Apollo 17 Recovery 1969 05 26 17 Recovery Apollo

Apollo 17 Recovery 1969 05 26 17 Recovery Apollo

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Interesting facts about space.

Though a moon day is equivalent to 28 earth days, surprisingly, the biological day cycle of the moon people is 24 earth hours. This shows that their biological clock has nothing to do with the sun rise and sun set in the moon. Perhaps the 24 hour period of time may be a unique biological 'interval of renewal' that nature has given to all human species. Usually moon people sleep about eight hours a day at "any time of convenience" and remain active during most of the remaining hours. The "time of convenience" varies for each individual. As a result of not having a particular day or night time, there are always people awake and active all of the time. Therefore, all community based activities take place all the time and continuously without stoppage. There are no holiday systems practiced in the moon. Every day is a working day and every hour is an active hour. Every hour is also a sleeping hour to whoever desires to consider it that way.



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.



and finally

Like Earth's own large Moon, Triton is locked in synchronous rotation with its planet--one side always faces Neptune. However, because of Neptune's odd orbital inclination, both of the moon's polar regions take turns facing the Sun. Spacecraft images of Triton reveal mounds and round pits formed from icy lava flows (cryovolanism), as well as smooth volcanic plains. The surface of the moon is only sparsely cratered, indicating that its surface is new--that is, it is constantly being resurfaced, probably by the "lava" flow from icy volcanoes. Triton is very bright--its fresh, sparkling, new ice-coating is believed to cover a heart of metal and rock. Triton's high density suggests that it contains more rock in its interior than the icy moons of Saturn and Uranus.

Other facts:

The current study's Franco-Belgian-Japanese collaboration looks forward to this mission. JAXA plans to enlist them to conduct tests on the Martian samples when they are returned to Earth. The samples will help the scientists determine whether Phobos is indeed made up of a mixture of Martian mantle and debris left in the wake of the tragic crash of the doomed, vanished protoplanet--as suggested by their supercomputer simulations.



Icy moons and tumbling, gleaming moonlets dance around within the lovely and very famous rings of the gas-giant planet Saturn. A study released in November 2012 now suggests that most of the moons inhabiting our own Solar System were born from ancient, primordial Saturn-like ring systems that swirled around newborn planets circling the young Sun. According to this study, most of our Solar System's regular satellites--which are those moons that lovingly embrace their parent planets in approximately equatorial orbits--formed in this way. In contrast, the most popular theory explaining moon-formation, suggests that moons emerged simultaneously with their parent planets, as a direct consequence of planetary formation.



According to the new theory, moon-formation starts at the very edge of a planetary ring, where a fragile baby moon can begin to emerge without the danger of being ripped apart by the fierce gravity of its parent planet. These dancing little moonlets, formed from ring-material, then travel outward. As the ring-system continually produces moonlet after moonlet after moonlet, the small icy worlds coalesce to form increasingly larger moons. The larger moons, in turn, may also merge together, as they dance outward from their parent planet.