by Chris Peterson » Sat Oct 18, 2008 3:00 pm
orin stepanek wrote:http://apod.nasa.gov/apod/ap081013.html
I know this photo talks about Phoenix passing through Ice plumes but I noticed in the upper right hand corner there seems to be a lack of fissures and the scene seems to have more craters. I'm wondering if this is probably a land mass. Could it be that if this moon was to thaw out that it would be very Earth-like? I know Enceladus it thought to have liquid oceans; but maybe there are continents as well.
Orin
(That should be Cassini, not Phoenix.)
I don't see how anything about Enceladus could be considered "Earth-like". It's only 500 km across (Colorado, where I live, is bigger than that!) I doubt there are any lithic masses near the present surface. The moon is very low density- 1.6 compared with 5.5 for Earth- so a good deal of its volume consists of water. Beneath all that water, there's a silicate core, possibly not even differentiated, but low iron in any case. Assuming the moon is anywhere near hydrostatic equilibrium, there's no way a section of the core could extend 100 km or more up through the ice to the surface.
If Enceladus were to thaw, it would simply go from an icy world to an ocean world, with no dry land.
[quote="orin stepanek"]http://apod.nasa.gov/apod/ap081013.html
I know this photo talks about Phoenix passing through Ice plumes but I noticed in the upper right hand corner there seems to be a lack of fissures and the scene seems to have more craters. I'm wondering if this is probably a land mass. Could it be that if this moon was to thaw out that it would be very Earth-like? I know Enceladus it thought to have liquid oceans; but maybe there are continents as well.
Orin[/quote]
(That should be Cassini, not Phoenix.)
I don't see how anything about Enceladus could be considered "Earth-like". It's only 500 km across (Colorado, where I live, is bigger than that!) I doubt there are any lithic masses near the present surface. The moon is very low density- 1.6 compared with 5.5 for Earth- so a good deal of its volume consists of water. Beneath all that water, there's a silicate core, possibly not even differentiated, but low iron in any case. Assuming the moon is anywhere near hydrostatic equilibrium, there's no way a section of the core could extend 100 km or more up through the ice to the surface.
If Enceladus were to thaw, it would simply go from an icy world to an ocean world, with no dry land.