Destroyed — no longer habitableMagnetic FieldHigh Activity
Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (12.4% 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: 12.4% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 14.6% (<15% - silicate rules never claimed it)✓ Temperature: 278K (240-380K temperate band)✓ Air + water ingredients: 21.7% O+H (>=15%) with an atmosphere
Habitability
Destroyed — no longer habitable
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
278 K (5 °C / 41 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
1.00 AU (150 million km)
Orbital Period
1.00 years
Atmosphere
Thin CO₂ atmosphere
Elemental Composition
He - Helium
31.0%
O - Oxygen
13.6%
Fe - Iron
11.5%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build