Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (56.3% 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: 56.3% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 0.0% (<15% - silicate rules never claimed it)✓ Temperature: 261K (240-380K temperate band)✓ Air + water ingredients: 15.5% O+H (>=15%) with an atmosphere
Habitability ScoreExtremely Harsh
25
Contributing Factors
water45
Limited water content - mostly frozen — shielded under ice and rock, a subsurface refuge could outlast the blast
geology90
Active geology recycles nutrients and drives carbon cycle
rotation100
Optimal rotation period - balanced day/night cycle, moderate weather, and good heat distribution
Organic Chemistry20
Limited organic chemistry potential
atmosphere70
Nitrogen atmosphere provides protection but not breathable
temperature70
Challenging but potentially habitable temperature
magnetic Field100
Magnetic field provides radiation protection — but the remnant's shock fronts flood this orbit with cosmic rays
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
261 K (-12 °C / 11 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
SNR-type (Supernova Remnant)
Distance from Star
0.80 AU (120 million km)
Orbital Period
221 days
Atmosphere
Thin nitrogen atmosphere
Elemental Composition
N - Nitrogen
28.2%
Al - Aluminum
14.1%
Ca - Calcium
14.1%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build