Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (34.1% 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: 34.1% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 0.0% (<15% - silicate rules never claimed it)✓ Temperature: 371K (240-380K temperate band)✓ Air + water ingredients: 41.8% O+H (>=15%) with an atmosphere
Habitability ScoreHighly Habitable
87
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
temperature40
Extreme temperature - very difficult for life
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
3.60x Earth (2.15e+25 kg)
Radius
1.53x Earth (9,764 km)
Surface Gravity
1.53x Earth (15.0 m/s²)
Surface Temperature
371 K (98 °C / 208 °F)
Rotation Period
29.0 hours/day (slower than Earth)
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
1.00 AU (150 million km)
Orbital Period
1.00 years
Atmosphere
Nitrogen-oxygen atmosphere over exotic mineral flats
Elemental Composition
Ca - Calcium
26.4%
O - Oxygen
22.0%
H - Hydrogen
19.8%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build