Now: perfect life
2 billion years: life rises
5 billion years: the oxygen runs out with 15-5 per life
7 billion years: it's water evaporates, and now it soon disappeared
9.5 billion years: the planet turns into a dwarf planet, until then control of this planet dies.
Exotic Terrestrial
Life possibleMagnetic FieldHigh Activity
Why is this a Exotic Terrestrial?
Your planet builds its crust from exotic minerals (18.0% 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: 18.0% (>=12% Ca/Ti/Al/K/Ni/U)✓ Standard rock: 13.5% (<15% - silicate rules never claimed it)✓ Temperature: 278K (240-380K temperate band)✓ Air + water ingredients: 34.2% O+H (>=15%) with an atmosphere
Habitability ScoreHighly Habitable
89
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 Chemistry80
Core organic elements (CHNO) present — but the ground itself is radioactive, and no magnetic field shields a world from its own crust
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
3.10x Earth (1.85e+25 kg)
Radius
1.46x Earth (9,290 km)
Surface Gravity
1.46x Earth (14.3 m/s²)
Surface Temperature
278 K (5 °C / 41 °F)
Rotation Period
24.0 hours/day
Orbital Environment
Star Type
G-type (Yellow (Sun-like))
Distance from Star
1.00 AU (150 million km)
Orbital Period
1.00 years
Atmosphere
Nitrogen-oxygen atmosphere over exotic mineral flats
Elemental Composition
O - Oxygen
23.4%
Fe - Iron
12.6%
H - Hydrogen
10.8%
Surface Characteristics
Pale mineral plains — carbonate flats, chalk mesas, and crusts no silicate world can build
✓ Conditions could support lifeThis planet’s modelled conditions could support biological processes: stable temperatures, liquid water and the chemistry life as we know it needs. That makes life possible, not present.