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10,000 Year Ice Core Revealed · Ryder Lee

• 0:06
  Speaker 1: They're trying to stop you from finding this different information.
• 0:10
  Speaker 1: And this chart was the gold standard that was there
• 0:12
  Speaker 1: to show what human history was in terms of why
• 0:16
  Speaker 1: things collapsed in the past, and because it disproved what
• 0:21
  Speaker 1: the new CO two was trying to tell you in
• 0:23
  Speaker 1: the way it works is like CO two drives climate.
• 0:25
  Speaker 1: It's warmer now than ever. But this is the very
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  Speaker 1: best set they had from you know, the beginning of
• 0:32
  Speaker 1: ice core drilling was this. They could reconstruct it by
• 0:36
  Speaker 1: seeing the CO two in it, and the CO two
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  Speaker 1: levels were actually lower when the temperature was warmer in
• 0:42
  Speaker 1: all of these spike events. So that disproved right there,
• 0:45
  Speaker 1: and they're like, oh, we can't. I mean the CO
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  Speaker 1: two is way alone, it was warmer than that way,
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  Speaker 1: we can't that excuse everybody, even a kindergartener, will see
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  Speaker 1: through it. That's my brand.
• 0:56
  Speaker 2: Yes, right, because they're blaming CO two higher CO two
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  Speaker 2: levels on global warming, But if it was lower whenever
• 1:03
  Speaker 2: it was hotter, then it doesn't make any sense. The
• 1:08
  Speaker 2: whole thing falls.
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  Speaker 1: And again, even the AI engines are built in to
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  Speaker 1: try to dissuade you from connecting on these small dots apart. Yeah,
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  Speaker 1: so anybody that's out there looking that. You can look
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  Speaker 1: this up as a GISP two. Now the ones that
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  Speaker 1: Antarctica also have their own data sets too that are
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  Speaker 1: very similar to this. But uh, there was a disruption
• 1:27
  Speaker 1: in their drill core or their core drilling, and nobody
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  Speaker 1: can really explain why they just kind of stopped doing
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  Speaker 1: it down there. I'm sure you have more information about
• 1:37
  Speaker 1: that than I do. But wherever you look, you can
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  Speaker 1: look at the Antarctic ice core drilling data as well.
• 1:43
  Speaker 1: A little bit deeper in aunt Arcca, but for some reason,
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  Speaker 1: the ice is supposed to be so much thicker down there,
• 1:50
  Speaker 1: but they never really got to the bottom like they
• 1:52
  Speaker 1: should have. And I'm just asking why, Like why didn't
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  Speaker 1: why didn't you guys reach rock layer down there? What
• 1:57
  Speaker 1: did you touch or see or experience and said made
• 2:00
  Speaker 1: you stop drilling down there? That was the whole question
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  Speaker 1: about their drilling on some of the stations, was like
• 2:07
  Speaker 1: why'd you stop? I thought the thing about science was
• 2:10
  Speaker 1: to keep going, keep going. I thought you were going
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  Speaker 1: to hit bedrocks somewhere down there and prove that the
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  Speaker 1: world was this, that or the other. And they just
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  Speaker 1: locked it up, threw away the key, never to go
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  Speaker 1: drilling another core down there. Man, I don't know what happened.
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  Speaker 2: But well, according to this reader's Digest Antarctica edition, there
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  Speaker 2: is a two hundred and sixty square kilometers one hundred
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  Speaker 2: square miles that has lakes, lush forest greenery in the
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  Speaker 2: middle of Antarctica. I think that that is a real
• 2:50
  Speaker 2: mystery of Antarctica, is that there's a one hundred square
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  Speaker 2: miles of lush greenery, lush forest and lakes in the
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  Speaker 2: center of Antarctica, and they don't know why. They don't
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  Speaker 2: know how, and they've been studying it for a long time.
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  Speaker 2: I mean, on a supposedly frozen continent. Further, it to
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  Speaker 2: be one hundred square miles of lush greenery and forested
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  Speaker 2: areas and trees and lakes is an anomaly, right.
