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A little interesting about space life.
The true reason you can't see the stars in photos and videos of Moon is not that the stars aren't there, but rather because of the omnipresent sunlight and the exposure limits of cameras.
and here is another
Methane and nitrogen present in Titan's atmosphere react together to create a variety of organic materials. Many planetary scientists think the heaviest materials somersault down to the surface of hydrocarbon-slashed Titan. Dr. Le Gall and her team propose that when those compounds splash into the sea, either by directly falling from the air as hydrocarbon rain, or through Titan's rivers, some are dissolved in the liquid methane. The compounds that do not dissolve, such as nitrites and benzene, sink down into the floor of this exotic sea.
Europa, is a fascinating, frigid little world. It is one of the four Galilean moons, discovered in January 1610 by the great Galileo Galilei when he was gazing up into the night sky with his small, primitive "spyglass". The other Galilean moons, the weird sisters of Europa, are Io, Ganymede, and Callisto.
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Alas, this is not the case with Phobos and Deimos. Phobos, the larger of the duo of little Martian moons, at 22 kilometers in diameter, is lazily tumbling towards Mars and will approach the Roche limit in about 20 million years. At this tragic point, it will shatter into fragments that will ultimately form a spectacular ring around its planet. Only Deimos will remain--bereft of its companion. Deimos is the smaller moon of the pair, and circles its parent-planet further out. This last remaining little moon will be a lonely object lingering in the Martian sky at this sad point--but it was not always thus. The new 2016 study suggests that Mars once possessed a very complex system of many moons.
Several theories have been around for a long time that have attempted to explain how Earth's Moon was born. The first theory suggests that the Moon was once part of Earth, and that it somehow budded off about 4.5 billion years ago. According to this theory, the Pacific Ocean basin is the most likely site for where this occurred. A second theory postulates that the interaction of Sun-orbiting and Earth-orbiting planetesimals (the ancient building-blocks of planets), in the early years of our Solar System, caused them to disintegrate. Earth's Moon then coalesced out of the shattered debris of the pulverized planetesimals. A third theory proposes that the Earth and Moon were born together out of the original nebula that gave rise to our Solar System, and a fourth theory suggests that the Moon was really born somewhere else in our Solar System, and was ultimately captured by Earth's gravity when it traveled too close.
A moon is an enchanting thing! There are more than 100 lovely moons circling the eight major planets in our Solar System, alone--including our own beloved Moon--the brightest and largest gleaming object suspended in the brilliantly starry night sky above the Earth. But how did the moons of our Solar System come into being?