part 4: volcanic hazards & monitoring

58
Part 4: Volcanic Hazards & Part 4: Volcanic Hazards & Monitoring Monitoring “Normal ” view has a Notes panel below with lecture notes and links to video lectures, activities, or web sites. •“Slide Show ” view has animated elements that pop up on clicking •Video & animations were removed to increase speed. Download information is in the Notes panel in Normal view. If you got this slide show on a DVD, the related animations will also be in a folder associated with the PowerPoint. • Modify slide show liberally for your own needs! Slide show prepared by Slide show prepared by Dr. Beth Pratt-Sitaula (Central Washington University) and Jenda Dr. Beth Pratt-Sitaula (Central Washington University) and Jenda Johnson (IRIS). Johnson (IRIS).

Upload: clark

Post on 13-Jan-2016

40 views

Category:

Documents


1 download

DESCRIPTION

Part 4: Volcanic Hazards & Monitoring. “ Normal ” view has a Notes panel below with lecture notes and links to video lectures, activities, or web sites. “ Slide Show ” view has animated elements that pop up on clicking - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: Part 4: Volcanic Hazards & Monitoring

Part 4: Volcanic Hazards & MonitoringPart 4: Volcanic Hazards & Monitoring

• “Normal” view has a Notes panel below with lecture notes and links to video lectures, activities, or web sites.

•“Slide Show” view has animated elements that pop up on clicking

•Video & animations were removed to increase speed. Download information is in the Notes panel in Normal view. If you got this slide show on a DVD, the related animations will also be in a folder associated with the PowerPoint.

• Modify slide show liberally for your own needs!

Slide show prepared by Slide show prepared by Dr. Beth Pratt-Sitaula (Central Washington University) and Jenda Johnson (IRIS).Dr. Beth Pratt-Sitaula (Central Washington University) and Jenda Johnson (IRIS).

Page 2: Part 4: Volcanic Hazards & Monitoring

Volcanoes are…

An opening on the planet’s surface where molten rock, ash, or gases escape from below

Aleutian Islands, AK; International Space Station photo

http://earthquake.usgs.gov/monitoring/anss/regions/hi/

Page 3: Part 4: Volcanic Hazards & Monitoring

1. Volcanoes are steep-sided and ooze hot runny lava

FALSE FALSE - - ““Hot runnyHot runny”” volcanoes are volcanoes are mostly flat or shield likemostly flat or shield like

Volcano Prior Knowledge SurveyVolcano Prior Knowledge Survey

TRUE/FALSE –> thumbs up OR downTRUE/FALSE –> thumbs up OR down

Page 4: Part 4: Volcanic Hazards & Monitoring

http://www.imdb.com/media/rm1327600128/tt0445548

Page 5: Part 4: Volcanic Hazards & Monitoring

Volcano Prior Knowledge SurveyVolcano Prior Knowledge Survey

2. The biggest eruptions flatten topography.

TRUE TRUE – – largest volumelargest volume eruptions eruptions lead to flood basalt plateaus; lead to flood basalt plateaus; most explosivemost explosive eruptions lead to eruptions lead to mountains getting blown to bitsmountains getting blown to bits

TRUE/FALSE –> thumbs up OR downTRUE/FALSE –> thumbs up OR down

Page 6: Part 4: Volcanic Hazards & Monitoring

http://www.imdb.com/media/rm1327600128/tt0445548

Page 7: Part 4: Volcanic Hazards & Monitoring

Volcano Prior Knowledge SurveyVolcano Prior Knowledge Survey

3. Magma chambers are…big chambers of liquid rock

FALSE - Magma FALSE - Magma ““chamberschambers”” form form when lava is injected in cracks and when lava is injected in cracks and crevasses and pushes against crevasses and pushes against existing rock. They are usually existing rock. They are usually more of a plumbing system than a more of a plumbing system than a chamber.chamber.

TRUE/FALSE –> thumbs up OR downTRUE/FALSE –> thumbs up OR down

Page 8: Part 4: Volcanic Hazards & Monitoring
Page 9: Part 4: Volcanic Hazards & Monitoring

SHOW ANIMATION “Mesozoic Subduction” from URL below.http://emvc.geol.ucsb.edu/2_infopgs/IP1GTect/cSubduction.html

Page 10: Part 4: Volcanic Hazards & Monitoring

• How many active volcanoes on Earth?

