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Interesting facts about space.
If the authors' proposal is correct, then it successfully explains why Neptune's moon system looks so strange compared to Jupiter's or Saturn's--which means that astronomers' models of how these primordial systems form around gaseous giant worlds still hold strong.
and here is another
Only some two weeks have passed since 'Yay' (water) played an important role in Burmese people's life. That was when in Tagu (March/April) during 'Thingyan' or 'Water Festival' - the 'Burmese New Year' - the people poured lots of water over one another to wash away all physical filth and dirt and the spiritual sins and evils in order to enter with a clean body and soul into the New Year. Meanwhile we are coping with the heat of the summer as best as we can. All my clothes are dry again and I have recovered from the cold I had caught during that time.
But ongoing studies about lunar chemistry are showing that it may be much wetter than planetary scientists initially hypothesized. In fact, these wetter conditions conflict with some aspects of the Giant Impact theory.
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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.
Mars hasn't always looked the way it does today. The planet suffered a monumental tilt billions of years ago. Before this great tilt occurred, the Martian poles were not where we see them now.
Earlier research had determined the quantity of material accreted onto the ancient Earth following the Moon-forming collision. These previous calculations were based on how the siderophile or "iron-loving" elements such as platinum and iridium show a strong tendency to wander down into our planet's core. Following each giant impact that the primordial Earth experienced, these elements would have leached from Earth's mantle and bonded with iron-rich, heavy material that was destined to travel down, down, down into our planet's heart.