Destroyed — no longer habitableMagnetic FieldLow Activity
Why is this a Ice World?Your planet orbits at 1.74 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: 1.74 AU (>3 AU) or Temperature <200K✓ Temperature: 211K✓ Water content: 40.9% for ice formation
Habitability
Destroyed — no longer habitable
Physical Properties
Mass
0.90x Earth (5.37e+24 kg)
Radius
0.97x Earth (6,151 km)
Surface Gravity
0.97x Earth (9.5 m/s²)
Surface Temperature
211 K (-62 °C / -79 °F)
Rotation Period
8.0 hours/day (faster than Earth)
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
1.74 AU (260 million km)
Orbital Period
2.30 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
H - Hydrogen
27.3%
O - Oxygen
27.3%
He - Helium
27.3%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present