The final planet in the gala solar system it's also a ice planet
Ice World
Magnetic FieldLow Activity
Why is this a Ice World?Your planet orbits at 367.40 AU from its star, resulting in frigid temperatures of 23K.
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: 367.40 AU (>3 AU) or Temperature <200K✓ Temperature: 23K✓ Water content: 43.8% for ice formation
Habitability ScoreUninhabitable
0
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 Chemistry20
Limited organic chemistry potential
atmosphere70
Nitrogen atmosphere provides protection but not breathable
temperature0
Near absolute zero - all molecular activity ceases, impossible for life (extreme seasons: at 122° the poles swing between months-long day and night: −7% habitability)
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
23 K (-250 °C / -419 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
F-type (White)
Distance from Star
367.40 AU (55 billion km)
Orbital Period
6,176 years
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
He - Helium
37.5%
O - Oxygen
33.3%
H - Hydrogen
20.8%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present