Why is this a Ice World?Your planet orbits at 94.90 AU from its star, resulting in frigid temperatures of 26K.
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: 94.90 AU (>3 AU) or Temperature <200K✓ Temperature: 26K✓ Water content: 30.1% for ice formation
Habitability ScoreUninhabitable
0
Contributing Factors
water20
Good water content - frozen solid, no liquid phase at this temperature
geology30
Geologically dead - no nutrient recycling
rotation60
Fast rotation - strong global wind patterns and weather systems, but manageable
Organic Chemistry100
All CHNOPS elements present - building blocks of life
atmosphere70
Nitrogen atmosphere provides protection but not breathable
temperature0
Near absolute zero - all molecular activity ceases, impossible for life
magnetic Field30
No magnetic field - vulnerable to solar radiation
Physical Properties
Mass
0.30x Earth (1.79e+24 kg)
Radius
0.67x Earth (4,265 km)
Surface Gravity
0.67x Earth (6.6 m/s²)
Surface Temperature
26 K (-247 °C / -412 °F)
Rotation Period
8.0 hours/day (faster than Earth)
Orbital Environment
Star Type
K-type (Orange)
Distance from Star
94.90 AU (14.2 billion km)
Orbital Period
1,105 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
O - Oxygen
24.1%
Si - Silicon
18.1%
C - Carbon
12.0%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present