Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (27.7% 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: 27.7% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 0.0% (<15% - silicate rules never claimed it)✓ Temperature: 322K (240-380K temperate band)✓ Air + water ingredients: 33.9% O+H (>=15%) with an atmosphere
Habitability ScoreHighly Habitable
91
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
temperature70
Challenging but potentially habitable temperature
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
322 K (49 °C / 120 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
K-type (Orange)
Distance from Star
0.66 AU (98.7 million km)
Orbital Period
234 days
Atmosphere
Nitrogen-oxygen atmosphere over exotic mineral flats
Elemental Composition
Ca - Calcium
21.4%
O - Oxygen
17.9%
H - Hydrogen
16.1%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build
✓ Conditions suitable for life detectedThis planet exhibits the necessary conditions to support biological processes, including stable temperatures, liquid water, and protective magnetic fields.