Filippo Biondi

And then just below that, there's the water table that begins.

And the water table goes down thousands of feet, right?

At least a couple of thousand feet, a thousand meters maybe we'll call it.

And within that water table underneath the solid bedrock that supports these massive structures...

You have all of this limestone that has been kind of degraded by water and the limestone is, of course, porous.

And so the water fills the pores and it creates kind of more unstable limestone structures that would change over time.

is according to, you know, the radar specialists and hydrogeologists.

I think that's what they're saying.

So I guess, how do you account for the water and the water damage that would have occurred?

And then maybe that's A. And then B might be, you know, if there are these tubes and these chambers, why aren't the chambers filled with water?

Yeah.

Yeah.

This question has not been asked to me.

I just measured.

has to be asked to specialists and hydro geologists.

Because I tell you, Matt, on my scans, we see everything.

We see the water table.

But inside the water table, there are these structures that are survived.

Okay, so probably there is the water, there is the bedrock, and there is everything.

There are the structures.