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System Name | octo1 |
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Processor | dual Xeon 2687W ES |
Motherboard | Supermicro |
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Case | Rosewill Thor |
I feel a little stupid for not having known this but it seems that the moon's rate of rotation is almost perfectly synchronized with its orbit - which is why we only see the same "face." Although technically this isn't completely true. When the moon is closest to earth its rotation is slightly slower and we see about 8 degrees more of the surface on one side. At the farthest point, the rotation is faster and we 8 degrees more on the other side. The phenomenon is called tidal locking.
In fact over the eons, earth's day has gone from about 6 hours to the current 24 as the moon has moved further and further from the earthThe rotational period of the moon wasn't always equal to its orbit around the planet. Just like the gravity of the moon affects ocean tides on the Earth, gravity from Earth affects the moon. But because the moon lacks an ocean, Earth pulls on its crust, creating a tidal bulge at the line that points toward Earth. [Infographic: Inside Earth's Moon]
Gravity from Earth pulls on the closest tidal bulge, trying to keep it aligned. This creates tidal friction that slows the moon's rotation. Over time, the rotation was slowed enough that the moon's orbit and rotation matched, and the same face became tidally locked, forever pointed toward Earth.
The moon is not the only satellite to suffer friction with its parent planet. Many other large moons in the solar system are tidally locked with their partner. Of the larger moons, only Saturn's moon Hyperion, which tumbles chaotically and interacts with other moons, is not tidally synchronized.
The situation is not limited to large planets. The dwarf planet Pluto is tidally locked to its moon Charon, which is almost as large as the former planet.
Earth (and other planets) do not escape completely unscathed. Just as the Earth exerts friction on the spin of the moon, the moon also exerts friction on the rotation of the Earth. As such, the length of day increases a few milliseconds every century.
Here's what would happen if the moon didn't rotateSedimentary rocks such as sandstone also testify to the quicker days of yore. As moon-spawned tides wash over rocks they deposit mineral specks, layer upon layer. In southern Australia, for example, these vertically accumulating tidal "rhythmites" have pegged an Earth day at 21.9 hours some 620 million years ago. This equates to a 400-day year, although other estimates suggest even brisker daily rotations then.