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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
On July 20, 1969, during one of the defining moments of the human history, Neil Armstrong became the first man to step on the surface of Earth's Moon. In his own words, it was truly "one small step for a man, one giant leap for mankind."
Even though the Moon is much closer than any other major astronomical object, Hubble Telescope still cannot register any object on the moon smaller than four metres across.
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On this full-moon day under the Bodhi tree he is said to have declared: "I know thee, never shall you build again these walls of pain." He made the 'knowledge' he had acquired in the course of his Enlightenment the basis of his following some 45 years of preaching and teaching as a religious philosopher while travelling as a mendicant. He was about 80 years old when he died in Kusinagara in Nepal after being poisoned.
Mars may be circled by many moons smaller than 160 to 330 feet in diameter, and a ring of dust has been predicted to circle Mars between Phobos and Deimos.
Most of Saturn's natural satellites are very small and icy dancing moonlets. However, the larger, icy midsized moons twirl around their enormous ringed planet in a lovely and mysterious dance. The largest of the icy moons is Rhea, Saturn's second-largest moon after the weird world that is Titan. Iapetus, the third largest of Saturn's moons, is two-faced, with one side composed of gleaming, very bright, highly reflective ice, and the other, dark and non-reflective, a blackened splotch staining the pristine white ice. Iapetus is larger than Mimas and Enceladus. There is an enormous impact crater on the moon Mimas, that stands out as a prominent feature on what is apparently a badly bombarded, heavily cratered world. The large impact crater Herschel on this 400-kilometer moon was excavated by a tumbling chunk of space-stuff made of rock, ice, or both, that came very close to powdering the entire little moon. Another icy moon, Enceladus, is a bewitching world, 500-kilometers in diameter, that is thought to harbor a global subsurface ocean beneath its frozen crust. Where there is liquid water there is always the possibility--though, by no means, the promise--of life. Enceladus also has the highest albedo of any other moon in our Solar System. This means that it has the most dazzlingly bright reflective surface. It also possesses a very active geology, rendering it almost free of craters because it is constantly being resurfaced by the emissions of gushing icy geysers that are responsible for fresh snow that keeps the surface of the little moon sparkling and smooth.