Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (37.1% 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: 37.1% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 5.7% (<15% - silicate rules never claimed it)✓ Temperature: 266K (240-380K temperate band)✓ Air + water ingredients: 25.7% O+H (>=15%) with an atmosphere
Habitability ScoreHighly Habitable
94
Contributing Factors
water85
Good water content - mostly frozen
geology90
Active geology recycles nutrients and drives carbon cycle
rotation100
Optimal rotation period - balanced day/night cycle, moderate weather, and good heat distribution
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
1.90x Earth (1.13e+25 kg)
Radius
1.24x Earth (7,891 km)
Surface Gravity
1.24x Earth (12.2 m/s²)
Surface Temperature
266 K (-7 °C / 19 °F)
Rotation Period
21.0 hours/day (faster than Earth)
Orbital Environment
Star Type
O-type (Blue Supergiant)
Distance from Star
365.40 AU (54.7 billion km)
Orbital Period
1,275 years
Atmosphere
Nitrogen-oxygen atmosphere over exotic mineral flats
Elemental Composition
Al - Aluminum
37.1%
N - Nitrogen
17.1%
O - Oxygen
14.3%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build