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It is important to know at any age!

How did Triton acquire so many strange properties, and why is Neptune's system of satellites so different from those predicted for a gaseous giant planet? Two planetary scientists, Dr. Raluca Rufu (Weizmann Institute of Science, Israel) and Dr. Robin Canup (Southwest Research Institute, US) demonstrate how Triton wreaked catastrophic havoc on Neptune's first generation of very unfortunate moons.



and here is another

Earth's lunar companion is thought to have been born about 4.51 billion years ago, according to a recent study. This means that our Moon was born soon after Earth's formation in the primeval Solar System. The average distance of Earth's Moon from our planet is about 238,900 miles--or approximately 1.28 light-seconds--and it is in synchronous rotation with Earth, always showing the same face, with the near side famous for its beautiful bewitching dark volcanic maria (Latin for seas) that are situated between prominent impact craters and the bright, very ancient, crustal highlands. Our Moon's surface is actually quite dark, even though it appears in the sky at night to be very bright, with a reflectance only a bit higher than that of old asphalt. The prominent position of our Moon in our planet's night sky, as well as its regular cycle of phases, have made our nearest and dearest celestial companion a valuable cultural influence since ancient times in art, mythology, language, and on calendars.



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.

Other facts:

When a moon is in an orbit around its parent-planet, all is well--just as long as the gravity that is holding the moon together in one piece exceeds the powerful, relentless pull of its planet. Alas, if a moon wanders too close, and the tidal forces of the parent-planet exceed the gravitational bind of the unlucky moon, the moon will fall apart. This is termed the Roche limit. Earth's relatively large Moon is a very fortunate natural satellite, and the limit here is a bit under 10,000 kilometers--while our Moon is a safe 385,000 kilometers away from our planet.



"Our model explains the diversity of these ice-rich moons and the evidence for their very active geology and dynamics. It also explains a puzzling fact about Titan, in that a giant impact would give it a high orbital eccentricity," Asphaug continued to explain to the press on October 18, 2012.



Another interesting piece of Apollo 11 trivia is the fact that the Apollo missions had actually been ongoing and this was actually the fifth mission of Project Apollo that involved human spaceflight. Aside from that, it was also the third voyage by humans to the moon; however, no human had ever stepped foot on the moon until this specific voyage.