It is characterized by a broad flat plain with a bed of finely ground gravel and sand and silt. During windstorms, large quantities of fine material is blown from the riverbed and deposited in locations generally downstream or west. The river itself is relatively shallow and wide and considered a class I float.
It is marked by an extensive, flat plain with a layer of finely ground particles, including gravel, sand, and silt. During strong winds, significant amounts of fine sediment are transported from the riverbed to locations typically downstream or westward. The river itself is shallow and wide, classified as a Class I float.