Why is this a Ice World?Your planet orbits at 1.00 AU from its star, resulting in frigid temperatures of 234K.
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: 1.00 AU (>3 AU) or Temperature <200K✓ Temperature: 234K✓ Water content: 95.0% for ice formation
Habitability ScoreUninhabitable
17
Contributing Factors
water34
Limited 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 Chemistry20
Limited organic chemistry potential
atmosphere28
Nitrogen atmosphere provides protection but not breathable (partially stripped by slow rotation)
temperature45
Extreme temperature - very difficult for life (large moon stabilizes the axial tilt - steady seasons)
magnetic Field100
Magnetic field provides radiation protection — but the remnant's shock fronts flood this orbit with cosmic rays
Physical Properties
Mass
1.00x Earth (5.97e+24 kg)
Radius
1.00x Earth (6,371 km)
Surface Gravity
1.00x Earth (9.8 m/s²)
Surface Temperature
234 K (-39 °C / -39 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
SNR-type (Supernova Remnant)
Distance from Star
1.00 AU (150 million km)
Orbital Period
309 days
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
O - Oxygen
90.1%
H - Hydrogen
9.9%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present