Dan Boone wrote:After a couple of years of no beaver activity in my ravines, this year there are again a couple of low trashy dams.  Nothing fancy, just the kind of nudged-up green sticks and muddy schmutz that a young beaver makes so that he can swim around instead of clambering over the rocks in a stream that's too shallow.  Having had my hopes dashed now several times in the past, I am not investing too much anticipation in this round of activity.  But each time this has happened in the past, the result has been a fairly considerable increase in sediment in the ravine in the area of beaver activity, with a widening of the notch, a shallowing of the angle of the banks, and an increase of bank vegetation after the beavers have moved on.  So it's all good.
		
 
 I was fascinated to come across the following diagram 
here that describes in visual terms the phenomenon I have been observing over a period of years in my own notch-cut ravines.  I would say I am at the early stages of (b) in this diagram, but the effect is unmistakable and the diagram gives me hope for the future!