Magma is a complex mixture of liquid, solid and gas

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Transcription:

Magma is a complex mixture of liquid, solid and gas Liquid molten silicate Solid early-formed minerals Gas Generally 0.1% to 5% of the magma by weight, but can be as much as 15% >90% of the gas in magma is water vapor or carbon dioxide Influences viscosity and melting point

Viscosity: how easily a liquid or fluid flows High viscosity: the liquid/fluid flows slowly under an imposed stress Low viscosity: the liquid/fluid flows rapidly under the same imposed stress For example, regular coffee has low viscosity as compared with Silly Putty, which has high viscosity at room temperature and pressure

Magma viscosity varies due to Temperature: hotter magma has lower viscosity Composition: less silica results in lower viscosity Dissolved water content: more dissolved water, lower viscosity Gas bubbles: fewer bubbles, lower viscosity

Origin of Magma Partial melting of the upper mantle produces mafic magmas that crystallize to form mafic rock like basalt and gabbro. Partial melting of the crust tends to produce felsic magmas that crystallize to form felsic rock like rhyolite and granite.

Mafic magmas result in shield volcanoes with broad bases and gentle slopes eruptions that are often spectacular, but are not explosive flows that might extend far beyond the vent or fissure

Felsic magmas result in composite/strata volcanoes with narrow bases and steep slopes eruptions that are often explosive and quite dangerous flows that might not extend past the volcano s flanks

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2003 by Vince Cronin Igneous Rocks and Volcanoes Satellite monitoring of the spread of volcanic sulfur dioxide around Earth after the 1991 eruption of Mt. Pinatubo in the Philippines. NOAA images by Robert Cary

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Small eruption on April 10, 1980. The bulge is in the middle-right of the picture.

USGS volcanologist Dave Johnston using a Correlation Mass Spectrometer to analyze gas emitted by Mt. St. Helens prior to its eruption on May 18, 1980.

Dave Johnston preparing for an aerial gas-sampling mission over Mt. St. Helens

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Dave Johnston resting at Coldwater II on May 17, 1980

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Volcanologist Stan Williams, Arizona State University

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