Why is this a Ice World?Your planet orbits at 302.60 AU from its star, resulting in frigid temperatures of 160K.
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: 302.60 AU (>3 AU) or Temperature <200K✓ Temperature: 160K✓ Water content: 28.9% for ice formation
Habitability ScoreUninhabitable
16
Contributing Factors
water11
Limited water content - frozen solid, no liquid phase at this temperature
geology60
Some geological activity provides slow nutrient cycling
rotation65
Slow rotation - significant day/night temperature variations, but life can adapt
Organic Chemistry54
Carbon and hydrogen present - organic chemistry possible (tidal pools cycle wet and dry - a boost for prebiotic chemistry)
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
1.00x Earth (5.97e+24 kg)
Radius
1.00x Earth (6,371 km)
Surface Gravity
1.00x Earth (9.8 m/s²)
Surface Temperature
160 K (-113 °C / -172 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
B-type (Blue Giant)
Distance from Star
302.60 AU (45.3 billion km)
Orbital Period
1,665 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
Si - Silicon
31.6%
O - Oxygen
26.3%
Fe - Iron
26.3%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present