Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (34.1% 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: 34.1% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 0.0% (<15% - silicate rules never claimed it)✓ Temperature: 355K (240-380K temperate band)✓ Air + water ingredients: 41.8% O+H (>=15%) with an atmosphere
Habitability ScoreHabitable
67
Contributing Factors
water100
Abundant liquid water at surface temperature
geology90
Active geology recycles nutrients and drives carbon cycle
rotation10
Near tidally locked - one hemisphere perpetually scorched, other frozen, narrow habitable twilight zone only
Organic Chemistry84
Core organic elements (CHNO) present (tidal pools cycle wet and dry - a boost for prebiotic chemistry)
atmosphere40
Nitrogen-oxygen atmosphere - breathable and protective (partially stripped by slow rotation)
temperature45
Extreme temperature - very difficult for life (large moon stabilizes the axial tilt - steady seasons)
magnetic Field100
Magnetic field provides radiation protection (a large close moon may help stir the core dynamo (speculative))
Physical Properties
Mass
3.60x Earth (2.15e+25 kg)
Radius
1.53x Earth (9,764 km)
Surface Gravity
1.53x Earth (15.0 m/s²)
Surface Temperature
355 K (81 °C / 179 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
O-type (Blue Supergiant)
Distance from Star
346.40 AU (51.8 billion km)
Orbital Period
1,177 years
Atmosphere
Nitrogen-oxygen atmosphere over exotic mineral flats
Elemental Composition
Ca - Calcium
26.4%
O - Oxygen
22.0%
H - Hydrogen
19.8%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build
Inside the Roche limit (2.80 planet radii): torn apart into a ring system.
Moon 2receding1.3% - 24.0 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Tidal braking locked the planet to its moon: one face forever moonward.
+5 temperature: large moon stabilizes the axial tilt - steady seasons+4 chemistry: tidal pools cycle wet and dry - a boost for prebiotic chemistry+5 magneticField: a large close moon may help stir the core dynamo (speculative)