii Stacked Interferograms Ascending, stack of Beam 4 3 Interferograms ascending S3

una Loa volcano, Stacked stacks Interferograms of RSAT interferogra

una Loa volcano, Stacked stacks Interferograms of RSAT interferogra

una Loa volcano, Stacked stacks Interferograms of RSAT interferogra

Mauna Loa volcano: Kinematic Model 2-D velocity field from ~80 acquisitions

Mauna Loa volcano: Kinematic Model

Mauna Loa volcano: Kinematic Model

Mauna Loa volcano: Kinematic Model

Mauna Loa magma plumbing system Opening along Rift Zone Kinematic model Dynamic model variable magma excess pressure, point source, halfspace uniform magma excess pressure, finite source, topography (Williams & Wadge - maximum dike inflation south method) of caldera beneath summit rese deep rift intrusion, 0.25 m/yr opening magma chamber, 4.5 km depth, 1-1.3 km radius

Mauna Loa magma plumbing system Opening along Rift Zone Dynamic model deep rift intrusion magma chamber 1-1.3 km radius uniform magma excess pressure, finite source, topography (Williams & Wadge - maximum dike inflation south of caldera beneath summit rese method)

Status stress changes Opening along Rift Zone Inflation of magma plumbing System - maximum encourages dike decollement inflation south of caldera beneath summit rese faulting!

Conclusions Fernandina: stress-transfer model predict location of 2005 circumferential dike Sierra Negra: sill propagation model pre 2005 eruptive dike Mauna Loa: decollement slip consistent wit changes due to the inflation of model magmatic sy

Conclusions Fernandina: stress-transfer model predict location of 2005 circumferential dike Sierra Negra: sill propagation model pre 2005 eruptive dike Mauna Loa: decollement slip consistent wit changes due to the inflation of model magmatic sy job ad: grad. student, opportuniti