Why is this a Ice World?Your planet orbits at 6.22 AU from its star, resulting in frigid temperatures of 120K.
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: 6.22 AU (>3 AU) or Temperature <200K✓ Temperature: 120K✓ Water content: 44.1% for ice formation
Habitability ScoreExtremely Harsh
26
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 Chemistry80
Core organic elements (CHNO) present
atmosphere70
Nitrogen atmosphere provides protection but not breathable
temperature20
Very cold - water frozen, challenging for life
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
1.90x Earth (1.13e+25 kg)
Radius
1.24x Earth (7,891 km)
Surface Gravity
1.24x Earth (12.2 m/s²)
Surface Temperature
120 K (-153 °C / -244 °F)
Rotation Period
18.0 hours/day (faster than Earth)
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
6.22 AU (930 million km)
Orbital Period
15.5 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
O - Oxygen
35.3%
H - Hydrogen
17.6%
Si - Silicon
17.6%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present