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A little interesting about space life.
Similar to the great lakes in North America, there are massive lakes in the hollow underground cave system. However unlike the great lakes, the caves roofs over the lakes of the moon are supported by the natural array of vertical pillars protruding through the waters like a massive cluster of Mangrove roots. The underside of the roof above the lakes and also the vertical pillars protruding through the waters are 'coated' by a gel like material. This gel shows many of the signs of being a living substance. It also emits light and carries out the function of 'cleaning' the moon's atmosphere by absorbing impurities which it assimilates as a nutrient. It rejects some part of the absorbed impurities as balls of waste exited into the lakes. The waste in turn is eaten by the fish or absorbed by plants in the lakes. The reflection of the softly glowing gel on the water enhances the lighting in the area of the lakes. At all places in the moon, the water in the lakes is clean, not salty and is suited for use directly for drinking. The waters of these lakes are however subject to massive tidal effects. These are due to the fluctuation of the resultant of the gravitational tugs of the earth and the sun as the earth spinning on its own axis and carrying the moon in orbit in turn orbits the sun. Because of the low moon gravity, the tidal effects are checked weakly and the water levels rise and fall by hundreds of feet. The tides force the water to spread hundreds of miles along the vast underground areas thus wetting the dry areas of the caves in a cyclic pattern. Because of these vast latitudinal and longitudinal fluctuations of water spread, there are artificial water stream formations all over the geological-structure of the moon. The streams of water flow over the cave surfaces and create huge waterfalls at some places. These waterfalls last for many days and appear and disappear in a cyclic pattern, following the tides.
and here is another
"Their motion is tied together in a way similar to that of three of Jupiter's large moons. If you were sitting on Nix, you would see Styx go around Pluto twice every time Hydra goes around three times," Dr. Hamilton commented in the June 3, 2015 HST Press Release.
The "chaos terrains" are those regions of the icy moon that are covered with shattered, scrambled, and rotated chunks of crust the size several city blocks. Galileo images show swirly and very rough-looking material between the broken blocks of ice, which indicates that the blocks may once have been lodged atop a bed of slushy stuff that ultimately froze at the very frigid surface temperatures of Europa.
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In the tragicomedy that characterizes human relationships, it has been said that the closer we get to someone, the weirder that person gets. Earth's Moon is our planet's closest neighbor in Space--mysterious, bewitching, bothersome, and bewildering, it has successfully hidden many of its secrets from the prying eyes of curious observers. In July 2017, using satellite data, a team of astronomers announced that they have, for the first time, detected widespread water hidden within ancient explosive volcanic material on Earth's nearest and dearest companion world. This discovery indicates that the interior of Earth's Moon contains large quantities of indigenous water that has finally been revealed in numerous volcanic deposits distributed across the lunar surface--and these ancient deposits contain unusually high amounts of imprisoned water compared with surrounding terrains. The discovery of water in these ancient lunar deposits, which are believed to be composed of glass beads created in the explosive fiery eruption of magma shooting out from the deep interior of the Moon, strengthens the theory that the lunar mantle is surprisingly water-rich.
Because the lunar atmosphere is very thin, it is far too sparse to prevent a steady shower of impacts from tumbling asteroids, comets, and meteoroids. These objects strike the lunar surface, leaving behind numerous crater scars. For example, Tycho Crater is over 52 miles wide.
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.