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Factlen ExplainerUranus CompositionScience ExplainerJun 19, 2026, 7:19 PM· 4 min read· in science

Deep Atmospheric Gas Reveals Uranus Has a True Icy Center

New measurements of carbon monoxide in Uranus's deep atmosphere indicate the planet contains significantly more ice than rock, resolving a long-standing mystery about its formation.

By Logan Price

Planetary Formation Theorists 40%Observational Astronomers 35%Space Exploration Advocates 25%
Planetary Formation Theorists
Scientists modeling the early Solar System who use chemical tracers to reconstruct where and how the planets formed.
Observational Astronomers
Researchers utilizing advanced telescopes to pierce the planet's hazy upper atmosphere and read its chemical signature.
Space Exploration Advocates
Mission planners who argue that remote observations must eventually be validated by sending a spacecraft directly to the planet.

For decades, Uranus has been the Solar System's most perplexing outlier. Tilted entirely on its side, lacking significant internal heat, and shrouded in a featureless cyan haze, the seventh planet has defied easy categorization.[6]

Now, a new analysis of the gas deep within Uranus's atmosphere has provided a crucial clue to its origins. By measuring the abundance of carbon monoxide, researchers have determined that the planet's interior contains significantly more ice than rock.[1]

The findings, reported this week, suggest that Uranus formed much more like its sister planet, Neptune, than previously thought. This challenges older models that posited distinct formation pathways or vastly different building blocks for the two ice giants.[1][3]

To understand the significance of this discovery, one must look back to the chaotic early days of the Solar System. The giant planets—Jupiter, Saturn, Uranus, and Neptune—all formed from a swirling protoplanetary disk of gas and dust surrounding the young Sun.[2]

The internal structure of an ice giant, featuring a massive supercritical fluid mantle.

While Jupiter and Saturn swept up massive amounts of hydrogen and helium to become gas giants, Uranus and Neptune grew more slowly. By the time their cores were massive enough to capture gas, the solar nebula was already dissipating.[3]

As a result, Uranus and Neptune are classified as "ice giants." In planetary science, "ice" does not just mean frozen water; it refers to volatiles like water, ammonia, and methane that exist in a hot, dense, supercritical fluid state deep within the planet's mantle.[6]

The exact ratio of these ices to heavier rocky material has long been a subject of intense debate. Because Uranus's atmosphere is incredibly cold—dropping to −224 degrees Celsius—most of its heavier elements are locked away deep below the visible cloud tops, making them exceptionally difficult to measure.[6]

Carbon monoxide serves as a vital chemical tracer in this context. At the extreme pressures and temperatures found deep in the troposphere, thermochemical equilibrium dictates the balance of carbon-bearing molecules.[7]

Uranus bridges the gap between rocky terrestrial worlds and massive gas giants.
Carbon monoxide serves as a vital chemical tracer in this context.

If a planet accreted a high proportion of icy planetesimals during its formation, its deep atmosphere should be highly enriched with oxygen, which in turn drives the production of carbon monoxide.[3][7]

The new data reveals a carbon monoxide signature that points definitively to an ice-dominated interior. The measured abundances indicate that Uranus's building blocks were rich in water and carbon monoxide ices, rather than dry silicate rock.[1]

This composition strongly implies that Uranus formed further out in the solar nebula, near the "carbon monoxide ice line"—the specific boundary where temperatures were low enough for carbon monoxide to freeze into solid grains.[5]

Previously, some dynamicists argued that Uranus might have formed closer to the Sun and migrated outward, or that it suffered a catastrophic giant impact that fundamentally altered its internal structure and knocked it onto its side.[4]

Uranus likely formed near the carbon monoxide ice line in the early solar nebula.

While the giant impact theory remains the best explanation for Uranus's extreme 98-degree axial tilt, the new chemical evidence suggests its fundamental building blocks were nearly identical to Neptune's.[1][4]

The alignment between Uranus and Neptune simplifies the narrative of the outer Solar System. It supports models which suggest the ice giants formed in a compact, volatile-rich configuration before being scattered outward by gravitational interactions with Jupiter and Saturn.[5]

This breakthrough also has profound implications for the study of exoplanets. Intermediate-mass planets similar in size to Uranus and Neptune are the most common type of world discovered in the galaxy, making our local ice giants the ultimate reference models.[2]

Despite these advances, remote observations can only pierce so far through the Uranian haze. The ultimate test of these formation models will require sending a spacecraft to sample the atmosphere directly.[4]

A proposed Uranus Orbiter and Probe mission would drop a sensor directly into the atmosphere.

The planetary science community has already mobilized around this goal. The National Academies' most recent Decadal Survey prioritized a Uranus Orbiter and Probe as the flagship mission for the 2030s, designed to drop a sensor directly into the cyan clouds.[4]

Until that probe descends, astronomers will continue to rely on the faint chemical whispers of molecules like carbon monoxide. For now, those whispers are telling a clearer story: Uranus is a true ice giant, born in the deep freeze of the outer solar nebula.[2]

Definitions

Ice Giant
A class of giant planet composed mainly of elements heavier than hydrogen and helium, such as oxygen, carbon, nitrogen, and sulfur.
Supercritical fluid
A state of matter where distinct liquid and gas phases do not exist, occurring at extremely high temperatures and pressures deep inside planets.
Protoplanetary disk
The rotating disk of dense gas and dust surrounding a newly formed star, from which planets eventually coalesce.
CO Ice Line
The specific distance from a young star where temperatures drop low enough for carbon monoxide gas to freeze into solid ice grains.
14.5x
Uranus's mass relative to Earth
−224 °C
Minimum atmospheric temperature
98 degrees
Uranus's extreme axial tilt
84 years
Orbital period around the Sun

Limits of the evidence

  • Whether Uranus and Neptune formed in their current orbits or migrated outward over time.
  • The exact mechanism that caused Uranus's extreme 98-degree axial tilt.
  • The precise isotopic ratios of noble gases within Uranus's atmosphere, which require an in situ probe to measure.

Sources

Source coverage

7 outlets

3 viewpoints surfaced

Planetary Formation Theorists 40%Observational Astronomers 35%Space Exploration Advocates 25%
  1. [1]New ScientistObservational Astronomers

    Gas from Uranus reveals it has an icy centre

    Read on New Scientist
  2. [2]Factlen Editorial TeamSpace Exploration Advocates

    Synthesis by Factlen editorial team

    Read on Factlen Editorial Team
  3. [3]Royal Society PublishingPlanetary Formation Theorists

    The origin of the ice giants: constraints from elemental abundances

    Read on Royal Society Publishing
  4. [4]National AcademiesSpace Exploration Advocates

    Origins, Worlds, and Life: A Decadal Strategy for Planetary Science and Astrobiology 2023-2032

    Read on National Academies
  5. [5]AstrobitesPlanetary Formation Theorists

    The Measured Compositions of Uranus and Neptune from Their Formation on the CO Iceline

    Read on Astrobites
  6. [6]WikipediaObservational Astronomers

    Uranus

    Read on Wikipedia
  7. [7]arXivObservational Astronomers

    Carbon, oxygen and nitrogen-bearing species in deep atmospheres

    Read on arXiv

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