5 February 2013
After Passage Creek receded following last week’s flood, I went down to the bridge and the floodplain to have a look around. Here’s a little bit of what I saw…
Let’s start at the bridge itself. The view is to the west, and Passage Creek flows north:
On the other side of the bridge, looking back in the opposite direction (that is, to the east), you can get a better sense of the debris piled upstream of the bridge, and sedimentary deposits on the bridge itself:
From the same (west) side of the bridge, looking downstream at the big debris clot:
Grass lineations show flood flow direction:
A fence in the floodplain, orthogonal to stream flow, acted as a strainer:
Looking east, back toward the bridge, you can see that sections of the road have been scoured of their gravel:
Here’s a comparison of sediment size in the scoured and unscoured portions of the road, with my Keen moon boots for scale:
So where did all that gravel go?
Downstream, of course…
Big “tongues” of gravel could be observed extended under the fence and across the floodplain fields, downstream of the road.
It’s interesting to me that these deposits (which formed by bedload movement of the gravel) are only a few meters long. Really, for such an impressive flood, that’s not very far for bedload to move. But I guess it’s the floodplain, rather than the stream channel itself.
Here’s another one, just east of the bridge:
Finally, there was some pretty ice to be seen down there: