No life — too cold for liquid waterMagnetic FieldExtreme Activity
Why is this a Gas Giant?Your planet has 18.4% hydrogen and helium, combined with a mass of 9534.0x 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.
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 (14/100).
Moon 2receding0.10% - 42.3 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Moon 3stable0.011% - 100.0 radii
Small and distant: a quiet, stable companion.
+5 temperature: large moon stabilizes the axial tilt - steady seasons+10 geology: tidal flexing sustains geologic activity+5 magneticField: a large close moon may help stir the core dynamo (speculative)