Volcanoes II

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Contents

Volcanoes

Anatomy of a volcano

anatomy of a volcano
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anatomy of a volcano
  • magma vs. lava

Ring of Fire around the Pacific

map of subduction zones in the Ring of Fire
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map of subduction zones in the Ring of Fire


types of volcanoes

  • review of eruptions styles

shield volcano

example of shield volcano (Skjaldbreidur)
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example of shield volcano (Skjaldbreidur)
  • 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:


composite or stratovolcano

cutaway drawing of a stratovolcano
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cutaway drawing of a 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


volcanic domes

  • high SiO2 content = rhyolite
  • mostly explosives
  • examples:


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


Origins of volcanoes

Mid-Ocean Ridge

  • basalt from asthenosphere
  • if MOR occurs on an island then it makes a shield volcano (Iceland)


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.


subduction zones

cartoon of the basic plate boundaries
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cartoon of the basic plate boundaries
  • 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

calculate the angle of subduction using distance to volcanoes


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)


hazards

lava flows

lava flow destroying house in Hawaii
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lava flow destroying house in Hawaii
  • 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


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


poisonous gases

more about volcanic emissions

  • CO2, CO (toxic), SO2 (toxic), H2S (toxic)
  • short term = toxic to breathe; long term = creates acid rain

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

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)
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