Planet LHS 3802 2 d
Icy body
Overview
| System: | LHS 3802 - All bodies | |
| Distance to Sol: | 62.45 ly | |
| Distance To Arrival: | 1,372 ls | |
| Is Landable: | Yes | |
| Terraforming: | Not terraformable | |
| Earth Masses: | 0.0017 | |
| Radius: | 1,054 KM | |
| Gravity: | 0.06 G | |
| Surface Temperature: | 45 K | |
| Volcanism: | No volcanism | |
| Atmosphere: | No atmosphere | |
| Orbital Period: | 37.8 D | |
| Semi Major Axis: | 0.01 AU | |
| Orbital Eccentricity: | 0.0004 | |
| Orbital Inclination: | 0.20 ° | |
| Arg Of Periapsis: | 40.44 ° | |
| Rotational Period: | 37.8 D - Tidally locked | |
| Axis Tilt: | -0.24 ° | |
| Materials: |
Sulphur (27.0%)
Carbon (22.7%)
Phosphorus (14.5%)
Iron (12.0%)
Nickel (9.1%)
Chromium (5.4%)
Germanium (3.5%)
Zinc (3.3%)
Cadmium (0.9%)
Niobium (0.8%)
Ruthenium (0.7%)
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Ice world composed mainly of water ice. Worlds like this will not have had much heating in the past, forming in the cooler regions of a star system and have retained many volatiles as solids in their crust.
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