An Interstellar Visitor Wrapped in Amorphous Glass Dust express

Original: "The Dust Mineralogy of Interstellar Comet 3I/ATLAS from JWST/MIRI Observations"
arXiv:2606.27535 · 2026-06-25 · CC BY 4.0 · 2 min
The James Webb Space Telescope has, for the first time, peered into the composition of dust around an interstellar object, and it looks nothing like our comets.

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In 2019, an unusual visitor, comet 3I/ATLAS, zoomed into the Solar System. It came from another star, and for the first time, astronomers were able to see what its dusty tail is made of. The MIRI instrument on the James Webb Space Telescope caught a characteristic emission peak at a wavelength of 10 microns. Such a signal is familiar from interstellar dust and from the distant disks around young stars where planets are just being born.

That peak revealed the dust's composition. Comets in our system are usually rich in crystalline silicates — tiny grains with an ordered structure, like sand grains shaped by nature. 3I/ATLAS is different: its dust is almost entirely amorphous silicates — shapeless, like solidified glass. It resembles the raw material of the interstellar medium more than the mixed-up stuff that makes up our comets.

Amorphous silicates are particles without a crystal lattice, like ordinary window glass. In space, they are often found in cold clouds of gas and dust.

Why is that? Perhaps 3I/ATLAS was born on the outskirts of its system, where material never passed through the furnace of temperatures near the star. There were no conditions for crystallization. Alternatively, over a billion years of wandering, cosmic rays might have shattered the crystals, turning them into an amorphous state. But the authors doubt this: the object is losing mass too quickly, and its dust spectrum differs from what is seen in "aged" comets of the Solar System.

The interstellar journey of 3I/ATLAS may have lasted more than a billion years — about as long as some stars live.

The telescope captured a signal that came to us from a wanderer that never knew our Sun. Its dust is a frozen story of another world, and now we are learning to read it.

Original abstract

as written by the authors arXiv:2606.27535

We present the first spectroscopic mineralogical analysis of the dust coma of an interstellar object (ISO) from JWST mid-infrared spectroscopy of 3I/ATLAS (3I). 3I exhibits a strong 10-micron emissivity feature commonly seen on asteroids, comets, disks, and the interstellar medium. Characterization of this 10-micron emissivity maximum reveals that 3I's dust composition is dominated by amorphous silicates, and that 3I is unlike Solar System comets, which show significant crystalline silicate dust. Instead, 3I's dust composition is more similar to circumstellar transition disks and the interstellar medium. We suggest 3I may have formed in a distant part of its home system out of interstellar medium-like material, without substantial incorporation of silicates condensed near its host star, unlike the mixing scenarios commonly hypothesized for Solar System comets. Alternatively, 3I's original crystalline silicates may have been amorphized during its Gyr-long journey, although we find this alternative less likely due to 3I's mass loss rate and distinct 10 micron feature as opposed to observed Solar System comets.

The dust grains in the coma of 3I/ATLAS resemble not beach sand but tiny shards of volcanic glass: they were never crystals.

In Arthur C. Clarke's novel "Rendezvous with Rama," humanity encounters an interstellar object, but its true nature turns out to be far more artificial than our icy wanderer.

Scientists
Michael FaradayHendrik LorentzEmile ClapeyronIsaac NewtonJohn MichellRobert Hooke
Concepts
dust cosmic dust analysis comet interstellar gas interstellar object asteroid belt young stellar object comet tail star formation gas oort cloud perovskite organic molecules in space ice grain molecular formation intracluster medium asteroid molecular cloud population iii stars ionized carbon astrochemical synthesis methanol