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A little interesting about space life.

Neptune is circled by only 14 moons, a considerably smaller number than Jupiter's 70. Also, most of Neptune's moons are extremely small. Triton, however, is an exception. In fact, Triton harbors 99.7% of the mass of Neptune's entire system of moons combined. The second-largest irregular moon in our Solar System, Phoebe of Saturn, sports only about 0.03% of Triton's mass. It is thought that Triton was snared by its adopted parent-planet some time after Neptune had already formed a system of moons. This means that the capture of the wandering Triton was likely a catastrophic event for Neptune's original moons, disrupting their orbits, and causing them to blast into each other--thus creating a rubble disc.



and here is another

However, the fact of the matter is that moon will always remain the best option for mankind. The reason for this stems from the fact that the moon can always act as a stepping stone to the rest of the solar system and beyond. This is only natural, as the moon is in a very close proximity to Earth. Only by taking a 3 day trip, it is possible to reach the Moon with standard chemical propulsion techniques. However, in retrospect, going to Mars would require almost 100 times the amount of trip time of moon, since Mars is about 1000 times further then the moon. The amount of life support that is required for a mission that will take 2 years or more is definitely very costly and more importantly, the technological capability is not there. Thus, with our present global financial and technical capability, the moon is the only realistic option.



and finally

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.

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In addition to the Giant Impact theory, there are several other models that have been proposed to explain how our Moon was born. One alternative model to the Giant Impact scenario suggests that Earth's Moon was once a part of our planet that simply budded off when our Solar System was in its infancy--approximately 4.5 billion years ago. According to this model, the Pacific Ocean basin would be the most likely cradle for lunar birth. A second model proposes that our Moon was really born elsewhere in our Solar System and, like the duo of tiny potato-shaped Martian moons, was eventually snared by the gravitational tug of a major planet. A third theory postulates that both Earth and Moon were born at about the same time from the same protoplanetary accretion disk, composed of gas and dust, from which our Sun's family of planets, moons, and smaller objects ultimately emerged.



Earth's Moon consists of a core, mantle, and crust. The lunar core is proportionally smaller than other terrestrial bodies' cores. The iron-rich, solid inner core is 149 miles in radius, and it is encased within a liquid iron shell that is about 56 miles thick. A partly molten layer with a thickness of 93 milles surrounds the iron core.



JAXA has announced a space mission scheduled to begin in 2022, with an expected return to Earth in 2026. "Its objective is to carry out close-up remote sensing and in-situ observations of both Phobos and Deimos, and to bring back samples from Phobos," commented Dr. Ryuki Hyodo in the July 4, 2016 CNRS Press Release. Dr. Hyodo is a planetary scientist, originally from Kobe University in Japan, and he is also currently collaborating with the IPG. "High-resolution impact simulations are still needed to understand more about the disk structure," he continued to explain to the press.