Kriovulkaan

'n Kriovulkaan (soms 'n ysvulkaan genoem) is 'n soort vulkaan wat vlugtige stowwe soos water, ammoniak of metaan by of onder hulle vriespunt in 'n ekstreme omgewing uitbars. Dit is basies die soort vulkanisme wat op aarde gesien word, met vloeistof en bevrore vlugtige stowwe as geologiese allegorieë van respektiewelik gesmelte en soliede rots.^[2]

↑ Lopes, R.M.C.; Kirk, R. L.; Mitchell, K. L.; LeGall, A.; Barnes, J. W. (19 Maart 2013). "Cryovolcanism on Titan: New results from Cassini RADAR and VIMS" (PDF). Journal of Geophysical Research: Planets. 118 (3): 416–435. Bibcode:2013JGRE..118..416L. doi:10.1002/jgre.20062.
↑ Darling, David (red.). "Cryovolcanism". Internet Encyclopedia of Science.

[Lopes_2013-1] Lopes, R.M.C.; Kirk, R. L.; Mitchell, K. L.; LeGall, A.; Barnes, J. W. (19 Maart 2013). "Cryovolcanism on Titan: New results from Cassini RADAR and VIMS" (PDF). Journal of Geophysical Research: Planets. 118 (3): 416–435. Bibcode:2013JGRE..118..416L. doi:10.1002/jgre.20062.

[IES-Cryovolcanism-2] Darling, David (red.). "Cryovolcanism". Internet Encyclopedia of Science.

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