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Ice Giant
✦ PrismatopiaMagnetic FieldExtreme Activity
Why is this a Ice Giant?Your planet has moderate mass (210.0x Earth) with significant water, carbon, and nitrogen content, characteristic of ice giants.
Ice giants like Uranus and Neptune have icy interiors with thick atmospheres of hydrogen and helium, but not enough to be classified as gas giants.
Classification Criteria:
✓ Mass: 210.0x Earth (5-20x range)✓ Water/Carbon/Nitrogen rich composition
Habitability ScoreUninhabitable
Contributing Factors
water15
No solid surface — any water is locked in a supercritical mantle and hot ice, not oceans
geology50
Extreme volcanic activity may be hazardous (tidal flexing sustains geologic activity)
rotation10
Near tidally locked - one hemisphere perpetually scorched, other frozen, narrow habitable twilight zone only
Organic Chemistry100
All CHNOPS elements present - building blocks of life (tidal pools cycle wet and dry - a boost for prebiotic chemistry)
atmosphere12
Hydrogen-rich atmosphere typical of gas giants (partially stripped by slow rotation)
temperature10
Frozen world - minimal potential for complex life
magnetic Field100
Magnetic field provides radiation protection
Physical Properties
Mass
210.00x Earth (1.25e+27 kg)Radius
5.94x Earth (37,869 km)Surface Gravity
5.94x Earth (58.3 m/s²)Surface Temperature
96 K (-178 °C / -288 °F)Rotation Period
16.0 hours/day (faster than Earth)Orbital Environment
Star Type
F-type (White)Distance from Star
40.50 AU (6.06 billion km)Orbital Period
226.1 yearsAtmosphere
Hydrogen and helium with water, methane, and ammonia ices
Elemental Composition
H - Hydrogen
36.4%
He - Helium
22.7%
C - Carbon
13.6%
Surface Characteristics
No solid surface - a deep volatile envelope over a supercritical water mantle and hot-ice interiorClosest Real Exoplanet
HD 140901 c71% similar
Orbiting HD 140901| Yours | HD 140901 c | |
|---|---|---|
| Mass | 210.0 × Earth | 572.0 × Earth |
| Radius | 8.98 × Earth | 13.4 × Earth |
| Density (composition) | 1.60 g/cm³ | 1.31 g/cm³ |
| Temperature | 95.6 K | 77.0 K |
| Starlight received | 0.00 × Earth | 0.01 × Earth |
| Star temperature | 6,750 K | 5,610 K |
MoonsLife may exist on a moon
Moon 1recedingOcean world - life0.056% - 6.9 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Tidal braking locked the planet to its moon: one face forever moonward.
Tidal heat sustains a subsurface ocean over a rock seafloor: a strong candidate for life (Europa-like, 51/100).
Moon 2recedingOcean world - life0.10% - 9.9 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Tidal heat sustains a subsurface ocean over a rock seafloor: a strong candidate for life (Europa-like, 91/100).
Moon 3rings0.079% - 3.2 radii
Inside the synchronous orbit: it spiraled inward and was torn apart at the Roche limit (Phobos's fate).