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<v Speaker 1>They're trying to stop you from finding this different information.

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<v Speaker 1>And this chart was the gold standard that was there

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<v Speaker 1>to show what human history was in terms of why

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<v Speaker 1>things collapsed in the past, and because it disproved what

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<v Speaker 1>the new CO two was trying to tell you in

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<v Speaker 1>the way it works is like CO two drives climate.

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<v Speaker 1>It's warmer now than ever. But this is the very

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<v Speaker 1>best set they had from you know, the beginning of

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<v Speaker 1>ice core drilling was this. They could reconstruct it by

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<v Speaker 1>seeing the CO two in it, and the CO two

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<v Speaker 1>levels were actually lower when the temperature was warmer in

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<v Speaker 1>all of these spike events. So that disproved right there,

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<v Speaker 1>and they're like, oh, we can't. I mean the CO

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<v Speaker 1>two is way alone, it was warmer than that way,

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<v Speaker 1>we can't that excuse everybody, even a kindergartener, will see

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<v Speaker 1>through it. That's my brand.

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<v Speaker 2>Yes, right, because they're blaming CO two higher CO two

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<v Speaker 2>levels on global warming, But if it was lower whenever

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<v Speaker 2>it was hotter, then it doesn't make any sense. The

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<v Speaker 2>whole thing falls.

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<v Speaker 1>And again, even the AI engines are built in to

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<v Speaker 1>try to dissuade you from connecting on these small dots apart. Yeah,

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<v Speaker 1>so anybody that's out there looking that. You can look

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<v Speaker 1>this up as a GISP two. Now the ones that

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<v Speaker 1>Antarctica also have their own data sets too that are

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<v Speaker 1>very similar to this. But uh, there was a disruption

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<v Speaker 1>in their drill core or their core drilling, and nobody

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<v Speaker 1>can really explain why they just kind of stopped doing

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<v Speaker 1>it down there. I'm sure you have more information about

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<v Speaker 1>that than I do. But wherever you look, you can

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<v Speaker 1>look at the Antarctic ice core drilling data as well.

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<v Speaker 1>A little bit deeper in aunt Arcca, but for some reason,

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<v Speaker 1>the ice is supposed to be so much thicker down there,

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<v Speaker 1>but they never really got to the bottom like they

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<v Speaker 1>should have. And I'm just asking why, Like why didn't

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<v Speaker 1>why didn't you guys reach rock layer down there? What

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<v Speaker 1>did you touch or see or experience and said made

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<v Speaker 1>you stop drilling down there? That was the whole question

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<v Speaker 1>about their drilling on some of the stations, was like

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<v Speaker 1>why'd you stop? I thought the thing about science was

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<v Speaker 1>to keep going, keep going. I thought you were going

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<v Speaker 1>to hit bedrocks somewhere down there and prove that the

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<v Speaker 1>world was this, that or the other. And they just

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<v Speaker 1>locked it up, threw away the key, never to go

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<v Speaker 1>drilling another core down there. Man, I don't know what happened.

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<v Speaker 2>But well, according to this reader's Digest Antarctica edition, there

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<v Speaker 2>is a two hundred and sixty square kilometers one hundred

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<v Speaker 2>square miles that has lakes, lush forest greenery in the

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<v Speaker 2>middle of Antarctica. I think that that is a real

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<v Speaker 2>mystery of Antarctica, is that there's a one hundred square

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<v Speaker 2>miles of lush greenery, lush forest and lakes in the

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<v Speaker 2>center of Antarctica, and they don't know why. They don't

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<v Speaker 2>know how, and they've been studying it for a long time.

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<v Speaker 2>I mean, on a supposedly frozen continent. Further, it to

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<v Speaker 2>be one hundred square miles of lush greenery and forested

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<v Speaker 2>areas and trees and lakes is an anomaly, right.

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<v Speaker 1>The only two possibilities I could think that would make

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<v Speaker 1>sense for that is a magnetic field line has established

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<v Speaker 1>itself for an incredibly long time highly electrified that raised

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<v Speaker 1>temperatures in that area, or there is a volcanic breakthrough

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<v Speaker 1>that allows heat to escape through that on multiple areas.

