Water World Life possible Magnetic Field Moderate Activity
Why is this a Water World? Your planet has abundant oxygen (32.0%) and hydrogen (16.4%), creating extensive water coverage while in the habitable temperature zone. Water worlds have deep global oceans covering most or all of their surface. They form when planets have high water content and orbit in the habitable zone.
✓ Oxygen: 32.0% + Hydrogen: 16.4% (water-forming elements) ✓ Temperature: 260K (habitable range) ✓ Distance: 1.15 AU (habitable zone)
Reading your planet’s atmosphere Dominant elements: O, H, N, P, Fe, He This is what a telescope would measure while your planet crosses in front of its star: starlight passes through the atmosphere and spreads into a rainbow band. Each dark line marks a wavelength the atmosphere absorbed. Every element absorbs its own signature wavelengths — hydrogen always darkens the same two spots, calcium another pair, and so on. Astronomers match the lines in a real spectrum against a library of these signatures to say what an atmosphere is made of, light-years away, without ever visiting. A deeper line generally means more of that element is present. For a real planet, distance is usually measured by parallax: as Earth orbits the Sun, a nearby star appears to shift very slightly against the distant background stars, and the size of that shift gives its distance directly — the same geometry surveyors use, at an interstellar scale. Close
Habitability Score Habitable
Contributing Factors water 89
Abundant water - mostly frozen geology 100
Active geology recycles nutrients and drives carbon cycle (tidal flexing sustains geologic activity) rotation 10
Near tidally locked - one hemisphere perpetually scorched, other frozen, narrow habitable twilight zone only Organic Chemistry 100
All CHNOPS elements present - building blocks of life atmosphere 40
Nitrogen-oxygen atmosphere - breathable and protective (partially stripped by slow rotation) temperature 70
Challenging but potentially habitable temperature magnetic Field 100
Magnetic field provides radiation protection Physical Properties Mass
2.00x Earth (1.19e+25 kg) Radius
1.26x Earth (8,027 km) This planet: 1.26× Earth radius Earth: 1× (baseline)
Surface Gravity
1.26x Earth (12.4 m/s²) Surface Temperature
260 K (-13 °C / 8 °F) Rotation Period
24.0 hours/day This planet: 24 h/day Earth: 24 h/day Orbital Environment Star Type
G-type (Yellow (Sun-like)) Distance from Star
1.15 AU (172 million km) Atmosphere Nitrogen and oxygen with water vapor, mild greenhouse effect
Surface Characteristics Vast oceans covering most of the surface, scattered islands or archipelagos Moons
Moon 1 merged 0.22% - 18.2 radii
Merged with an adjacent moon: too close for both to hold a stable orbit.
Moon 2 receding 0.22% - 8.2 radii Stand on this moonOutside the synchronous orbit: slowly receding, like Luna (~cm per year).
Tidal braking locked the planet to its moon: one face forever moonward.
Moon 3 merged 0.022% - 16.7 radii
Merged with an adjacent moon: too close for both to hold a stable orbit.
Moon 4 receding 0.035% - 14.6 radii Stand on this moonOutside the synchronous orbit: slowly receding, like Luna (~cm per year).
+10 geology: tidal flexing sustains geologic activity
Habitability ✓ Conditions could support life This 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.