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Today – 4/13. More volcanoes!. First Mars shot - hill. Matian basalt. Martian dune field. Frozen Martian Sea. Last Time. Hotspots – mantle plumes reach the surface; decompression melting to form basaltic magma; Hawaii, Mars, Venus; independent of plate boundaries
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Today – 4/13 • More volcanoes!
Last Time • Hotspots – mantle plumes reach the surface; decompression melting to form basaltic magma; Hawaii, Mars, Venus; independent of plate boundaries • Intrusive v. extrusive: coarse v. fine texture depends on cooling rate • Three kinds of volcano: shield, stratovolcano, caldera – depends on magma type
Last Time – Shield Volcano • Built up from repeated basalt flows • Basalt has high Fe / Mg, high temperature, low Si, low gas content, low viscosity (stickiness) • MOR’s, hotspots, areas of continental extension
Stratovolcano • Built from alternating layers of pyroclastic & andesite lava flows • Magma – intermediate temperature, gas content, composition, viscosity • St. Helens, Monserrat, Pinatubo, Tambora • Form above subduction zones • Wet melting of the mantle
Mount Ngauruhoe, New Zealand Classic Stratovolcano --- 1000s of feet high.
PyroclasticFlows- - - - - MayonPhilippines1968- - - - -Hot: 600oCFast: 60 to 100 mph
Cascade Volcanic Arc-----Lassen PeakCrater Lake Mt.St.Helens Mt. Rainier- - - -Part of Pacific Ring of Fire.
Mt. Saint Helens, May, 1980 Eruption After Before
Mount St. Helens Volcanocam • http://www.fs.fed.us/gpnf/volcanocams/msh/
Space Needle view Seattle, WA and Mount Rainier:Most dangerous volcano in North America?
Volcanoes – Agents of Climate Change Mount Pinatubo, Philippines 1991
Mt. Pinatubo Ash Circles the Earth Earth’s surface cooled 1 °F for two years.
Climatic Effects of Volcanism • Volcanic particles in stratosphere interact with man-made CFC’s to destroy ozone. Particles settle out in 2-3 years, ozone layer recovers. • Volcanoes add CO2 to the atmosphere (10% of anthropogenic emissions), contributing to long-term global warming • SO2 in the stratosphere reacts with water to form sulfuric acid, which absorbs solar energy and re-radiates it into space, creating short term cooling. Sulfuric acid droplets settle out after several years
Tambora, April 1815 • Largest stratovolcano eruption in recorded history • 1816 – year without a summer. June snow in New England, frost in July and August. Crop failure – oats from 12 cents to 92 cents. Settlers move to midwest, Mary Shelley writes Frankenstein. Famine in Europe.
Caldera Explosions • Caldera – LARGE volcanic crater caused by the collapse of a magma chamber after a big eruption • Convergent margins, hotspots under continents • Wet melting of the continental crust • Inconceivably cataclysmic • Often called “supervolcanoes” • Magma – low temperature, high gas content, high viscosity, high silica content = HIGHLY explosive
CalderasOften formed by explosive eruption. Crater Lake fills caldera formed by collapse during massive eruption of Mt. Mazama 6600 years ago.
Caldera Formation Eruption Collapse Figure 7.12: Sequence of events in the formation of Crater Lake.
Last Big One – 74 Ka, Toba, Sumatra • 2,800 cubic kilometers of material ejected • Cause of the human genetic bottleneck?
Long Valley Caldera, California - A very dangerous volcanohttp://quake.wr.usgs.gov/recenteqs/Maps/Long_Valley.html Left: Cross section of Long Valley Caldera. Right: Lasers monitor ground swelling at Long Valley Caldera
Yellowstone Hotspot Volcanoes Go to the Movie
Internal Heat Generation Earth • Remnant heat from formation, much of which is stored in the liquid core • Decay of radioactive elements Satellites of large planets • Gravitational energy turned into heat – “tidal friction”
Io v. Titan • Io – moon of Jupiter • Sulfur / silicate magma • Titan – moon of Saturn • Ammonia-water solution magma
Igneous Rock Bodies Small ones • Sill – horizontal tabular body • Dike – vertical tabular body • Volcanic neck – pipelike remains of a vent Big ones • Pluton – large igneous intrusion • Batholith – really large igneous intrusion
Igneous Rock Bodies Figure 7.15 on page 148 of The Blue Planet
Igneous intrusive landforms Plutons and Batholiths: Large igneous intrusive rock bodies. Crystallized deep within crust. Exposed by uplift and erosion.
Igneous intrusive rocks formed close to surface: Dikes, Sills, Volcanic Necks Sills Volcanic Necks Dikes
Beneficial Aspects of Volcanoes • Outgassing formed oceans, atmosphere • Ash produces rich, fertile soil • Mineral deposits • Geothermal energy • Beautiful sunsets!
Geyser, New Zealand Water circulates through cooling magma bodies.
Hot brines deposit minerals with copper, lead, zinc, gold, silver.
Gold & Quartz Veins gold Deposited in fractures by hot water (50 to 200 oC). quartz
Volcanic Hazards • Ash falls – choke people, animals, kill animals that eat it, collapse roofs – worsened by rain • Pyroclastic flows – suffocation and burning, knock over anything in their way • Mudflows (lahars) – ice and snow melt, rain on ash flow • Volcanic landslide • Lava flow • Poisonous gas emission – Lake Nyos in Cameroon, 1700 CO2 suffocation deaths http://perso.wanadoo.fr/mhalb/nyos/webcam.htm
Igneous Rocks Tell Their Story • Just as sedimentary strata record the environments of their deposition, igneous rock bodies and layers record the history of magmatism and volcanism in and on the Earth. Rock types and rock distribution tell what kind of activity occurred and radioisotopic dating tells when