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What is a moonquake? Earth's Moon
might appear to be dead, calm and

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still on the outside, but below
the surface, the Moon is an active,

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vibrating body. We know this because
humans have caused moonquakes ourselves with the

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Apollo missions, and the remains of
that technology are still causing tremors on the

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Moon as we speak. So today
we are going to investigate the truth behind

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the mysterious moonquake. This is the
space race. On November nineteenth, nineteen

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sixty nine, the Apollo twelve mission, commanded by Pede Conrad and albeen,

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landed on the surface of the Moon
in a region known as the Ocean of

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Storms. Part of their mission was
to deploy a payload known as the Apollo

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Lunar Surface Experiment Package, a collection
of scientific instruments that included a remote seismic

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monitoring station, the kind of device
that we would typically use to detect an

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earthquake. After complete eating their moonwalk
and returning to the command module, Apollo

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twelve released their lunar ascent stage on
a trajectory back to the Moon's surface.

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They purposefully crashed the vehicle into the
Moon. It impacted the surface forty miles

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away from the landing site with the
force of about one ton of TNT.

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The seismic monitoring station was then able
to measure the resulting shockwave from that impact.

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It took eight minutes for the moonquake
to build up and reach its peak,

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and then another hour for the tremor
to fully dissipate. A similar event

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happened on Apollo thirteen. They never
landed on the Moon due to a technical

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failure en route, but one thing
that Apollo thirteen did accomplish was generating a

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massive moonquake. As part of their
mission profile, the third stage of the

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Saturn five rocket, known as the
S four B, would be deployed on

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a crash course for the Moon.
The S four B was a hydrogen propulsion

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stage that consisted of two large fuel
tanks and a J two rocket, an

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engine much larger and heavier than the
lunar ascent vehicle, so when this thing

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hit the Moon, it generated the
force of eleven and a half tons of

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TNT, creating shockwaves thirty times greater
and lasting four times longer than the Apollo

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twelve impact. In both of these
experiments, the vibrations recorded by the remote

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seismic monitoring station lasted much longer than
scientists had expected, far longer than any

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equivalent vibrations on the Earth, and
this observation led NASA officials to comment that

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the moon quote rang like a bell. Those particular words would go on to

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birth one of the more fringe conspiracy
theories out there, known as the hollow

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Moon. The idea is that since
the moon rang like a bell, and

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bells are hollow, then the moon
must therefore also be hollow. The generally

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agreed upon explanation for the hollow moon
is that we are actually being orbited by

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an ancient alien spaceship. So,
first of all, an object does not

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need to be hollow in order to
vibrate or even to ring. Case in

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point, the glockenspiel, which uses
solid metal bars to create sustaining bell like

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tones, or even its more primitive
sister instrument, the xylophone, which creates

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ringing musical notes from blocks of wood. And second off, the moon isn't

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hollow anyway. We'll get to the
real reason that the moon rings like a

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bell in a little bit, but
first let's talk about some natural tremors on

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the Moon that are not created by
humans crashing stuff into it. The Apollo

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Lunar Surface Experiment packages that were deployed
on the Moon between nineteen sixty nine and

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nineteen seventy two continued to operate and
monitor activity for several years until they were

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remotely shut down in nineteen seventy seven, and in that time NASA was able

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to record a large amount of data
about the natural seismic activity of the Moon.

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This is fascinating information to have because
we know that earthquakes are caused by

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the movement of tectonic plates that make
up the surface of the Earth, but

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the the Moon does not have tectonic
plates. The surface is all one continuous

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shell. So what causes moonquakes well. One known variety of lunar activity is

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the emergent thermal quake. This is
the easiest one to understand because we know

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that each half of the Moon will
experience fourteen days of continuous sunlight followed by

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fourteen days of continuous darkness, and
since the Moon has no atmosphere to insulate

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the surface and maintain a consistent temperature, the surface can range from positive two

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hundred and fifty degrees fahrenheit during the
daylight periods to negative two hundred and eight

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fahrenheit during the night time periods,
and just like any other solid material that

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is exposed to these drastic temperature swings, the surface of the Moon will actually

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expand and contract as it moves from
day to night. This movement causes significant

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vibrations to travel through the surface of
the Moon. Another common seismic activity on

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the Moon is the tidal moonquake.
On Earth, we experience the physical effect

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of the Moon's gravity in the rising
and falling of the ocean tides. By

