Editing Talk:2775: Siphon
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:::In order for accumulating ores to not just start a low-level fizzle (as above), over millenia, you might need separate ore-patches either side of a fault to come together in a suddenish techtonic slip, rather than a slow buckling of layers to increase effective ore-densities. And then you've got earthquakes, already, so not sure if the very low-grade nuclear explosion that is awfully close to being possible in this chance contrived example (at one end of the probability curve, unless U<sup>238</sup> content is somehow preferentially leached out?) is going to be noticable. | :::In order for accumulating ores to not just start a low-level fizzle (as above), over millenia, you might need separate ore-patches either side of a fault to come together in a suddenish techtonic slip, rather than a slow buckling of layers to increase effective ore-densities. And then you've got earthquakes, already, so not sure if the very low-grade nuclear explosion that is awfully close to being possible in this chance contrived example (at one end of the probability curve, unless U<sup>238</sup> content is somehow preferentially leached out?) is going to be noticable. | ||
:::But ''just'' hot enough for lava? If not already close to melting, anyway, under local temperatures and pressures? Not sure we've seen anything like it, even if it is technically feasible given enough happenstance setups by geology(/exo-geology), since planets formed. [[Special:Contributions/172.70.91.152|172.70.91.152]] 09:16, 14 May 2023 (UTC) | :::But ''just'' hot enough for lava? If not already close to melting, anyway, under local temperatures and pressures? Not sure we've seen anything like it, even if it is technically feasible given enough happenstance setups by geology(/exo-geology), since planets formed. [[Special:Contributions/172.70.91.152|172.70.91.152]] 09:16, 14 May 2023 (UTC) | ||
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== Title Text-Radiation == | == Title Text-Radiation == |