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A little interesting about space life.
Of the four terrestrial, rocky planets of the inner Solar System (Mercury, Venus, our Earth, and Mars), both Mercury and Venus are moonless. Earth possesses one lone Moon, but it is a very large one--the fifth largest moon in our entire Solar System, in fact. Mars, on the other hand, has two tiny misshapen moons that resemble rocky potatoes, and are lumpy and dark, as they travel in their nearly circular orbits close to the plane of the Martian equator. The Martian moons, Phobos and Deimos, are probably asteroids that were captured by Mars long ago.
and here is another
In order to spot such a remote exomoon, the authors of this new study, The Hunt for Exomoons with Kepler (HEK): III. The First Search for an Exomoon around a Habitable-Zone Planet, used a technique that models the dips and features of the parent star's light-curve (stellar brightness vs. time), which are caused by transits of the planet (and any accompanying moons) in front of the face of its star. This is a complicated and difficult endeavor because numerous and diverse models of planet-moon dynamics must be taken into consideration. Each one of these models possesses parameters that describe physical properties belonging to the planet or moon, as well as parameters describing the orbital system. The authors use what is termed Bayesian statistics to account for the fact that the true orbital model of this planetary system is still not known--and this enables them to calculate if a model with our without a moon fits the observed light-curve the best.
How am I so sure of this? Simple. Because I've personally been using the moon to my advantage for more than 20 years, and know how effective it is. Have you ever had one of those epic days fishing where it seemed like no matter what you threw in the water, you caught fish? If you have, it was more than likely due to the fact that the moon was in a certain phase, rather than your skills as an angler (I hate to burst anyone's bubble, but it's true).
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"For decades scientists have thought Jupiter's moon Europa was a likely place for life, but now we have specific, exciting regions on the icy moon to focus our future studies, " Dr. Don Blankenship, senior research scientist at the University of Texas at Austin's Institute for Geophysics, commented in the November 16, 2011 National Geographic News.
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 Apollo 11's lunar module, Eagle, landed on the surface of the moon on the 20th of July, 1969. It landed at approximately 20:17:40 UTC. An interesting fact is that the Eagle had barely enough fuel left for 25 seconds more, as the two men had encountered some difficulties during landing due to their training at NASA. Things were quite a bit different in reality and the several alarms that were going off certainly didn't help to calm the already likely nerve-wracking maneuver.