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- Change in Earth's Orbit Climates Historical
- Cool Nebula Wallpapers
- Color of Saturn Planet
- Comparing Planets Outer
- Computer Model of Solar System
- Chalk Solar System
- Cernan Astronaut
- Colorful Nebula
- Cool Space Pictures Galaxy
- China Moon Rover 2019
- Cheetah in a Space Suit
- Center Space Shuttle Building
- Cosmos Space Hd
- Cassini-Huygens Mission NASA
- Composition of Planet Mars
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Interesting facts about space.
Many surface crusts are made of a material known as lunar regolith. Lunar regolith transforms into translucent forms through a process called agglutination when the regolith is subjected to high heat. In many places, parts of the moon's surface consist of translucent material embedded in the moon's outer crust. These surfaces allow a substantial degree of sunlight to penetrate into the caves. Most of this glass like surface material has been naturally formed, millions of years ago. Amongst the translucent surface areas, there are also many areas of near clear-glass transparency. Due to refraction of the sunlight that penetrates into the caves, massive rainbow like color beams frequently appear in very many places inside the caves. Due to the vastness and the complexity of the spectrum of rainbow colors intermingling with each other, there is a stunningly beautiful visual effect inside the caves. The glow from the moon's outer surface when seen from inside the caves, gives a further dimension of beauty for the visual enjoyment of the people of the moon.
and here is another
Who would you believe? It really doesn't matter what the studies show. Believe it or don't believe it. It's your choice. But if I were you, and I were out on the town on a full-moonlit night, I might take just a little extra precaution and keep the pepper spray handy. Werewolves beware.
Earth's bewitching large Moon was probably born as the result of an immense impact, when a Mars-size protoplanet named Theia smashed into Earth about 4.5 billion years ago. This cataclysmic collision is thought to have hurled a vast amount of Earth-stuff and Theia-stuff into orbit around our ancient planet. Debris from the two unfortunate bodies gradually accumulated to give birth to our Moon, as tumbling little newborn moonlets crashed into one another and melded together into one large object.
- Women Astronauts in Space
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- Married Couple to Mars
- Solar System Collision
- Blood Moons Perry Stone
- What Are the Galaxies Names
- Nuclear-Powered Space Probe
- NASA Curiosity Tracking Status
- NASA Future Space Vehicles
- History of Astronomy PowerPoint
- Blue Star Flower Cluster
- Probe NASA Asteroid Collision
- JPL Mars Rover Control Room
- Mars Rover Competition of 2019
Kepler-22b is an extrasolar planet that circles Kepler-22, a G-type star that is situated about 600 light-years from our own planet in the constellation Cygnus. This intriguing new world, that resides beyond our Solar System, was first spotted by NASA's highly productive, though ill-fated, Kepler Space Telescope in 2011. Kepler-22b has the distinction of being the first known transiting extrasolar planet to reside within the so-called habitable zone of its star. The habitable zone is the term used to describe that Goldilocks region around a star where water can exist in its life-loving liquid state. Planets dwelling in this fortunate region are not too hot, not too cold, but just right for water and, hence, life to exist. A planet that circles its star in the habitable zone suggests that there is the possibility--though not the promise--of life as we know it to exist on that world.
Because the lunar atmosphere is very thin, it is far too sparse to prevent a steady shower of impacts from tumbling asteroids, comets, and meteoroids. These objects strike the lunar surface, leaving behind numerous crater scars. For example, Tycho Crater is over 52 miles wide.
According to the new theory, moon-formation starts at the very edge of a planetary ring, where a fragile baby moon can begin to emerge without the danger of being ripped apart by the fierce gravity of its parent planet. These dancing little moonlets, formed from ring-material, then travel outward. As the ring-system continually produces moonlet after moonlet after moonlet, the small icy worlds coalesce to form increasingly larger moons. The larger moons, in turn, may also merge together, as they dance outward from their parent planet.