Upper Dells

I believe some people call this Teakettle, while others call it Upper Dells. A couple early smooth waves lead to a ledge/hole within the dells. (This can be sticky at some flows, but is often played. At good flows it has strong eddies drawing you back upstream river-left.) Coming out of this dells, river-left spills across a spline of rock mostly parallel to the flow, while the main (center/right) current slides off into a large rock forming a wave/hole to river-right.