Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (55.9% 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: 55.9% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 1.1% (<15% - silicate rules never claimed it)✓ Temperature: 278K (240-380K temperate band)✓ Air + water ingredients: 19.0% O+H (>=15%) with an atmosphere
Habitability ScoreUninhabitable
12
Contributing Factors
water90
Good water content
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 — but the ground itself is radioactive, and no magnetic field shields a world from its own crust
atmosphere70
Nitrogen atmosphere provides protection but not breathable
temperature100
Optimal temperature range for liquid water and 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
278 K (5 °C / 41 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
1.00 AU (150 million km)
Orbital Period
1.00 years
Atmosphere
Thin CO₂ and nitrogen atmosphere
Elemental Composition
U - Uranium
55.9%
He - Helium
14.5%
H - Hydrogen
12.8%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build