Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (33.3% 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: 33.3% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 8.3% (<15% - silicate rules never claimed it)✓ Temperature: 275K (240-380K temperate band)✓ Air + water ingredients: 25.0% O+H (>=15%) with an atmosphere
Habitability ScoreExtremely Harsh
29
Contributing Factors
water90
Good water content
geology100
Active geology recycles nutrients and drives carbon cycle (tidal flexing sustains geologic activity)
rotation10
Near tidally locked - one hemisphere perpetually scorched, other frozen, narrow habitable twilight zone only
Organic Chemistry80
Core organic elements (CHNO) present — but the ground itself is radioactive, and no magnetic field shields a world from its own crust
atmosphere40
Nitrogen-oxygen atmosphere - breathable and protective (partially stripped by slow rotation)
temperature100
Optimal temperature range for liquid water and life (large moon stabilizes the axial tilt - steady seasons) (extreme seasons: at 90° the poles swing between months-long day and night, softened by deep oceans: −13% habitability)
magnetic Field100
Magnetic field provides radiation protection (a large close moon may help stir the core dynamo (speculative))
Physical Properties
Mass
2.00x Earth (1.19e+25 kg)
Radius
1.26x Earth (8,027 km)
Surface Gravity
1.26x Earth (12.4 m/s²)
Surface Temperature
275 K (2 °C / 36 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
1.12 AU (168 million km)
Orbital Period
1.19 years
Atmosphere
Nitrogen-oxygen atmosphere over exotic mineral flats
Elemental Composition
H - Hydrogen
12.5%
O - Oxygen
12.5%
U - Uranium
12.5%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Tidal braking locked the planet to its moon: one face forever moonward.
Moon 2merged10% - 21.7 radii
Merged with an adjacent moon: too close for both to hold a stable orbit.
+5 temperature: large moon stabilizes the axial tilt - steady seasons+10 geology: tidal flexing sustains geologic activity+5 magneticField: a large close moon may help stir the core dynamo (speculative)
Habitability
✓ Conditions suitable for life detectedThis planet exhibits the necessary conditions to support biological processes, including stable temperatures, liquid water, and protective magnetic fields.