Why is this a Earth Like?Your planet has a balanced composition with all CHNOPS elements, proper mass (3.5x Earth), and sits in the habitable zone at 0.71 AU.
Earth-like planets have the perfect combination of composition, temperature, mass, and magnetic field to potentially support complex life as we know it.
Classification Criteria:
✓ All CHNOPS elements present (C, H, N, O, P, S)✓ Mass: 3.5x Earth (0.5-2.0x range)✓ Temperature: 281K (250-320K range)✓ Magnetic field present✓ Distance: 0.71 AU (habitable zone)
Habitability ScoreMarginal
43
Contributing Factors
water90
Good water content — shielded under ice and rock, a subsurface refuge could outlast the blast
geology100
Active geology recycles nutrients and drives carbon cycle (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
atmosphere40
Nitrogen-oxygen atmosphere - breathable and protective (partially stripped by slow rotation)
temperature100
Optimal temperature range for liquid water and life (large moon stabilizes the axial tilt - steady seasons)
magnetic Field100
Magnetic field provides radiation protection (a large close moon may help stir the core dynamo (speculative)) — but the remnant's shock fronts flood this orbit with cosmic rays
Physical Properties
Mass
3.50x Earth (2.09e+25 kg)
Radius
1.52x Earth (9,673 km)
Surface Gravity
1.52x Earth (14.9 m/s²)
Surface Temperature
281 K (8 °C / 47 °F)
Rotation Period
16.0 hours/day (faster than Earth)
Orbital Environment
Star Type
SNR-type (Supernova Remnant)
Distance from Star
0.71 AU (106 million km)
Orbital Period
185 days
Atmosphere
Nitrogen-oxygen atmosphere with trace CO₂, water vapor, and argon
Elemental Composition
O - Oxygen
25.0%
Si - Silicon
22.9%
Fe - Iron
16.7%
Surface Characteristics
Rocky surface with continents, oceans, and active plate tectonics. Diverse biomes if life present.
Inside the Roche limit (2.80 planet radii): torn apart into a ring system.
Moon 2receding1.0% - 7.3 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Tidal braking locked the planet to its moon: one face forever moonward.
+5 temperature: large moon stabilizes the axial tilt - steady seasons+10 geology: tidal flexing sustains geologic activity+5 magneticField: a large close moon may help stir the core dynamo (speculative)