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Difference between revisions of "Ross Planetoid"
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− | Smaller than some asteroids, the Ross Planetoid exists at a gravitational sink where ice fragments have collected over the millennia and begun to compact under their own weight into the seed of what might eventually become a planet. Ross presents a unique opportunity for the [[Cambridge Research Institute]] to study planetary formation and extend their | + | Smaller than some asteroids, the Ross Planetoid exists at a gravitational sink where ice fragments have collected over the millennia and begun to compact under their own weight into the seed of what might eventually become a planet. Ross presents a unique opportunity for the [[Cambridge Research Institute]] to study planetary formation and extend their [[Terraforming]] technology. |
[[Category: Bretonia]] | [[Category: Bretonia]] | ||
+ | [[Category: Cambridge]] |
Latest revision as of 11:54, 23 February 2019
Ross Planetoid | |
Location | 5F, Cambridge Bretonia |
Technical information | |
Docking | No |
Terrain | N/A |
Diameter | 200 km |
Mass | 0.66 x 10e20 kg |
Temperature | N/A |
Escape velocity | N/A |
Smaller than some asteroids, the Ross Planetoid exists at a gravitational sink where ice fragments have collected over the millennia and begun to compact under their own weight into the seed of what might eventually become a planet. Ross presents a unique opportunity for the Cambridge Research Institute to study planetary formation and extend their Terraforming technology.