Why is this a Ice World?Your planet orbits at 47434.20 AU from its star, resulting in frigid temperatures of 25K.
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: 47434.20 AU (>3 AU) or Temperature <200K✓ Temperature: 25K✓ Water content: 51.5% for ice formation
Habitability ScoreUninhabitable
0
Contributing Factors
water22
Abundant water - frozen solid, no liquid phase at this temperature
geology60
Some geological activity provides slow nutrient cycling
rotation10
Near tidally locked - one hemisphere perpetually scorched, other frozen, narrow habitable twilight zone only
Organic Chemistry84
Core organic elements (CHNO) present (tidal pools cycle wet and dry - a boost for prebiotic chemistry)
atmosphere28
Nitrogen atmosphere provides protection but not breathable (partially stripped by slow rotation)
temperature0
Near absolute zero - all molecular activity ceases, impossible for life
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
1.60x Earth (9.56e+24 kg)
Radius
1.17x Earth (7,452 km)
Surface Gravity
1.17x Earth (11.5 m/s²)
Surface Temperature
25 K (-248 °C / -414 °F)
Rotation Period
1.0 hours/day (faster than Earth)
Orbital Environment
Star Type
O-type (Blue Supergiant)
Distance from Star
47434.20 AU (7.1 trillion km)
Orbital Period
1,886,152 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
O - Oxygen
43.0%
H - Hydrogen
16.9%
Si - Silicon
9.6%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present