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A little interesting about space life.
The model indicates that Triton originated as part of a binary system, much like Pluto and its large moon Charon. "It's not so much that Charon orbits Pluto, but rather both move around their mutual center of mass, which lies between two objects," Agnor added.
and here is another
Of the hundreds of bewitching moons in our Sun's family, Titan is remarkable for being the only one boasting a dense atmosphere and large liquid reservoirs on its surface, rendering it in many ways more like the four rocky, terrestrial planets of the warm and well-lit inner Solar System. Indeed, both Earth and Titan possess atmospheres dominated by nitrogen--more than 95 percent nitrogen in Titan's case. However, unlike our Earth, Titan's atmosphere has very little oxygen; the remainder of its atmosphere is primarily composed of methane and trace quantities of other gases--such as ethane. At the truly frigid temperatures found at the Saturn system's great distance from our Sun, Titan's methane and ethane can exist on the surface in their liquid form.
The prevailing theory of lunar formation--the Giant Impact hypothesis--proposes that our Moon was born as the result of a disastrous collision between our still-forming proto-Earth and a doomed Mars-sized body named Theia--and this impact is thought to have created a partially vaporized, extremely hot disk of material that swirled around our infant planet. Eventually, this primordial disk cooled off, and ultimately accreted to form our Moon. In February 2018, a team of astronomers announced that their ongoing research is revealing that Earth's Moon may be wetter than initially thought, which raises important questions about some aspects of this origin story.
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In July 2017, a team of astronomers announced that they had used satellite data to find--for the first time--signs of widespread water hidden beneath ancient volcanic material on Earth's Moon. The scientists' discovery suggests that the interior of our Moon holds large quantities of indigenous water. This plentiful, but well-hidden water, reveals its secret presence in numerous volcanic deposits, that had been explosively distributed across our Moon's surface when ancient lunar volcanoes erupted. These primordial deposits contain unusually large amounts of imprisoned water compared with nearby terrains. The detection of water within these lunar deposits, is believed to be made up of glass beads that formed as a result of the explosive fiery eruption of magma, hurled out from deep within our Moon. This finding supports the theory that the lunar mantle is surprisingly soggy.
The crust of Earth's Moon is 43 miles thick on the near-side hemisphere, and 93 miles on the far-side. It is composed of silicon, magnesium, oxygen, calcium, aluminum, and iron. There are also trace amounts of titanium, uranium, thorium, hydrogen, and potassium.
"What people frequently forget in this field is that you never have just one big impact. We have to worry about how big the next biggest impact was," and whether that impact blurred the effects of the previous giant impact, he continued to explain.