Rocky Terrestrial
No life — too hot for liquid waterMagnetic FieldModerate Activity
Why is this a Rocky Terrestrial?Your planet is dominated by silicate (45.6%) and iron (0.0%) content, forming a rocky terrestrial body.Rocky terrestrial planets are primarily composed of silicate rocks and metals. They're the most common type of small planet in the universe.
✓ Silicon: 45.6% + Iron: 0.0% + Magnesium: 0.0%✓ Mass: 1.0x Earth (terrestrial range)
Habitability ScoreMarginal
Contributing Factorswater90
Good water contentgeology90
Active geology recycles nutrients and drives carbon cyclerotation10
Near tidally locked - one hemisphere perpetually scorched, other frozen, narrow habitable twilight zone onlyOrganic Chemistry50
Carbon and hydrogen present - organic chemistry possibleatmosphere14
Dense CO₂ atmosphere with extreme greenhouse effect (partially stripped by slow rotation)temperature45
Extreme temperature - very difficult for 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)) Physical Properties
Mass
1.00x Earth (5.97e+24 kg)Radius
1.00x Earth (6,371 km)Surface Gravity
1.00x Earth (9.8 m/s²)Surface Temperature
350 K (77 °C / 171 °F)Rotation Period
24.0 hours/dayOrbital Environment
Star Type
M-type (Red Dwarf)Distance from Star
0.15 AU (22.4 million km)Atmosphere
Thin CO₂ atmosphere
Surface Characteristics
Rocky surface with impact craters, possible volcanic featuresMoons
Moon 1recedingIce lost: volcanic rock10% - 20.4 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Tidal braking locked the planet to its moon: one face forever moonward.
Too warm for ice and too small to hold an atmosphere: the ice sublimated, leaving bare rock.
Tidal flexing melts its interior: an actively volcanic surface (Io-like).
+5 temperature: large moon stabilizes the axial tilt - steady seasons+5 magneticField: a large close moon may help stir the core dynamo (speculative)