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The reason for this similarity is simple It also reveals how the first images of the far side of the moon were taken in 1959 by luna 3. We almost always see the same surface when we stare at the moon, the same patterns of craters and cavities, thanks to the way that the moon moves, rotating and revolving around earth
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So, what about the other surface of our only natural satellite? The video shows how the moon's rotation and orbit are in sync with earth's, and how this creates the phenomenon of tidal locking The distinctive pattern of bright highlands and dark lunar maria on the moon has been turned towards us for millennia, visible to every human who has ever stood on earth
But why do we only see this one side of the moon
We know that earth spins about its axis, so why don’t we get to see the full lunar surface as our moon does the same? This means that one full ‘day’ of the moon (meaning the length of time it takes for the moon to rotate around itself once) is about 4 weeks long If the moon didn’t rotate at all, we would see all of its sides The only way for us to see such a constant face of the moon is if it’s also rotating
There’s a great visualization of this. The moon orbits earth in synchronous rotation, always keeping the same face toward us Learn how humans have explored the nearside and farside of the moon with space missions and satellites. Over billions of years, the earth’s gravity has forced the moon to spin synchronously with its orbit
However, things are a bit more complicated than that
Viewed from earth, the moon appears to rock slowly backwards and forwards so that we see a slightly different face throughout the lunar month There are two main reasons for this. Have you noticed we always see the same face of the moon 🌕 it’s not a trick — it’s science
This video explains tidal locking — how earth’s gravity slowed the moon’s spin until it.
