Why is this a Ice World?Your planet orbits at 23.90 AU from its star, resulting in frigid temperatures of 61K.
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: 23.90 AU (>3 AU) or Temperature <200K✓ Temperature: 61K✓ Water content: 40.4% for ice formation
Habitability ScoreUninhabitable
17
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 Chemistry50
Carbon and hydrogen present - organic chemistry possible
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
1.80x Earth (1.07e+25 kg)
Radius
1.22x Earth (7,750 km)
Surface Gravity
1.22x Earth (11.9 m/s²)
Surface Temperature
61 K (-212 °C / -349 °F)
Rotation Period
25.0 hours/day (slower than Earth)
Orbital Environment
Star Type
K-type (Orange)
Distance from Star
23.90 AU (3.58 billion km)
Orbital Period
139.7 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
O - Oxygen
31.9%
Fe - Iron
17.7%
H - Hydrogen
17.0%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present