Volcanoes II
From GeoClasses
Contents |
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Volcanoes
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Anatomy of a volcano
- magma vs. lava
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Ring of Fire around the Pacific
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types of volcanoes
- review of eruptions styles
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shield volcano
- largest volcano, shaped like arc or shield
- usually islands in ocean
- nonexplosive = low SiO2 content in magma
- lava flows down sides = basalt
- may have tephra (ejected volcanic debris = ash, cinders, blocks, bombs)
- tephra forms pyroclastic deposits or rocks
- may create lava tubes underground
- creates a summit caldera - collapse of summit with lava lake inside (Evil Dark Lord)
- examples:
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composite or stratovolcano
- cone shaped
- intermediate SiO2 = more viscous = andesite
- made from alternating layers of explosive tephra and ash and lava flow
- steep slope forms from angle of repose of pyroclastic deposits
- can make horizontal explosions like Mt St Helens
- examples: Mt St Helens, Mt. Rainier, Mt. Fuji in Japan
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volcanic domes
- high SiO2 content = rhyolite
- mostly explosives
- examples:
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cinder cones
- small volcanoes made of tephra (mostly ash and some bombs)
- sometimes found on flanks of larger volcanoes or along fissures
- examples:
- exercise on cinder cones on Earth, the moon, and Mars
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Origins of volcanoes
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Mid-Ocean Ridge
- basalt from asthenosphere
- if MOR occurs on an island then it makes a shield volcano (Iceland)
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hot spots
- areas within a tectonic plate where magma comes to the surface to produce volcanic activity
- can be oceanic or continental
- examples:
- Exercise: use the Hawaian Island and Emperor Seamount Chain to determine plate motion and speed.
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subduction zones
- creates composite volcanoes
- rising magma mixes with oceanic crust (andesite)
- or continental crust (higher SiO2 content = rhyolite)
- creates very explosive eruption, calderas, domes, cinder cones, or composite volcanoes
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calculate the angle of subduction using distance to volcanoes
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Other volcanic features:
- flood basalts - huge horizontal accumulations of basalt lava flows that cover the land (ex: Columbia Plateau in Washington, created 17-14 mya)
- hot springs and geysers - groundwater that is heated by hot rock (ex: Yellowstone)
- caldera explosions - huge eruptions 1000 times the size of Mt St Helens, have not happened in last few 100,000 years (ex: 600,000 years ago, Yellowstone; ex: 700,000 years ago, Long Valley, CA)
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hazards
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lava flows
- 1. pahoehoe - smooth ropy surface, hotter basalt, moves 1 m/hr
- 2. aa - rough blocky surface, cooler more viscous basalt, moves slower - few meters/day
- people have tried many methods to stop lava flows, but mixed success
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pyroclastic (explosive) activity
- ash fall - can cover large expanses with thick blankets
- lateral blasts (horizontal)
- pyroclastic flows - avalanches of hot ash, rock, glass, gas - cannot be outrun
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poisonous gases
more about volcanic emissions
- CO2, CO (toxic), SO2 (toxic), H2S (toxic)
- short term = toxic to breathe; long term = creates acid rain
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debris flows and mud flows
- lahars (Indonesian name): mudflows created when pyroclastics mix with water to make mudslides or lahars
- when volcanic eruptions melt ice and snow, sediment mixed with water
- areas near volcanoes in Cascades (Mt Rainer) are at risk and also Hawaiian Islands
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Predicting eruptions
USGS movie about predicting earthquakes]
- seismic activity (earthquakes)
- underground monitoring
- eruption preceeded by large amount of magma rising to surface - changes temperature (more melting of snow and ice in mountains), hydrologic (groundwater may heat)
- topographic monitoring (land swells as magma moves up)
- volcanic gases (composition and amount of gas escaping changes before eruption)

