National Geographic Asteroid Belt space pictures this week volcanic vortices and asteroid Geographic National Asteroid Belt

National Geographic Asteroid Belt space pictures this week volcanic vortices and asteroid Geographic National Asteroid Belt

We found 10++ Images in National Geographic Asteroid Belt:




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A little interesting about space life.

The moon's internal geological structure is very strange and unique. It has vast areas of hollow underground caves. This is because the moon passed through boiling and molten states before it cooled down to its stable present day temperature. Some caves are miles and miles in length and breath. These caves exist at varying depths below the moon's surface. Almost all the caves are internally connected to each other and it is possible to trace many paths through interconnected caves to fully 'circumnavigate' the moon without ever stepping out on to its outer surface. The tops of the caves that form the crust of the moon's surface are supported on massive vertical rock pillars that rise out of the bottom surface. These vertical support structures are very hard and rocklike and naturally contoured in shell like formations endowing them with heavy load bearing capabilities. To visualize the interior of these caves a comparable earth structure would be the NFL football domes. They would compare in size with some of the smaller caves but none of the caves in the moon are formed in a particular shape, pattern, length, breadth or height, and are quite irregular in shape. Surface terrain is also to a large extent irregular and variable.



and here is another

Last night there was a full moon. One of my dogs was very on edge, starting at every sound, staring out into the darkness at something I could neither hear nor see. The other 4 dogs were sound asleep. Did she sense something different about the moonlit night?



and finally

The Waving Flag. According to this argument, frequently cited by the people who think that the moon landings were nothing more but a hoax, is that the star-spangled banner of the United States of America seemed to wave and flutter as Neil Armstrong planted it to the ground. This wouldn't have been much of an issue except for the fact that there is virtually no atmosphere on the moon, and therefore no wind whatsoever to have such an effect on any flag.

More information:

The Cassini-Huygens mission is a collaborative NASA/European Space Agency/Italian Space Agency robotic spacecraft that is observing the Saturn system. The spacecraft was initially constructed to sport two components: One is the European Space Agency-designed Huygens Probe named in honor of the Dutch mathematician and astronomer Christiaan Huygens (1629-1695), who discovered Titan. Huygens also studied the rings of Saturn. The second component, the NASA-designed Cassini Orbiter, was named for the Italian-French astronomer Giovanni Dominico Cassini (1625-1712) who discovered four of Saturn's other moons. After a long, difficult journey through interplanetary space, that took it from Earth to Saturn, Cassini-Huygens finally reached the realm of the ringed planet on July 1, 2004. On December 25, 2004, the Huygens Probe was deliberately severed from the Cassini Orbiter, and began its descent down to the long-veiled and hidden surface of Titan--sending back, to waiting astronomers on Earth, an abundance of valuable information about the mysterious moon-world. Titan, at last, had its hidden face unveiled--revealing its well-kept secrets. The mission will continue until 2017.



Over the passage of billions of years, this ceaseless rain of falling objects have pulverized the lunar surface, creating fragments ranging in size from a fine powder to enormous, heavy boulders. Almost the entire lunar surface is literally blanketed by a pile of ground up rubble composed of charcoal gray, powdery dust and rocky debris collectively termed the lunar regolith. Beneath the regolith there is a region composed of shattered bedrock that is called the megaregolith.



The more widely accepted theory that the planets and regular moons formed together from the same swirling cloud of gas and dust, works well as an explanation for the larger moons of our Solar System, such as the four Galilean moons--Io, Europa, Ganymede, and Callisto--orbiting the giant planet Jupiter. However, the multitude of smaller moons, swarming around the giant planets, "have so far been considered a by-product," Dr. Crida commented in the November 29, 2012 Scientific American.