Volcanoes may not just exist on moons and planets. A comet orbiting between Saturn and Jupiter seems to have its own signs of icy volcanism, spewing frozen material instead of hot lava. Rather than a single stagnant mound, however, the eruptions come from a single location multiple times before eventually traveling to another point in the icy crust.

The slow rotation of the comet allows the crust to weaken over the course of its day, while carbon monoxide piles up on the surface again during the night. Eventually, the pressure building beneath the surface erupts. Unlike the jets spotted on other comets, the cold ‘lava’ bursts through suddenly and explosively, with no signs of gradual buildup.

“It’s an abrupt event,” says Richard Miles a cometary scientist with the British Astronomical Association who presented the results at the Division for Planetary Sciences meeting in Pasadena, California. Once the explosion is complete, it shuts down without the slow decline common to jets. “It’s done, and everything tapers out. It’s what you would expect from cryovolcanism.”

An active enigma

Comet 29P/Schwassmann-Wachmann is the most active of all known comets. Shortly after its 1927 discovery, the comet’s brightness began to dramatically change. While many comets grow brighter as they travel closer to the sun, 29P orbits in an almost-perfect circle, maintaining a fairly consistent distance from the star. Despite its stable orbit, the comet can make remarkable changes in brightness, making it a favorite for amateur astronomers to observe.

Miles and his colleagues studied the comet over more than a decade, identifying 64 outbursts from the tiny object. The icy body can have as few as three to four outbursts a year, though some years released seven to eight eruptions. By tracking their location over the surface of the comet, the scientists found that many of the eruptions came from the same regions. While some reappeared after a day or so, others took as long as 20 years to reappear, based on earlier observations. It was their repeated appearance that led Miles and his team to dub them as cryovolcanic. Unlike normal volcanoes, which spew molten lava, cryovolcanoes erupt frozen gases that move much like their warmer cousins.

Cryvolcanoes may be common on the icy moons of the solar system, including Jupiter’s moons Europa and Ganymede and Saturn’s moon Titan. Dwarf planets may also host the frigid fountains, as both Pluto and Ceres have features identified as possible cryovolcanoes. Comet 29P doesn’t have features on the ground that resemble icy volcanoes. Instead, Miles interprets the activity as potentially volcanoic.