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It is important to know at any age!
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.
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Dr. Rufu and Dr. Canup studied the scenario in which Neptune once, when it was young, had a typical prograde system of moons orbiting it that was similar to those of the other gas giants in our Solar System. The two authors propose that Triton may have originally been a KBO that wandered away from its home in the Kuiper Belt, only to be snared by Neptune. The interactions that resulted from the capture of Triton between retrograde moons and Neptune's original, prograde moons may have then resulted in the destruction of this orderly system, leaving in its wake only the ruthless Triton and Neptune's moons that are still around today.
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.
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Our Moon makes a complete orbit around Earth in 27 Earth days and it rotates (spins) at that same rate--meaning, in that same amount of time. Because our planet is also moving--rotating on its axis as it circles our Star--from our viewpoint, our lunar companion appears to circle us ever 29 days.
The more widely accepted theory that the planets and regular moons formed together from the same swirling cloud of gas and dust, works well as an explanation for the larger moons of our Solar System, such as the four Galilean moons--Io, Europa, Ganymede, and Callisto--orbiting the giant planet Jupiter. However, the multitude of smaller moons, swarming around the giant planets, "have so far been considered a by-product," Dr. Crida commented in the November 29, 2012 Scientific American.
Songs, poems, odes, reveries. The Moon has been the subject of endless adoration since the beginning of time. Mysterious and changeable, sometimes occulted by clouds or (gasp!) the Earth itself, our satellite, our iridescent child, the Moon floats suspended in the sky, enticing us to dream, to wonder, to reflect. To garden in the moonlight, to walk in the woods with the moon shining through foliage or bare branches, whenever we have the chance to have her silvery light embrace us we know we are being touched by the hand of the divine feminine and we are blessed.