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Planet profiles

TRAPPIST-1 f

Ice World · 40 light-years away · Last reviewed October 14, 2026

TRAPPIST-1 f rendered in TerraForge from its measured mass, orbit and star
TerraForge's rendering of TRAPPIST-1 f, generated by our physics engine from its measured mass, size, orbit and star. An illustration of what the science suggests, not a photograph.
TerraForge classification
Ice World
Host star
TRAPPIST-1 (M8.0 V)
Distance
40 light-years
Orbit
9.21 days
Mass
1.04 × Earth
Radius
1.04 × Earth
Discovered
2017, transit

Figures from the NASA Exoplanet Archive. The classification is TerraForge’s, from its physics model.

In bulk, TRAPPIST-1 f is the member of its family that most resembles Earth: its mass and its width are both about 1.04 times Earth's. It lies in its star's habitable zone, the range of distances where liquid water could last on a surface given the right atmosphere. Yet it receives only about as much energy from its dim red star as Mars gets from the Sun, and it completes an orbit every 9.21 days.

Planet f was announced in Nature in February 2017 by a team led by Michaël Gillon, from transits seen with NASA's Spitzer Space Telescope and telescopes on the ground. A transit is the small dip in starlight when a planet crosses in front of its star. The same study found the six inner planets moving in a near-resonant pattern: their periods of 1.51, 2.42, 4.04, 6.06, 9.21 and 12.35 days form nearly whole-number ratios. That suggests the planets formed farther out and migrated inward.

Those tightly linked orbits also let astronomers weigh the planets. Each planet tugs on its neighbours and slightly shifts when their transits happen. Using these timing shifts, a 2021 study led by Eric Agol measured all seven masses to within 3 to 5 percent. It found that one rocky recipe, lighter than Earth's, fits every planet. Either they hold less iron, about 21 percent by weight against Earth's 32, or they have Earth-like iron plus extra light material, such as water at the surface.

Webb's first transit spectra of f come from five transits observed with its NIRISS instrument, in a study led by Olivia Lim, accepted for publication in 2026. At least one stellar flare struck during every visit. Unlike spectra of planets closer in, f's showed no clear contamination from spots on the star, though the team cautions this may not hold in future visits. The cleanest visits rule out atmospheres dominated by hydrogen and helium thicker than about 20 millibars, roughly 2 percent of Earth's surface pressure. For heavier atmospheres, such as nitrogen or carbon dioxide, the limits depend on how the data are processed, so whether f has air remains open. Webb has found little to no atmosphere on b and c, the two innermost planets.

TerraForge's model, working only from f's mass, orbit and star, classifies it as an ice world at 222 K, near the archive's equilibrium temperature of 218 K, the temperature from starlight alone with no greenhouse warming. That is a fair reading of a Mars-like energy budget, and Agol's study leaves room for surface water. But f's density matches its rocky siblings, and without a detected atmosphere nobody can yet say whether its surface is ice, bare rock or ocean.

Sources

  1. Seven temperate terrestrial planets around the nearby ultracool dwarf star TRAPPIST-1 — Nature (arXiv:1703.01424)
  2. Ultracool Dwarf and the Seven Planets — ESO
  3. Refining the transit timing and photometric analysis of TRAPPIST-1: Masses, radii, densities, dynamics, and ephemerides — The Planetary Science Journal (arXiv:2010.01074)
  4. Atmospheric Reconnaissance of TRAPPIST-1 f with JWST NIRISS SOSS: No Evidence for the Transit Light Source Effect — The Astronomical Journal, accepted (arXiv:2608.17207)
A banded gas giant with four moons in different colors: a yellow sulfur moon, two rust-red rock moons and a blue water moon

New: Choose What Your Moons Are Made Of 🌙

Every moon used to be grey rock, white ice or blue ocean, decided for you. Now each one has a "Made of" choice in the builder's Moons tab — silicate rock, iron, water ice, carbon, sulfur, or nitrogen and methane ice — and the physics decides what that becomes. Put water ice too close to the star and it boils off to bare rock. Put sulfur where a neighbouring moon keeps it tidally flexed and it erupts in Io's yellows. Give a Titan-sized moon nitrogen ice far from the sun and it wraps itself in haze. Hang a water moon about the mass of Earth off a giant planet in the habitable zone and it can hold air and open seas — scored for life on the same scale as a planet, with a day as long as its orbit. A tint slider nudges the colour, but only as far as that material could really go.

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