Why is this a Ice World?Your planet orbits at 2.10 AU from its star, resulting in frigid temperatures of 249K.
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: 2.10 AU (>3 AU) or Temperature <200K✓ Temperature: 249K✓ Water content: 45.4% for ice formation
Habitability ScoreMarginal
40
Contributing Factors
water72
Good water content - mostly frozen
geology60
Some geological activity provides slow nutrient cycling
rotation10
Near tidally locked - one hemisphere perpetually scorched, other frozen, narrow habitable twilight zone only
Organic Chemistry54
Carbon and hydrogen present - organic chemistry possible (tidal pools cycle wet and dry - a boost for prebiotic chemistry)
atmosphere28
Nitrogen atmosphere provides protection but not breathable (partially stripped by slow rotation)
temperature40
Extreme temperature - very difficult for life
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
0.80x Earth (4.78e+24 kg)
Radius
0.93x Earth (5,914 km)
Surface Gravity
0.93x Earth (9.1 m/s²)
Surface Temperature
249 K (-24 °C / -12 °F)
Rotation Period
22.0 hours/day (faster than Earth)
Orbital Environment
Star Type
K-type (Orange)
Distance from Star
2.10 AU (314 million km)
Orbital Period
3.64 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
O - Oxygen
38.9%
C - Carbon
19.6%
H - Hydrogen
13.0%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present