A Sulfur Lava Flow on Mauna Loa

Item Description

dc.contributor.author	Skinner, Brian J	en_US
dc.date.accessioned	2008-11-25T05:44:12Z	en_US
dc.date.available	2008-11-25T05:44:12Z	en_US
dc.date.issued	1970-01	en_US
dc.identifier.citation	Skinner BJ. 1970. A sulfur lava flow on Mauna Loa. Pac Sci 24(1): 144-145.	en_US
dc.identifier.issn	0030-8870	en_US
dc.identifier.uri	http://hdl.handle.net/10125/4035	en_US
dc.description.abstract	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.	en_US
dc.language.iso	en-US	en_US
dc.publisher	University of Hawai'i Press	en_US
dc.title	A Sulfur Lava Flow on Mauna Loa	en_US
dc.type	Article	en_US
dc.type.dcmi	Text	en_US