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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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"We've found a likely solution to the long-standing problem of how Triton arrived in its peculiar orbit. In addition, this mechanism introduces a new pathway for the capture of satellites by planets that may be relevant to other objects in the Solar System," explained Dr. Craig Agnor, a researcher from the University of California, Santa Cruz, in the May 10, 2006 issue of Time Magazine.
So if your are feeling a bit off balance today, now you know why. The most common use of this phrase is traditionally used to emphasize a rare or highly unlikely event. All those things you may have put off saying or doing, the getting around to it tasks that you have shelved and only ever do once in a blue moon..today is the day for it! So seize the day and get to it! Get the romance happening and re-inject your life with some blue moon rarities!
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The February 2018 study, conducted by Carnegie and JPL astronomers, created detailed scenarios in order to determine whether existing theories about the catastrophic Giant Impact theory could explain a wet Moon that is still depleted in other volatile elements like sodium and potassium.
The inner Solar System is dramatically different from the distant realm of the giant planets. The inner region of our Solar System, where our Earth is situated, is almost entirely moon-less. Of the four relatively small, rocky worlds--Mercury, Venus, our Earth, and Mars--Mercury and Venus are barren of moons, and Mars is orbited by two fascinating, but very small, potato-shaped moons named Phobos and Deimos. The duo of Martian moons are often considered to be captured asteroids that long ago escaped from their birthplace in the Main Asteroid Belt between Mars and Jupiter. According to this scenario, Phobos and Deimos, during their dangerous journey from their original home, were snared by the gravity of their adopted Red Planet when our 4.56 billion-year-old Solar System was young. In the warm and well-lit inner Solar System, only Earth's large Moon is a significant moon-world in its own right.
Following the final giant impact that was responsible for lunar-birth, the Earth's mantle should have been depleted of iridium, platinum, and other similar elements. Although these elements still dwell in Earth's mantle, only small quantities remain. This indicates that only a small amount of material accreted onto Earth after the Moon-forming blast by the doomed Theia. Any such elements lingering in the Earth's crust that "love iron" arrived after that horrendous collision.