• How many volcanoes erupt per year?

• How many people are killed by volcanoes?

~1,500 active volcanoes~1,500 active volcanoes

~60 volcanoes erupt per year~60 volcanoes erupt per year

~200,000 in the last 200 years~200,000 in the last 200 years

Some volcano statsSome volcano stats

Page 11: Part 4: Volcanic Hazards & Monitoring

Where does molten rock come from?

Modified from USGS Graphics

Page 12: Part 4: Volcanic Hazards & Monitoring

Where do volcanoes form?

• Subduction zones

• “Hot spots”

• Mid-ocean ridges

• Continental rift zones

Page 13: Part 4: Volcanic Hazards & Monitoring

Rocks melt under certain circumstances

1. Heating

2. Decompression

3. Reducing melting temp by adding water

Page 14: Part 4: Volcanic Hazards & Monitoring

Types of Volcanoes

Flood Basalts

Millions km3 of horizontal

basalt layers

Columbia Flood Basalts Photo by Thor Thordarsson

Page 15: Part 4: Volcanic Hazards & Monitoring

Why do different magmas behave differently & make very different volcanoes?

• VISCOSITY

• VOLATILES

• VOLUME

“3 Vs” •WATER

•CARBON DIOXIDE

•Sulfur dioxide

•Hydrogen sulfide

Page 16: Part 4: Volcanic Hazards & Monitoring

Viscosity determines:

1. The flow rate of magma

2. VOLATILE trapping

vs

Page 17: Part 4: Volcanic Hazards & Monitoring

Viscosity depends on chemical composition

http://volcanoes.usgs.gov/images/pglossary/VolRocks.php

Page 18: Part 4: Volcanic Hazards & Monitoring

Types of Volcanoes

Flood Basalts

Millions km3 of horizontal

basalt layers

Columbia Flood Basalts Photo by Thor Thordarsson

Page 19: Part 4: Volcanic Hazards & Monitoring

Flood basalts

• Extremely low viscosity

• Few volatiles (non-explosive)

• Very very large volume

http://www.fas.org/irp/imint/docs/rst/Sect17/Sect17_3.html

Page 20: Part 4: Volcanic Hazards & Monitoring

Flood basalts - HAZARDS

• Bury your state in lava

• Huge green house gas release

• Geologic ennui (if you find basalt dull)

http://www.fas.org/irp/imint/docs/rst/Sect17/Sect17_3.html

Page 21: Part 4: Volcanic Hazards & Monitoring

Columbia River Flood Basalts

• Over 300 separate flows averaging 580 km3 EACH• 3.5 km thick in places• Erupted 17.5-6 Ma• ~90% erupted 16-15 Ma http://geosphere.gsapubs.org/content/4/3/480.full.pdf+html

Thor Thordarsson

Page 22: Part 4: Volcanic Hazards & Monitoring

Shield Volcanoes

• Low viscosity

• Few volatiles (non-explosive)

• Large volume

Mauna Loa, Hawaii USGS

Page 23: Part 4: Volcanic Hazards & Monitoring

Shield Volcanoes - HAZARDS

• Lava flows

• Volcanic gasses (esp. CO2)

Medicine Lake Volcano, CA USGS

Page 24: Part 4: Volcanic Hazards & Monitoring

Cinder cone (or scoria cone)

• Moderate viscosity

• Some volatiles

• Small volume

Image released to public domain by Q Myers (English Wikipedia)

~600 m

Lava Butte, OR

Page 25: Part 4: Volcanic Hazards & Monitoring

Stratovolcano

• Mod–high viscosity

• Few-many volatiles (mod-very explosive)

• Mod-large volume

Mt Rainier and Seattle, WA

&

Page 26: Part 4: Volcanic Hazards & Monitoring

Stratovolcano – multiple types of eruption processes

Lava dome

Ash cloud

Pyroclastic flows

USGS Mt. St. Helens, 1984

USGS Mt Mayon, Philippines, 2006

http://www.tulane.edu/~sanelson/geol111/igneous.htm

Page 27: Part 4: Volcanic Hazards & Monitoring

Stratovolcano - Mt St Helens

Before 1980 eruptionbuilt up

USGS

USGS

After 1980 eruptionblown to bits

Page 28: Part 4: Volcanic Hazards & Monitoring

Stratovolcano - HAZARDS• Pretty much all types of volcanic hazards

USGS

Page 29: Part 4: Volcanic Hazards & Monitoring

Stratovolcanoes – PACIFIC NW

Most Cascade volcanoes are stratovolcanoes (typical for subduction zones)

