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.
Characterized by an expansive, flat plain covered with a layer of finely ground particles, including gravel, sand, and silt. During gusty weather conditions, substantial quantities of fine sediment are eroded from the riverbed and redeposited in areas generally downstream or to the west. The river's shallow depth and broad width classify it as a Class I float.