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A little interesting about space life.

Many surface crusts are made of a material known as lunar regolith. Lunar regolith transforms into translucent forms through a process called agglutination when the regolith is subjected to high heat. In many places, parts of the moon's surface consist of translucent material embedded in the moon's outer crust. These surfaces allow a substantial degree of sunlight to penetrate into the caves. Most of this glass like surface material has been naturally formed, millions of years ago. Amongst the translucent surface areas, there are also many areas of near clear-glass transparency. Due to refraction of the sunlight that penetrates into the caves, massive rainbow like color beams frequently appear in very many places inside the caves. Due to the vastness and the complexity of the spectrum of rainbow colors intermingling with each other, there is a stunningly beautiful visual effect inside the caves. The glow from the moon's outer surface when seen from inside the caves, gives a further dimension of beauty for the visual enjoyment of the people of the moon.



and here is another

On July 20, 1969, during one of the defining moments of the human history, Neil Armstrong became the first man to step on the surface of Earth's Moon. In his own words, it was truly "one small step for a man, one giant leap for mankind."



and finally

No Satellite Pictures. Even with all of our telescopes on Earth and the incredibly powerful Hubble Telescope, none of them has ever taken any pictures with any of the landing sites of the Moon. This often misleads us to the thought: are they really out there?

More information:

Until 1610, when Galileo Galilei discovered the quartet of large Galilean moons orbiting Jupiter--Io, Europa, Ganymede, and Callisto--Earth's Moon was the Moon, because it was the only moon known to exist. Now, we know differently. There are over 100 known moons in our Solar System alone, and probably many, many more, circling distant alien planets belonging to the families of stars beyond our Sun. Most of the moons in our own Solar System are relatively small, icy worldlets that contain only small amounts of rocky material. The faraway multitude of sparkling, frozen moons that inhabit our Sun's family are mostly found circling the quartet of outer gaseous giant planets--Jupiter, Saturn, Uranus, and Neptune. In this dimly lit region, far from our Star's heat and light, these tiny icy moons perform a strange and lovely ballet around their large, gaseous host planets. The quartet of giant gaseous planets, that inhabit our Solar System's outer suburbs, are enshrouded by heavy atmospheres of gas, and they are accompanied in their travels around our Sun, by their own orbiting entourage of moons and moonlets.



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.



Jupiter, like Saturn, is circled by more than 60 known satellites. Many of them are tiny moonlets, measuring only a few miles across, and are probably captured asteroids or minor planets--or their shattered remains.