Why is this a Ice World?Your planet orbits at 1914.80 AU from its star, resulting in frigid temperatures of 113K.
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: 1914.80 AU (>3 AU) or Temperature <200K✓ Temperature: 113K✓ Water content: 47.6% for ice formation
Habitability ScoreExtremely Harsh
20
Contributing Factors
water22
Abundant water - 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 Chemistry20
Limited organic chemistry potential
atmosphere70
Nitrogen atmosphere provides protection but not breathable
temperature20
Very cold - water frozen, challenging for 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
113 K (-160 °C / -256 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
O-type (Blue Supergiant)
Distance from Star
1914.80 AU (286 billion km)
Orbital Period
15,298 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
O - Oxygen
38.1%
He - Helium
28.6%
H - Hydrogen
19.0%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present