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<v Speaker 1>Or perhaps the magnetic field line caused the volcanic breakthroughs.

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<v Speaker 1>And those two are intertwined to allow a heated spot

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<v Speaker 1>to exist within the ice that has some sort of

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<v Speaker 1>bare around it, because the positive pressure coming out can

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<v Speaker 1>push away that cold air. Those neutrinos coming out of

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<v Speaker 1>there too, is a whole other thing that you know,

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<v Speaker 1>This intense neutrino emission coming out doesn't make sense either

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<v Speaker 1>unless there's some energy source down there, so you start

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<v Speaker 1>to look at it, you know. Admiral Bird, I do believe,

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<v Speaker 1>also talked about that on a couple of reconnaissance flights.

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<v Speaker 1>There have been several pilots that had talked about seeing

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<v Speaker 1>this green area, so it didn't surprise me. It's not

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<v Speaker 1>the first one.

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<v Speaker 2>That paragraph that I just read from there is connected

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<v Speaker 2>to the operation Hydro Admiral Bird. That was the big

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<v Speaker 2>discovery that they found in Antarctica was this one hundred

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<v Speaker 2>square miles of lush greenery and forest.

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<v Speaker 1>Now, if I could throw another thing out there about

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<v Speaker 1>that related directly to this. When we get into a

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<v Speaker 1>more wee can magnetic field, we get more cosmic rays

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<v Speaker 1>come in. These cosmic rays energetic particles, They excite these

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<v Speaker 1>different types of magma chambers. It depends what the magma

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<v Speaker 1>is comprised of.

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<v Speaker 2>What's made of.

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<v Speaker 1>So if it's made of silica, which everybody knows silica,

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<v Speaker 1>you know, crystals, this sort of thing, it's called silica

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<v Speaker 1>rich magma. When the cosmic rays come in, it gets

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<v Speaker 1>excited for some reason that on that specific type type

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<v Speaker 1>of magma has like an amplified effect above any other

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<v Speaker 1>types of you know, liquid rock magma in our Earth's crust.

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<v Speaker 1>Now all along, if you look at a map of Antarcticle,

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<v Speaker 1>you see that large peninsula out there, well underneath those

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<v Speaker 1>ice shelves, the volcanic activity is just ramped up tremendously,

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<v Speaker 1>and say the last five years more or less. It

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<v Speaker 1>did start around ten twelve years ago, and it was

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<v Speaker 1>getting warmer, and people are going to look at these

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<v Speaker 1>punch throughs. They're starting to get like from beneath surface melting,

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<v Speaker 1>not above surface, beneath the surface. Right, it was changing

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<v Speaker 1>water currents because the warm water was circulating at a

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<v Speaker 1>different speed than the cold water, and they started to

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<v Speaker 1>get these gyres and different things happening. Icebergs will break

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<v Speaker 1>off and they would just spin, and like that doesn't

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<v Speaker 1>make sense. They should be moving with the current, not

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<v Speaker 1>spinning and just stuck there and there was a huge

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<v Speaker 1>amount of ice anomalies. And I'm not gonna say just

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<v Speaker 1>like more or less sea ice. I'm just talking about

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<v Speaker 1>a part of an ice shelf would break off. It

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<v Speaker 1>didn't behave remotely close to where they thought it would

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<v Speaker 1>or how it would move after it broke off. Subsurface

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<v Speaker 1>heating did that. So just remember warm water and cold

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<v Speaker 1>water move the density is different and they move at

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<v Speaker 1>different speed. So there's a lot of things in that,

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<v Speaker 1>like cold air and warm air, foggy air or clear air.

