Editing Talk:2775: Siphon

Jump to: navigation, search
Ambox notice.png Please sign your posts with ~~~~

Warning: You are not logged in. Your IP address will be publicly visible if you make any edits. If you log in or create an account, your edits will be attributed to your username, along with other benefits.

The edit can be undone. Please check the comparison below to verify that this is what you want to do, and then save the changes below to finish undoing the edit.
Latest revision Your text
Line 39: Line 39:
 
:::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)
βˆ’
::::Any sufficiently large rock containing sufficiently high concentrations of radioactive materials (such as the Earth) will partially melt.  The energy is released slowly by decay not through fission.  The large size ensures that the center is well enough insulate that slow heating accumulates until it reaches lava temperatures.  The finite size ensures that enough heat leaks out that the magma does not become gas.[[Special:Contributions/162.158.158.170|162.158.158.170]] 18:29, 16 May 2023 (UTC)
 
  
 
== Title Text-Radiation ==
 
== Title Text-Radiation ==

Please note that all contributions to explain xkcd may be edited, altered, or removed by other contributors. If you do not want your writing to be edited mercilessly, then do not submit it here.
You are also promising us that you wrote this yourself, or copied it from a public domain or similar free resource (see explain xkcd:Copyrights for details). Do not submit copyrighted work without permission!

To protect the wiki against automated edit spam, we kindly ask you to solve the following CAPTCHA:

Cancel | Editing help (opens in new window)

Template used on this page: