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: 12.1% (<15% - silicate rules never claimed it)✓ Temperature: 281K (240-380K temperate band)✓ Air + water ingredients: 35.6% O+H (>=15%) with an atmosphere
Habitability ScoreHighly Habitable
98
Contributing Factors
water90
Good water content
geology90
Active geology recycles nutrients and drives carbon cycle
rotation100
Optimal rotation period - balanced day/night cycle, moderate weather, and good heat distribution
Organic Chemistry100
All CHNOPS elements present - building blocks of life
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
3.50x Earth (2.09e+25 kg)
Radius
1.52x Earth (9,673 km)
Surface Gravity
1.52x Earth (14.9 m/s²)
Surface Temperature
281 K (8 °C / 46 °F)
Rotation Period
21.0 hours/day (faster than Earth)
Orbital Environment
Star Type
B-type (Blue Giant)
Distance from Star
98.10 AU (14.7 billion km)
Orbital Period
307.3 years
Atmosphere
Nitrogen-oxygen atmosphere over exotic mineral flats
Elemental Composition
O - Oxygen
25.0%
H - Hydrogen
10.6%
Al - Aluminum
10.6%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build
✓ Conditions suitable for life detectedThis planet exhibits the necessary conditions to support biological processes, including stable temperatures, liquid water, and protective magnetic fields.