Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (18.8% 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: 18.8% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 9.0% (<15% - silicate rules never claimed it)✓ Temperature: 292K (240-380K temperate band)✓ Air + water ingredients: 37.6% O+H (>=15%) with an atmosphere
Habitability ScoreHabitable
70
Contributing Factors
water100
Abundant water
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
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)
magnetic Field100
Magnetic field provides radiation protection (a large close moon may help stir the core dynamo (speculative))
Physical Properties
Mass
2.50x Earth (1.49e+25 kg)
Radius
1.36x Earth (8,647 km)
Surface Gravity
1.36x Earth (13.3 m/s²)
Surface Temperature
292 K (19 °C / 65 °F)
Rotation Period
28.0 hours/day (slower than Earth)
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
0.99 AU (148 million km)
Orbital Period
360 days
Atmosphere
Nitrogen-oxygen atmosphere over exotic mineral flats
Elemental Composition
H - Hydrogen
18.8%
O - Oxygen
18.8%
He - Helium
8.3%
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 2rings0.032% - 6.0 radii
Inside the synchronous orbit: it spiraled inward and was torn apart at the Roche limit (Phobos's fate).
Moon 3receding0.40% - 12.8 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Tidal braking locked the planet to its moon: one face forever moonward.
Moon 4rings0.010% - 2.8 radii
Inside the Roche limit (2.80 planet radii): torn apart into a ring system.
Moon 5stable0.010% - 45.9 radii
Small and distant: a quiet, stable companion.
Moon 6merged0.63% - 14.8 radii
Merged with an adjacent moon: too close for both to hold a stable orbit.
Moon 7merged0.010% - 19.0 radii
Merged with an adjacent moon: too close for both to hold a stable orbit.
Moon 8stable0.010% - 69.8 radii
Small and distant: a quiet, stable companion.
+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.