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Difference between revisions of "La Trinite"

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(Created page with "{{Version|4.88.0.0}} {{Planet Infobox | name = La Trinite | image = | owner = | system = Provence | sector = 4G | house = {{House Link | Gallia}} | population = | docki...")
 
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{{Planet Infobox
 
| name = La Trinite
 
| name = La Trinite
| image =  
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| image = La Trinite.jpg
 
| owner =  
 
| owner =  
 
| system = [[Provence]]
 
| system = [[Provence]]
 
| sector = 4G
 
| sector = 4G
| house = {{House Link | Gallia}}
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| house = [[Border Worlds]]
 
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| docking = No
 
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La Trinite is the largest and heaviest moon of [[Planet Nice]]. Its crust consists of water ice and rock in near equal proportions, although rock outcrops on the surface are quite rare. La Trinite has a thin atmosphere that has resulted from evaporation of nitrogen from the moon's surface. It mostly consists of nitrogen and helium. The core of the moon is still surprisingly hot, and internal heat allows its surface temperature to rise as high as -100°C or even higher in polar regions.
 
La Trinite is the largest and heaviest moon of [[Planet Nice]]. Its crust consists of water ice and rock in near equal proportions, although rock outcrops on the surface are quite rare. La Trinite has a thin atmosphere that has resulted from evaporation of nitrogen from the moon's surface. It mostly consists of nitrogen and helium. The core of the moon is still surprisingly hot, and internal heat allows its surface temperature to rise as high as -100°C or even higher in polar regions.
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[[Category: Border Worlds]]
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[[Category: Provence]]

Latest revision as of 10:58, 16 February 2019

La Trinite
La Trinite.jpg
Location 4G, Provence
Border Worlds
Technical information
Docking No
Terrain Ice
Diameter 6,711 km
Mass 1.05 x 10e24 kg
Temperature -210°C to -94°C
Escape velocity 6.71 km/sec

La Trinite is the largest and heaviest moon of Planet Nice. Its crust consists of water ice and rock in near equal proportions, although rock outcrops on the surface are quite rare. La Trinite has a thin atmosphere that has resulted from evaporation of nitrogen from the moon's surface. It mostly consists of nitrogen and helium. The core of the moon is still surprisingly hot, and internal heat allows its surface temperature to rise as high as -100°C or even higher in polar regions.