Magnetic Field Extreme Activity
Why is this a Gas Giant? Your planet has 87.0% hydrogen and helium, combined with a mass of 1286.0x 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: 87.0% (>60% required) ✓ Mass: 1286.0x Earth (>10x required)
Habitability Score Uninhabitable
Contributing Factors water 15
No solid surface — any water is locked in a supercritical mantle and hot ice, not oceans geology 40
Extreme volcanic activity may be hazardous 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 5
Near absolute zero - all molecular activity ceases, impossible for life (large moon stabilizes the axial tilt - steady seasons) magnetic Field 100
Magnetic field provides radiation protection Physical Properties Mass
1286.00x Earth (7.68e+27 kg) Radius
10.87x Earth (69,282 km) This planet: 10.87× Earth radius Earth: 1× (baseline)
Surface Gravity
10.87x Earth (106.7 m/s²) Surface Temperature
23 K (-250 °C / -419 °F) Rotation Period
33.0 hours/day (slower than Earth) This planet: 33 h/day Earth: 24 h/day Orbital Environment Star Type
O-type (Blue Supergiant) Distance from Star
47434.20 AU (7.1 trillion km) Orbital Period
1,886,152 years 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
Moon 1 merged 0.080% - 8.2 radii
Merged with an adjacent moon: too close for both to hold a stable orbit.
Moon 2 receding 0.35% - 13.9 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Tidal braking locked the planet to its moon: one face forever moonward.
Moon 3 rings 10% - 1.7 radii
Inside the Roche limit (1.79 planet radii): torn apart into a ring system.
Moon 4 rings 0.0050% - 7.1 radii
Inside the synchronous orbit: it spiraled inward and was torn apart at the Roche limit (Phobos's fate).
Moon 5 receding 10% - 51.1 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
+5 temperature: large moon stabilizes the axial tilt - steady seasons +4 chemistry: tidal pools cycle wet and dry - a boost for prebiotic chemistry