Magnetic Field Moderate Activity
Why is this a Carbon World? Your planet's carbon (26.8%) outweighs its oxygen (8.1%), 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: 26.8% (>=20% required) ✓ Carbon exceeds Oxygen: 26.8% > 8.1% ✓ Mass: 1.0x Earth (<=8x hycean ceiling)
Habitability Score Extremely Harsh
Contributing Factors water 64
Abundant water - likely as steam geology 90
Active geology recycles nutrients and drives carbon cycle rotation 30
Very slow rotation - extreme temperature swings between eternal day and night sides Organic Chemistry 54
Carbon and hydrogen present - organic chemistry possible (tidal pools cycle wet and dry - a boost for prebiotic chemistry) atmosphere 40
Atmosphere present but composition not ideal for life temperature 15
Extremely hot - hostile to known life forms magnetic Field 100
Magnetic field provides radiation protection Physical Properties Mass
1.00x Earth (5.97e+24 kg) Radius
1.00x Earth (6,371 km) This planet: 1.00× Earth radius Earth: 1× (baseline)
Surface Gravity
1.00x Earth (9.8 m/s²) Surface Temperature
469 K (196 °C / 384 °F) Rotation Period
24.0 hours/day This planet: 24 h/day Earth: 24 h/day Orbital Environment Star Type
G-type (Yellow (Sun-like)) Distance from Star
1.27 AU (190 million km) 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 receding 10% - 94.0 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
+4 chemistry: tidal pools cycle wet and dry - a boost for prebiotic chemistry