It seems most of the examples thus far of structurally controlled drainage have been in arid to semi arid areas, so I wanted to post an example from a markedly wet area. The GE image shows the glacially excavated area between Sudbury, Ontario and Killarney on the northern shore of the Georgian Bay. The geological map, from here, provides some context; at the link is a nice time line of events in the region. Of particular interest is the shift from rounded "organic" forms in the Southern Province's folded metasediments to more angular fault- and joint-controlled lakes and streams in the crystalline granites and gneisses of the Grenville Province to the east. The Grenville front can be seen from the bottom middle to the right top of the image, and the town of Sudbury and associated mining operations at the top middle.

This is a fantastic area for canoeing, backpacking, blueberries, and of course most importantly, geology.