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Published byCharlotte Hall Modified over 9 years ago
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Generally slow moving Temperature ranges from: ~850°C to 1100°C Flow pattern and direction is predictable Damage: Lots of property damage, little loss of life
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Hot, dense clouds of ash and gases Speeds can easily exceed 100 km/hr Temperatures often >1000°C Unpredictable Generally associated with stratovolcanoes
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Freshly deposited volcanic ash Very unstable when wet Bury towns Chokes drainage systems Ex: Tacoma On top of an ancient mudflow
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Volcanic dust and ash: If in the stratosphere: Affects are global and long-term Affects global temperatures (blocks sunlight) Kratatau, 1883 Tambora, 1815 Pinatubo, 1991 If in the troposphere: Local temperature changes and effects Short-term
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SO2 from gases emitted during the eruption In troposphere: removed as acid rain In stratosphere: stays for years Can circle the globe May cause ozone depletion
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Tsunamis – Earthquakes and land movement Famine Disease Political strife Social, economical, emotional stress Etc.
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