Why is this a Ice World?Your planet orbits at 150.00 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: 150.00 AU (>3 AU) or Temperature <200K✓ Temperature: 25K✓ Water content: 42.7% for ice formation
Habitability ScoreUninhabitable
0
Contributing Factors
water60
Water present but mostly frozen
geology60
Some geological activity provides slow nutrient cycling
rotation65
Slow rotation - significant day/night temperature variations, but life can adapt
Organic Chemistry80
Core organic elements (CHNO) present
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
2.90x Earth (1.73e+25 kg)
Radius
1.43x Earth (9,085 km)
Surface Gravity
1.43x Earth (14.0 m/s²)
Surface Temperature
25 K (-248 °C / -415 °F)
Rotation Period
40.0 hours/day (slower than Earth)
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
150.00 AU (22.4 billion km)
Orbital Period
1,837 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
O - Oxygen
35.8%
He - Helium
20.3%
H - Hydrogen
13.8%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present