Randall Carlson

It doesn't really have the relevance to our own story on the planet as these events do. Right. Because our ancestors were here during all of this. Um, was that the end or was there more?

It doesn't really have the relevance to our own story on the planet as these events do. Right. Because our ancestors were here during all of this. Um, was that the end or was there more?

Let's go, okay, so then here we go. This is the east fork of the Jemez River, northern New Mexico, and I've hiked miles up this creek, and my friend Brad is standing on that eight-foot boulder. The modern creek, these boulders that you see, are not the product of the modern Jemez River. They're relics of an ancient event.

Let's go, okay, so then here we go. This is the east fork of the Jemez River, northern New Mexico, and I've hiked miles up this creek, and my friend Brad is standing on that eight-foot boulder. The modern creek, these boulders that you see, are not the product of the modern Jemez River. They're relics of an ancient event.

Let's go, okay, so then here we go. This is the east fork of the Jemez River, northern New Mexico, and I've hiked miles up this creek, and my friend Brad is standing on that eight-foot boulder. The modern creek, these boulders that you see, are not the product of the modern Jemez River. They're relics of an ancient event.

And to the best I've been able to date this, it's occurring right around that same epoch, around the Younger Dryas. Let's go to the next one. Look at those, now imagine as you're looking at that, the power of the water necessary to transport those boulders. Those boulders didn't just appear there, you know, out of some, you know, people look at this and the boulders are there.

And to the best I've been able to date this, it's occurring right around that same epoch, around the Younger Dryas. Let's go to the next one. Look at those, now imagine as you're looking at that, the power of the water necessary to transport those boulders. Those boulders didn't just appear there, you know, out of some, you know, people look at this and the boulders are there.

And to the best I've been able to date this, it's occurring right around that same epoch, around the Younger Dryas. Let's go to the next one. Look at those, now imagine as you're looking at that, the power of the water necessary to transport those boulders. Those boulders didn't just appear there, you know, out of some, you know, people look at this and the boulders are there.

Their mind doesn't go, okay, how did these boulders get here? You know, were they just naturally always here? No, they weren't. They were transported and dumped there. That's my friend Brad, and there's Jesse when he was younger in the red shirt there. He's been out with me on a lot of these trips. Nice.

Their mind doesn't go, okay, how did these boulders get here? You know, were they just naturally always here? No, they weren't. They were transported and dumped there. That's my friend Brad, and there's Jesse when he was younger in the red shirt there. He's been out with me on a lot of these trips. Nice.

Their mind doesn't go, okay, how did these boulders get here? You know, were they just naturally always here? No, they weren't. They were transported and dumped there. That's my friend Brad, and there's Jesse when he was younger in the red shirt there. He's been out with me on a lot of these trips. Nice.

Yeah. Yeah, he is. All right, so now this might be where we should wrap it up for now. You see Lake Superior up on the right? Okay, what I want you to do is look at, you can actually see the flow pattern coming down, and you can see where this great flow split. right there in the middle of the picture. Now look at Lake Superior. These are flows like the

Yeah. Yeah, he is. All right, so now this might be where we should wrap it up for now. You see Lake Superior up on the right? Okay, what I want you to do is look at, you can actually see the flow pattern coming down, and you can see where this great flow split. right there in the middle of the picture. Now look at Lake Superior. These are flows like the

Yeah. Yeah, he is. All right, so now this might be where we should wrap it up for now. You see Lake Superior up on the right? Okay, what I want you to do is look at, you can actually see the flow pattern coming down, and you can see where this great flow split. right there in the middle of the picture. Now look at Lake Superior. These are flows like the

more greater magnitude than if you had the entire great lakes and look at those prominences, those would have been islands.

more greater magnitude than if you had the entire great lakes and look at those prominences, those would have been islands.

more greater magnitude than if you had the entire great lakes and look at those prominences, those would have been islands.

Yeah. Just ridiculous. Yes. It's just ridiculous. And I can remember the first time I saw this digital elevation map, it was a black and white one. And I'm going, wait a minute. No, no, this can't be. And I start researching and the more I looked, you know, the more I could see. And it was like evidence like this, that I was able to trace some of these flows back to their points of origin.

Yeah. Just ridiculous. Yes. It's just ridiculous. And I can remember the first time I saw this digital elevation map, it was a black and white one. And I'm going, wait a minute. No, no, this can't be. And I start researching and the more I looked, you know, the more I could see. And it was like evidence like this, that I was able to trace some of these flows back to their points of origin.

Yeah. Just ridiculous. Yes. It's just ridiculous. And I can remember the first time I saw this digital elevation map, it was a black and white one. And I'm going, wait a minute. No, no, this can't be. And I start researching and the more I looked, you know, the more I could see. And it was like evidence like this, that I was able to trace some of these flows back to their points of origin.