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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: – Temperature – Composition – Dissolved gases
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Factors Controlling Viscosity Composition – ↑ SiO 2 ; ↑ Viscosity – ↓ SiO 2 ; ↓ 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 Magma TypeBasaltAndesiteRhyolite SiO 2 50%60%70% Viscosity LowIntermediateHigh Gas content LowIntermediateHigh Explosiveness NonexistentIntermediateExplosive Basalt Andesite Rhyolite
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What is Extruded? Lava Dissolved Gases Pyroclastic Material
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Types of Lava Aa Pahoehoe – Smooth, ropy surface – Rough, jagged surface – Higher viscosity – Lower temperature – Lower viscosity – Higher temperature
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Dissolved Gases - Volatiles H 2 O CO 2 SO 2 HCl – steam – Greenhouse gas – “Rotten egg” smell – 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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Volcano Anatomy Vent –Opening near surface Crater –Steep-walled depression Conduit –Narrow pipe Magma Chamber –Stored magma
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Types of Volcanoes –Mauna Loa – the largest volcano in Hawaii –Compare Mauna Loa with Mt. Rainier –May be found on the flanks of shield and composite cones Shield Volcanoes Composite Cone (Stratovolcanoes) Cinder Cone
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Shield Volcanoes Broad, gently sloping - “Warrior’s Shield” Covers large area Erupts mainly basalt in a relatively quiet eruption
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Shield Volcano Hawaiian Islands Mauna Loa, Hawaii
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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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Composite (Stratovolcano) Associated with subduction zones Large, classic-shaped Alternating layers of lava and pyroclastic material Violent eruptions
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Composite Volcano Cascade Ranges Mount Lassen, California
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Deadly Volcanoes Nuée Ardentes Pyroclastic flow of hot ash and gas Also known as “glowing avalanche” Move at speeds up to 200 km/hr Montserrat, 1996
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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 Lahars Causes: Volcanic mudflow – Heat melts snow and ice – Rainfall eroding loose volcanic debris – Landslides of water-saturated debris – Consist of water, rock, ash, and mud – May travel >80 km distance at 35-60 km/hr Nevado del Ruiz, Colombia In 1985, 23,000 people died
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Mount St. Helens, Washington Lateral Blast before During After
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Mount St. Helens, Washington Lateral Blast Pyroclastic flow Lahar
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Predicting Eruptions Seismicity Geomorphology Gas content Geophysical properties – Ground shaking – Changes in ground surface shape – Electrical conductivity, gravity anomaly –↑SO 2
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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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