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It is important to know at any age!
Similar to the great lakes in North America, there are massive lakes in the hollow underground cave system. However unlike the great lakes, the caves roofs over the lakes of the moon are supported by the natural array of vertical pillars protruding through the waters like a massive cluster of Mangrove roots. The underside of the roof above the lakes and also the vertical pillars protruding through the waters are 'coated' by a gel like material. This gel shows many of the signs of being a living substance. It also emits light and carries out the function of 'cleaning' the moon's atmosphere by absorbing impurities which it assimilates as a nutrient. It rejects some part of the absorbed impurities as balls of waste exited into the lakes. The waste in turn is eaten by the fish or absorbed by plants in the lakes. The reflection of the softly glowing gel on the water enhances the lighting in the area of the lakes. At all places in the moon, the water in the lakes is clean, not salty and is suited for use directly for drinking. The waters of these lakes are however subject to massive tidal effects. These are due to the fluctuation of the resultant of the gravitational tugs of the earth and the sun as the earth spinning on its own axis and carrying the moon in orbit in turn orbits the sun. Because of the low moon gravity, the tidal effects are checked weakly and the water levels rise and fall by hundreds of feet. The tides force the water to spread hundreds of miles along the vast underground areas thus wetting the dry areas of the caves in a cyclic pattern. Because of these vast latitudinal and longitudinal fluctuations of water spread, there are artificial water stream formations all over the geological-structure of the moon. The streams of water flow over the cave surfaces and create huge waterfalls at some places. These waterfalls last for many days and appear and disappear in a cyclic pattern, following the tides.
and here is another
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.
Because the lunar atmosphere is very thin, it is far too sparse to prevent a steady shower of impacts from tumbling asteroids, comets, and meteoroids. These objects strike the lunar surface, leaving behind numerous crater scars. For example, Tycho Crater is over 52 miles wide.
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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.
This new method is based on the fact that elements composing our planet's crust that have a tendency to combine with iron--such as iridium and platinum--arrived at Earth after this last giant collision.
Therefore, the planetary ring-spreading model can explain how the majority of regular moons were born in our Solar System.