Destroyed — no longer habitableMagnetic FieldHigh Activity
Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (13.8% 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: 13.8% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 11.3% (<15% - silicate rules never claimed it)✓ Temperature: 302K (240-380K temperate band)✓ Air + water ingredients: 46.1% O+H (>=15%) with an atmosphere
Habitability
Destroyed — no longer habitable
Physical Properties
Mass
2.10x Earth (1.25e+25 kg)
Radius
1.28x Earth (8,159 km)
Surface Gravity
1.28x Earth (12.6 m/s²)
Surface Temperature
302 K (29 °C / 85 °F)
Rotation Period
25.0 hours/day (slower than Earth)
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
1.04 AU (156 million km)
Orbital Period
1.06 years
Atmosphere
Thin CO₂ and nitrogen atmosphere
Elemental Composition
O - Oxygen
24.0%
H - Hydrogen
22.1%
Fe - Iron
7.9%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build