Magnetic Field Low Activity
Why is this a Gas Dwarf? Your planet has an unusual composition that doesn't fit standard classifications, or lacks the elements needed for complex geological processes. Barren worlds can form from uncommon element combinations or may be remnants of larger bodies that lost their atmospheres and volatile materials.
Composition doesn't match standard planet types Mass: 8.2x Earth Temperature: 91K
Habitability Score Uninhabitable
Contributing Factors water 50
Limited water content geology 70
Some geological activity provides slow nutrient cycling (tidal flexing sustains geologic activity) rotation 10
Near tidally locked - one hemisphere perpetually scorched, other frozen, narrow habitable twilight zone only Organic Chemistry 80
Core organic elements (CHNO) present atmosphere 12
Hydrogen-rich atmosphere typical of gas giants (partially stripped by slow rotation) temperature 10
Frozen world - minimal potential for complex life magnetic Field 100
Magnetic field provides radiation protection Physical Properties Mass
8.20x Earth (4.90e+25 kg) Radius
2.02x Earth (12,847 km) This planet: 2.02× Earth radius Earth: 1× (baseline)
Surface Gravity
2.02x Earth (19.8 m/s²) Surface Temperature
91 K (-183 °C / -297 °F) Rotation Period
10.0 hours/day (faster than Earth) This planet: 10 h/day Earth: 24 h/day Orbital Environment Star Type
G-type (Yellow (Sun-like)) Distance from Star
9.42 AU (1.41 billion km) Atmosphere Deep hydrogen-helium envelope with photochemical haze
Surface Characteristics No solid surface - a thick gas envelope wrapped around a small deep core (a mini-Neptune) Moons Life may exist on a moon
Moon 1 receding Ocean world 0.080% - 6.0 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Tidal braking locked the planet to its moon: one face forever moonward.
A thin tidal-warmed subsurface ocean may exist, but conditions are marginal (22/100).
Moon 2 receding Ocean world - life 0.10% - 9.5 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Tidal heat sustains a subsurface ocean over a rock seafloor: a strong candidate for life (Europa-like, 96/100).
+10 geology: tidal flexing sustains geologic activity