It's been 47 years since we made our 1st footprints on the moon — here's what you might not know about Earth's dusty companion
NASA
It's one of the most defining moments in American history: On July 21, 1969, Neil Armstrong became the first person ever to walk on the moon, taking what he called "one small step for a man and one giant leap for mankind."
Forty-seven years later, we're still learning new things about Earth's dusty companion. And some of the things that we do know about it are pretty mindblowing.
Here are a few facts about the moon that you might not know.
An astronaut's footprint can last a million years on the surface of the moon.
NASAIt may have been decades since we last set foot on the moon, but its surface is still marked with the historic footprints of the 12 astronauts who stomped across it. That's because the moon has no atmosphere. It exists in the vacuum of space where there are no gentle breezes to sweep up the dust and erase the footprints.
There are such a thing as moonquakes.
NASADuring the Apollo missions, astronauts place seismometers at their landing sights around the moon. They found that the moon actually experiences moonquakes, similar to earthquakes on Earth.
There are at least four different types of these moonquakes:
- Deep quakes hundreds of miles below the surface, likely caused by tides.
- Shallow quakes about a couple dozen miles below the surface.
- Vibrations that occur when meteorites hit.
- Quakes caused when the sun heats up the moon's icy crust.
Some of these moonquakes can register up to 5.5 on the Richter scales, which on Earth would be powerful enough to crack plaster. Unlike earthquakes, which only last up to a few minutes, moonquakes can go on and on for as long as ten minutes.
The moon is not shaped like a perfect sphere. In fact, it's more like an egg.
NASAThe moon is kind of shaped like an egg. That's because the moon's center of mass is actually a few miles closer to Earth than its actual geometric center.
In addition to being off-centered, the moon also has a sort of lumpy gravitational field due to pockets of concentrated mass located under some of its basins. One possible explanation for this is that asteroids hitting the moon billions of years ago caused regions of the moon to melt. As these regions dried, they became more dense and concentrated.
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