Why is this a Ice World?Your planet orbits at 58.40 AU from its star, resulting in frigid temperatures of 40K.
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: 58.40 AU (>3 AU) or Temperature <200K✓ Temperature: 40K✓ Water content: 45.9% 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
rotation65
Slow rotation - significant day/night temperature variations, but life can adapt
Organic Chemistry84
Core organic elements (CHNO) present (tidal pools cycle wet and dry - a boost for prebiotic chemistry)
atmosphere70
Nitrogen atmosphere provides protection but not breathable
temperature0
Near absolute zero - all molecular activity ceases, impossible for life
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
0.70x Earth (4.18e+24 kg)
Radius
0.89x Earth (5,657 km)
Surface Gravity
0.89x Earth (8.7 m/s²)
Surface Temperature
40 K (-234 °C / -388 °F)
Rotation Period
18.0 hours/day (faster than Earth)
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
58.40 AU (8.74 billion km)
Orbital Period
446.3 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
O - Oxygen
32.0%
H - Hydrogen
27.8%
Si - Silicon
15.5%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present