Destroyed many proto-planets during the formation of the system and therefore migrated outside the habitable zone and grew to a huge mass, even capturing planets to be used as moons
Why is this a Ice World?Your planet orbits at 0.57 AU from its star, resulting in frigid temperatures of 197K.
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: 0.57 AU (>3 AU) or Temperature <200K✓ Temperature: 197K✓ Water content: 45.6% for ice formation
Habitability ScoreExtremely Harsh
22
Contributing Factors
water36
Abundant water - frozen solid, no liquid phase at this temperature
geology60
Some geological activity provides slow nutrient cycling
rotation30
Very slow rotation - severe temperature swings between eternal day and night sides
Organic Chemistry100
All CHNOPS elements present - building blocks of life
atmosphere42
Nitrogen atmosphere provides protection but not breathable (partially stripped by slow rotation)
temperature20
Very cold - water frozen, challenging for life
magnetic Field30
No magnetic field - vulnerable to solar radiation
Physical Properties
Mass
4.00x Earth (2.39e+25 kg)
Radius
1.59x Earth (10,113 km)
Surface Gravity
1.59x Earth (15.6 m/s²)
Surface Temperature
197 K (-76 °C / -105 °F)
Rotation Period
256.0 hours/day (slower than Earth)
Orbital Environment
Star Type
M-type (Red Dwarf)
Distance from Star
0.57 AU (85.3 million km)
Orbital Period
287 days
Atmosphere
Thin nitrogen and methane atmosphere
Elemental Composition
O - Oxygen
31.3%
H - Hydrogen
28.6%
Fe - Iron
15.0%
Surface Characteristics
Frozen surface covered in water ice, possible subsurface ocean if tidal heating present