Stratovolcano

Page 30: Part 4: Volcanic Hazards & Monitoring

shield vs composite

Mauna Loa’s full height = 19,000 ft + 13,000 ft = 32,000 ft

below sea level

above sea level

Mt Rainer = 14,400 ft

Page 31: Part 4: Volcanic Hazards & Monitoring

Caldera formation

Magma chamber partially emptied during eruption

Center collapses down and forces out more magma

Caldera is formed

Coke w/dry ice

• High viscosity• Many volatiles (very explosive)• Large volume

http://pubs.usgs.gov/fs/2002/fs092-02/

Page 32: Part 4: Volcanic Hazards & Monitoring

Caldera formation - HAZARDS• Ash falls• Pyroclastic flows• Volcanic landslides• Volcanic gasses

http://pubs.usgs.gov/fs/2002/fs092-02/

Page 33: Part 4: Volcanic Hazards & Monitoring

Crater Lake Caldera, OR

Page 34: Part 4: Volcanic Hazards & Monitoring

Continental Hotspot CalderaYellowstone, WY

http://pubs.usgs.gov/fs/fs100-03/

Page 35: Part 4: Volcanic Hazards & Monitoring

Yellowstone Eruptions

http://www.nps.gov/yell/naturescience/eruptions.htm

http://pubs.usgs.gov/fs/2005/3024/

Page 36: Part 4: Volcanic Hazards & Monitoring

Snake River Plain, IdahoPossible Hot Spot Trail from SW to NE over last 16 Ma

16 Ma

10 Ma

5 Ma 2 Ma1.3 Ma

0.6 Ma

ID

UT

WY

NV

OR

Image after Smith & Siegel (2000), Windows into the Earth: the Geological Story of Yellowstone and Grand Teton National Parks

80 km

Page 37: Part 4: Volcanic Hazards & Monitoring

Proposed relationship between flood basalts & hotspots

Columbia Flood Basalts

Yellowstone hotspot track~16 Ma

Page 38: Part 4: Volcanic Hazards & Monitoring

Cascade Volcanoes

Show real roll-over

Page 39: Part 4: Volcanic Hazards & Monitoring

Below Cascade volcanoes

Page 40: Part 4: Volcanic Hazards & Monitoring

Major rock types

CLASSIFICATION OF INTRUSIVE ROCKS

Gabbro Diorite Granodiorite Granite

Page 41: Part 4: Volcanic Hazards & Monitoring

Volcanic Hazards

• Pyroclastic flow (a.k.a. ash flow)

• Lahar (a.k.a. mud flow or debris flow)

• Gases

• Ash falls

• Volcanic Landslides

• Lava Flows

• Tsunamis USGS

Page 42: Part 4: Volcanic Hazards & Monitoring

Show Understanding Volcanic Hazards clips

Page 43: Part 4: Volcanic Hazards & Monitoring

Mt Rainier Lahar Hazard

Page 44: Part 4: Volcanic Hazards & Monitoring

Ash fall hazard

USGS

Page 45: Part 4: Volcanic Hazards & Monitoring

The Science of PredictionMonitoring Volcanic Activity

Page 46: Part 4: Volcanic Hazards & Monitoring

Signs of Volcanic Activity

Scientists look for five signs that volcanic processes are at work

• Eruption History

• Volcanic Gases

• Heat and Hydrothermal Activity

• Earthquakes

• Ground deformation

Page 47: Part 4: Volcanic Hazards & Monitoring

Monitoring

Scientists use many tools to monitor volcanoes

Since erupting volcanoes are dangerous, they prefer tools that can be set up and left

Image from USGS (2002) Volcano Hazards Program: Strategy for reducing volcanic risk http://volcanoes.usgs.gov/

Page 48: Part 4: Volcanic Hazards & Monitoring

Volcanic Gases

Volcanic gases are hazardous and hard to sample – they can be detected using :

• Spectrometers mounted on ground or airplane

• Samples collected by hand and analyzing in a laboratory

Image from USGS Volcano Hazards Program “Measuring volcanic gases: emission rates of sulfur dioxide and carbon dioxide in volcanic plumes.” http://volcanoes.usgs.gov/About/What/Monitor/Gas/plumes.html

