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Interesting facts about space.
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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How did Triton acquire so many strange properties, and why is Neptune's system of satellites so different from those predicted for a gaseous giant planet? Two planetary scientists, Dr. Raluca Rufu (Weizmann Institute of Science, Israel) and Dr. Robin Canup (Southwest Research Institute, US) demonstrate how Triton wreaked catastrophic havoc on Neptune's first generation of very unfortunate moons.
Dr. Li continued to note that "Other studies have suggested the presence of water ice in shadowed regions at the lunar poles, but the pyroclastic deposits are at locations that may be easier to access. Anything that helps save future lunar explorers from having to bring lots of water from home is a big step forward, and our results suggest a new alternative."
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The new study was published in the April 3, 2014 issue of the journal Nature, and it may provide a solution to a long-standing mystery of lunar origins pertaining to why Earth and its lovely companion appear to sport virtually identical compositions.
Crida and Charnoz tested their new model to find out whether it could be applied to other planets in addition to Saturn. Their investigation has brought to light several valuable facts. This scenario for moon-birth from planet-rings succeeds in offering an explanation as to why the largest moons dwell farther away from their parent planet than the smaller moons. It further explains the gathering of moons close to the Roche limit--their birthplace--on the outermost fringes of the rings. This distribution is in agreement with what is seen in the Saturn-system. The same scenario can also apply to the moons of other giant planets, such as the ice-giants Uranus and Neptune. The Uranus-system and the Neptune-system are also organized in a similar way. This discovery suggests that long ago, when these planets were young, they also sported impressive rings like those of Saturn--which ultimately vanished when their moons were born. Finally, this scenario can also explain the formation of Earth's Moon, and the moons of the dwarf planet Pluto. According to Crida and Charnoz's calculations, under special circumstances a single moon--like Earth's own--can be born from a primordial ring around its planet. This may well have occurred in both the case of Earth's single large Moon, and for Pluto's largest moon, Charon.
Therefore, the planetary ring-spreading model can explain how the majority of regular moons were born in our Solar System.