No life — too cold for liquid water Magnetic Field Extreme Activity
Why is this a Gas Giant? Your planet has 51.3% hydrogen and helium, combined with a mass of 41.0x 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: 51.3% (>60% required) ✓ Mass: 41.0x 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 100
Optimal rotation period - balanced day/night cycle, moderate weather, and good heat distribution Organic Chemistry 80
Core organic elements (CHNO) present atmosphere 30
Hydrogen-rich atmosphere typical of gas giants temperature 10
Frozen world - minimal potential for complex life magnetic Field 100
Magnetic field provides radiation protection Physical Properties Mass
41.00x Earth (2.45e+26 kg) Radius
3.45x Earth (21,969 km) This planet: 3.45× Earth radius Earth: 1× (baseline)
Surface Gravity
3.45x Earth (33.8 m/s²) Surface Temperature
53 K (-220 °C / -364 °F) Rotation Period
21.0 hours/day (faster than Earth) This planet: 21 h/day Earth: 24 h/day Orbital Environment Star Type
G-type (Yellow (Sun-like)) Distance from Star
27.20 AU (4.07 billion km) Orbital Period
141.9 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 rings 0.010% - 5.9 radii
Inside the synchronous orbit: it spiraled inward and was torn apart at the Roche limit (Phobos's fate).
Moon 2 rings 0.018% - 1.5 radii
Inside the Roche limit (1.79 planet radii): torn apart into a ring system.
Moon 3 rings 0.010% - 2.8 radii
Inside the synchronous orbit: it spiraled inward and was torn apart at the Roche limit (Phobos's fate).