Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (17.2% 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: 17.2% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 0.0% (<15% - silicate rules never claimed it)✓ Temperature: 314K (240-380K temperate band)✓ Air + water ingredients: 20.7% O+H (>=15%) with an atmosphere
Habitability ScoreExtremely Harsh
23
Contributing Factors
water20
Very dry - minimal water
geology90
Active geology recycles nutrients and drives carbon cycle
rotation30
Very slow rotation - extreme temperature swings between eternal day and night sides
Organic Chemistry25
Carbon and hydrogen present - organic chemistry possible - chlorine-laced environment attacks organic molecules
atmosphere30
CO₂ atmosphere with moderate greenhouse effect (partially stripped by slow rotation)
temperature70
Challenging but potentially habitable temperature
magnetic Field30
No magnetic field - vulnerable to solar radiation
Physical Properties
Mass
4.40x Earth (2.63e+25 kg)
Radius
1.64x Earth (10,440 km)
Surface Gravity
1.64x Earth (16.1 m/s²)
Surface Temperature
314 K (41 °C / 105 °F)
Rotation Period
370.0 hours/day (slower than Earth)
Orbital Environment
Star Type
F-type (White)
Distance from Star
6.11 AU (914 million km)
Orbital Period
13.2 years
Atmosphere
Thin CO₂ atmosphere
Elemental Composition
Cr - Chromium
34.5%
C - Carbon
19.0%
H - Hydrogen
19.0%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build