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Curious facts about cosmic life and their inhabitants.
Triton also possesses a thin atmosphere composed mainly of nitrogen, and a smaller quantity of methane. This atmosphere probably is the result of Triton's cryovolcanism, which is enhanced by seasonal heating from the Sun. Although little is currently known of Pluto's atmosphere, it is thought to be primarily composed of nitrogen with some carbon monoxide and methane added to the mix--and it is extremely tenuous. Pluto's very thin atmosphere may exist as a gas only when Pluto is nearest to the Sun (perihelion). For most of Pluto's very long year, the atmospheric gases are frozen in the form of ice on its extremely frigid surface. One year on Triton is almost 248 Earth-years long--or 90,471 Earth-days!
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"The distribution of these water-rich deposits is the key thing. They're spread across the surface, which tells us that the water found in the Apollo samples isn't a one-off. Lunar pyroclastics seem to be universally water-rich, which suggests the same may be true of the mantle," Dr. Milliken continued to explain in the Brown University Press Release.
In addition to shedding new light on the lunar water-mystery, the new research could also have important implications for future exploration of Earth's Moon. The volcanic beads do not harbor a lot of water--only about.05 percent by weight--but the deposits are large, and the water could potentially be extracted.
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"More generally, our findings clarify how giant impacts give birth to satellites and can create a diverse variety of satellite systems," Dr. Charnoz told the press on July 4, 2016. He added that the team could apply their method to other regions of our Universe:
Now, by pinpointing the precise birthday of the Moon, Dr. Jacobson and his team can help to explain why the Moon and our planet are so mysteriously similar in their compositions.
"A late Moon-forming event, as suggested by our work, is very consistent with an identical Earth and Moon," Dr. Jacobson told Space.com.