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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.
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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.
Although Europa was visited by the two spacecraft Pioneer 10 and Pioneer 11 in the early 1970s, and the twin Voyagers in 1979, these early flybys only produced grainy, dim images. However, these early pictures revealed enough about the little moon to make it intriguing. Pale yellow icy plains were seen in the Voyager images. The plains also tantalizingly displayed red and brown mottled areas. Long cracks were observed, running for thousands of miles over the shattered eggshell-like crust. On Earth, similar cracks would suggest such features as high mountains and deep canyons. But nothing higher than a few kilometers was seen on the moon. In fact, Europa is one of the smoothest bodies in our Solar System.
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The research published in the July 4, 2016 issue of Nature Geoscience highlights the main factor differentiating moon-birth around Mars and Earth: the differing rotation speeds of the two planets prompted "completely different tidal actions," Dr. Charnoz explained in the July 4, 2016 CNRS Press Release. Dr. Charnoz proposes that at the time of their respective impacts, "Earth took less than four hours to spin on its axis whereas Mars rotated very slowly over a 24-hour period." The result of this important difference caused Earth to hold on to its single, large Moon, while the Martian collision created a dozen smaller moons alongside a larger moon. As time went by, Martian tidal action--resulting from the planet's slow rotation rate--caused most of the moons, including the largest one, to crash back down to the surface of their parent-planet. As a result, only the two most distant moons, Phobos and Deimos, survived as testimony to the ancient catastrophe.
Dr. Jacobson believes that this new study showing a later lunar birthday means that our planet's impact history was more turbulent than earlier thought. The alteration in Earth's bombardment rate, he suggests, also means an alteration in the quantity of energy that went into our planet's oceans and atmosphere. It also has implications for the history of our planet's surface temperature--which is important because liquid water could not exist until the surface had cooled off sufficiently.
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.