 Okay, so we're standing on the severe fault right now This side over here is Basalt you see the dark black color over here again is the eocene pig member of the clarion formation And it's the red Red rock so right now. I'm gonna show you exactly what was going on here What a normal fault means So let me figure this out Richard, how do you think I should do this this one's deposited in the lake Later the lava flows came out and they were deposited on top and across in various places and then after that The fault broke and this one has dropped down. So now that it's next to it rather than being on top of something like that Just use that This rock right here is 40 million years old. This is from the eocene clarion formation and it's a lake deposit this is what we saw earlier and This right here is a piece of the basalt which is my scene which is 10 million years ago and what this would look like in a In cross-section something like this the clarion some more rocks and then the the basalt was deposited on top of it now on the fault When the fault occurred these rocks would drop down along it like that and now they're sitting right next to the clarion formation which They really didn't have any association before Right now. We're on this basalt here on the basalt side And if you can look in the distance there you can see how this this line of this this fault moves right right along into the distance So again the red rocks on that side and the basalt on that side Richard you why does the basalt have more trees and then the red the soil probably? It will erode faster and it's probably more More minerals than nutrients in it Yeah, then just take it then just take a pan from this