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Voyager 2 flew by Neptune back in 1989, and its observations revealed a number of active geysers, situated within the polar cap heated by the Sun. The geysers hurl out plumes to the impressive height of up to 8 kilometers. Triton has a relatively high density that indicates rocks account for approximately two-thirds of its mass, and ices (mostly water ice) compose the remaining one-third.
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Over the years, several theories have been proposed to explain the mechanism involved in Triton's capture by Neptune. One theory suggests that Triton was snared in a three-body encounter. According to this scenario, Triton is the lone survivor of a binary Kuiper Belt Object (KBO) that had been fatally jostled during a destructive close encounter with Neptune.
Numerical simulations have been conducted that show that there is a 0.41 probability that Neptune's moon Halimede blasted into Nereid in the past. Even though it is not known if this collision really did occur, both moons display similar grey colors. This implies that Halimede could be a chunk of Nereid that broke off during the collision.
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Some studies which have been performed in certain cities within the United States show that there is no correlation between the full moon phase and such things as a rise in suicides, crime rate, dog bites or births. And yet, other studies completed by such individuals as psychologists and other human behaviorists have shown that there is, in fact, a peak in certain kinds of behavior associated with a loss of contact with reality during full moons. These include murder, arson, dangerous driving and kleptomania, which is an irresistible impulse to steal due to an emotional rather than economical need.
"The key question is whether those Apollo samples represent the bulk conditions of the lunar interior or instead represent unusual or perhaps anomalous water-rich regions within an otherwise 'dry' mantle. By looking at the orbital data, we can examine the large pyroclastic deposits on the Moon that were never sampled by the Apollo or Luna missions. The fact that nearly all of them exhibit signatures of water suggests that the Apollo samples are not anomalous, so it may be that the bulk interior of the Moon is wet," explained Dr. Ralph Milliken in a July 24, 2017 Brown University Press Release. Dr. Milliken is the lead author of the new research and an associate professor in Brown University's Department of Earth, Environmental and Planetary Sciences. Brown University is in Providence, Rhode Island.
The vanished, ill-fated, large moon could have been a few hundred kilometers in diameter. The large moon would also have allowed a handful of other smaller moons to form--including the duo of small, shapeless ones that survive today. However, this large inner moon would have been born close to or within the Roche limit. This is why it is likely that it crashed into Mars as a result of tidal forces within several million years--and the collection of other small moons followed their leader. Only Phobos and Deimos kept their distance.