Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (15.4% 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: 15.4% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 0.0% (<15% - silicate rules never claimed it)✓ Temperature: 288K (240-380K temperate band)✓ Air + water ingredients: 57.7% O+H (>=15%) with an atmosphere
Habitability ScoreMarginal
46
Contributing Factors
water100
Abundant water
geology90
Active geology recycles nutrients and drives carbon cycle
rotation60
Fast rotation - strong global wind patterns and weather systems, but manageable
Organic Chemistry80
Core organic elements (CHNO) present — but the ground itself is radioactive, and no magnetic field shields a world from its own crust
atmosphere100
Nitrogen-oxygen atmosphere - breathable and protective
temperature100
Optimal temperature range for liquid water and life
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
1.70x Earth (1.02e+25 kg)
Radius
1.19x Earth (7,604 km)
Surface Gravity
1.19x Earth (11.7 m/s²)
Surface Temperature
288 K (15 °C / 59 °F)
Rotation Period
13.0 hours/day (faster 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
38.5%
O - Oxygen
19.2%
N - Nitrogen
11.5%
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.
Habitability
✓ Conditions could support lifeThis planet’s modelled conditions could support biological processes: stable temperatures, liquid water and the chemistry life as we know it needs. That makes life possible, not present.