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  Speaker 1: The only two possibilities I could think that would make
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  Speaker 1: sense for that is a magnetic field line has established
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  Speaker 1: itself for an incredibly long time highly electrified that raised
• 3:40
  Speaker 1: temperatures in that area, or there is a volcanic breakthrough
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  Speaker 1: that allows heat to escape through that on multiple areas.
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  Speaker 1: Or perhaps the magnetic field line caused the volcanic breakthroughs.
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  Speaker 1: And those two are intertwined to allow a heated spot
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  Speaker 1: to exist within the ice that has some sort of
• 3:59
  Speaker 1: bare around it, because the positive pressure coming out can
• 4:02
  Speaker 1: push away that cold air. Those neutrinos coming out of
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  Speaker 1: there too, is a whole other thing that you know,
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  Speaker 1: This intense neutrino emission coming out doesn't make sense either
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  Speaker 1: unless there's some energy source down there, so you start
• 4:20
  Speaker 1: to look at it, you know. Admiral Bird, I do believe,
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  Speaker 1: also talked about that on a couple of reconnaissance flights.
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  Speaker 1: There have been several pilots that had talked about seeing
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  Speaker 1: this green area, so it didn't surprise me. It's not
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  Speaker 1: the first one.
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  Speaker 2: That paragraph that I just read from there is connected
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  Speaker 2: to the operation Hydro Admiral Bird. That was the big
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  Speaker 2: discovery that they found in Antarctica was this one hundred
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  Speaker 2: square miles of lush greenery and forest.
• 4:56
  Speaker 1: Now, if I could throw another thing out there about
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  Speaker 1: that related directly to this. When we get into a
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  Speaker 1: more wee can magnetic field, we get more cosmic rays
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  Speaker 1: come in. These cosmic rays energetic particles, They excite these
• 5:09
  Speaker 1: different types of magma chambers. It depends what the magma
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  Speaker 1: is comprised of.
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  Speaker 2: What's made of.
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  Speaker 1: So if it's made of silica, which everybody knows silica,
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  Speaker 1: you know, crystals, this sort of thing, it's called silica
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  Speaker 1: rich magma. When the cosmic rays come in, it gets
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  Speaker 1: excited for some reason that on that specific type type
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  Speaker 1: of magma has like an amplified effect above any other
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  Speaker 1: types of you know, liquid rock magma in our Earth's crust.
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  Speaker 1: Now all along, if you look at a map of Antarcticle,
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  Speaker 1: you see that large peninsula out there, well underneath those
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  Speaker 1: ice shelves, the volcanic activity is just ramped up tremendously,
• 5:48
  Speaker 1: and say the last five years more or less. It
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  Speaker 1: did start around ten twelve years ago, and it was
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  Speaker 1: getting warmer, and people are going to look at these
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  Speaker 1: punch throughs. They're starting to get like from beneath surface melting,
• 5:58
  Speaker 1: not above surface, beneath the surface. Right, it was changing
• 6:01
  Speaker 1: water currents because the warm water was circulating at a
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  Speaker 1: different speed than the cold water, and they started to
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  Speaker 1: get these gyres and different things happening. Icebergs will break
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  Speaker 1: off and they would just spin, and like that doesn't
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  Speaker 1: make sense. They should be moving with the current, not
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  Speaker 1: spinning and just stuck there and there was a huge
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  Speaker 1: amount of ice anomalies. And I'm not gonna say just
• 6:19
  Speaker 1: like more or less sea ice. I'm just talking about
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  Speaker 1: a part of an ice shelf would break off. It
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  Speaker 1: didn't behave remotely close to where they thought it would
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  Speaker 1: or how it would move after it broke off. Subsurface
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  Speaker 1: heating did that. So just remember warm water and cold
• 6:35
  Speaker 1: water move the density is different and they move at
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  Speaker 1: different speed. So there's a lot of things in that,
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  Speaker 1: like cold air and warm air, foggy air or clear air.
