Mike Collins

That area was not covered by ice. Right. Um, and, uh, but let's take our dates back far enough. I think, you know, when we're talking about stuff like what the younger drives to different things, you have this impact that would have decimated what North America, well, we're talking basically then ground zero. It would make sense, you know, that North America would be noticeably, um,

lacking in some of these um maybe more preserved or not or or different types of megalithic type constructions now or if you found them let's say sage wall is a wall and that whole area is something possibly um it's also right smack in the middle of a what was an incredibly active region being the boulder batholith

lacking in some of these um maybe more preserved or not or or different types of megalithic type constructions now or if you found them let's say sage wall is a wall and that whole area is something possibly um it's also right smack in the middle of a what was an incredibly active region being the boulder batholith

lacking in some of these um maybe more preserved or not or or different types of megalithic type constructions now or if you found them let's say sage wall is a wall and that whole area is something possibly um it's also right smack in the middle of a what was an incredibly active region being the boulder batholith

the amount of you're talking about you know 10,000 plus years of weathering than if we're dating it back that far So it kind of makes sense that, you know, like, I mean, that region there is very, the amount of damage that could be done to stone from weather and especially things like vegetation, tree roots can destroy stone quick, very quick.

the amount of you're talking about you know 10,000 plus years of weathering than if we're dating it back that far So it kind of makes sense that, you know, like, I mean, that region there is very, the amount of damage that could be done to stone from weather and especially things like vegetation, tree roots can destroy stone quick, very quick.

the amount of you're talking about you know 10,000 plus years of weathering than if we're dating it back that far So it kind of makes sense that, you know, like, I mean, that region there is very, the amount of damage that could be done to stone from weather and especially things like vegetation, tree roots can destroy stone quick, very quick.

I don't think people realize how quickly trees can absolutely decimate stuff. I mean, you have, clearly you have, at Sage Wall, you have,

I don't think people realize how quickly trees can absolutely decimate stuff. I mean, you have, clearly you have, at Sage Wall, you have,

I don't think people realize how quickly trees can absolutely decimate stuff. I mean, you have, clearly you have, at Sage Wall, you have,

breaks in the wall that make no sense if it was constructed well if this thing is that old it makes it looks like that there there has been cracking that has happened from weathering and stuff 100 so how does a wall like that form naturally um generally there's like cracks or grooves or different things in the ground or maybe even another rock or stuff and so you know

breaks in the wall that make no sense if it was constructed well if this thing is that old it makes it looks like that there there has been cracking that has happened from weathering and stuff 100 so how does a wall like that form naturally um generally there's like cracks or grooves or different things in the ground or maybe even another rock or stuff and so you know

breaks in the wall that make no sense if it was constructed well if this thing is that old it makes it looks like that there there has been cracking that has happened from weathering and stuff 100 so how does a wall like that form naturally um generally there's like cracks or grooves or different things in the ground or maybe even another rock or stuff and so you know

those areas fill up with what, like magma lava or whatever, and then they solidify along that, whether it's a fault line or that area, that space. And then just crack due to? Maybe continued movement or pressure or movement in the region. That area is real close to the continental divide there. which is just a bit further west past Butte. So you have a lot of geological activity in that region.

those areas fill up with what, like magma lava or whatever, and then they solidify along that, whether it's a fault line or that area, that space. And then just crack due to? Maybe continued movement or pressure or movement in the region. That area is real close to the continental divide there. which is just a bit further west past Butte. So you have a lot of geological activity in that region.

those areas fill up with what, like magma lava or whatever, and then they solidify along that, whether it's a fault line or that area, that space. And then just crack due to? Maybe continued movement or pressure or movement in the region. That area is real close to the continental divide there. which is just a bit further west past Butte. So you have a lot of geological activity in that region.

But yeah, generally, the dikes don't quite look like that with the horizontal layering and blocks. That's what makes it really unique.

But yeah, generally, the dikes don't quite look like that with the horizontal layering and blocks. That's what makes it really unique.

But yeah, generally, the dikes don't quite look like that with the horizontal layering and blocks. That's what makes it really unique.

Keweenaw.