Habitability
30/ 100
Extremely Harsh

Jarvarian

Lava World

Magnetic FieldExtreme Activity
Why is this a Lava World?A moon inside the synchronous orbit spiraled in and struck the planet. The impact remelted the surface into a global magma ocean.
Tidal decay drags close-in moons down over millions of years. A large enough impactor liquefies the crust, strips atmosphere, and resets the surface - whatever the orbit's temperature would otherwise allow.
Classification Criteria:
✓ Moon inside the synchronous orbit (tidal decay)✓ Impactor massive enough to remelt the crust- Orbit itself was fine: 1.00 AU, 278K equilibrium
Habitability ScoreExtremely Harsh
30
Contributing Factors
water50
Limited water content
geology50
Extreme volcanic activity may be hazardous (impact-resurfaced crust)
rotation10
Near tidally locked - one hemisphere perpetually scorched, other frozen, narrow habitable twilight zone only
Organic Chemistry84
Core organic elements (CHNO) present (tidal pools cycle wet and dry - a boost for prebiotic chemistry)
atmosphere38
Nitrogen-oxygen atmosphere - breathable and protective (partially stripped by slow rotation) (atmosphere partially stripped by the moon impact)
temperature15
Optimal temperature range for liquid water and life (surface remelted by the moon impact - molten regardless of orbit)
magnetic Field100
Magnetic field provides radiation protection

Physical Properties

Mass
1.00x Earth (5.97e+24 kg)
Radius
1.00x Earth (6371 km)
Surface Gravity
1.00x Earth (9.8 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 (149597871 million km)

Atmosphere

Nitrogen-oxygen atmosphere with trace CO₂, water vapor, and argon

Elemental Composition

O - Oxygen
31.3%
Si - Silicon
25.0%
N - Nitrogen
12.5%

Surface Characteristics

Surface remelted by a catastrophic moon impact - a global magma ocean cooling into scarred rock
Moons
Moon 1rings0.098% - 2.1 radii

Inside the Roche limit (2.80 planet radii): torn apart into a ring system.

Moon 2crashed0.10% - 5.6 radii

Inside the synchronous orbit: tidal decay dragged it down - it struck the planet ages ago.

Moon 3receding0.10% - 15.0 radii

Outside the synchronous orbit: slowly receding, like Luna (~cm per year).

+4 chemistry: tidal pools cycle wet and dry - a boost for prebiotic chemistry-2 atmosphere: atmosphere partially stripped by the moon impact+10 geology: impact-resurfaced crust-85 temperature: surface remelted by the moon impact - molten regardless of orbit