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Entering orbit…
Habitability
15/ 100
Uninhabitable
GJ 1002 c rendered in TerraForge from its measured mass, orbit and star

GJ 1002 c

Also written GJ 1002c

Ice World16 light years awayFound 2022
Mass
1.36 × Earth
Radius
1.10 × Earth
Gravity
1.12 g
Surface (est.)
201 K
Year
21.2 days
From Earth
15.8 ly
Mass
1.36 × Earth
Radius
1.10 × Earth
Gravity
1.12 g
Surface (est.)
201 K
Year
21.2 days
From Earth
15.8 ly

GJ 1002 system

Type
M-type (Red Dwarf)
Spectral type
M5.5 V
Temperature
3,024 K
Radius
0.137 ☉
Mass
0.12 ☉
Planets
2
Luminosity
1.41e-3 ☉

Published by the NASA Exoplanet Archive. This world’s temperature and habitability score are computed from this star’s measured luminosity, not from a stand-in for its class.

Habitable zone

Star and planets drawn to scale: the star is 14 times as wide as GJ 1002 c, so only its edge is in view. Orbits spaced as in the star system view.

Estimated: this planet doesn't transit its star, so its size is inferred, not measured

GJ 1002 c, from the NASA Exoplanet Archive (found 2022). Measured: 1.36 Earth masses, 0.0738 AU, a 3024 K M-type star. Composition inferred from an estimated bulk density of 1.02x Earth's, modeled rather than measured since this isn't a transiting planet — the radius is the archive's estimate, so it can't settle how much water there is; read as rock and iron, with a day locked to its 21.2-day year, as anything orbiting this close would be.

Surface. Frozen surface covered in water ice, possible subsurface ocean if tidal heating present

Ice World
Life unlikely — too cold for liquid waterModerate Activity
GJ 1002 c orbits at 0.07 AU from its star, resulting in frigid temperatures of 201K.
Ice worlds form beyond the frost line where temperatures are low enough for water and other volatiles to freeze solid. They may have subsurface oceans beneath thick ice shells.
Classification Criteria:
✓ Distance: 0.07 AU (>3 AU) or Temperature <200K✓ Temperature: 201K✓ Water content: 34.4% for ice formation

Reading GJ 1002 c’s atmosphere

Dominant elements: O, Si, Fe, N, C, HThis is what a telescope would measure while GJ 1002 c 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.GJ 1002 c sits about 16 light-years away, found by the radial velocity method. Most catalogued distances trace back to 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.
Habitability ScoreUninhabitable
15
Contributing Factors
temperature21
Extreme cold - very difficult for life
atmosphere28

Thin nitrogen and methane atmosphere

Nitrogen atmosphere provides protection but not breathable (partially stripped by slow rotation)
water20
Limited water content - frozen solid, no liquid phase at this temperature
magnetic Field30
No magnetic field - vulnerable to solar radiation
geology90
Active geology recycles nutrients and drives carbon cycle
Organic Chemistry80
Core organic elements (CHNO) present
rotation10
Near tidally locked - one hemisphere perpetually scorched, other frozen, narrow habitable twilight zone only

Physical Properties

Mass
1.36x Earth (8.12e+24 kg)
Radius
1.11x Earth (7,059 km)
This planet: 1.11× Earth radiusEarth: 1× (baseline)
Surface Gravity
1.11x Earth (10.9 m/s²)
Surface Temperature
201 K (-72 °C / -98 °F)
Rotation Period
508.8 hours/day (slower than Earth)
This planet: 509 h/dayEarth: 24 h/day

Elemental Composition

A dark ringed planet hanging over the horizon of a rocky moon, its rings lit by a distant sun

New: Stand on Your Moons 🌒

A planet's surface view isn't the only ground any more. Press the surface button on a planet with moons and it asks where to stand: the planet itself, or any moon still in orbit, each tagged with what it became — ocean, ice, carbon, volcanic. Every moon gets its own ground and sky from its own physics: airless rock under a black sky, ice cracked by geysers over a hidden sea, sulfur plains shaking with eruptions, or orange haze you can't see the sun through. And hanging over the horizon, there's the planet you built.

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