 Okay, so we can also look at the opposite, which is the flow speed increasing through time. And so let's say, if we start, we'll just do the opposite. So let's say we start at 10 centimeters per second and increase our flow speed through time. So again, at 10 centimeters per second, everything smaller than and including very core sand gets deposited. As we move up to 20 centimeters per second here in the spot right here, we can now transport pebbles. So we'll say small pebbles. So then we have the question about what actually gets deposited here. When you're increasing the flow speed through time, you're actually able to start transporting and eroding more and more sand. So when the flow speed is actually increasing, you don't have deposition, you actually have erosion. Because you can move more grains through time. So by the time we actually get up to, for example, 100 centimeters per second, we can still transport cobbles. But we don't actually have anything being deposited until the flow speed goes down again. So basically we have the relationship when you increases, you have removal of grains and nothing is deposited. That's the generalization. But often what that would look like is a break in the sediment here. And so you could call it, we could call it maybe a micro-inconformity.