No life — too cold for liquid waterMagnetic FieldLow Activity
Why is this a Ice World?Your planet orbits at 3.65 AU from its star, resulting in frigid temperatures of 66K.
Ice worlds form beyond the frost line where temperatures are low enough for water and other volatiles to freeze solid. They may have subsurface oceans beneath thick ice shells.
Classification Criteria:
✓ Distance: 3.65 AU (>3 AU) or Temperature <200K✓ Temperature: 66K✓ Water content: 34.4% for ice formation
Habitability ScoreUninhabitable
11
Contributing Factors
water11
Limited water content - frozen solid, no liquid phase at this temperature
geology60
Some geological activity provides slow nutrient cycling
rotation65
Slow rotation - significant day/night temperature variations, but life can adapt
Organic Chemistry80
Core organic elements (CHNO) present
atmosphere70
Nitrogen atmosphere provides protection but not breathable
temperature10
Frozen world - minimal potential for complex life (strong seasons from a 54° tilt: −5% habitability)
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
0.70x Earth (4.18e+24 kg)
Radius
0.89x Earth (5,657 km)
Surface Gravity
0.89x Earth (8.7 m/s²)
Surface Temperature
66 K (-207 °C / -341 °F)
Rotation Period
55.0 hours/day (slower than Earth)
Orbital Environment
Star Type
M-type (Red Dwarf)
Distance from Star
3.65 AU (546 million km)
Orbital Period
12.7 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
O - Oxygen
31.3%
Si - Silicon
25.0%
N - Nitrogen
12.5%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present