Carbon World Magnetic Field Low Activity
Why is this a Carbon World? Your planet's carbon (100.0%) 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: 100.0% (>=20% required) ✓ Carbon exceeds Oxygen: 100.0% > 0.0% ✓ Mass: 0.5x Earth (<=8x hycean ceiling)
Habitability Score Uninhabitable
Contributing Factors water 0
No water - the recipe has no hydrogen and oxygen to form it (water stripped by extreme rotation) geology 60
Some geological activity provides slow nutrient cycling rotation 0
Catastrophic rotation - centrifugal forces would destroy surface structures and prevent atmosphere retention Organic Chemistry 20
Limited organic chemistry potential atmosphere 4
Atmosphere present but composition not ideal for life (severely compromised by extreme rotation) temperature 10
Frozen world - minimal potential for complex life magnetic Field 100
Magnetic field provides radiation protection Physical Properties Mass
0.50x Earth (2.99e+24 kg) Radius
0.79x Earth (5,057 km) This planet: 0.79× Earth radius Earth: 1× (baseline)
Surface Gravity
0.79x Earth (7.8 m/s²) Surface Temperature
59 K (-214 °C / -353 °F) Rotation Period
1.0 hours/day (faster than Earth) This planet: 1 h/day Earth: 24 h/day Orbital Environment Star Type
G-type (Yellow (Sun-like)) Distance from Star
22.20 AU (3.32 billion km) Orbital Period
104.6 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