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If tidal and radiogenic heating were switched off, how long would each ocean survive against its own ice shell? A Stefan-type freezing calculation gives 0.08093 billion years for a 100-kilometre Europan ocean, 0.00566 billion years for a 30-kilometre Enceladus ocean and 0.6861 billion years for a 300-kilometre Titan ocean, with initial freezing rates through a 20-kilometre shell of 3.089, 3.974 and 3.279 millimetres per year respectively. Every timescale is far shorter than the age of the solar system: no ocean in this set is a passive fossil, and each present-day ocean certifies sustained heating over geological time. Enceladus is the extreme case, its ocean freezing in a few million years unheated. Computed from stated assumptions, not measured.
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William Alexander Aldred (2026) studied this question.
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