Planets: Difference between revisions
→Terrestrial Planets: replaced image (higher quality) |
→Terrestrial Planets: added image (alternate appearance) |
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|''Typically formed in the cooler regions of a star system these worlds have a small metal core and thick rocky mantle with a crust of very deep ice. Geological activity is common in these worlds because of the large quantities of volatiles in the crust, often creating a thin, sometimes seasonal atmosphere.'' | |''Typically formed in the cooler regions of a star system these worlds have a small metal core and thick rocky mantle with a crust of very deep ice. Geological activity is common in these worlds because of the large quantities of volatiles in the crust, often creating a thin, sometimes seasonal atmosphere.'' | ||
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|[[File:High metal content world Wredguia HY-G c24-11 A 1.png|thumb|center]][[File:High-Metal-Content-Planets-180px.png|thumb|center]] | |[[File:High metal content world Wredguia ZF-F d11-23 1.png|thumb|center]][[File:High metal content world Wredguia HY-G c24-11 A 1.png|thumb|center]][[File:High-Metal-Content-Planets-180px.png|thumb|center]] | ||
|High metal content world | |High metal content world | ||
|Common | |Common | ||