Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (40.0% 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: 40.0% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 0.0% (<15% - silicate rules never claimed it)✓ Temperature: 249K (240-380K temperate band)✓ Air + water ingredients: 40.0% O+H (>=15%) with an atmosphere
Habitability ScoreUninhabitable
5
Contributing Factors
water80
Abundant water - mostly frozen
geology90
Active geology recycles nutrients and drives carbon cycle
rotation30
Very slow rotation - severe temperature swings between eternal day and night sides
Organic Chemistry20
Limited organic chemistry potential — but the ground itself is radioactive, and no magnetic field shields a world from its own crust
atmosphere100
Nitrogen-oxygen atmosphere - breathable and protective
temperature40
Extreme temperature - very difficult for life
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
1.00x Earth (5.97e+24 kg)
Radius
1.00x Earth (6,371 km)
Surface Gravity
1.00x Earth (9.8 m/s²)
Surface Temperature
249 K (-24 °C / -12 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
O-type (Blue Supergiant)
Distance from Star
394.80 AU (59.1 billion km)
Orbital Period
1,432 years
Atmosphere
Nitrogen-oxygen atmosphere over exotic mineral flats
Elemental Composition
U - Uranium
40.0%
H - Hydrogen
20.0%
N - Nitrogen
20.0%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build