Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (52.6% 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: 52.6% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 0.0% (<15% - silicate rules never claimed it)✓ Temperature: 323K (240-380K temperate band)✓ Air + water ingredients: 15.8% O+H (>=15%) with an atmosphere
Habitability ScoreExtremely Harsh
30
Contributing Factors
water50
Limited water content
geology90
Active geology recycles nutrients and drives carbon cycle
rotation65
Slow rotation - significant day/night temperature variations, but life can adapt
Organic Chemistry20
Limited organic chemistry potential
atmosphere100
Nitrogen-oxygen atmosphere - breathable and protective
temperature70
Challenging but potentially habitable temperature
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
3.40x Earth (2.03e+25 kg)
Radius
1.50x Earth (9,580 km)
Surface Gravity
1.50x Earth (14.8 m/s²)
Surface Temperature
323 K (50 °C / 122 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
0.74 AU (111 million km)
Orbital Period
233 days
Atmosphere
Nitrogen-oxygen atmosphere over exotic mineral flats
Elemental Composition
U - Uranium
26.3%
N - Nitrogen
15.8%
Al - Aluminum
15.8%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build