A scientist collects gas samples (Note the protective equipment)

Page 49: Part 4: Volcanic Hazards & Monitoring

Volcanic Gases

• Trees and animals can be effected by gasses and aid detection

• Trees at Mammoth Mt, CA died when CO2 suffocated their roots

Image from USGS Fact Sheet 172-96 “Invisible CO2 Gas Killing Trees at Mammoth Mountain, California” http://pubs.usgs.gov/fs/fs172-96/

Page 50: Part 4: Volcanic Hazards & Monitoring

Heat & Hydrothermal Activity

Hydrothermal activity demonstrates presence of magma, not necessarily magma movement

Thermal features can be monitored by:• Night aerial observations

• Thermal (infrared) imaging

• Direct temperature measurements

Image from (2007) USGS Mount St. Helens, Washington Forward Looking Infrared Images http://vulcan.wr.usgs.gov/Imgs/Jpg/MSH/MSH07/MSH07_area_new_growth_on_dome_06-26-07_FLIR_med.jpg

Infrared image of Mt. St. Helens’ new lava

dome June 26th 2007

Page 51: Part 4: Volcanic Hazards & Monitoring

Earthquakes

• Moving magma and volcanic fluids cause quakes

• Most volcanic earthquakes are:• <3 Magnitude• Shallower than 10 km• Occur in swarms

Magma risesMagma and gases exert pressure

Rocks break, triggering earthquakes

Image from USGS Volcano Hazards Program “Monitoring Volcano Seismicity.” http://volcanoes.usgs.gov/activity/methods/seismic/index.php

Page 52: Part 4: Volcanic Hazards & Monitoring

Earthquakes

Scientists can tell where Mt. St. Helens’ magma source is by looking at earthquake pattern.

Page 53: Part 4: Volcanic Hazards & Monitoring

Ground Deformation

• Volcanoes change shape before, during, and after eruptions

• Deformation is caused by trapped and pressurized gases or fluids (monitor gas emissions too!)

• Usually accompanied by swarms of shallow earthquakes (monitor seismicity too!)

Image from USGS Volcano Hazards Program “Monitoring Volcano Seismicity.” http://volcanoes.usgs.gov/activity/methods/seismic/index.php

Page 54: Part 4: Volcanic Hazards & Monitoring

Ground Deformation

Deformation is measured using:

•Tiltmeters (big, underground carpenter’s level)

•Global Positioning System (satellites triangulate position)

•Leveling Survey (periodic repeat measurements)

GPS site Augustine Volcano, Alaska

Mt St Helens image from USGS Volcano Hazards Program “Monitoring Volcano Ground Deformation.” http://volcanoes.usgs.gov/activity/methods/deformation/tilt/msh.php

Tiltmeter at Mt St Helens’ crater floor

Page 55: Part 4: Volcanic Hazards & Monitoring

Science of Prediction

Even though scientists could not predict the exact moment when Mt. St. Helens would erupt, they were able to save many lives by predicting that it would erupt.

Table 1. SUMMARY OF VOLCANIC-ALERT LEVELS

NORMAL Typical background activity of a volcano in a non-eruptive state After a change from a higher level: Volcanic activity considered to have ceased, and volcano reverted to its normal, non- eruptive state.

ADVISORY Elevated unrest above known background

activity After a change from a higher level: Volcanic activity has decreased significantly but continues to be closely monitored for possible renewed increase.

WATCH Heightened/escalating unrest with increased potential for eruptive activity (timeframe variable) OR a minor eruption underway that poses limited hazards

WARNING Highly hazardous eruption underway or imminent

Table from USGS Volcano Hazards Program “USGS Volcanic Activity Alert – Notification System” http://volcanoes.usgs.gov/activity/alertsystem/

Page 56: Part 4: Volcanic Hazards & Monitoring

Volcanic monitoring animations by

http://www.iris.edu/hq/programs/education_and_outreach/animations#CC

Page 57: Part 4: Volcanic Hazards & Monitoring

Mt St Helens erupted a lava dome 2004-2008

What direction did the GPS stations move during this eruption?

– Outwards?

– Inwards?

http://vulcan.wr.usgs.gov/Volcanoes/MSH/Eruption04/Monitoring/February2008/

Page 58: Part 4: Volcanic Hazards & Monitoring

Mt St Helens GPS data 2004-5

Lisowski et al, UNAVCO proposal, 2008