This is a multin world and it has one giant Moon named Gara Gara is the reason why this planet is a lava world including this planet is close to its star the first planet of the star system this star is named Amethyst and it's an a type star
Volcanic World
Magnetic FieldExtreme Activity
Why is this a Volcanic World?Runaway tidal heating from its moons drives volcanism across a cold crust - the planet is kneaded like Io.
Resonant, close-in moons pump orbital eccentricity, and the resulting tidal flexing dissipates enormous heat in the interior. Only a fraction of the surface is molten at once, so the ground between the vents stays as cold as the orbit allows - Io's own equilibrium temperature is about 110 K.
Classification Criteria:
✓ Close-in moons in a resonant configuration✓ Tidal heat flux beyond the runaway threshold- The orbit is not what melted it: 0.80 AU, 486K equilibrium
Habitability ScoreUninhabitable
0
Contributing Factors
water0
No water - the recipe has no hydrogen and oxygen to form it
geology40
Extreme volcanic activity may be hazardous
rotation10
Near tidally locked - one hemisphere perpetually scorched, other frozen, narrow habitable twilight zone only
Organic Chemistry50
Carbon and hydrogen present - organic chemistry possible
atmosphere16
Atmosphere present but composition not ideal for life (partially stripped by slow rotation)
temperature0
Extremely hot - hostile to known life forms (large moon stabilizes the axial tilt - steady seasons) (runaway tidal heating keeps the surface molten regardless of orbit)
magnetic Field100
Magnetic field provides radiation protection (a large close moon may help stir the core dynamo (speculative))
Physical Properties
Mass
1.80x Earth (1.07e+25 kg)
Radius
1.22x Earth (7,750 km)
Surface Gravity
1.22x Earth (11.9 m/s²)
Surface Temperature
486 K (213 °C / 416 °F)
Rotation Period
20.0 hours/day (faster than Earth)
Orbital Environment
Star Type
F-type (White)
Distance from Star
0.80 AU (120 million km)
Orbital Period
229 days
Atmosphere
Volcanic outgassing - sulfur compounds and vaporized rock
Elemental Composition
C - Carbon
52.3%
Fe - Iron
17.4%
Si - Silicon
17.4%
Surface Characteristics
Runaway tidal heating drives volcanism across a cold crust - lava lakes and sulfur plains between frozen plains
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Tidal braking locked the planet to its moon: one face forever moonward.
+5 temperature: large moon stabilizes the axial tilt - steady seasons-85 temperature: runaway tidal heating keeps the surface molten regardless of orbit+5 magneticField: a large close moon may help stir the core dynamo (speculative)