Gas Giant Magnetic Field Extreme Activity
Why is this a Gas Giant? Your planet has 79.1% hydrogen and helium, combined with a mass of 60.0x Earth, which exceeds the gas giant threshold. Gas giants form when massive cores capture enormous atmospheres of light gases. They typically form beyond the 'frost line' where volatiles can condense.
✓ Hydrogen + Helium: 79.1% (>60% required) ✓ Mass: 60.0x Earth (>10x required)
Habitability Score Marginal
Contributing Factors water 50
Limited water content geology 50
Extreme volcanic activity may be hazardous (tidal flexing sustains geologic activity) rotation 10
Near tidally locked - one hemisphere perpetually scorched, other frozen, narrow habitable twilight zone only Organic Chemistry 84
Core organic elements (CHNO) present (tidal pools cycle wet and dry - a boost for prebiotic chemistry) atmosphere 12
Hydrogen-rich atmosphere typical of gas giants (partially stripped by slow rotation) temperature 40
Extreme temperature - very difficult for life magnetic Field 100
Magnetic field provides radiation protection Physical Properties Mass
60.00x Earth (3.58e+26 kg) Radius
3.91x Earth (24,942 km) This planet: 3.91× Earth radius Earth: 1× (baseline)
Surface Gravity
3.91x Earth (38.4 m/s²) Surface Temperature
207 K (-67 °C / -88 °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
1.81 AU (271 million km) Atmosphere Hydrogen and helium dominated with trace methane and ammonia
Surface Characteristics No solid surface - thick gaseous envelope with possible rocky core deep within Moons Life may exist on a moon
Moon 1 stable Ocean world 0.010% - 4.3 radii
Small and distant: a quiet, stable companion.
Tidal braking locked the planet to its moon: one face forever moonward.
A thin tidal-warmed subsurface ocean may exist, but conditions are marginal (27/100).
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).
Moon 3 receding 10% - 67.1 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
+10 geology: tidal flexing sustains geologic activity +4 chemistry: tidal pools cycle wet and dry - a boost for prebiotic chemistry