Why is this a Ice World?Your planet orbits at 162.10 AU from its star, resulting in frigid temperatures of 235K.
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: 162.10 AU (>3 AU) or Temperature <200K✓ Temperature: 235K✓ Water content: 50.0% for ice formation
Habitability ScoreHabitable
64
Contributing Factors
water68
Abundant water - mostly frozen
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
temperature40
Extreme temperature - very difficult for life
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
1.20x Earth (7.17e+24 kg)
Radius
1.06x Earth (6,770 km)
Surface Gravity
1.06x Earth (10.4 m/s²)
Surface Temperature
235 K (-38 °C / -37 °F)
Rotation Period
20.0 hours/day (faster than Earth)
Orbital Environment
Star Type
B-type (Blue Giant)
Distance from Star
162.10 AU (24.2 billion km)
Orbital Period
652.6 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
O - Oxygen
41.2%
H - Hydrogen
17.6%
N - Nitrogen
11.8%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present