Randall Carlson

I mean, they're literally decades behind. Yeah.

I mean, they're literally decades behind. Yeah.

Some of them are. Yeah. Yeah.

Some of them are. Yeah. Yeah.

Some of them are. Yeah. Yeah.

You know, 20 years ago you had almost total, you know, like you had a group of geologists that were acknowledging that the channel scab lands was catastrophically produced and, But what I could show you, and again, this is more time than we'd have to get into here. I can show you, for example, you have a study on Lake Wisconsin and its catastrophic outburst.

You know, 20 years ago you had almost total, you know, like you had a group of geologists that were acknowledging that the channel scab lands was catastrophically produced and, But what I could show you, and again, this is more time than we'd have to get into here. I can show you, for example, you have a study on Lake Wisconsin and its catastrophic outburst.

You know, 20 years ago you had almost total, you know, like you had a group of geologists that were acknowledging that the channel scab lands was catastrophically produced and, But what I could show you, and again, this is more time than we'd have to get into here. I can show you, for example, you have a study on Lake Wisconsin and its catastrophic outburst.

Then you can go to the plains of North and South Dakota and you'll find separate studies there. You can go over to study on Connecticut River or the Hudson River. What hasn't happened, though, is integrating all of this into a coherent model. That hasn't happened. That's what I'm trying to do. I'm trying to get, you know, we got to look at the big picture here.

Then you can go to the plains of North and South Dakota and you'll find separate studies there. You can go over to study on Connecticut River or the Hudson River. What hasn't happened, though, is integrating all of this into a coherent model. That hasn't happened. That's what I'm trying to do. I'm trying to get, you know, we got to look at the big picture here.

Then you can go to the plains of North and South Dakota and you'll find separate studies there. You can go over to study on Connecticut River or the Hudson River. What hasn't happened, though, is integrating all of this into a coherent model. That hasn't happened. That's what I'm trying to do. I'm trying to get, you know, we got to look at the big picture here.

What was happening with the cutting of Grand Coulee, and if you look at Grand Coulee, you'll see that, and then you look at Lake Seneca, one of the Finger Lakes, they're almost the same.

What was happening with the cutting of Grand Coulee, and if you look at Grand Coulee, you'll see that, and then you look at Lake Seneca, one of the Finger Lakes, they're almost the same.

What was happening with the cutting of Grand Coulee, and if you look at Grand Coulee, you'll see that, and then you look at Lake Seneca, one of the Finger Lakes, they're almost the same.

So Grand Coulee, zoom out a little, Ryan. God, I've been up and down this Coulee more times than I can count. But this was one of the main discharge of the, over here, over the Canadian Rockies, the ice sheet was called the Cordieran. And the southern terminus of the Cordilleran Ice Sheet was right at the head of Upper Grand Coulee. If you zoom in, Ryan, on Upper Grand Coulee, okay, good.

So Grand Coulee, zoom out a little, Ryan. God, I've been up and down this Coulee more times than I can count. But this was one of the main discharge of the, over here, over the Canadian Rockies, the ice sheet was called the Cordieran. And the southern terminus of the Cordilleran Ice Sheet was right at the head of Upper Grand Coulee. If you zoom in, Ryan, on Upper Grand Coulee, okay, good.

So Grand Coulee, zoom out a little, Ryan. God, I've been up and down this Coulee more times than I can count. But this was one of the main discharge of the, over here, over the Canadian Rockies, the ice sheet was called the Cordieran. And the southern terminus of the Cordilleran Ice Sheet was right at the head of Upper Grand Coulee. If you zoom in, Ryan, on Upper Grand Coulee, okay, good.

Now, all right, so you see where the Grand Coulee Dam is, took its name from Grand Coulee. There it is. And that, interestingly, Grand Coulee Dam almost marks the exact point of the southern margin of that lobe of the Cordilleran Ice Sheet right there. But you can see, pull up just a little bit, and we'll see, no, I'm sorry, go the other way. Go the other way. Stop right there.

Now, all right, so you see where the Grand Coulee Dam is, took its name from Grand Coulee. There it is. And that, interestingly, Grand Coulee Dam almost marks the exact point of the southern margin of that lobe of the Cordilleran Ice Sheet right there. But you can see, pull up just a little bit, and we'll see, no, I'm sorry, go the other way. Go the other way. Stop right there.

Now, all right, so you see where the Grand Coulee Dam is, took its name from Grand Coulee. There it is. And that, interestingly, Grand Coulee Dam almost marks the exact point of the southern margin of that lobe of the Cordilleran Ice Sheet right there. But you can see, pull up just a little bit, and we'll see, no, I'm sorry, go the other way. Go the other way. Stop right there.