Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (18.5% 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: 18.5% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 3.4% (<15% - silicate rules never claimed it)✓ Temperature: 374K (240-380K temperate band)✓ Air + water ingredients: 53.0% O+H (>=15%) with an atmosphere
Habitability ScoreMarginal
59
Contributing Factors
water100
Abundant water - likely as steam
geology90
Active geology recycles nutrients and drives carbon cycle
rotation100
Optimal rotation period - balanced day/night cycle, moderate weather, and good heat distribution
Organic Chemistry50
Carbon and hydrogen present - organic chemistry possible
atmosphere35
Dense COâ‚‚ atmosphere with extreme greenhouse effect
temperature40
Extreme temperature - very difficult for life
magnetic Field100
Magnetic field provides radiation protection
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
374 K (101 °C / 213 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
0.99 AU (148 million km)
Orbital Period
360 days
Atmosphere
Thin COâ‚‚ atmosphere
Elemental Composition
O - Oxygen
34.7%
H - Hydrogen
18.3%
Ti - Titanium
16.0%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build