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dc.contributor.author Cox, Malcolm E. en_US
dc.date.accessioned 2011-08-30T00:16:47Z en_US
dc.date.accessioned 2011-09-29T20:11:13Z en_US
dc.date.available 2011-08-30T00:16:47Z en_US
dc.date.available 2011-09-29T20:11:13Z en_US
dc.date.issued 1980 en_US
dc.identifier.citation Cox ME. 1980. Ground radon survey of a geothermal area in Hawaii. Geophys. Res. Lett. 7(4): 283-286. en_US
dc.identifier.uri http://hdl.handle.net/10125/21043 en_US
dc.description.abstract Rates of ground radon emanation, in the Puna geothermal area on the lower east rift of Kilauea volcano, were measured by alpha particle sensitive cellulose nitrate films. The survey successfully defined an area of thermal significance associated with the rift structure, and suggests that a thermally driven ground gas convection system exists within, and peripheral to, the rift. This type of survey was found suitable for the basaltic island environment characteristic of Hawaii and is now used in Hawaii as a routine geothermal exploration. en_US
dc.description.sponsorship Department of Energy Contract No. EW-78-S-07-0713. en_US
dc.format.extent 4 p. en_US
dc.language.iso en-US en_US
dc.publisher American Geophysical Union en_US
dc.relation.ispartofseries Hawaii Institute of Geophysics Contribution No. 988 en_US
dc.subject geothermal. Exploration en_US
dc.subject radon en_US
dc.subject.lcsh Radon en_US
dc.subject.lcsh Geothermal resources--Hawaii en_US
dc.title Ground Radon Survey of a Geothermal Area in Hawaii (Publication) en_US
dc.type Article en_US
dc.type.dcmi Text en_US

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