No life — too cold for liquid waterMagnetic FieldExtreme Activity
Why is this a Volcanic World?Runaway tidal heating from its moons drives volcanism across a cold crust - the planet is kneaded like Io.
Resonant, close-in moons pump orbital eccentricity, and the resulting tidal flexing dissipates enormous heat in the interior. Only a fraction of the surface is molten at once, so the ground between the vents stays as cold as the orbit allows - Io's own equilibrium temperature is about 110 K.
Classification Criteria:
✓ Close-in moons in a resonant configuration✓ Tidal heat flux beyond the runaway threshold- The orbit is not what melted it: 165.70 AU, 228K equilibrium
Habitability ScoreUninhabitable
0
Contributing Factors
water56
Good water content - mostly frozen
geology40
Extreme volcanic activity may be hazardous
rotation10
Near tidally locked - one hemisphere perpetually scorched, other frozen, narrow habitable twilight zone only
Organic Chemistry100
All CHNOPS elements present - building blocks of life
atmosphere16
Atmosphere present but composition not ideal for life (partially stripped by slow rotation)
temperature0
Extreme temperature - very difficult for life (runaway tidal heating keeps the surface molten regardless of orbit)
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
3.50x Earth (2.09e+25 kg)
Radius
1.52x Earth (9,673 km)
Surface Gravity
1.52x Earth (14.9 m/s²)
Surface Temperature
228 K (-45 °C / -49 °F)
Rotation Period
16.0 hours/day (faster than Earth)
Orbital Environment
Star Type
B-type (Blue Giant)
Distance from Star
165.70 AU (24.8 billion km)
Orbital Period
674.5 years
Atmosphere
Volcanic outgassing - sulfur compounds and vaporized rock
Elemental Composition
O - Oxygen
20.2%
Si - Silicon
17.1%
H - Hydrogen
14.0%
Surface Characteristics
Runaway tidal heating drives volcanism across a cold crust - lava lakes and sulfur plains between frozen plains