26 Geomorphology, Sedimentology and Stratigraphy
Friday, 3 April 2009
1:00 PM - 5:00 PM
EFFECTS OF LAND-COVER HISTORY AND GEOLOGIC SETTING ON CHANNEL PROCESSES, LAKE SUPERIOR SOUTH SHORE STREAMS
Paper number: 26-4
Program: Technical Sessions
Time: 2:00 PM – 2:20 PM
Authors
Abstract
The major source of sediment in most Lake Superior south-shore streams has been and continues to be sand from landslides and mass wasting of valley sides where steep channels intersect relict glacial lake shorelines from approximately 220 to 320 meters above sea level. Overbank sedimentation and natural levee formation affect downstream channel morphology, floodplain connectivity, and riparian vegetation. Sandy historical overbank deposits are 1-3 meters thick, making entrenched channels look and hydraulically behave like incised channels. Storage of historical overbank sediment and its effects on channel processes can last for centuries and millennia. Reducing runoff and sedimentation and restoring flood-plain connectivity are challenges facing rehabilitation efforts.