This is an old revision of this page, as edited by Henrygb (talk | contribs) at 01:50, 23 February 2005 (merged info from Cryovolcanoes - not checked). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.
Revision as of 01:50, 23 February 2005 by Henrygb (talk | contribs) (merged info from Cryovolcanoes - not checked)(diff) ← Previous revision | Latest revision (diff) | Newer revision → (diff)Cryovolcanoes are pseudo-volcanoes believed to be present on Titan, the largest moon of Saturn. Unlike volcanoes on Earth which spew hot lava, cryvolcanoes bring super-cool "lava" to the surface of their planets. They are volcanic-like vents that spew forth ice, water or vapor-phase volatiles, with some gas driven solid fragments instead of lava. It is suggetsed that they could be present on Titan, one of Saturn's moons. However it has only been seen on Triton, the biggest of Neptune's moons. Also it is said that they might be active in Europa and Enceladus.
This term was coined by NASA in late 2004, when the Cassini space probe observed cryvolcanoes and cryogenic lakes for the first time.