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Furthermore, shallow moonquakes lasted a remarkably long time. Once they got going, all continued more than 10 minutes. "The moon was ringing like a bell," Neal says.
On Earth, vibrations from quakes usually die away in only half a minute. The reason has to do with chemical weathering, Neal explains: "Water weakens stone, expanding the structure of different minerals. When energy propagates across such a compressible structure, it acts like a foam sponge—it deadens the vibrations." Even the biggest earthquakes stop shaking in less than 2 minutes.
The moon, however, is dry, cool and mostly rigid, like a chunk of stone or iron. So moonquakes set it vibrating like a tuning fork. Even if a moonquake isn't intense, "it just keeps going and going," Neal says. And for a lunar habitat, that persistence could be more significant than a moonquake's magnitude.
The giant impact hypothesis states that the Moon was created out of the debris left over from a collision between the Earth and a Mars-sized body, sometime around 4 Ga (four billion years ago).
Originally posted by Phage
The seismic experiments carried out on the Apollo missions showed that the Moon is composed almost entirely of material comparable in density to that of Earth's mantle. The average density of the moon is less than earth because it has a very small iron core in comparison to Earth.www.astronomynotes.com...
The Moon's density is fairly uniform throughout and is only about 3.3 times the density of water. If it has an iron core, it is less than 800 kilometers in diameter. This is a sharp contrast from planets like Mercury and the Earth that have large iron-nickel cores and overall densities more than 5 times the density of water. The Moon's mantle is made of silicate materials, like the Earth's mantle, and makes up about 90% of the Moon's volume.
State-of-the-art seismological techniques applied to Apollo-era data suggest our moon has a core similar to Earth's. Uncovering details about the lunar core is critical for developing accurate models of the moon's formation. The data sheds light on the evolution of a lunar dynamo -- a natural process by which our moon may have generated and maintained its own strong magnetic field.
The team's findings suggest the moon possesses a solid, iron-rich inner core with a radius of nearly 150 miles and a fluid, primarily liquid-iron outer core with a radius of roughly 205 miles. Where it differs from Earth is a partially molten boundary layer around the core estimated to have a radius of nearly 300 miles. The research indicates the core contains a small percentage of light elements such as sulfur, echoing new seismology research on Earth that suggests the presence of light elements -- such as sulfur and oxygen -- in a layer around our own core.
Interesting. Would one of the ancient units of measurement happen to be the cubit by chance?
They discovered a possible correlation between ancient units of measurement
Originally posted by Pokoia
Hi OP,
About the long time ringing of the moon after an impact, consider the following.
What does Earth have that the Moon does not have?
Large volume of water.
Large volume of loose stones, like sand.
An well filled atmosphere.
Maybe that's enough to explain the difference in dampening, because all that stuff will dampen out a signal pretty quick.
Great point!
Reminds me last year we discovered silica volcanos on the moon.
How dense is silica? Does it supress vibration?
If the core was silica, would that explain the 60% less density of the moon?
Good place to start. Then go from there.
(sorry on a iPhone can't research efficiently)
The Earth has a plasma core. Not a Nickel Iron core. The Earth and all other larger heavenly bodies are mostly heated by several mini black holes. They are located at the boundary of the plasma and the solid shell.
Originally posted by thepupils
Reminds me last year we discovered silica volcanos on the moon.
How dense is silica? Does it supress vibration?
If the core was silica, would that explain the 60% less density of the moon?
The first piece of evidence that suggested the Moon might be hollow appeared in November, 1969, after seismometers were set up on the moon's surface by the astronauts of Apollo 12. As the astronauts took off for Earth, the ascent stage of the lunar module was discarded and it fell onto the moon's surface. It created a tremor that was picked up by the seismometers. NASA found that the Moon was "ringing like a bell" and continued to do so for around an hour.
Yeah it's kind of crazy. The size of the moon and the size of the sun being similar is a coincidence, but what's that got to do with the hollow moon theory? The other part of that math is basically that there are 12 months in a year...that's not a coincidence. no matter what the orbital period of the moon was the math will come out similarly..where's the coincidence in that? There isn't one that I can see.
Originally posted by ChaoticOrder
but I don't think this theory is totally crazy; the Moon does have some really odd features, take for instance the "coincidental" math shown in this picture[1]:
The answer may be even simpler than that if you look at the root cause.
The giant impact hypothesis states that the Moon was created out of the debris left over from a collision between the Earth and a Mars-sized body, sometime around 4 Ga (four billion years ago).
So if the Moon is essentially made of the same stuff as Earth, one might wonder why it is so much less dense compared to Earth. Well lets turn to our resident expert Phage to see what he has to say about it. According to him, the Moon is much less dense because its iron core is a lot smaller than that of Earths[6].
Hollow Moon proponents would, however, have to account for the incredible density of the Moon's crust if it were in fact hollow. As gravitational pull is determined by mass, a hollow moon would require an inordinately dense crust to achieve observed gravitational values.
What you didn't mention about the giant impact hypothesis is that the impact was believed to be off-center. As a result of this, the dense part of the Earth's core might have remained somewhat intact after the impact.
We have seasons on Earth due to our axis' inclination and our orbit around the Sun.
Thanks... the only problem with that video is, for some reason it edits out the rest of the impact, it only shows the initial contact point and then cuts to a later time.
Originally posted by ProudBird
There is a video of the computer simulation of this event.....which occurred VERY early in the Solar System's formation phase:
The varying densities of the two bodies (Earth and Moon) afterwards are well understood, based on this model.