In an attempt to learn a little more about our favorite part of the Fraser (and avoid running aground yet again) I was reading a report on Minto Channel from UBC Dept of Geology.
Historical Changes of Minto Channel during the Twentieth Century
Part of that was so amazing I just have to share. The following relates to: gravel and rocks moved by the river water.
"we know that the average annual transportation of material past the Agassiz-Rosedale bridge is in the order of 200,000 tonnes... that is material larger than 2mm, that is all material larger than sand..."
"the bed material transported downstream from the mouth of the Harrison river is less than 100,000 tonnes per year, on average."
That means that there is 100,000 tonnes of aggregate accumulating each year between Rosedale and the Harrison. (200,000 past Rosedale less the 100,000 that passes Harrison)
"Such material when piled 5 metres deep would occupy a square measuring 110 metres on each side."
It's not surprising that we can already wade across at Peg Leg. It sure would be helpful if that were dredged again.