Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (16.3% 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: 16.3% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 14.0% (<15% - silicate rules never claimed it)✓ Temperature: 294K (240-380K temperate band)✓ Air + water ingredients: 34.9% O+H (>=15%) with an atmosphere
Habitability ScoreHabitable
68
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 Chemistry100
All CHNOPS elements present - building blocks of life
atmosphere28
Nitrogen atmosphere provides protection but not breathable (partially stripped by slow rotation)
temperature100
Optimal temperature range for liquid water and 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
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
294 K (21 °C / 70 °F)
Rotation Period
15.0 hours/day (faster than Earth)
Orbital Environment
Star Type
B-type (Blue Giant)
Distance from Star
100.90 AU (15.1 billion km)
Orbital Period
320.5 years
Atmosphere
Thin CO₂ and nitrogen atmosphere
Elemental Composition
O - Oxygen
23.3%
H - Hydrogen
11.6%
S - Sulfur
9.3%
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.
+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.