Project Jukebox

Digital Branch of the University of Alaska Fairbanks Oral History Program

Changes in river channel at upper end of Wenrich Slough

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Sam Demientieff trying to figure out why there is open water in this area at the upper end of Wenrich Slough below Wenrich Island, because it is shallow and does not have the current and depth that the main channel of the Tanana River does. He discusses how the channels of the river have changed through time.
Date Process Observed: 
Monday, December 17, 2007