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Valena Berry and Rachel Valena Berry and Rachel Kenney
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Southern Chilean Andres, South America 6.21 miles NE of the town of Chaitén on the Gulf of Corcovado
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Elliptical Caldera: 1.55 x 2.49 miles wide Summit Elevation: 3,681 Ft. Last eruption: 9,400 yrs ago.
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Ash plume rose over 13.05 miles in altitude and drifted SSE. Lightning storm with eruption. Dubbed a ‘Dirty Thunderstorm’. Ashfall continued to occur daily in large plumes through to the 6 th of May.
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May 2 nd : Government declared state of emergency and evacuated several hundred people from the town of Chaitén 6.21 miles SE of the volcano. May 3 rd through the 6 th : reported 4,000 to 5,000 people evacuated from Chaitén and surrounding area. May 5 th : evacuation of Futaleufú, 40.4 miles ESE, took place. ~11.81 inches of ash had accumulated. One elderly person died during the evacuation.
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A new lava dorm growth on the large one within the caldera. 24 th of May, observation of a vigorous explosion from the old dome and the new dome overtakes it in height. Ash plumes continue to rise, but only 1.86 to 3.11 miles in height.
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Early in the month, ash and steam plumes rose to 4.35 miles in altitude. 6,200 acres of forest to the N and NE sides burned by pyroclastic flows and lateral explosions.
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Ash plumes remain at 1.86 miles in altitude. Lahars overtake drainages during June 27 th and 28 th, especially in the Chaitén and Amarrillo rivers.
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Agriculture Impacts Main concerns: Lahars and Tephra Farm Land Area Affected: Effects: Good and Bad Livestock Death: Livestock buried in pastures Skin Fungal infections Accelerated wear on teeth and gums Government provided farm-recovery funds
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Structural Damage Urban and Rural Communities: Individual town: Futeleufú 300mm ash (11.81 inches) Disrupted water, electricity, transportation, and telecommunication. Residential/commercial damage: Gutters Roof cladding corrosion Structural roof damage Internal ash contamination Hydro-electric dams Bridges destroyed by lahars Aviation Mass flight cancellations Closed airports Ash in airspace weeks after Turbine damage
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Volcanic Lightning Storm: How do they form? A “shear layer” of intense horizontal winds and “updraught” from the volcano create multiple vortices that counter-rotate. Eddies form inside, because of instability Expanding umbrella becomes cooler on the outside and denser than the surrounding air Supercells form within the updraught as well as precipitation Fun Fact: Miller experiment Faulting: Sitting on an active secondary fault Mostly strike-slip faulting Possibly the cause of the eruption
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Continuing Activity by August 2008: 120 m Lava dome Earthquakes at summit Boulders avalanching into crater Volcano degassing/ash
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