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A little interesting about space life.
The lakes are the main supporting source sustaining life in the moon. The lakes support an array of living organisms including fish of various varieties and some small sized aquatic mammals also, like on the earth. Only a limited range of water plants grow in the lakes and these are all found in all the lakes in the moon. The most abundant water plant variety resembles seaweeds, but is very much thicker and stronger than the earth's variety. These water plants which grow very rapidly and proliferate in vast quantities are the primary source of food and nutrient for the moon people.
and here is another
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.
Most of the moons dwelling in our Sun's family were probably born from primordial disks of dust and gas, orbiting around newly formed planets, when our Solar System was very young about 4.5 billion years ago. There are at least 150 moons circling the planets in our Solar System--and about 25 moons are currently awaiting official confirmation of their discovery.
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Moons are natural satellites that circle around another body that, in turn, circles around its parent-star. The moon is held in place by both its own gravity and the gravitational pull of its planet. Some planets have moons, while others do not. Several asteroids are known to be circled by very small moons, and some dwarf planets--such as Pluto--also have moons. One of Pluto's quintet of moons, Charon, is about half the size of Pluto itself. Some planetary scientists propose that Charon is really a large chunk of Pluto that was torn off in a catastrophic collision with another wandering world long ago. Because Charon is almost 50% the size of Pluto, the two tiny icy bodies are sometimes considered to be a double-planet.
The research published in the July 4, 2016 issue of Nature Geoscience highlights the main factor differentiating moon-birth around Mars and Earth: the differing rotation speeds of the two planets prompted "completely different tidal actions," Dr. Charnoz explained in the July 4, 2016 CNRS Press Release. Dr. Charnoz proposes that at the time of their respective impacts, "Earth took less than four hours to spin on its axis whereas Mars rotated very slowly over a 24-hour period." The result of this important difference caused Earth to hold on to its single, large Moon, while the Martian collision created a dozen smaller moons alongside a larger moon. As time went by, Martian tidal action--resulting from the planet's slow rotation rate--caused most of the moons, including the largest one, to crash back down to the surface of their parent-planet. As a result, only the two most distant moons, Phobos and Deimos, survived as testimony to the ancient catastrophe.
The more widely accepted theory that the planets and regular moons formed together from the same swirling cloud of gas and dust, works well as an explanation for the larger moons of our Solar System, such as the four Galilean moons--Io, Europa, Ganymede, and Callisto--orbiting the giant planet Jupiter. However, the multitude of smaller moons, swarming around the giant planets, "have so far been considered a by-product," Dr. Crida commented in the November 29, 2012 Scientific American.