![FarmerDave](/data/avatars/m/0/348.jpg?1640368481)
FarmerDave
Well-known member
- Joined
- Dec 13, 2006
- Messages
- 14,185
I'm with you on this, Dwight. What was described earlier that beavers could step water over a ridge is simply impossible unless it's the YellaWood beavers and they figured out how to build an Archimedes screw. Water flows downhill. I wasn't going to say anything but let's get real. Beaver dams are a mixed bag when it comes to trout, but mostly beneficial for brook trout. Most definitely beneficial to the overall environment.I don't doubt that they could back water up and across low divides. And some places do have very low divides.
But most of our trout streams have much higher divides between them, and it's hard to believe that beaver dams could raise the water high enough to go over those divides. The beaver dams I've seen are roughly 3 feet high or so. Maybe 4 ft.? I don't recall ever seeing one 6 feet high.
I have no doubt that there are places where headwaters can intermingle. I know of two of them in Ohio where this happens from time to time during flooding, and both involve very flat swampy land. Some of it flows North, and some flows south. If there are any in PA, I'd look in the flatter swampier and formerly glaciated areas south of Erie. Beaver dams would be enough to divert some water over those divides, but they simply can't move water over a ridge.
So, how did brook trout spread to their current or previous ranges? Simple. When glaciers melt, it produces a lot of water all along it. Those glaciers covered most of the northern hemisphere with up to 2 miles thick of ice. The weight of that ice compressed the land, so as the glaciers melted, plenty of water was left behind in the depression. The ground rebounded slowly. In fact, land that was formerly glaciated is still expanding and contracting to this day even though the last great glaciers receded about 16K years ago. Look up "glacial isostatic adjustment."