Planet Flousop A 4
Rocky ice world
Overview
| System: | Flousop - All bodies | |
| Distance to Sol: | 17.36 ly | |
| Distance To Arrival: | 24 ls | |
| Is Landable: | Yes | |
| Terraforming: | Not terraformable | |
| Earth Masses: | 0.0066 | |
| Radius: | 1,410 KM | |
| Gravity: | 0.14 G | |
| Surface Temperature: | 132 K | |
| Volcanism: | Iron magma | |
| Atmosphere: | No atmosphere | |
| Orbital Period: | 0.8 D | |
| Semi Major Axis: | 0.00 AU | |
| Orbital Eccentricity: | 0.0350 | |
| Orbital Inclination: | -5.05 ° | |
| Arg Of Periapsis: | 31.28 ° | |
| Rotational Period: | 1.0 D - Tidally locked | |
| Axis Tilt: | -0.41 ° | |
| Materials: |
Sulphur (19.8%)
Iron (18.7%)
Carbon (16.6%)
Nickel (14.1%)
Phosphorus (10.6%)
Manganese (7.7%)
Zinc (5.1%)
Vanadium (4.6%)
Molybdenum (1.2%)
Tungsten (1.0%)
Polonium (0.5%)
|
|
| Stations: |
|
|
| Attractions: |
|
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.
View
Advertisement