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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.



and here is another

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.



and finally

The relatively light regions of the Moon are known as the highlands. The dark features, the lunar maria, are impact basins that were later filled with lava between 4.2 and 1.2 million years ago. These light and dark regions were created by rocks of different ages and compositions. This provides evidence for how the ancient crust may have crystallized from a global lunar ocean of magma. The impact craters have been preserved for billions of years, and they provide observers with an impact history for our Moon and other bodies that inhabit the inner Solar System.

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"The key question is whether those Apollo samples represent the bulk conditions of the lunar interior or instead represent unusual or perhaps anomalous water-rich regions within an otherwise 'dry' mantle. By looking at the orbital data, we can examine the large pyroclastic deposits on the Moon that were never sampled by the Apollo or Luna missions. The fact that nearly all of them exhibit signatures of water suggests that the Apollo samples are not anomalous, so it may be that the bulk interior of the Moon is wet," explained Dr. Ralph Milliken in a July 24, 2017 Brown University Press Release. Dr. Milliken is the lead author of the new research and an associate professor in Brown University's Department of Earth, Environmental and Planetary Sciences. Brown University is in Providence, Rhode Island.



In order to do precisely that, Dr. Li and Dr. Milliken used laboratory-based measurements of samples returned from the Apollo missions, combined with a detailed temperature profile of the areas of interest on the lunar surface. Using the new thermal correction, the two astronomers studied the data derived from the Moon Mineralogy Mapper, which is an imaging spectrometer that was carried aboard India's Chandrayaan-1 lunar orbiter.



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.