Why is this a Ice World?Your planet orbits at 30.70 AU from its star, resulting in frigid temperatures of 57K.
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: 30.70 AU (>3 AU) or Temperature <200K✓ Temperature: 57K✓ Water content: 64.5% for ice formation
Habitability ScoreUninhabitable
19
Contributing Factors
water22
Abundant water - frozen solid, no liquid phase at this temperature
geology60
Some geological activity provides slow nutrient cycling
rotation100
Optimal rotation period - balanced day/night cycle, moderate weather, and good heat distribution
Organic Chemistry80
Core organic elements (CHNO) present
atmosphere70
Nitrogen atmosphere provides protection but not breathable
temperature10
Frozen world - minimal potential for complex life
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
1.40x Earth (8.36e+24 kg)
Radius
1.12x Earth (7,127 km)
Surface Gravity
1.12x Earth (11.0 m/s²)
Surface Temperature
57 K (-216 °C / -357 °F)
Rotation Period
16.0 hours/day (faster than Earth)
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
30.70 AU (4.59 billion km)
Orbital Period
170.1 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
H - Hydrogen
43.0%
O - Oxygen
43.0%
He - Helium
10.2%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present