Carbon World Magnetic Field Extreme Activity
Why is this a Carbon World? Your planet's carbon (33.3%) 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: 33.3% (>=20% required) ✓ Carbon exceeds Oxygen: 33.3% > 0.0% ✓ Mass: 7.4x 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 40
Extreme volcanic activity may be hazardous rotation 0
Catastrophic rotation - centrifugal forces would destroy surface structures and prevent atmosphere retention Organic Chemistry 50
Carbon and hydrogen present - organic chemistry possible atmosphere 4
Atmosphere present but composition not ideal for life (severely compromised by extreme rotation) temperature 5
Scorching - hot enough to melt lead, though rock stays solid; no chance for life magnetic Field 100
Magnetic field provides radiation protection Physical Properties Mass
7.40x Earth (4.42e+25 kg) Radius
1.95x Earth (12,415 km) This planet: 1.95× Earth radius Earth: 1× (baseline)
Surface Gravity
1.95x Earth (19.1 m/s²) Surface Temperature
747 K (474 °C / 885 °F) Rotation Period
1.0 hours/day (faster than Earth) This planet: 1 h/day Earth: 24 h/day Orbital Environment Star Type
O-type (Blue Supergiant) Distance from Star
158.20 AU (23.7 billion km) Orbital Period
363.3 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 rings 1.4% - 1.7 radii
Inside the Roche limit (1.92 planet radii): torn apart into a ring system.