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the same measure, the gravity of
the Earth will also have an effect on

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the surface of the Moon, pulling
and stretching the surface material. This will

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also cause some residual seismic activity.
And then, of course, the Moon

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also experiences a pretty high frequency of
natural impacts. In addition to humans throwing

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chunks of spaceships at it, the
Moon gets hit by asteroids of varying sizes

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all the way from micrometeorites to metal
boulders, each one leaving behind a seismic

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footprint. We know all of this
information because of the scientific instruments left behind

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by Apollo Missions twelve and beyond.
With Apollo seventeen, the final crude lunar

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mission carrying the most advanced instruments on
a payload named the Lunar Seismic Profiling Experiment.

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At the time, this was cutting
edge research, but it was also

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the nineteen seventies, so the communication
between the instruments on the Moon and the

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receivers on Earth was relatively low bandwidth
by modern standards. However, in twenty

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twenty three, researchers at the California
Institute of Technology found a way to extract

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more detail from the Lunar Seismic Profiling
Experiment data. They used artificial intelligence and

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machine learning algorithms to fill in the
missing pieces of the seismic recordings. This

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AI upscaling gave the researchers enough detail
to begin separating naturally occurring moonquakes from external

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influences. One of the more amazing
discoveries was that the Apollo seventeen lunar lander,

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which was left behind only around one
hundred meters from the seismic measuring equipment,

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is actually causing moonquakes itself. So
what's been happening is that the lander

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has been traveling through the lunar day
and night cycle for years, and as

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the temperatures swing from one extreme to
the other, the metal structure has been

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expanding and contracting. That movement of
the metal over the ground was enough to

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cause vibrations that traveled through the surface
and reached the monitoring equipment. Now,

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this is an incredibly subtle tremor.
If you were standing on the Moon next

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to the lander, you wouldn't actively
notice the vibration. But the fact that

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these micro moonquakes were present enough to
be extracted from fifty year old recording data

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just reinforces the fact that the Moon's
surface is a very strong conductor of vibrations,

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even very tiny ones. So does
this new discovery lend any more credibility

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to the hollow moon theory? How
could the moon be so incredibly resonant without

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being a hollow bell after all?
Well, let's go back to the xylophone

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for a minute. The keys of
the instrument are made from simple wooden blocks

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that are sized to create a specific
pitch. But not every type of wood

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is suitable to make a xylophone block. Only hardwood varieties that have been thoroughly

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dried out can resonate freely enough to
be musical. A soggy, softwood is

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going to deaden the vibration before it
can ring out. If we think about

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the surface of the Earth, it's
covered in a lot of water. The

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more moisture there is present in the
surface materials, the less dense their structure

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will be. This damp material works
like a sponge to absorb and deaden the

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vibrations created by an earthquake. It
helps to keep the most severe effect localized

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to one area. If we think
about the surface of the Moon, it

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is totally dry. No moisture exists
on the Moon. The entire crust of

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the Moon is one continuous, cold, and rigid structure. So even if

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a moonquake is less intense than an
earthquake, there is nothing to deaden the

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vibrations on the Moon. They just
continue to move back and forth through the

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body of the Moon like a ringing
bell until the solid stone eventually stops them.

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Okay, so the Moon might not
be hollow, but it definitely is

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unusual, at least by Earth's standards, and this, unfortunately, is something

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that we are going to have to
be considered of as we move forward with

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the eventual settlement and colonization of the
Moon. We know that mining and long

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term construction on the Moon is an
eventual goal of Mass's Artemis program. We

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know that China and their allies also
want to establish a permanent base on the

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Moon. What we don't know is
how this massive increase in surface activity is

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going to affect the environment of the
Moon. If one relatively small lunar lander

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scraping back and forth over a few
millimeters of surface as it expands and contracts

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with the temperature, can create enough
vibration through the Moon's surface to be detectable

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with a primitive seismograph, then what
do we think that a mining operation is

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going to do. Or the frequent
landing and takeoff of a giant vehicle like

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the SpaceX starship. We are going
to have to accept the fact that a

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colonized Moon will end up going into
a constant state of seismic activity, a

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permanent moonquake, in addition to all
of the naturally occurring moonquakes. So just

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one of the many obstacles that humanity
will need to overcome on a very long

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and difficult journey to becoming a multiplanetary
civilization.
