A Sulfur Lava Flow on Mauna Loa
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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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