NASA Science Experiments analyzing old nasa apollo seismometer data reveals that Experiments Science NASA

NASA Science Experiments analyzing old nasa apollo seismometer data reveals that Experiments Science NASA

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A little interesting about space life.

Only after Triton's orbit became circular, around its adopted parent-planet, could some of the rubble re-accrete to form the moons of Neptune that astronomers observe today. Triton's highly disruptive invasion of the Neptune system may be the reason why the moons of Neptune do not conform to the 10,000:1 ratio of mass between parent-planet and moon-offspring that literally all of the moons observed in the satellite systems of the other giant planets in our Solar System conform to.

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Over the years, several theories have been proposed to explain the mechanism involved in Triton's capture by Neptune. One theory suggests that Triton was snared in a three-body encounter. According to this scenario, Triton is the lone survivor of a binary Kuiper Belt Object (KBO) that had been fatally jostled during a destructive close encounter with Neptune.

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Numerical simulations have been conducted that show that there is a 0.41 probability that Neptune's moon Halimede blasted into Nereid in the past. Even though it is not known if this collision really did occur, both moons display similar grey colors. This implies that Halimede could be a chunk of Nereid that broke off during the collision.

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Some studies which have been performed in certain cities within the United States show that there is no correlation between the full moon phase and such things as a rise in suicides, crime rate, dog bites or births. And yet, other studies completed by such individuals as psychologists and other human behaviorists have shown that there is, in fact, a peak in certain kinds of behavior associated with a loss of contact with reality during full moons. These include murder, arson, dangerous driving and kleptomania, which is an irresistible impulse to steal due to an emotional rather than economical need.

Triton also possesses a thin atmosphere composed mainly of nitrogen, and a smaller quantity of methane. This atmosphere probably is the result of Triton's cryovolcanism, which is enhanced by seasonal heating from the Sun. Although little is currently known of Pluto's atmosphere, it is thought to be primarily composed of nitrogen with some carbon monoxide and methane added to the mix--and it is extremely tenuous. Pluto's very thin atmosphere may exist as a gas only when Pluto is nearest to the Sun (perihelion). For most of Pluto's very long year, the atmospheric gases are frozen in the form of ice on its extremely frigid surface. One year on Triton is almost 248 Earth-years long--or 90,471 Earth-days!

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.