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A little interesting about space life.
When Apollo 11 landed on the Moon in 1969, we were presented with our first human contact with the moon. The mission was able to accomplish the task of not only landing on the Moon, but also to return to the Earth with samples from the Moon. These samples along with subsequent presented us with answers regarding the composition of the Moon, which also gave us some basic facts that any theory about how the moon was created must answer/address. We learned:The Moon does not contain an iron core like our Earth does, due to the fact that the Moon's density is only 3.34 grams per cubic centimeter (compared to the Earth's which is 5.52 grams per cubic centimeter).Samples collected from the surface of the Moon reveal that it underwent extreme heat and baking, much more than what the Earth experienced.
and here is another
Neptune is circled by only 14 moons, a considerably smaller number than Jupiter's 70. Also, most of Neptune's moons are extremely small. Triton, however, is an exception. In fact, Triton harbors 99.7% of the mass of Neptune's entire system of moons combined. The second-largest irregular moon in our Solar System, Phoebe of Saturn, sports only about 0.03% of Triton's mass. It is thought that Triton was snared by its adopted parent-planet some time after Neptune had already formed a system of moons. This means that the capture of the wandering Triton was likely a catastrophic event for Neptune's original moons, disrupting their orbits, and causing them to blast into each other--thus creating a rubble disc.
Earth's Moon consists of a core, mantle, and crust. The lunar core is proportionally smaller than other terrestrial bodies' cores. The iron-rich, solid inner core is 149 miles in radius, and it is encased within a liquid iron shell that is about 56 miles thick. A partly molten layer with a thickness of 93 milles surrounds the iron core.
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"That thermally emitted radiation happens at the same wavelengths that we need to use to look for water. So in order to say with any confidence that water is present, we first need to account for and remove the thermally emitted component," Dr. Milliken continued to explain in the July 24, 2017 Brown University Press Release.
Astronomers have for years contemplated two competing hypotheses explaining the origin of the Martian moons. The first proposes that Phobos and Deimos are, indeed, escapees from the Main Asteroid Belt. Alas, this viewpoint begs the question of why they should have been so cruelly captured by their adopted parent-planet in the first place. An alternative theory points to the possibility that the moons were born from the debris left by a violent collision between Mars and a primordial protoplanet--a baby planet still under construction. However, this theory also suffers from uncertainty because it does not explain precisely how this particular tragic mechanism gave rise to Phobos and Deimos.
A moon is a natural body that is in orbit around another body that circles our Sun. The moon is kept in its orbit by its host's gravity, as well as by the gravity of the moon itself. Some planets host moons; some do not. Some asteroids have moons, and some dwarf planets--such as Pluto--are also circled by moons.