ðə sˈɛdