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Interesting facts about space.
From ancient times, through the transparent areas of the moon's crust the people of the moon had seen a beautiful planet like object in the sky. This was our earth. They believed that it was heaven (meaning "pleasure place" in their language)... the place that they will be born in after their death. This heaven was visible only from certain cities of the moon. The entire moon population was aware of this heaven from their school education and also from reports by people who had seen it. Like certain religious pilgrimages on earth, part of the purpose of the "moon people's continuous movement habit" was to observe this heaven during their lifetime. Most people had seen the heaven when they arrived at cities from which it was visible. However, it should be understood that the primary purpose of the movement habit was not to satisfy a need to see the heaven. The primary purpose of the habitual journeying was really not known. Whenever the moon people approached a place from where they could see this beautiful heaven in space for the first time, they had the background knowledge that getting to heaven was an event that would take place at the end of their lifetimes. They were therefore very excited and overwhelmed by it. However, when they actually got to look at the object which was heaven they would glare at it for long hours without blinking as it was so utterly beautiful and enjoyable to look at - like a glowing blue colored gem hanging by itself. Just looking at it gave them a sense of deep fulfillment.
and here is another
However, the truth is, during their entire voyage to the Moon and back to Earth, Armstrong, Aldrin and Collins only received amount of radiation equal to about 0.1% of the deadly dose. Their total exposure was approximately 11 milisieverts, and radiation dose lethal to an average human being is aroung 8,000 millisieverts.
When these photos were taken, it was full daylight on the Moon. Because there is only an extremely thin atmosphere on the Moon,the sky appears black. In addition, sunlight at the Moon's surface was incomparably strong with the starlight; the stars simply faded in comparison with the sun. If the astronauts used sufficiently long exposures, stars would, indeed, be visible.
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Saturn, along with its frozen retinue of icy rings, dazzling moons, and sparkling moonlets, orbits our Sun about ten times farther out than the Earth. Astronomers received their first collection of detailed data about Titan when the Cassini/Huygens orbiter and lander arrived there in 2004. The Huygens lander successfully obtained revealing images when it drifted down to Titan's tormented, hydrocarbon-slashed surface, as well as when it was still floating slowly and softly down through the moon's thick, foggy, orange atmosphere--which has 1.4 times greater pressure than that of our own planet. These pictures, when combined with other studies using instruments aboard the Cassini orbiter, reveal to curious planetary scientists that Titan's geological features include lakes and river channels filled with methane, ethane, and propane. Titan's strange surface also shows mountains and sand dunes--and it is pockmarked by craters. The rippling dunes form when fierce winds sweep up loose particles from the surface and then tosses them downwind. However, the sands of Titan are not like the sands on our Earth. Titan's "sand" is both bizarre and alien, probably composed of very small particles of solid hydrocarbons--or, possibly, ice imprisoned within hydrocarbons--with a density of about one-third that of the sand on our own planet. Furthermore, Titan's gravity is low. In fact, it is only approximately one-seventh that of Earth. This means that, working in combination with the low density of Titan's sand particles, they carry only the small weight of a mere four percent that of terrestrial sand. Titan's "sand" is about the same light-weight as freeze-dried grains of coffee!
Moons are natural satellites that orbit another body that, in turn, circles its parent-star. A moon is held in place by both its own gravity and the gravitational grip of its host planet. Some planets have moons; some do not. Several asteroids in our Solar System also are orbited by very small moons--and some dwarf planets, such as Pluto, also have moons. One of Pluto's five moons, Charon, is almost 50% the size of Pluto. For this reason, the two frozen worlds inhabiting our Solar System's remote twilight zone, are sometimes classified as a double-planet.
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.