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Volcanoes A Hot Topic
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What is a volcano? A mountain formed by lava and/or pyroclastic material
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Nature of Volcanoes Explosive vs. Effusive (Erupts violently)
(Quiet eruptions)
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Nature of Eruption Controlled by Viscosity
A material’s resistance to flow Factors controlling viscosity: Composition Temperature Dissolved gases
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Factors Controlling Viscosity
Composition ↑ SiO2; ↑ Viscosity ↓ SiO2; ↓ Viscosity Temperature ↑ temperature; ↓ Viscosity Dissolved Gases ↓ pressure; Gases come out of solution How easily gases escape determine eruptive style
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Factors Controlling Viscosity
Basalt Andesite Rhyolite Magma Type Basalt Andesite Rhyolite SiO2 50% 60% 70% Viscosity Low Intermediate High Gas content Explosiveness Nonexistent Explosive
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What is Extruded? Lava Dissolved Gases Pyroclastic Material
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Types of Lava Aa Pahoehoe Rough, jagged surface Higher viscosity
Lower temperature Pahoehoe Smooth, ropy surface Lower viscosity Higher temperature
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Dissolved Gases - Volatiles
H2O steam CO2 Greenhouse gas SO2 “Rotten egg” smell HCl Acid rain
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Pyroclastic Material Ground-hugging avalanche that rushes down the side of a volcano Material consists of: Hot ash Pumice Rock fragments Dust
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Types of Volcanoes Shield Volcanoes Composite Cone (Stratavolcano)
Largest, quiet eruption Composite Cone (Stratavolcano) Most explosive Cinder Cones Small, classic shape
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Shield Volcanoes Broad, gently sloping - “Warrior’s Shield”
Covers large area – lava tubes carry lava great distance Erupts mainly basalt
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Shield Volcano Hawaiian Islands
Mauna Loa, Hawaii
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Composite (Stratovolcano)
Alternating layers of lava and pyroclastic material Large, classic-shaped Associated with subduction zones Multiple eruptions
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Composite Volcano Cascade Ranges
Mount Lassen, California
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Cinder Cones Cone built by cinders – lava fragments
Explosive, but small One eruptive event
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Cinder Cones California
Cima Volcanic Field Amboy Crater
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Deadly Volcanoes Lateral Blasts
An explosion of rock, ash, and gas released at side of volcano May exceed speed of sound St. Pierre, 1902; 29,000 killed
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Deadly Volcanoes Nuée Ardentes
Pyroclastic flow of hot ash and gas Also known as “glowing avalanche” Mt. Pelee is in Martinique. A stratovolcano caused by the subduction of the North American Plate under the Carribean Plate Move at speeds up to 200 km/hr Montserrat, 1996
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Deadly Volcanoes Lahars
Volcanic mudflow Consist of water, rock, ash, and mud May travel >80 km distance at km/hr Nevado del Ruiz, Colombia Causes: In 1985, 23,000 people died Heat melts snow and ice Rainfall eroding loose volcanic debris Landslides of water-saturated debris
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Mount St. Helens, Washington
After During before Lateral Blast
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Mount St. Helens, Washington
Lateral Blast Pyroclastic flow Lahar
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Predicting Eruptions Seismicity Geomorphology Geophysical properties
Ground shaking Geomorphology Changes in ground surface shape Geophysical properties Electrical conductivity, gravity anomaly Gas content ↑SO2
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Mount Pinatubo, Philippines Successful Prediction
Erupted in 1991 Prediction saved 1,000’s of lives Cloud circled entire equator Global temperatures decreased
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