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Hadley Rille, the Apollo 15 site, may be a collapsed lava tube but the crater didn't expose it, it obscured it, see photo. It's way bigger than the lava tubes and channels in Hawaii.
originally posted by: TinfoilTP
With how cratered the moon is, we would see at least one example of a giant lava tube busted open and exposed. Nobody has seen any.
Sinuous rilles are probably the most recognizable of small volcanic features on the Moon. Many partially resemble river valleys on the Earth. However, the lunar rilles usually flow away from small pit structures. Also, the lunar samples indicate that the Moon has always been bone dry. Thus, the sinuous rilles probably mark lava channels or collapsed lava tubes that formed during mare volcanism.
This photo shows the Hadley Rille on the southeast edge of Mare Imbrium. It is fairly well known because Apollo 15 landed there (see next image). The rille begins at the curved gash in the bottom left corner, and is clearest in the rectangular, mare-floored valley shown here. In the upper left, it gets much shallower and it slowly fades out of sight in Palus Putredinis. In all, the rille is over 75 miles (120 km) long. It is up to 5000 feet (1500 m) across and is over 950 feet (300 m) deep in places. It formed nearly 3.3 billion years ago . In contrast, lava channels on Hawaii are usually under 6 miles (10 km) long and are only 150 - 300 feet (50-100 m) wide.
originally posted by: NiZZiM
This article is pretty cool and reminds me of the Apollo mission that "rang the moon like a bell".
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.
originally posted by: AdmireTheDistance
The astronauts on the Apollo missions left seismic sensors on the moon, and when the LM of Apollo XII and the S-IVB stage of Apollo XIII impacted the moon, they caused seismic reverberations, which were measured by the sensors (and, incidentally, are exactly what you would expect to see with a solid body). The 'ringing' refers to seismic 'ringing', not any sort of sound....
originally posted by: smurfy
originally posted by: AdmireTheDistance
The astronauts on the Apollo missions left seismic sensors on the moon, and when the LM of Apollo XII and the S-IVB stage of Apollo XIII impacted the moon, they caused seismic reverberations, which were measured by the sensors (and, incidentally, are exactly what you would expect to see with a solid body). The 'ringing' refers to seismic 'ringing', not any sort of sound....
Okay, but solid body is not quite true either when it comes to the Moon. It's likely that it has a solid iron core, but it has a fluid, molten layer outside of that, and thought to have yet another pliable layer outside of that. It's just more solid and dryer that the Earth.
How that can compare exactly to what a strictly, 'Solid body' is doesn't make sense.