Why is this a Ice World?Your planet orbits at 18.10 AU from its star, resulting in frigid temperatures of 52K.
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: 18.10 AU (>3 AU) or Temperature <200K✓ Temperature: 52K✓ Water content: 62.5% for ice formation
Habitability ScoreUninhabitable
16
Contributing Factors
water22
Abundant water - frozen solid, no liquid phase at this temperature
geology60
Some geological activity provides slow nutrient cycling
rotation100
Optimal rotation period - balanced day/night cycle, moderate weather, and good heat distribution
Organic Chemistry20
Limited organic chemistry potential
atmosphere70
Nitrogen atmosphere provides protection but not breathable
temperature10
Frozen world - minimal potential for complex life
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
1.00x Earth (5.97e+24 kg)
Radius
1.00x Earth (6,371 km)
Surface Gravity
1.00x Earth (9.8 m/s²)
Surface Temperature
52 K (-221 °C / -366 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
K-type (Orange)
Distance from Star
18.10 AU (2.71 billion km)
Orbital Period
92.0 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
O - Oxygen
50.0%
H - Hydrogen
25.0%
Fe - Iron
25.0%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present