Planet (Lava)
So-called "lava planets" (properly "magmatic planets") fall into one of three groups: solar magmatics, which orbit sufficiently close to their star that the surface never cools enough to solidify; gravitational magmatics, which experience gravitational shifts sufficiently strong to regularly and significantly fracture cooling crusts; and magmatoids, which are for largely-unexplained reasons simply incapable of cooling and forming a persistent crust. All three types generally exhibit the same external phenomena - huge red-orange lava fields being a defining feature - but the latter two types are sometimes capable of briefly solidifying for a period measured in years or perhaps decades.
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Astronautic
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Cargo capacity | 0 m3 |
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Mass | 99,999,999,999,999,996,863,366,107,917,975,552 kg |
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Volume | 1 m3 |
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Baseprice | 0 ISK |