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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
The temperatures around the equatorial and mid latitude surface at daytime and in the night are around 225oF and minus 298oF respectively. As the moon day is approximately 28 earth days, heating and cooling of the moon's surfaces affects the inside cave temperature significantly. The temperature difference in the opposite side of the moon makes the air in the cave move from one area to the other creating complex wind movements. When high speed wind flows across the vertical rock structures, it makes gurgling sounds in the caves, resulting in eerie or weird echo effects. The blowing wind helps to mitigate the high humidity conditions.
Unfortunately, even though mankind has gone to the moon in 1969, this is still not a simple feat in the 21st century. Most of the know how accumulated during the lunar flights have been lost due to the fact that production facilities have been dismantled and many experts who worked on the lunar missions either have retired or died. Right now, it would be impossible to replicate the Saturn 5 rockets that were used to launch the original Moon Mission. Thus, due to this, it has become impossible to fly to the moon again without some sort of a preparation. Hence, many scientists state that going to Mars is a better option as compared to going to the Moon.
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"This is still very much an area of active research, so there is much that scientists including our Department of Terrestrial Magnetism staff scientist Erik Hauri, as well as many other Carnegie colleagues and alumni, are figuring out about how much water exists on the Moon. This is a highly important and challenging question to answer given that we have limited knowledge on the history and distribution of lunar water," explained Dr. Miki Nakajima in a February 26, 2018 Carnegie Institution Press Release. Dr. Nakajima, who is of the Carnegie Institution of Washington (D.C.), along with California Institute of Technology's (Caltech's) Dr. David Stevenson, set out to determine whether prevailing lunar formation models need to be adjusted to explain more recent higher estimates of the quantity of water on Earth's Moon. Caltech is in Pasadena.
A fourth, more recent model, is based on the existence of a synestia. A synestia is a doughnut-shaped cloud composed of vaporized molten rock. This recently discovered inhabitant of the Universe is believed to take shape when planet-sized bodies catastrophically blast into one another with both high energy and angular momentum. Soon after the discovery of these puffy celestial "doughnuts" in 2017, planetary scientists came to the realization that they may have a new way to explain Moon-birth. The ancient collisions, that create a synestia, are so violent that the objects that form from these cosmic crash-ups melt and partially vaporize. Ultimately, after having cooled off sufficiently to solidify, they create (almost) spherical planets, such as those inhabiting our own Solar System.
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.