Gas Giant Magnetic Field Extreme Activity
Why is this a Gas Giant? Your planet has 100.0% hydrogen and helium, combined with a mass of 72.0x 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: 100.0% (>60% required) ✓ Mass: 72.0x 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 30
Very slow rotation - extreme temperature swings between eternal day and night sides Organic Chemistry 20
Limited organic chemistry potential atmosphere 18
Hydrogen-rich atmosphere typical of gas giants (partially stripped by slow rotation) temperature 0
Inferno world - temperatures exceed all possibility of life magnetic Field 100
Magnetic field provides radiation protection Physical Properties Mass
72.00x Earth (4.30e+26 kg) Radius
4.16x Earth (26,504 km) This planet: 4.16× Earth radius Earth: 1× (baseline)
Surface Gravity
4.16x Earth (40.8 m/s²) Surface Temperature
1,918 K (1,645 °C / 2,993 °F) Rotation Period
17.0 hours/day (faster than Earth) This planet: 17 h/day Earth: 24 h/day Orbital Environment Star Type
B-type (Blue Giant) Distance from Star
2.10 AU (314 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
Moon 1 rings 1.3% - 1.7 radii
Inside the Roche limit (1.79 planet radii): torn apart into a ring system.
Moon 2 receding 0.13% - 16.7 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Moon 3 rings 0.0014% - 3.2 radii
Inside the synchronous orbit: it spiraled inward and was torn apart at the Roche limit (Phobos's fate).
+4 chemistry: tidal pools cycle wet and dry - a boost for prebiotic chemistry