By Maitreyi Mantha from Dogonews
While the volcanoes on Earth eject fiery lava, ash, and smoke, those on Ceres, a dwarf planet that orbits between Mars and Jupiter, have been spewing ice throughout its history. The chain of events leading to the discovery began in 2015 when NASA’s spacecraft Dawn, sent to explore the asteroid belt where Ceres resides, captured some high-resolution images of its icy, rocky terrain. On the dwarf planet’s crater-covered surface, was a solitary 4-km ( 13,000 feet) tall mountain.
NASA researchers, excited at the discovery of the dwarf planet’s first cryovolcano, or ice volcano, named it Ahuna Mons. They estimated its age to be about 200 million years – too old to be erupting but young enough to suggest recent volcanic activity. What puzzled the experts, however, was the “young” Ahuna Mons’ lonely existence. It was hard to believe the 4.6 billion-year-old Ceres, whose core had cooled many years ago, had suddenly become active within the last few million years. Michael Sori, a researcher at the University of Arizona Lunar and Planetary Laboratory, said, “It’s pretty difficult to come up with a reason why Ceres, or any other body, would be volcanically dead for the first 99 percent of its life and then all of a sudden turn on yesterday, relatively speaking.”
The volcano’s discovery led Sori and his team to believe that Ceres had been geologically active throughout its existence. They suspected that the ice volcanoes, raised over time, had been flattened due to a natural process known as viscous relaxation. This is similar to when a blob of viscous material, such as honey or putty, collapses under its own weight and oozes outward before eventually flattening into the surrounding area. “Rocks don’t do that under normal temperatures and timescales, but ice does,” Sori said. Given that Ceres is made from both ice and rock, the theory was certainly plausible.
To confirm the hypothesis, the researchers studied images taken by Dawn’s onboard camera for evidence of older, deformed volcanoes that looked like relaxed domes or mountains which had been flattened over time. Sure enough, after scouring Ceres’ 1 million-square-mile surface, the team was able to discover 22 such formations, Ahuna Mons included. They ranged from 16 km (52,493 feet) to 86 km (282,200 feet) wide and 1.1 km (3,608 feet) to 4 km (13,000 feet) high. The scientists compared the structures to computer simulations, to determine the age of each collapsed formation. “We found that one volcano forms every 50 million years,” Sori said.
The researchers, who published their findings in the journal Nature Astronomy on September 17, 2018, estimate that the volcanoes probably spew an average of 3,000 cubic yards of cryovolcanic material each year. Though enough to fill a movie theater or four Olympic-sized swimming pools, it is substantially lower than the rocky volcanoes on Earth which generate more than 1 billion cubic yards of material in a year. Moreover, volcanic eruptions on Ceres are much more subdued than those on Earth. Instead of exploding violently, Ceres’ volcanoes gradually release a mixture of ice, rock, and other chemicals onto the surface.
The cause of the cryovolcanic eruptions on the dwarf planet is still a mystery. Researchers hope they may be able to find answers as space probes are sent out to investigate other solar system bodies where evidence of ice volcanoes has been detected. These include Pluto and its moon Charon, as well as Jupiter’s moon Europa, which, some scientists suspect, is home to numerous ice volcanoes.
Discovered in 1801 by Italian astronomer Giuseppe Piazzi, Ceres, which orbits 200 million miles away from the sun, was the first asteroid to be discovered. It is also the largest object in the asteroid belt and the only dwarf planet located in the inner solar system.
I think the article is very interesting. I learned about viscous relaxation and how volcanoes over 200 million years are still active. I think it is a big discovery that can lead us to bigger observations. I will definitely take a look at Nature Astronomy.
LikeLike
A dwarf planet has been discovered and there is a volcano on it, I personally think that is very cool. This is important to us because it is part of our solar system. Since the volcano has been around for about 200 million year that most likely means that this dwarf planet has been around for about about 200 million years as well. This is a very interesting finding and I can’t wait to see what other wonders scientist find on this dwarf planet.
LikeLike
I was so suprized that there was something called a cryovolcano that was basicly a ice valcano.I learned that there was a dwarf panet called ceres. Also I learned that ice volcanoes on ceres spew their “lava” gradually and volcanoes on earth would violently explode out lava. I thought all of this was really interesting mainly because there was something called a cryovolcano. -NF
LikeLike
I find it really interesting that there is such thing as an ice volcano/cryovolcano!I wonder how this actually happens. I think it’s like Earth where tectonics plates have something to do with volcanic and earthquakes. Also, why is it ice and not lava/magma? And how does ice ooze out? If ice is an solid, how does it ooze out? I enjoyed this article. I learned that there are such things and other types of volcanoes and they can erupt ice!.
LikeLike
I think it’s very cool that there is a volcano on a dwarf planet. Especially its an Ice volcano, That’s very interesting. Also they say its like 200 years old to erupt but there’s a suggestion that there’s still recent activity. Even though they don’t know the cause of eruptions and it would be cool if they did I thought this was a very cool thong/blog to read!
LikeLike
I was surprised when I read that there were volcanoes on other planets. I was also surprised when I read that there were ice volcanoes. I still don’t get why the volcanoes spew out ice. I know that the Earth’s mantle produces the magma but why can’t there be mantles on other dwarf planets?
LikeLike
I was surprised when I read that there were volcanoes on other planets. I was also surprised when I read that there were ice volcanoes. I still don’t get why the volcanoes spew out ice. I know that the Earth’s mantle produces the magma but why can’t there be mantles on other dwarf planets?
LikeLike
I thought it was really cool how this planet had a completely cooled down core. I was surprised when they said that the volcanoes though they look like weird flattened craters erupt ice. Even though the core was frozen that would still be really interesting because won’t the ice just freeze to a solid. So is the ice that’s coming up in a liquid or is it just chunks of ice. I think this could help us to know what could be the potential opposite of our ash spewing volcanoes.
LikeLike
I think this is really cool and interesting. The volcano has not been active for 99% of it’s life then suddenly it erupts like that. The volcano is useful to us because it is the complete opposite of what the volcanoes here are like. Here the lava can go threw many things. There the dwarf planet is too cold so that the “lava” would go threw things. This would help us because we could look at other planets or dwarf planets and see that they have volcanoes similar to this one. Then we would know what could happen to the other planets and see what changes they would make.
LikeLike