Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (14.8% 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: 14.8% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 3.2% (<15% - silicate rules never claimed it)✓ Temperature: 353K (240-380K temperate band)✓ Air + water ingredients: 71.3% O+H (>=15%) with an atmosphere
Habitability ScoreExtremely Harsh
27
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 Chemistry50
Carbon and hydrogen present - organic chemistry possible — but the ground itself is radioactive, and no magnetic field shields a world from its own crust
atmosphere35
Dense CO₂ atmosphere with extreme greenhouse effect
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
353 K (80 °C / 176 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
O-type (Blue Supergiant)
Distance from Star
212.80 AU (31.8 billion km)
Orbital Period
566.8 years
Atmosphere
Thin CO₂ atmosphere
Elemental Composition
H - Hydrogen
42.1%
O - Oxygen
29.2%
U - Uranium
14.4%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build