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Interesting facts about space.
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.
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However, it's not true that we have no satellite pictures of the moon landing sites. In fact, we have a number of satellites orbiting around the Moon which have taken many pictures of all the landing sites before. These images clearly show the equipment left on the moon by astronauts, their footprints, and all the wheel tracks left by their moon-buggies.
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!
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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.
The first observations of Mars as an object traveling in Earth's night sky was recorded by the ancient Egyptian astronomers, and by 1534 BCE the ancient astronomers were familiar with the retrograde movement of the planet. By the time of the Neo-Babylonian Empire, the Babylonian astronomers were making regular records of the positions of the planets, as well as systematic detections of their behavior. In the case of Mars, the ancient astronomers realized that it made 42 circuits of the zodiac every 79 years. These scientists of long ago even invented arithmetic methods so that they could make minor corrections pertaining to the predicted positions of the planets inhabiting our Solar System. The ancient astronomers referred to the planets as "wandering stars".
Saturn is the smaller of the two gas-giant planets dwelling in the outer regions of our Solar System, far from the friendly light and warmth of our incandescent golden Star, the Sun. The larger of the two gas-giants is Jupiter, which is also the largest planet in our Solar System. Some scientists think that the two gas giants do not have solid surfaces hidden beneath their immense and heavy gaseous envelopes, although others think that they probably do contain relatively small cores of rocky-icy material. The two other large denizens of the outer limits of our Sun's family are Uranus and Neptune, which are classified as ice-giants, because they have large icy cores buried beneath their heavy atmospheres which, though massive, are not nearly as heavy as the gaseous atmospheres borne by the two gas-giants.