Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (33.1% 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: 33.1% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 9.9% (<15% - silicate rules never claimed it)✓ Temperature: 275K (240-380K temperate band)✓ Air + water ingredients: 39.7% O+H (>=15%) with an atmosphere
Habitability ScoreHighly Habitable
94
Contributing Factors
water100
Abundant water
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
temperature100
Optimal temperature range for liquid water and life
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
2.40x Earth (1.43e+25 kg)
Radius
1.34x Earth (8,530 km)
Surface Gravity
1.34x Earth (13.1 m/s²)
Surface Temperature
275 K (2 °C / 35 °F)
Rotation Period
37.0 hours/day (slower than Earth)
Orbital Environment
Star Type
A-type (Blue-White)
Distance from Star
7.01 AU (1.05 billion km)
Orbital Period
13.1 years
Atmosphere
Nitrogen-oxygen atmosphere over exotic mineral flats
Elemental Composition
U - Uranium
33.1%
O - Oxygen
23.1%
H - Hydrogen
16.5%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build