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Entering orbit…
Habitability
9/ 100
Uninhabitable
Kepler-1642 b rendered in TerraForge from its measured mass, orbit and star

Kepler-1642 b

Also written Kepler-1642b, Kepler 1642b, Kepler 1642 b

Sub-Neptune1350 light years awayFound 2016
Mass
10.30 × Earth
Radius
3.20 × Earth
Gravity
1.01 g
Surface (est.)
700 K
Year
12.2 days
From Earth
1,350 ly
Mass
10.30 × Earth
Radius
3.20 × Earth
Gravity
1.01 g
Surface (est.)
700 K
Year
12.2 days
From Earth
1,350 ly

Kepler-1642 system

Type
G-type (Yellow (Sun-like))
Temperature
5,355 K
Radius
0.84 ☉
Mass
0.88 ☉
Planets
2
Luminosity
0.394 ☉

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 29 times as wide as Kepler-1642 b, so only its edge is in view. Orbits spaced as in the star system view.

Kepler-1642 b, from the NASA Exoplanet Archive (found 2016). Measured: 10.3 Earth masses, 0.102 AU, a 5355 K G-type star. Composition inferred from a measured bulk density of 0.31x Earth's, too low for bare rock at this size, suggesting a rocky core under roughly a 10% hydrogen/helium envelope by mass, with an assumed 24-hour day — rotation cannot be measured for exoplanets.

Surface. No solid surface - a hydrogen-helium envelope wrapped around a rocky core (a sub-Neptune)

Sub-Neptune
Life unlikely — too hot for liquid waterMagnetic FieldLow Activity
Kepler-1642 b is a sub-Neptune: a 10.3x Earth core wrapped in a deep hydrogen-helium envelope, with no solid surface to stand on.
Sub-Neptunes are the most common planets Kepler found, though our own solar system has none. Too light to be a giant, they still hold on to a thick envelope of light gas over a rocky or icy core.
Classification Criteria:
✓ Mass: 10.3x Earth (under 20x, below the giants)✓ A hydrogen-helium envelope over the core

Reading Kepler-1642 b’s atmosphere

Dominant elements: O, Si, Fe, N, C, HThis is what a telescope would measure while Kepler-1642 b 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.Kepler-1642 b sits about 1350 light-years away, found by the transit 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
9
Contributing Factors
temperature4
Scorching - hot enough to melt lead, though rock stays solid; no chance for life
atmosphere30

Deep hydrogen-helium envelope with photochemical haze

Hydrogen-rich atmosphere typical of gas giants
water15
No solid surface — any water is locked in a supercritical mantle and hot ice, not oceans
magnetic Field100
Magnetic field provides radiation protection
geology60
Some geological activity provides slow nutrient cycling
Organic Chemistry80
Core organic elements (CHNO) present
rotation100
Optimal rotation period - balanced day/night cycle, moderate weather, and good heat distribution

Physical Properties

Mass
10.30x Earth (6.15e+25 kg)
Radius
2.18x Earth (13,862 km)
This planet: 2.18× Earth radiusEarth: 1× (baseline)
Surface Gravity
2.18x Earth (21.3 m/s²)
Surface Temperature
700 K (427 °C / 800 °F)
Rotation Period
24.0 hours/day
This planet: 24 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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