A Sulfur Lava Flow on Mauna Loa

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v24n1-144-145.pdf (967.2 KB)
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1970-01
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Skinner, Brian J.
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University of Hawai'i Press
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The presence of sulfur crystals formed by condensation around fumarolic vents is a common and widely observed phenomenon in volcanic regions. The flowage of sulfur in a molten state is very rare, however, and is sufficiently unique to suggest a permanent record of its occurrence.
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Skinner BJ. 1970. A sulfur lava flow on Mauna Loa. Pac Sci 24(1): 144-145.
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http://hdl.handle.net/10125/4035
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Pacific Science Volume 24, Number 1, 1970
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