Hi, YouTubers.
I'm glad you're all here.
Thank you Very much for joining me. Once Again.
Today Is August 23.
There has been 14 earthquakes that USGS
has reported within the last 24 hours.
They're at the Yellowstone National Park
or the Yellowstone Super Volcano.
It's now up to 15.
The majority of the earthquakes have been by
Hedgeon Lake and the Madison River area.
You can see that here.
The depth of the earthquakes have been varying from 67
miles below sea level to 19 miles below sea level.
This is kind of like the outside rim of the
caldera, where this would be along within the caldera.
And that's probably why they're shallower.
So we got one here.
Down there at the Madison River Plateau.
Let's see what else we got.
Trying to look for the shallower ones.
Again.
26 miles.
Mammoth or Madison River?
They call it the mammoth area. Another One.
Yeah, shallow 2.4 Miles.
Now, that one's shallow.
13 miles.
That's Unusual.
They're seeing it's a -04.
There is a lot of earthquakes.
That they are not reporting.
So during the last major eruption, the unzipping occurred
starting up here by the Madison River area.
And we had multiple smaller eruptions until it got down
here by Heart Lake and then the two resurgent domes.
Yellowstone has two resurgent domes
where the ground is rising.
Most volcanoes only have one, and at that
time, both resurgent domes collapsed at the same
time, creating the last super eruption.
As I already stated, there's been 40
smaller eruptions since the last major eruption.
I downloaded data from three different monitors.
Here we got so Debute, and that's only
because it's been showing signs of screaming.
A little west.
I couldn't get that data to download.
Here we have the borehole that's
up by the Madison River area.
This is the borehole for the Madison River area.
And we got Maple Creek.
And you can see all the ones marked In Red.
There's more than 15 here on the stream view.
This is what it's currently showing.
The bottom is Soda Butte. The middle one.
Here Maple Creek.
And at the top we have Madison River.
And you notice we got one quick right Here.
Well, there's Other ones.
We Got some smaller ones, two smaller
ones within two and A half Hours.
Let's See 1234 within two and a
half Hours, most recently for the Screaming.
Now, what do I mean by the Screaming
of a volcano and of Course would Depend
on how long it was making this noise.
You can do a Google search on Wiredcom.
They have an article about this.
It says that the earth began to screen.
Now they Realize back in 2009 from Redoubt Volcano
there in Alaska that it was making noises, a
different type of Noise before it Erupted.
Volcanic Eruptions are usually preceded
by increase in Earthquake activity.
Published in Nature geoscience Science describes how
special Harmonic Micro quakes may result from
small, highly energized faults, scraping like a
finger nails like fingernails on a chalkboard.
Some describe it as a tea kettle whistle.
A similarly order pattern of tremors neatly spaced
like the teeth of a comb have been
seen before in the drum beat earthquakes accompanied
by the minor eruption of Mount St.
Helens between 2004 and 2006.
Here's an example of the comb of
a teeth, what they call drum beats.
Right through here and right through here.
Let me pull it over through there.
According to Durham who was doing some
research about these, what they thought at
that time was unusual signatures.
He said that fault pressure builds up more
than 100 times higher than the atmospheric pressure
in a blink of an eye.
The repeating pops are probably caused by friction.
As a viscous magma slips past the rock around
it the molten figure nails on the rocky chalkboard.
Eventually in the moments just before the
volcano explodes the friction gives away to
gliding an instant column before the storm.
Well it gets so loud that
the machinery can't pick it up.
The Smithsonian magazine had an
article about volcanoes screaming.
It turns out there are some volcanoes
that actually do scream, emitting a tea
kettle like screech prior to an eruption.
The thick magma sticks to the rock surface inside the
conduit until the pressure is enough to move it higher
where it sticks until the pressure moves it again.
Essentially each time the magma moves
it creates a small earthquake.
By the time the volcano is ready to explode the
quakes are happening so quickly they become one sound.
So at about 10:37 A.m.
Today here we have So did and this is what happened.
Let me show you the seismic signature.
It's see that at we got another one right there.
This is the most recent from when I pulled the files.
You can see it down here.
You notice too right here.
These are all rounded tops.
This is what's called either
harmonic or volcanic tremors.
This was put out by USGS.
We got tectonic.
See they got the sharpened points.
