1793  (1933)  [The river] has changed its course back to what it was at the entrance of the Chenaux 5 Leagues below the Grand Calumet.
1896  We continued through the winding chanals (anglicized as "schnys"). . . .
1928  . . . the great western river had already received a considerable portion of the discharge of the Athabasca through the Chenal des Quatre Fourches.