2004
2004
2007
This is the Topographical Change Detection for the Feshie RiverÂ
Using GCD I was able to identify the four geomorphic units. The scale is from green to red, green being higher elevations and red being lower elevations. There are clear patterns in the the geomorphic change. By 2007 there was more aggradation and more bars present with less intense erosion and incision.
Bank Erosion (Gray)
Channel Bed Lowering (Black)
Channel Bed Rising (Blue)
Bar Development (Purple)