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Predicting volcanic eruptions
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F D C B A
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Outline • Review of igneous rocks, magmas, and types of volcanoes
• Peaceful vs. explosive eruptions • Predicting volcanic eruptions • Airplane flight paths and risks posed by volcanic ash
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Texture Chemical Composition Plutonic Volcanic
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Plutonic & volcanic equivalents
Felsic Rhyolite Granite Obsidian Quartz monzonite Andesite Gabbro Basalt Mafic Plutonic Volcanic
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2) Dissolved gases in the magma
What controls whether an eruption is a peaceful lava flow or explosive? SiO2 Viscosity of the magma SiO2 — Composition (How much SiO2?) — Temperature 2) Dissolved gases in the magma Dissolved gases
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Magmas vs. Eruptions Peaceful… Explosive! Mafic Felsic SiO2
Temperature ( °C) ( °C) Viscosity
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Low SiO2 magmas = Low gas content = Shield volcanoes
High-SiO2 magmas = High gas content = Composite volcanoes
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Explosivity of volcanoes
VEI Description Plume Height Volume How often Example 0 non-explosive m s m3 daily Kilauea 1 gentle m ,000s m3 daily Stromboli 2 explosive km ,000,000s m3 weekly Galeras, 1992 3 severe km ,000,000s m3 yearly Ruiz, 1985 4 cataclysmic km ,000,000s m 's of years Galunggung, 1982 5 paroxysmal km km 's of years St. Helens, 1980 6 colossal km s km 's of years Krakatau, 1883 7 super-colossal 25 km s km 's of years Tambora, 1815 8 mega-colossal 25 km ,000s km ,000's of years Yellowstone, 2 Ma
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Haleakala, Maui Shield volcano
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Peaceful eruption
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Composite volcanoes — think subduction!
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Volcanism around the globe
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The Tectonic Plates
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Mount St. Helens — Before
Composite volcano
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Explosive volcanism Mount St. Helens — May 18, 1980
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Mount St. Helens — After
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Predicting eruptions Before an eruption, magma moves into the area beneath the volcano and collects in a magma chamber; this magma movement causes changes in the volcano that scientists can measure.
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Predicting eruptions 1. Gas released -
Measure volume and composition 2. Small earthquakes produced Measure with seismometer, look for harmonic tremors 3. Slight swelling of the volcano slope. Measure with tiltmeter, GPS 4. Hydrologic changes
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Seismicity at Mount St. Helens in 1980
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Seismicity at Mt. St. Helens in the last 10 years
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Seismicity and depths of seismicity Mount St
Seismicity and depths of seismicity Mount St. Helens in the last 10 years
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Notice how big these earthquakes are...
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How is seismicity before a volcanic eruption
different from seismicity related to subduction zones?
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How is seismicity before a volcanic eruption
different from seismicity related to subduction zones? They differ in the… • Size (magnitude) of the earthquakes • Location of the hypocenters • Types of seismic waves generated • Cause of the quakes
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Regular, constant shaking related to
Harmonic tremors Examples from Mt. St. Helens Regular, constant shaking related to magma moving underneath a volcano
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Harmonic tremors vs. P- and S-waves
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New lava dome Mount St. Helens February 25, 2005
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Mt. Rainier
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Mt. Ranier The periodic melting of glacier ice from Mt
Mt. Ranier The periodic melting of glacier ice from Mt. Rainier has generated at least 50 major lahars over the past 10,000 years. A major mudflow descends down the White River once every 600 years. More than 300,000 people now live in the area covered by these extensive lahars!
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Lahar or mud flow — One of the deadliest hazards
that occur with snow melt or rain
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Mayon volcano, Philippines
Ash — Most common type of eruption Pyroclastic flows — One of the deadliest hazards
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Mt. Pinatubo — the Philippines — June 1991
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Clark Air Force base before and after — The Philippines 1991
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