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Sudden Earth Events VOLCANOES
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Where are Volcanos Found?
What is a Volcano? Opening in Earth’s crust that releases solid rock, magma, steam & ash May be active (erupting) or dormant (no occurring eruption) or extinct Ring of Fire Formed by edges of Pacific plate Where are Volcanos Found?
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Reasons Volcanoes Form
SUBDUCTION ZONES Result of converging plates One plate is pushed downward & melts Magma is eventually forced through an opening
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Mount Vesuvius
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PLUMES Result of diverging plates Rising magma leaks into the crust Can form new islands on the surface
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Types of Volcanoes Based on Thickness of magma Amount of gas
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Types of Volcanoes Strato Steep sides & high peaks Thick magma
Strato Steep sides & high peaks Thick magma Large amounts of gas (usually) Violent eruptions Ex. Mount Vesuvius (Italy) Mount St. Helens (US)
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2. Cinder cone Steep sides, shorter peaks Cylindrical shape Magma is less thick High amounts of gas Generally harmless eruptions Ex. Stromboli (Italy), Paricutin (Mexico)
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Shield volcano Largest volcanoes Broad, gentle sloping sides Usually build up from the sea floor Runny magma High or low amounts of gas Ex. Mauna Loa (Hawaii)
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Effects of Volcanos Lava Ash Fragments of rock less than 2mm in size
Lahars Mudflows formed from ash, debris and water
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Avalanches & landslides
Pyroclastic flows Mixture of hot gas, ash, and other rocks travelling very quickly down the slopes
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Mount St. Helens Back from the Dead
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Monitoring a Volcano 1. Shape of Volcano Tilt Crack openings
2. Seismicity The frequency, magnitude, location, and type of earthquakes
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3. Gas Geochemistry Gas samples are collected from active vents Gases include carbon dioxide and sulfur dioxide Composition of the gas Rate of gas emission
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4. Geology 5. Hydrologic Regime Lava & rock samples
Changes in ground water Temperature Level Rates of streamflow Stream & ice accumulation
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