No life — too cold for liquid waterMagnetic FieldLow Activity
Why is this a Ice World?Your planet orbits at 1.30 AU from its star, resulting in frigid temperatures of 244K.
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: 1.30 AU (>3 AU) or Temperature <200K✓ Temperature: 244K✓ Water content: 37.5% for ice formation
Habitability ScoreHabitable
62
Contributing Factors
water68
Good water content - mostly frozen
geology60
Some geological activity provides slow nutrient cycling
rotation65
Slow rotation - significant day/night temperature variations, but life can adapt
Organic Chemistry100
All CHNOPS elements present - building blocks of life (tidal pools cycle wet and dry - a boost for prebiotic chemistry)
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
244 K (-29 °C / -20 °F)
Rotation Period
22.0 hours/day (faster than Earth)
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
1.30 AU (194 million km)
Orbital Period
1.48 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
O - Oxygen
30.0%
Si - Silicon
20.0%
H - Hydrogen
15.0%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present