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A little interesting about space life.
When once a man and woman get together, their bond is maintained permanently. If a child is born, the mother stays with the baby for three months. During this time the baby is usually breast fed by the mother or sometimes by other mothers. Children including infants are brought up in the community centers. Hence children do not develop social bonding to their parents. In fact nobody knows who their parents are. The moon people laid a very strong emphasis on educating the children and the children are kept in the community education system until they reach 16 years of age. The children learn academic subjects as well as all domestic practical work required for community activities. There are also chores that have to be carried out during non-study time. From a very early age, children are assigned specific responsibilities. The chores are selected suitably by community leaders with due regard to the age of the child. The children select their own names during the school period according to their sole independent choice. However the first part of the name carries the name of the city. For instance children from the city of "Vaaadi" would have names like Vaaadi Tukuuu, Vaaadi Bekiii, Vaaadi Zukooo, etc., - short names but pronounced with a long dragging accent. Written records of births or any other type of identification mechanism does not exist.
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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!
"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.
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If this ancient catastrophic impact really did occur, there should be deposits of these tragic moons on the Martian surface. The Japanese Aerospace Exploration Agency (JAXA) is currently planning a sample return mission to Phobos and Deimos, the Martian Moons Explorer, and NASA has plans to eventually return samples to Earth from the surface of Mars-- perhaps as soon as the 2020s. At the conclusion of their paper, the authors note, "Our scenario provides further motivation for a sample return mission to the Martian satellites."
This later-forming time line for lunar birth is reasonable, Dr. William Hartmann noted in the April 2, 2014 National Geographic News. Dr. Hartmann, a researcher at the Planetary Science Institute in Tucson, Arizona, was one of the first to propose the giant impact theory of lunar formation. However, he added that the new study might depend too much on the idea of using the last giant impact as a marker for when such events occurred in the history of our planet.
According to this theory, the Saturn system began with a family of several relatively large moons, analogous to the four large Galilean moons of Jupiter--Io, Europa, Ganymede, and Callisto. However, strange and violent things happened in the Saturn system that drove its large moons onto a collision course with destiny. According to the theory, there were a few dramatic moon mergers, forming the Titan that we now know--but there was also a sufficiently large quantity of moon-stuff left over from the collisions to create the icy mid-sized satellites--Mimas, Iapetus, Enceladus, Tethys, Dione, and Rhea!