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It is important to know at any age!

Voyager 2 flew by Neptune back in 1989, and its observations revealed a number of active geysers, situated within the polar cap heated by the Sun. The geysers hurl out plumes to the impressive height of up to 8 kilometers. Triton has a relatively high density that indicates rocks account for approximately two-thirds of its mass, and ices (mostly water ice) compose the remaining one-third.



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Who would you believe? It really doesn't matter what the studies show. Believe it or don't believe it. It's your choice. But if I were you, and I were out on the town on a full-moonlit night, I might take just a little extra precaution and keep the pepper spray handy. Werewolves beware.



and finally

During the 2013 experiment, the radar instrument spotted echoes emanating from the seafloor and determined the depth of Ligeia Mare along Cassini's track over that strange methane sea. This represented the first-ever detection of the bottom of an extraterrestrial sea. The astronomers were amazed to find that depths in this distant, alien sea were as great as 525 feet at the deepest point along the track the radar pointed.

Other facts:

The research proposes that the shoreline surrounding Ligeia Mare is possibly porous and may be saturated with liquid hydrocarbons. The data span a period running from local winter to spring, and the astronomers expected that--in a way similar to seasides on Earth--the surrounding solid terrains on Titan would warm much more rapidly than the sea.



The research published in the July 4, 2016 issue of Nature Geoscience highlights the main factor differentiating moon-birth around Mars and Earth: the differing rotation speeds of the two planets prompted "completely different tidal actions," Dr. Charnoz explained in the July 4, 2016 CNRS Press Release. Dr. Charnoz proposes that at the time of their respective impacts, "Earth took less than four hours to spin on its axis whereas Mars rotated very slowly over a 24-hour period." The result of this important difference caused Earth to hold on to its single, large Moon, while the Martian collision created a dozen smaller moons alongside a larger moon. As time went by, Martian tidal action--resulting from the planet's slow rotation rate--caused most of the moons, including the largest one, to crash back down to the surface of their parent-planet. As a result, only the two most distant moons, Phobos and Deimos, survived as testimony to the ancient catastrophe.



Earth's Moon is a brilliant, beguiling, bewitching companion world. The largest and brightest object in our planet's night sky, it has for eons been the source of wild magical tales, myths, and poetry--as well as an ancient symbol for romantic love. Some traditional tales tell of a man's face etched on its bright surface, while still others whisper haunting childhood stories of a "Moon Rabbit". Lovely, ancient, and fantastic stories aside, Earth's Moon is a real object, a large rocky sphere that has been with our planet almost from the very beginning, when our Solar System was first forming over four billion years ago. But where did Earth's Moon come from? In April 2014, a team of planetary scientists announced that they had pinned down the birth date of the Moon to within 100 million years of the formation of our Solar System, and this new discovery indicates that Earth's Moon was most likely born about 4.47 billion years ago in a gigantic collision between a Mars-sized object and the primordial Earth.