cqaigy2
Super Member
I've seen what you are talking about, the water is full of slush in the creek or river, it slows a bit and starts to freeze up. Once it starts to freeze, the water backs up and can get up on top of the ice.
Honestly - I think your spelling is correct. I tried four time with spell check - gave up. The "ice slivers" do not sink to the bottom. They become so thick in the water that - at first - a few will stick somewhere. Then after that it's a simple progression. Once a few - then more. Finally there is a place on the creek where they are really jammed/piled up. Water will back up behind this "pile up" and overflow the banks.
The "normal" water temp in the creek when this happens is - +28F or +29F. YES - it is below freezing. The water movement of the creek is what keeps things flowing. When the water backs up and slows down - the creek itself begins to freeze. It becomes a real mess.
I misspoke when I said they sink to the bottom. They will usually "catch up" or "stick" to something on the bottom. Water movement is always slower at the water/dirt interface. This is where you find the beginning of the problem.
Pretty, and looked like a nice day to boot.