No life — no phosphorus — DNA and ATP are built on itMagnetic FieldHigh Activity
Why is this a Exotic Terrestrial?Your planet builds its crust from exotic minerals (24.7% 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: 24.7% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 10.2% (<15% - silicate rules never claimed it)✓ Temperature: 265K (240-380K temperate band)✓ Air + water ingredients: 38.6% O+H (>=15%) with an atmosphere
Habitability ScoreHighly Habitable
86
Contributing Factors
water93
Abundant water - mostly frozen
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
atmosphere100
Nitrogen-oxygen atmosphere - breathable and protective
temperature70
Challenging but potentially habitable temperature
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
1.20x Earth (7.17e+24 kg)
Radius
1.06x Earth (6,770 km)
Surface Gravity
1.06x Earth (10.4 m/s²)
Surface Temperature
265 K (-8 °C / 18 °F)
Rotation Period
10.0 hours/day (faster than Earth)
Orbital Environment
Star Type
M-type (Red Dwarf)
Distance from Star
0.22 AU (32.9 million km)
Orbital Period
69 days
Atmosphere
Nitrogen-oxygen atmosphere over exotic mineral flats
Elemental Composition
H - Hydrogen
23.3%
Ni - Nickel
17.2%
O - Oxygen
15.3%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build