Charles (Chuck) Bryant

So the other interesting thing about this one is volcanoes can produce platinum.

Yeah.

Or at least, you know, part of like groups of platinum metals.

And that could account for that spike we talked about in South Africa.

Josh said you were dismissed.

All right.

So that was the YDs.

I guess we could talk a little bit about what happened afterward.

Afterward is where we are, the Holocene period.

And that was when the climate finally worked itself out.

That pendulum stopped swinging and things started warming up and stabilizing.

And, you know, people started thriving again.

The animals came out.

The birds started chirping.

The bees started pollinating.

And it led to, you know, not the modern, modern era, but just, you know, what we know now is planet Earth.

Yeah.

I mean, the current the current shape of our planet happened after the Younger Dryas, like the way the coastlines were shaped.

I mentioned the Rockies and the Alps, you know, those those mountain ranges all over the world.

Even they I was about to say took their final shape that, of course, that's not true, but took the shape that we know and love today.