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<v Speaker 1>You know, you get all these different density differences in

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<v Speaker 1>the way that things behave and move amongst themselves. So

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<v Speaker 1>think about that for a second. What is going What

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<v Speaker 1>are they seeing or finding as these areas of ice

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<v Speaker 1>are melted from beneath Are they creating giant cavity and

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<v Speaker 1>pocket Because you got to think, okay, so Greenland ice

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<v Speaker 1>is you know, a mile and a half thick. If

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<v Speaker 1>you had a volcano that was beneath that and melting

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<v Speaker 1>away for let's say a thousand years, but it was

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<v Speaker 1>still colding off to the top to keep the roof

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<v Speaker 1>of it always frozen, so that it'd be that boundary layer,

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<v Speaker 1>that equilibrium point, Like how large could that cavern become

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<v Speaker 1>heated from beneath the earth, and you gotta suspect that

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<v Speaker 1>the same thing would be happening in Antarctica, and that's

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<v Speaker 1>maybe the real positive pressure is coming because if that

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<v Speaker 1>was an air filled void, it would push out under

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<v Speaker 1>the path of least resistance, but it would have more

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<v Speaker 1>pressure than just the ambient atmosphere around it, you know,

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<v Speaker 1>because if it levor vortices or you know Shauberger vortex principles,

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<v Speaker 1>you can speed water up to make it spin faster

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<v Speaker 1>by just putting it in a circular motion with the

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<v Speaker 1>same with air. And you think, like her or tornadoes

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<v Speaker 1>spin slower, why do they spin so fast? Twelve Schallburger principles.

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<v Speaker 1>So that pressure difference could be the reason you have

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<v Speaker 1>the green there. But if the volcanoes were really kicking

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<v Speaker 1>because of more cosmic rays because we have a weakened

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<v Speaker 1>magnetic field, then what is being melted and shown down there?

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<v Speaker 1>Because before they're finding you know, way back in the

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<v Speaker 1>day when this is another thing that was when they

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<v Speaker 1>were doing the initial ice core drilling, like they came

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<v Speaker 1>into some areas that weren't really that deep, that were

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<v Speaker 1>you know, a thousand feet deep fifteen hundred feet deep,

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<v Speaker 1>and they did hit bedrock, but they were finding, you know,

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<v Speaker 1>tropical fossils down there, things that were growing on the

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<v Speaker 1>equator previously, right, So that stunned them anyway, like how

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<v Speaker 1>in the what and the heck? Then we started to

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<v Speaker 1>find all the same things in the Arctic as well

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<v Speaker 1>as they started doing more research. But that's nothing because

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<v Speaker 1>all the tales, all of the stories, all of the

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<v Speaker 1>accounts tell us that this has happened through history that

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<v Speaker 1>somehow they just found like, oh, there's our Well wait,

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<v Speaker 1>if you would have looked at the old tales going

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<v Speaker 1>back some seven thousand or eight thousand years through most cultures,

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<v Speaker 1>we've they've talked about this, the repeating cycle of when

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<v Speaker 1>it does this, So that's your first clue history.

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<v Speaker 2>And one hundred square miles is nothing to scoff at.

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<v Speaker 2>That's a lot. That's a big amount of land that

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<v Speaker 2>has lakes. And whenever they flew into this part, they

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<v Speaker 2>actually landed on the lake. So the lake was big

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<v Speaker 2>enough for a plane to land on the lake. That's

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<v Speaker 2>a pretty big lake.

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<v Speaker 1>Yeah, it would be. And it just backs up validation

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<v Speaker 1>that other processes are at work, whether the greenery is there,

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<v Speaker 1>whether there's cave melting from beneath. Just the thing about

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<v Speaker 1>the whole volcanic ranges in ridges inside, all around the

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<v Speaker 1>planet anywhere, their silica ridge magma are just going off

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<v Speaker 1>the hook. Like these slow eruptions like I was seen

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<v Speaker 1>and kill Away which is starting to fountain off at

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<v Speaker 1>Now that's another one, like we're really starting to see

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<v Speaker 1>a lot of effects now of these what we're previously

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<v Speaker 1>when say dormant but slow oozing or barely or they

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<v Speaker 1>would take decades off at a time or they're barely

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<v Speaker 1>is smidging, you know, coming out, and now they're just roaring.

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<v Speaker 1>Three thousand foot tall fountains of Lavaka