Why is this a Ice World?Your planet orbits at 2.07 AU from its star, resulting in frigid temperatures of 210K.
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: 2.07 AU (>3 AU) or Temperature <200K✓ Temperature: 210K✓ Water content: 34.4% for ice formation
Habitability ScoreMarginal
57
Contributing Factors
water27
Water present but mostly frozen (low gravity lets water escape to space)
geology30
Geologically dead - no nutrient recycling
rotation100
Optimal rotation period - balanced day/night cycle, moderate weather, and good heat distribution
Organic Chemistry100
All CHNOPS elements present - building blocks of life
atmosphere70
Nitrogen atmosphere provides protection but not breathable
temperature40
Extreme temperature - very difficult for life
magnetic Field30
No magnetic field - vulnerable to solar radiation
Physical Properties
Mass
0.20x Earth (1.19e+24 kg)
Radius
0.58x Earth (3,726 km)
Surface Gravity
0.58x Earth (5.7 m/s²)
Surface Temperature
210 K (-63 °C / -82 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
K-type (Orange)
Distance from Star
2.07 AU (310 million km)
Orbital Period
3.56 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
O - Oxygen
25.4%
C - Carbon
21.0%
H - Hydrogen
18.1%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present