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Interesting facts about space.
When moon people moved from one city to another, the moving group always mixed with others who had arrived there from the other six directions. At every new occasion, they always merged into new groups without seeking to stay with their original group. The mixing up of groups was a continuous process that took place at every city center. As a result of mixing into groups and splitting their journeys into seven directions at each city center, after a few years, it was always difficult to find another person from one's original group. This was not applicable at the individual level to a couple of a male and female as such couples always stayed together. By constantly moving from one area to another, the people were exposed to almost the entire vast area of their habitat during their life time and also made them have the opportunity to intermingle with the entire noon population of around 2 million persons. The average life span of moon people is over 100 earth years and this might be due to the type of food they ate, the ritualistic walking habit they perform for more than half their life time and perhaps the greatest influence might be the lives free from conflict and stress that they lead.
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NASA's Voyager 1 spacecraft was the first to visit Titan back in 1980. Although Voyager 1 made a truly heroic journey, it proved unsuccessful in its efforts to obtain close-up pictures of Titan's veiled surface. This adventurous, early space mission was not able to obtain the desired images because it could not cut through the dense orange smog--and the resulting images showed only some minor brightness and color variations in Titan's atmosphere. In 1994, the Hubble Space Telescope (HST) did succeed in obtaining some precious and revealing images of Titan's well-hidden surface--showing the existence of a bright and sparkling continent dubbed Xanadu--after the "Xanadu" of Samuel Taylor Coleridge's romantic poem Kubla Khan. Titan's Xanadu glitters as if lit by the cold fires of a multitude of sparkling rhinestones.
Now everything turns green and colourful, the air is cool and clear and people - especially, of course, children - are happily dancing in the first showers, also called 'Mango showers' as they bring forth the delicious mangoes which will soon be ripe and available in abundance. So, I hope you have enjoyed the celebration of the full-moon of Kason and have become familiar with what it is that makes this festival so full of meaning to the Burmese people. I suggest that we have a rest now because soon we will celebrate the next festival, the 'Full Moon of Waso' in the month of Waso (June/July) that marks the beginning of the 'Buddhist Lent.
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The inner Solar System is dramatically different from the distant realm of the giant planets. The inner region of our Solar System, where our Earth is situated, is almost entirely moon-less. Of the four relatively small, rocky worlds--Mercury, Venus, our Earth, and Mars--Mercury and Venus are barren of moons, and Mars is orbited by two fascinating, but very small, potato-shaped moons named Phobos and Deimos. The duo of Martian moons are often considered to be captured asteroids that long ago escaped from their birthplace in the Main Asteroid Belt between Mars and Jupiter. According to this scenario, Phobos and Deimos, during their dangerous journey from their original home, were snared by the gravity of their adopted Red Planet when our 4.56 billion-year-old Solar System was young. In the warm and well-lit inner Solar System, only Earth's large Moon is a significant moon-world in its own right.
The crust of Earth's Moon is 43 miles thick on the near-side hemisphere, and 93 miles on the far-side. It is composed of silicon, magnesium, oxygen, calcium, aluminum, and iron. There are also trace amounts of titanium, uranium, thorium, hydrogen, and potassium.
Planetary scientists usually calculate the Moon's age by using the radioactive decay of elements like uranium, explained Dr. John Chambers in the April 2, 2014 National Geographic News. Dr. Chambers is a planetary scientist at the Carnegie Institution for Science in Washington, D.C. By studying an element with a recognized decay rate, and knowing its concentration in Moon rocks or the Earth's surface, scientists are able to calculate back in time to when the material first formed. However, there are numerous and varying radioactive materials that can provide differing timelines, added Dr. Chambers, who was not involved in the study.