Jon,<br /><br />That would be possible.<br /><br />I think if Enceladaus had an "off-center" core, then this would create a lot of tidal stress in the ice blanket swaddling the core, especially in the ice antipodal to the center of the core mass offset location, causing a localized warm pocket there. I am still waiting to see a close-pass flyby trajectory analysis to see if Enceldaus' mass distribution is symmetrically uniform, or not. As you may remember, I have been predicting we will find that its mass distribution is substantially asymmetric. So I view the non-observation of sodium as consistent with my proposal.<br /><br />Alternatively, if the source of Enc's water is frictional warming along fissure and fracture lines cause by gravitational tidal stress and perhaps a recent 'flip' sideways, then this warming mechanism also does not require contact with a rocky core, and the water could be sodium free. This mechanism was proposed in a recent paper, as you know. This too is consistent with non-observation of sodium.<br /><br />However, if the source of Enc's internal heat engine is radiogenic, then I would expect the water pocket to be touching exposed rock. In this case, the water pocket should contain sodium. This is inconsistent with observation, decreasing the likelyhood that Enc's internal engine is radiogenic.<br /> <div class="Discussion_UserSignature"> <div class="Discussion_UserSignature" align="center"><em><font color="#0000ff">- - - - - - - - - - - - - - - - - - - - - -</font></em> </div><div class="Discussion_UserSignature" align="center"><font color="#0000ff"><em>I really, really, really miss the "first unread post" function.</em></font> </div> </div>