Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (24.2% 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: 24.2% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 9.1% (<15% - silicate rules never claimed it)✓ Temperature: 282K (240-380K temperate band)✓ Air + water ingredients: 42.4% O+H (>=15%) with an atmosphere
Habitability ScoreHighly Habitable
96
Contributing Factors
water100
Abundant liquid water at surface temperature
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
1.10x Earth (6.57e+24 kg)
Radius
1.03x Earth (6,577 km)
Surface Gravity
1.03x Earth (10.1 m/s²)
Surface Temperature
282 K (9 °C / 48 °F)
Rotation Period
26.0 hours/day (slower than Earth)
Orbital Environment
Star Type
F-type (White)
Distance from Star
2.49 AU (372 million km)
Orbital Period
3.45 years
Atmosphere
Nitrogen-oxygen atmosphere over exotic mineral flats
Elemental Composition
H - Hydrogen
21.2%
O - Oxygen
21.2%
N - Nitrogen
15.2%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build