 So last year, 2020, I joined the team and we conducted a survey using drones to map the slip again and see what changed. And we came up with images that are fantastic. The reason they're so good is because they're not just pretty pictures. They are geo-referenced and digital so that we can quantify change over the years. We are standing at the Cottonbrook landslide in Stowe and we are looking at how this landslide formed and how it changed over time. You can see a little mound of tan colored sediments just here about the same level where I'm standing. And then below me is a pretty deep ravine. So the interesting thing is in 2019, when this happened, there was no ravine. Between 2019-2020, this formed the creek change location and cut down kind of like a Grand Canyon effect. All of this material and flushed it downstream towards the reservoir. It really does take a team effort to figure out how landslides happen and to try to predict them. So the overall goal of this project is to understand mechanisms of mass wasting and how they impact communities. And see if we can understand processes well enough to apply that knowledge elsewhere in Vermont and provide service to the state. This does form part of UVM's land grant mission of service to the state and we are proud to be a part of that. Landslides are becoming more frequent and people have noticed that with increased especially catastrophic rainstorms or rains that are long in duration, landslides of all types tend to form soon after that. And so we are expecting landslides to increase in frequency. They're very hard to predict, but we are expecting that. And we are part of a national effort to try to map landslides, understand them and come up with mitigation strategies.