No life — no phosphorus — DNA and ATP are built on itMagnetic FieldHigh Activity
Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (34.1% calcium/titanium/aluminum-family rock formers) instead of the silicate-iron recipe every standard rocky world uses.
Exotic terrestrials are temperate solid worlds whose geology skipped the silicate playbook - carbonate plains, titanium-gray mesas, alkali flats. They can hold air, water ingredients, and real habitability, but with no silicate continents or iron core they are their own class, not earth-likes.
Classification Criteria:
✓ Exotic rock formers: 34.1% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 0.0% (<15% - silicate rules never claimed it)✓ Temperature: 268K (240-380K temperate band)✓ Air + water ingredients: 41.8% O+H (>=15%) with an atmosphere
Habitability ScoreHighly Habitable
87
Contributing Factors
water96
Abundant water - mostly frozen
geology90
Active geology recycles nutrients and drives carbon cycle
rotation65
Slow rotation - significant day/night temperature variations, but life can adapt
Organic Chemistry80
Core organic elements (CHNO) present
atmosphere100
Nitrogen-oxygen atmosphere - breathable and protective
temperature70
Challenging but potentially habitable temperature
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
1.60x Earth (9.56e+24 kg)
Radius
1.17x Earth (7,452 km)
Surface Gravity
1.17x Earth (11.5 m/s²)
Surface Temperature
268 K (-5 °C / 22 °F)
Rotation Period
42.0 hours/day (slower than Earth)
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
1.92 AU (287 million km)
Orbital Period
2.66 years
Atmosphere
Nitrogen-oxygen atmosphere over exotic mineral flats
Elemental Composition
Ca - Calcium
26.4%
O - Oxygen
22.0%
H - Hydrogen
19.8%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build