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Please use this identifier to cite or link to this item: http://hdl.handle.net/2014/28034

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dc.contributor.authorDuxbury, N.S.en_US
dc.contributor.authorBrown, R.H.en_US
dc.date.accessioned2004-10-01T17:26:37Z-
dc.date.available2004-10-01T17:26:37Z-
dc.date.issued1995-03en_US
dc.identifier.citationHouston, TXen_US
dc.identifier.clearanceno95-0073en_US
dc.identifier.urihttp://hdl.handle.net/2014/28034-
dc.description.abstractA mechanism is suggested and modeled whereby there may be boiling geysers on Triton. The geysers would be of nitrogen considering that Voyager detected cryovolcanic activity, that solid nitrogen conducts heat much less than water ice, and that there is internal heat on Triton.en_US
dc.format.extent70548 bytes-
dc.format.mimetypeapplication/pdf-
dc.language.isoen_US-
dc.subject.otherTriton planetary geology geysersen_US
dc.titleThe Plausibility of Boiling Geysers on Tritonen_US
Appears in Collections:JPL TRS 1992+

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