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: 30.00 AU, 76K equilibrium
Habitability ScoreUninhabitable
0
Contributing Factors
water22
Abundant water - frozen solid, no liquid phase at this temperature
geology40
Extreme volcanic activity may be hazardous
rotation10
Near tidally locked - one hemisphere perpetually scorched, other frozen, narrow habitable twilight zone only
Organic Chemistry80
Core organic elements (CHNO) present
atmosphere16
Atmosphere present but composition not ideal for life (partially stripped by slow rotation)
temperature0
Frozen world - minimal potential for complex life (large moon stabilizes the axial tilt - steady seasons) (runaway tidal heating keeps the surface molten regardless of orbit)
magnetic Field100
Magnetic field provides radiation protection (a large close moon may help stir the core dynamo (speculative))
Physical Properties
Mass
14.00x Earth (8.36e+25 kg)
Radius
2.41x Earth (15,355 km)
Surface Gravity
2.41x Earth (23.6 m/s²)
Surface Temperature
76 K (-197 °C / -322 °F)
Rotation Period
16.0 hours/day (faster than Earth)
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
30.00 AU (4.49 billion km)
Orbital Period
164.3 years
Atmosphere
Volcanic outgassing - sulfur compounds and vaporized rock
Elemental Composition
H - Hydrogen
40.0%
He - Helium
25.0%
C - Carbon
15.0%
Surface Characteristics
Runaway tidal heating drives volcanism across a cold crust - lava lakes and sulfur plains between frozen plains
Inside the Roche limit (1.79 planet radii): torn apart into a ring system.
Moon 2receding1.6% - 6.8 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Tidal braking locked the planet to its moon: one face forever moonward.
+5 temperature: large moon stabilizes the axial tilt - steady seasons-85 temperature: runaway tidal heating keeps the surface molten regardless of orbit+5 magneticField: a large close moon may help stir the core dynamo (speculative)