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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.
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Over the years, several theories have been proposed to explain the mechanism involved in Triton's capture by Neptune. One theory suggests that Triton was snared in a three-body encounter. According to this scenario, Triton is the lone survivor of a binary Kuiper Belt Object (KBO) that had been fatally jostled during a destructive close encounter with Neptune.
With the discoveries of 132 confirmed extrasolar planets and more than three thousand planet candidates, the Kepler mission revolutionized scientific understanding of planets residing beyond our own Star. Much of the attention surrounding these discoveries has focused on identifying an Earth-analog--a planet about the size of our own world dwelling within the precious Goldilocks zone around its distant star. Now, for the first time, Dr. David M. Kipping of the Harvard-Smithsonian Center for Astrophysics (CfA) in Cambridge, Massachusetts, and his team, have started to hunt for a habitable moon around Kepler-22b!
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The two scientists found clear evidence of water in nearly all of the large pyroclastic deposits that had been mapped earlier across our Moon's surface, including deposits near the Apollo 15 and 17 landing sites where the water-bearing glass bead samples were collected.
Therefore, the planetary ring-spreading model can explain how the majority of regular moons were born in our Solar System.
If you were to take an Apollo 11 quiz in school, you would likely find that one of the main focuses is the fact that it was the first mission to carry humans to the moon. It was on this voyage that the famous words, "That's one small step for man; one giant leap for mankind," were uttered by Neil Armstrong as he became the first human being to ever set foot on the moon.