Why is this a Ice World?Your planet orbits at 1.10 AU from its star, resulting in frigid temperatures of 211K.
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: 1.10 AU (>3 AU) or Temperature <200K✓ Temperature: 211K✓ Water content: 58.9% for ice formation
Habitability ScoreHabitable
72
Contributing Factors
water53
Water present but mostly frozen (low gravity lets water escape to space)
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
0.60x Earth (3.58e+24 kg)
Radius
0.84x Earth (5,374 km)
Surface Gravity
0.84x Earth (8.3 m/s²)
Surface Temperature
211 K (-62 °C / -80 °F)
Rotation Period
22.0 hours/day (faster than Earth)
Orbital Environment
Star Type
K-type (Orange)
Distance from Star
1.10 AU (165 million km)
Orbital Period
1.38 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
O - Oxygen
50.6%
H - Hydrogen
16.7%
Fe - Iron
13.8%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present