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The sunlight that penetrates through the transparent crust helps the growth of vegetation in the caves to a substantial extent. However sunlight is not the main light source in the caves. The types of vegetation found in the moon are markedly different from the ones on earth. The plants commonly seen in the caves are quite short and look very much like the miniature trees, bushes and shrubs grown using Japanese "Bonsai" techniques.
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Food supplies come directly from various water plants that grow in the lakes in abundance. The moon people consume a mix of raw food as well as cooked food. The flowers, seeds, leaves, stems and the bulbs of the water plants are their staple diet. These foods contain all the proteins and other necessary ingredients necessary for healthy living.
However, the truth is, during their entire voyage to the Moon and back to Earth, Armstrong, Aldrin and Collins only received amount of radiation equal to about 0.1% of the deadly dose. Their total exposure was approximately 11 milisieverts, and radiation dose lethal to an average human being is aroung 8,000 millisieverts.
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"For decades scientists have thought Jupiter's moon Europa was a likely place for life, but now we have specific, exciting regions on the icy moon to focus our future studies, " Dr. Don Blankenship, senior research scientist at the University of Texas at Austin's Institute for Geophysics, commented in the November 16, 2011 National Geographic News.
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.
Planetary scientists usually calculate the Moon's age by using the radioactive decay of elements like uranium, explained Dr. John Chambers in the April 2, 2014 National Geographic News. Dr. Chambers is a planetary scientist at the Carnegie Institution for Science in Washington, D.C. By studying an element with a recognized decay rate, and knowing its concentration in Moon rocks or the Earth's surface, scientists are able to calculate back in time to when the material first formed. However, there are numerous and varying radioactive materials that can provide differing timelines, added Dr. Chambers, who was not involved in the study.