Just got a update from David on the Clay bank situation.
Slesse Creek, considerbale siltation from above the old slide and from a side creek.
Ranger Run, side channel cutting and contributing silt.
Thurston camp, massive slide across the river, from over bedrock, many seams of gravel so may be less harmful.
Slesse Park Slide, the work done here holding up.
Tolmie, major slump covering about 8 groynes that are holding well. Thanks to the work of CRAC or it could have been worse.
Siscoe slide, holding well.
Willow run, river now away from the clay banks.
Prognosis,
Siltation from the mentioned glacial clay banks will effect the lower Chilliwack Vedder River for many months causing sealing of spawning beds and chocking of the river bed.
The mentioned siltation will have determental effect on steelhead migration this winter and sportfishing opportunities.
The Gap Analysis study of the clay banks that CRAC has applied for funding through the Living Rivers fund for this winter is now more urgent than ever.
Does not look good as Pistol Pete has mentioned for this season. When and if it clears it most likely silt up quickly after rain. Lets hope for a cold winter or it will not be a good season for steelheading.
We will just have to wait and see but we may be back to a situation we had a number of years ago, I hope I am just being too pessimistic, time will tell on this statement.