 Walworth County. This happens to be in 2014. You can see those profiles laying up here. Again, deeper organic matter in that range land side of things. Converted, I don't know how many years ago was it native range, or Elf Elf crested for a long period of time. Native range, super granular structure, really nice looking on the surface. Plady structure, really evident. And then after we cut to the to the looking at our slide set, we can also see that that that organic matter in that surface on this native range almost starts at about 15%. Diminishes as we go down in that profile, and at some point, you know, then you start looking at, well, what are the differences in organic matter from one side of the fence to the other? Well, if we go to that next slide and look at that difference, well, native range, compared to that converted crop line, we have 45 tons of organic matter that's different from one side of the fence to the other. If we look at that whole profile, 45 tons. So what do we mean in terms of nitrogen or mineralizable nitrogen and moisture? Well, you know, it's just huge. So we looked at that mineralizable and we probably 80 to 100 pounds of in a year. Now, guess why we don't have to put nitrogen fertilizer on a rangeland. That fuel tank is still full. And then if we look at that water hole capacity, that 45 tons, that's probably about three and a half to four acre inches of water. 150,000 gallons of water hole capacity difference from one side of the fence to the other. It's management. It's all about soil structure. It's all about what we've done to soils and we can build that back. We can do that. One of these samples is actually a no-till field that's been no-till for almost 20 years now. In turn, that the clod that you have over there been really conventionally tilled and conventionally tilled around here is using a vertical tillage tool. Structurally looks a lot different. Maybe we should have immersed these clods and just see what kind of differences we end up with here. Let's do it. All right.