No life — too cold for liquid waterMagnetic FieldLow Activity
Why is this a Ice World?Your planet orbits at 3.22 AU from its star, resulting in frigid temperatures of 243K.
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: 3.22 AU (>3 AU) or Temperature <200K✓ Temperature: 243K✓ Water content: 32.3% for ice formation
Habitability ScoreMarginal
51
Contributing Factors
water37
Limited water content - mostly frozen
geology60
Some geological activity provides slow nutrient cycling
rotation100
Optimal rotation period - balanced day/night cycle, moderate weather, and good heat distribution
Organic Chemistry100
All CHNOPS elements present - building blocks of life
atmosphere70
Nitrogen atmosphere provides protection but not breathable
temperature40
Extreme temperature - very difficult for life
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
0.90x Earth (5.37e+24 kg)
Radius
0.97x Earth (6,151 km)
Surface Gravity
0.97x Earth (9.5 m/s²)
Surface Temperature
243 K (-30 °C / -23 °F)
Rotation Period
28.0 hours/day (slower than Earth)
Orbital Environment
Star Type
F-type (White)
Distance from Star
3.22 AU (482 million km)
Orbital Period
5.07 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
Si - Silicon
32.3%
O - Oxygen
28.0%
H - Hydrogen
8.6%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present