Shallow volcanic earthquakes long with rounded tops, a
surface event and then we got harmonic tremors.
They're smaller than the volcanic tremors but they
both indicate that magma is on the move
and it's recharging for another eruption.
Yellowstone has been recharging for
about 6000 years, slowly growing.
All right so I'm just going to jump around here.
Yeah I got my grandkids, two of my grandkids.
Yeah look at that.
And we'll just look at some of these
smaller earthquakes because that's probably where they're at.
Yeah.
See how it went silent there? Yes.
Another one and another one and another one.
See how we had the earthquake and then it
went quiet just like that other article showed in
another one and they're all in red.
Yeah look at that.
Let's look at some of the smaller ones.
We'll pull it over and see what we got here.
Again.
This is So debute.
I started watching Yellowstone probably
about ten years ago.
See there's another one after El Ural
went off and let's pull this up.
It had never shown activity like
this until maybe a month ago.
I want to say maybe a little bit longer.
1512 Universal Times, the last
earthquake they are reporting 1551.
This one they're not reporting comes in it's
a magnitude to 2.73 and it was deep.
You can see here in the hot gases that it brought
up there was another one right there marked in red.
1454.
Did I say this was 1551? Okay.
And this one here at 14 point
that comes in as a magnitude 2.81.
All right, let's see this one here.
Well that one they are reporting, they're saying it's
a magnitude 0.3 by Hedgeon Lake right there.
And I really shortened up the seismic signature.
Yes, magnitude 1.72.
All right.
The next one marked in red would
be this one right here at 1431.
Again by hedge and lake.
They're saying it's a 0.1.
I don't know who's reading the monitors there at USBs.
Oh, I'm sorry, USGS.
But it's a magnitude 1.61.
Look at them all.
This is for Maple Creek.
And see there's those earthquakes that they talk about
being the comb, the teeth of a comb and
someone was asking what is blobs of magma now
a blob of magma because magma is kind of
thick and oozy just like what the name suggests.
It's a blob, a thick oozing blob, kind of
like gelatin of magma that's coming into the system.
Yeah, see that there?
Think of goo that would probably be a good
here we got the goo, the blobs of magma.
You can see they got the thickening of
the lines and we got the combs of
the teeth which are actually drum beats.
So you can do a Google search.
Magma is molten rock beneath the Earth
surface that can cool into rock.
Blobs of molten magma can rise through the crust.
If a blob of magma yeah, you think they
would come up with something better than blob.
If a blob of magma gets stuck in
the crust it cools slowly into rock.
In the past blobs of magma got stuck in
the crust and cooled slowly into the granite of
the High Sierra and then can come down here.
It says here what are mantle blobs?
The mantle blobs are properly known as long
low shear wave velocity provinces, or Ll SVP.
This means when seismic waves generated by
an earthquake travels through these deep mantle
plumes the waves slow down.
So along the Firehole River there was at one
time a dyke intrusion, a crack in the ground
that built up a dam of magma that cooled.
And I have noticed and they know that this
dike intrusion prevents the heat, the heated water, et
cetera from the Mallard Lake Resurgent dome to move
down and across back in 2018 and 2019.
That's why most of the increase in activity for Yellowstone
was on the northern side of the Firehole River.
And I noticed today, too, that on the northern
side of the Firehole River, the steam coming from
a lot of the geysers was dirty.
I took some screen captures.
You can see here some of the different geysers.
And see the gray looking steam.
Here's another screen capture I took this morning.
Now, this is caused by the heated water
melting the rock, and the rock that's melted
is carried up by the steam.
This is what it's currently showing.
I wish they would zoom in, but it's iron
sulfide, and that melts at 2181 degrees Fahrenheit.
It produces hydrogen sulfide gas.
It's known as sewer gas, swamp
gas, stink damp or sour damp.
It's colorless gas, known for
his pungent, rotten egg smell.
But we can only see it because of the rock
particles that don't melt that rise up with the steam.
They're currently looking at beehive.
So that's all I have for you right now.
Any thoughts or comments or questions,
please put it down below.
Please stay safe.
Keep prepping.
Don't ever stop prepping.
There's always something extra to
add to the prepper supplies.
Thank you for taking your time to watch.
Thank you for subscribing.
Please stay safe and I'll talk to you later.
God bless you. Bye.