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level spin. And in both cases you have rapid cumulus growth over these areas where you have this localized ground level spin and these trigger either Colorado landspouts or Alberta landspouts. And we often call these classic Colorado landspouts or classic Alberta landspouts. And it's almost identical. It's the same mechanisms that generate these landspouts. And what you want to take away from this is that they're topographically induced or at least the topographic of the area help aid the movement of air in a certain way that helps induce these landspouts. And the sweet spot in Alberta is what we call the Q-Chordor. And this is the this area of convergence right along the Queen Elizabeth to highway corridor and this is that road that runs between Calgary and Edmonton. So if you map things out you'll see right around Didsbury and Olds. You'll have a bunch of landspouts.