Magnetic Field Low Activity
Why is this a Carbon World? Your planet's carbon (52.3%) outweighs its oxygen (0.0%), so the mineralogy flips from silicate rock to carbide - a graphite crust over a diamond mantle. Carbon worlds form in carbon-rich disks where there isn't enough oxygen to bind it all into silicates. Instead carbon condenses directly into graphite, carbides, and - under pressure at depth - diamond. They form water-poor, so no life takes hold.
✓ Carbon: 52.3% (>=20% required) ✓ Carbon exceeds Oxygen: 52.3% > 0.0% ✓ Mass: 0.6x Earth (<=8x hycean ceiling)
Habitability Score Uninhabitable
Contributing Factors water 0
No water - the recipe has no hydrogen and oxygen to form it geology 60
Some geological activity provides slow nutrient cycling rotation 100
Optimal rotation period - balanced day/night cycle, moderate weather, and good heat distribution Organic Chemistry 50
Carbon and hydrogen present - organic chemistry possible atmosphere 40
Atmosphere present but composition not ideal for life temperature 10
Frozen world - minimal potential for complex life magnetic Field 100
Magnetic field provides radiation protection Physical Properties Mass
0.60x Earth (3.58e+24 kg) Radius
0.84x Earth (5,374 km) This planet: 0.84× Earth radius Earth: 1× (baseline)
Surface Gravity
0.84x Earth (8.3 m/s²) Surface Temperature
53 K (-221 °C / -365 °F) Rotation Period
19.0 hours/day (faster than Earth) This planet: 19 h/day Earth: 24 h/day Orbital Environment Distance from Star
68.30 AU (10.2 billion km) Orbital Period
495.1 years Atmosphere Carbon monoxide and methane haze over a graphite surface
Surface Characteristics Graphite plains and carbide ridges over a diamond mantle - a glittering coal-black world Moons
Moon 1 stable 0.00014% - 6.6 radii
Small and distant: a quiet, stable companion.