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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.

and here is another

Dr. Lieber and his colleagues did a study to test the theory of full-moon "lunacy". They studied data on murders in Dade County of Florida which covered 15 years and a total of 1,887 deaths by homicide. When they compared the deaths with the phases of the moon, they found that the two rose and fell together for the entire 15 years! With the approach of a full or new moon, there was a sharp spike in the murder rate, and then a decline during the first and last quarters of the moon.

and finally

Kepler-22b is an extrasolar planet that circles Kepler-22, a G-type star that is situated about 600 light-years from our own planet in the constellation Cygnus. This intriguing new world, that resides beyond our Solar System, was first spotted by NASA's highly productive, though ill-fated, Kepler Space Telescope in 2011. Kepler-22b has the distinction of being the first known transiting extrasolar planet to reside within the so-called habitable zone of its star. The habitable zone is the term used to describe that Goldilocks region around a star where water can exist in its life-loving liquid state. Planets dwelling in this fortunate region are not too hot, not too cold, but just right for water and, hence, life to exist. A planet that circles its star in the habitable zone suggests that there is the possibility--though not the promise--of life as we know it to exist on that world.

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Triton is the largest of Neptune's 13 moons. It is an unusual world, twirling around its planet in the wrong direction. Many astronomers think that some time in the remote past, Triton was nudged out of its home in the Kuiper Belt, and during its wanderings in the darkness of interplanetary space, at last swept close enough to Neptune to feel the irresistible lure of that planet's gravity. As Neptune drew Triton into its gravitational embrace, that luckless wanderer from the Kuiper Belt underwent a sea-change from a comet-like denizen of our Solar System's outer limits, to a moon of one of the major planets. So, there Triton whirls around in its new home, circling its planet Neptune, but circling it backwards. And like all moons, it is now a dependent of its parent planet. As a matter of fact, the moon was given the name of Triton as an allusion to the demigod Triton's dependence on the sea-god Neptune in Greek mythology.

The vanished, ill-fated, large moon could have been a few hundred kilometers in diameter. The large moon would also have allowed a handful of other smaller moons to form--including the duo of small, shapeless ones that survive today. However, this large inner moon would have been born close to or within the Roche limit. This is why it is likely that it crashed into Mars as a result of tidal forces within several million years--and the collection of other small moons followed their leader. Only Phobos and Deimos kept their distance.

In 2010 and 2011, the French astrophysicists devised their model to explain how the moons of Saturn were born. They based their findings on data derived from the Cassini probe--that is investigating the Saturn-system--and on numerical simulations. The team found that Saturn's bewitching rings, which are slender disks composed of tiny chunks of gleaming ice surrounding the giant planet, gave rise to the icy moons. This happened because the rings spread as time went by--and when the rings attained a critical distance from the planet (termed the Roche limit), their ends melded together and created small worldlets that broke off and floated away. In this way the rings created the icy moons orbiting Saturn.