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  Speaker 1: You know, you get all these different density differences in
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  Speaker 1: the way that things behave and move amongst themselves. So
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  Speaker 1: think about that for a second. What is going What
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  Speaker 1: are they seeing or finding as these areas of ice
• 6:56
  Speaker 1: are melted from beneath Are they creating giant cavity and
• 6:59
  Speaker 1: pocket Because you got to think, okay, so Greenland ice
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  Speaker 1: is you know, a mile and a half thick. If
• 7:07
  Speaker 1: you had a volcano that was beneath that and melting
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  Speaker 1: away for let's say a thousand years, but it was
• 7:12
  Speaker 1: still colding off to the top to keep the roof
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  Speaker 1: of it always frozen, so that it'd be that boundary layer,
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  Speaker 1: that equilibrium point, Like how large could that cavern become
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  Speaker 1: heated from beneath the earth, and you gotta suspect that
• 7:25
  Speaker 1: the same thing would be happening in Antarctica, and that's
• 7:27
  Speaker 1: maybe the real positive pressure is coming because if that
• 7:29
  Speaker 1: was an air filled void, it would push out under
• 7:34
  Speaker 1: the path of least resistance, but it would have more
• 7:37
  Speaker 1: pressure than just the ambient atmosphere around it, you know,
• 7:41
  Speaker 1: because if it levor vortices or you know Shauberger vortex principles,
• 7:46
  Speaker 1: you can speed water up to make it spin faster
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  Speaker 1: by just putting it in a circular motion with the
• 7:53
  Speaker 1: same with air. And you think, like her or tornadoes
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  Speaker 1: spin slower, why do they spin so fast? Twelve Schallburger principles.
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  Speaker 1: So that pressure difference could be the reason you have
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  Speaker 1: the green there. But if the volcanoes were really kicking
• 8:08
  Speaker 1: because of more cosmic rays because we have a weakened
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  Speaker 1: magnetic field, then what is being melted and shown down there?
• 8:15
  Speaker 1: Because before they're finding you know, way back in the
• 8:18
  Speaker 1: day when this is another thing that was when they
• 8:20
  Speaker 1: were doing the initial ice core drilling, like they came
• 8:23
  Speaker 1: into some areas that weren't really that deep, that were
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  Speaker 1: you know, a thousand feet deep fifteen hundred feet deep,
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  Speaker 1: and they did hit bedrock, but they were finding, you know,
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  Speaker 1: tropical fossils down there, things that were growing on the
• 8:34
  Speaker 1: equator previously, right, So that stunned them anyway, like how
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  Speaker 1: in the what and the heck? Then we started to
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  Speaker 1: find all the same things in the Arctic as well
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  Speaker 1: as they started doing more research. But that's nothing because
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  Speaker 1: all the tales, all of the stories, all of the
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  Speaker 1: accounts tell us that this has happened through history that
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  Speaker 1: somehow they just found like, oh, there's our Well wait,
• 8:55
  Speaker 1: if you would have looked at the old tales going
• 8:56
  Speaker 1: back some seven thousand or eight thousand years through most cultures,
• 8:59
  Speaker 1: we've they've talked about this, the repeating cycle of when
• 9:03
  Speaker 1: it does this, So that's your first clue history.
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  Speaker 2: And one hundred square miles is nothing to scoff at.
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  Speaker 2: That's a lot. That's a big amount of land that
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  Speaker 2: has lakes. And whenever they flew into this part, they
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  Speaker 2: actually landed on the lake. So the lake was big
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  Speaker 2: enough for a plane to land on the lake. That's
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  Speaker 2: a pretty big lake.
• 9:32
  Speaker 1: Yeah, it would be. And it just backs up validation
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  Speaker 1: that other processes are at work, whether the greenery is there,
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  Speaker 1: whether there's cave melting from beneath. Just the thing about
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  Speaker 1: the whole volcanic ranges in ridges inside, all around the
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  Speaker 1: planet anywhere, their silica ridge magma are just going off
• 9:50
  Speaker 1: the hook. Like these slow eruptions like I was seen
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  Speaker 1: and kill Away which is starting to fountain off at
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  Speaker 1: Now that's another one, like we're really starting to see
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  Speaker 1: a lot of effects now of these what we're previously
• 9:59
  Speaker 1: when say dormant but slow oozing or barely or they
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  Speaker 1: would take decades off at a time or they're barely
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  Speaker 1: is smidging, you know, coming out, and now they're just roaring.
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  Speaker 1: Three thousand foot tall fountains of Lavaka