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Discover the mysteries of the Sideways Ice Giant, from its tilted cyan clouds and ghostly rings to the frozen moons that circle its frigid skies, and trace humanity’s quest to unveil the secrets of this distant, enigmatic world.
Uranus has no solid surface—its visible “surface” is a frigid cloud deck of hydrogen, helium, and methane. Deeper inside, an “icy” mantle of water, ammonia, and methane surrounds a rocky core.
Uranus’ atmosphere is dominated by hydrogen and helium, tinted cyan by trace methane that absorbs red light. High-altitude haze layers and faint cloud bands drift in temperatures near –224 °C.
Despite being four times Earth’s diameter, Uranus’ low density gives it a surface gravity only slightly weaker than Earth’s. A 100 kg person on Earth would weigh about 89 kg on Uranus.
Uranus spins once every 17 h 14 m—but on its side. Its 98° axial tilt means it essentially rolls around the Sun, producing extreme seasons lasting decades.
Bright methane-ice haze caps appear over each pole during summer, reflecting sunlight and giving the planet a softly glowing crown.
Voyager 2 discovered a “Great Dark Spot” in 1986; Hubble has since watched similar storm vortices form and fade in Uranus’s upper clouds.
Thirteen ultra-dark, razor-thin rings—dominated by the dense ε-ring—encircle Uranus, shepherded by tiny moons like Cordelia and Ophelia.
Largest Uranian moon; scarred by canyons hundreds of kilometers long, hinting at ancient tectonic activity.
The outermost big moon, heavily cratered with bright ejecta rays that stand out against its dark surface ice.
Brightest major moon with intricate networks of fault valleys suggesting relatively recent resurfacing.
Features 20-km-high cliffs and patchwork “coronae,” making it one of the most bizarre landscapes in the Solar System.
The major moons of Uranus likely coalesced from a disk of debris created after a giant impact tilted the planet on its side. Their mixed ice-rock composition supports an origin from Uranus’s own material rather than captured objects.
The Uranus Orbiter & Probe mission—top priority of NASA’s 2023 Planetary Decadal Survey—aims for a launch in the early 2030s. It would conduct multiple close flybys of Ariel, Miranda, Titania, and Oberon, mapping their geology and searching for subsurface oceans.
Voyager 2 remains the only spacecraft ever to visit Uranus. During its historic fly-by it discovered 11 new moons, imaged dark rings, and revealed a magnetic field tilted 59° from the planet’s rotation axis.
As of 2025, no spacecraft are operating at Uranus or heading there. The planet’s only close
visit was Voyager 2 on 24 January 1986.
NASA’s proposed Uranus Orbiter & Probe flagship—endorsed by
the 2023 Planetary Decadal Survey—is still in formulation, targeting a mid-2030s launch but
not yet approved. Until then, Uranus awaits its next explorer.
Top flagship priority of the 2023 Planetary Decadal Survey: a long-lived orbiter paired with an atmospheric entry probe to study Uranus’ interior, rings, moons and extreme magnetosphere.
An ESA medium-class mission concept to orbit Uranus for three years, mapping the magnetic field, sampling the plasma environment and conducting close fly-bys of the major moons.
A joint NASA-ESA concept for a one-hour descent through Uranus’ cloud tops to directly measure noble gases, isotopes and cloud chemistry—key to constraining planet-formation models.
Looking toward the 2040s–2050s, scientists are sketching out bold concepts that could push Uranus exploration even further:
Uranus’ cloud-top temperatures hover near –220 °C, stressing batteries, lubricants and structural materials.
Uranus has narrow, dark rings and abundant moonlet debris that orbiters must traverse during insertion and tour phases.
At 19.8 AU the Sun’s intensity is just 0.25 % of Earth’s, making solar panels largely impractical for primary power.
The only close-range, true-colour view of Uranus, taken ~81,000 km away during the 1986 fly-by. The faint rings were brightened here to show their structure.
Perseverance Rover, Jezero Crater
A string of giant methane-ice storms stripped across the planet’s mid-latitudes; Hubble caught the outbursts glowing cyan.
Adaptive-optics on the Keck II telescope picked up a southern auroral oval (false-colour green), pinpointing Uranus’ wildly tilted magnetic axis.
Voyager 2’s high-res mosaic of moon Ariel shows fresh tectonic canyons cutting through older impact scars—evidence of internal activity.
A processed three-filter view exaggerates high-altitude hazes (pink) and a warmer equator—one of the earliest multi-spectral looks inside the frigid atmosphere.
By stacking long exposures, Hubble revealed two new outer rings and faint shepherd moons—proof the Uranian system is more dynamic than once thought.
Earth-based near-IR images resolved multiple bright storm cells and traced winds exceeding 360 km h-¹, confirming powerful seasonal convection.