Planet LHS 3802 2 a
Icy body
Overview
| System: | LHS 3802 - All bodies | |
| Distance to Sol: | 62.45 ly | |
| Distance To Arrival: | 1,373 ls | |
| Is Landable: | Yes | |
| Terraforming: | Not terraformable | |
| Earth Masses: | 0.0013 | |
| Radius: | 952 KM | |
| Gravity: | 0.06 G | |
| Surface Temperature: | 46 K | |
| Volcanism: | Carbon dioxide geysers | |
| Atmosphere: | No atmosphere | |
| Orbital Period: | 3.2 D | |
| Semi Major Axis: | 0.00 AU | |
| Orbital Eccentricity: | 0.0012 | |
| Orbital Inclination: | -0.00 ° | |
| Arg Of Periapsis: | 194.60 ° | |
| Rotational Period: | 3.2 D - Tidally locked | |
| Axis Tilt: | -0.37 ° | |
| Materials: |
Sulphur (27.1%)
Carbon (22.8%)
Phosphorus (14.6%)
Iron (12.1%)
Nickel (9.1%)
Chromium (5.4%)
Manganese (5.0%)
Arsenic (1.6%)
Tellurium (0.9%)
Molybdenum (0.8%)
Tin (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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