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It is important to know at any age!
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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For most of the 20th century, astronomers thought that Pluto was a lonely little world, a solitary ball of ice circling our Sun, so very far from the comforting warmth and delightful light of our brilliant Star. However, in 1992, the discovery of the first KBO (other than Pluto), made astronomers come to the realization that Pluto is not far from the madding crowd of a vast population of other Kuiper Belt ice balls.
The exact composition of these bodies of liquid remained unknown until 2014, when the radar instrument aboard Cassini was first used to show that Ligeia Mare, the second largest sea on Titan, is richly endowed with methane. Ligeia Mare is similar in size to two of the Great Lakes on Earth combined--Lake Huron and Lake Michigan! The new study, published in the February 25, 2016 issue of the Journal of Geophysical Research: Planets, which used the radar instrument in a different mode, independently confirmed the 2014 result. "It's a marvelous feat of exploration that we're doing extraterrestrial oceanography on an alien moon," commented Dr. Steve Wall in an April 26, 2016 Jet Propulsion Laboratory (JPL) Press Release. Dr. Wall, who is of the JPL in Pasadena, California, is Cassini radar team deputy lead.
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Alas, this is not the case with Phobos and Deimos. Phobos, the larger of the duo of little Martian moons, at 22 kilometers in diameter, is lazily tumbling towards Mars and will approach the Roche limit in about 20 million years. At this tragic point, it will shatter into fragments that will ultimately form a spectacular ring around its planet. Only Deimos will remain--bereft of its companion. Deimos is the smaller moon of the pair, and circles its parent-planet further out. This last remaining little moon will be a lonely object lingering in the Martian sky at this sad point--but it was not always thus. The new 2016 study suggests that Mars once possessed a very complex system of many moons.
The moment that man stepped foot on the moon is definitely one of the more admirable historical moments of all time. Being that it is so admirable and so absolutely intriguing that this event actually occurred; many people want to learn more about it. Apollo 11 trivia is helpful to those who want to learn a great deal of information about this voyage into space in a very short period of time. In fact, several of the facts that you would learn through trivia would take you hours, if not days, to find in a book - or even surfing online.
The crew was able to complete the mission, which would have put a big smile on the face of former President John F. Kennedy. President Kennedy had set a goal to put a man on the moon prior to the end of the decade (1960's) and this goal had now not only been fulfilled, but broadcast worldwide for any who wished to see the triumphant event. Clearly, this amazing feat proves that anything is possible.