Randall Carlson

And see, at the time I was researching them, I did not know about the oriented lakes of Alaska, which, you know, again, what we've got is this kind of converging trajectory here. And I believe that's based upon the work of... Oh, heck Chris knows him. I know him.

And see, at the time I was researching them, I did not know about the oriented lakes of Alaska, which, you know, again, what we've got is this kind of converging trajectory here. And I believe that's based upon the work of... Oh, heck Chris knows him. I know him.

Yes.

Yes.

Yes.

Yeah. So I met Zamora. We talked, I thought very interesting. He, he proposes Saginaw bay as being a impact point. And then the Carolina base is the secondary fallout of the, that it smashed into the ice sheet. Right.

Yeah. So I met Zamora. We talked, I thought very interesting. He, he proposes Saginaw bay as being a impact point. And then the Carolina base is the secondary fallout of the, that it smashed into the ice sheet. Right.

Yeah. So I met Zamora. We talked, I thought very interesting. He, he proposes Saginaw bay as being a impact point. And then the Carolina base is the secondary fallout of the, that it smashed into the ice sheet. Right.

Well, see, I don't know. I, my thought, my interpretation is that the Michigan basin could be impact produced, but a way older. Um, but I'm not, you know, there's, I have, I probably behind on my research on that. I have an idea that I've proposed that I think that perhaps the impact that might date back to younger dry ice or the end of the ice ages, Lake Nipigon.

Well, see, I don't know. I, my thought, my interpretation is that the Michigan basin could be impact produced, but a way older. Um, but I'm not, you know, there's, I have, I probably behind on my research on that. I have an idea that I've proposed that I think that perhaps the impact that might date back to younger dry ice or the end of the ice ages, Lake Nipigon.

Well, see, I don't know. I, my thought, my interpretation is that the Michigan basin could be impact produced, but a way older. Um, but I'm not, you know, there's, I have, I probably behind on my research on that. I have an idea that I've proposed that I think that perhaps the impact that might date back to younger dry ice or the end of the ice ages, Lake Nipigon.

which is up along the northern shore of Lake Superior. Yeah, there we go. Now, zoom in on the southern shore of Lake Nipigon, and you're gonna see all kinds of evidence of catastrophic outburst flows. You're gonna see channels. You're gonna see recessional cataracts. All of this, these are landscapes that are created by catastrophic discharges of water.

which is up along the northern shore of Lake Superior. Yeah, there we go. Now, zoom in on the southern shore of Lake Nipigon, and you're gonna see all kinds of evidence of catastrophic outburst flows. You're gonna see channels. You're gonna see recessional cataracts. All of this, these are landscapes that are created by catastrophic discharges of water.

which is up along the northern shore of Lake Superior. Yeah, there we go. Now, zoom in on the southern shore of Lake Nipigon, and you're gonna see all kinds of evidence of catastrophic outburst flows. You're gonna see channels. You're gonna see recessional cataracts. All of this, these are landscapes that are created by catastrophic discharges of water.

Go over to the west and you'll see the Black Sturgeon River. There, there's a large, yeah, that comes down. Follow that down. Yeah, look at that channel right there. Now that probably was carrying capacity. And look, notice the underfit condition again. You're going to see that all over, over and over again. Okay.

Go over to the west and you'll see the Black Sturgeon River. There, there's a large, yeah, that comes down. Follow that down. Yeah, look at that channel right there. Now that probably was carrying capacity. And look, notice the underfit condition again. You're going to see that all over, over and over again. Okay.

Go over to the west and you'll see the Black Sturgeon River. There, there's a large, yeah, that comes down. Follow that down. Yeah, look at that channel right there. Now that probably was carrying capacity. And look, notice the underfit condition again. You're going to see that all over, over and over again. Okay.

So that was probably carrying a discharge of close to a hundred million cubic feet per second at its peak based on the size of it. Um, so yeah, there was an enormous catastrophic discharge emanating from that basin.

So that was probably carrying a discharge of close to a hundred million cubic feet per second at its peak based on the size of it. Um, so yeah, there was an enormous catastrophic discharge emanating from that basin.

So that was probably carrying a discharge of close to a hundred million cubic feet per second at its peak based on the size of it. Um, so yeah, there was an enormous catastrophic discharge emanating from that basin.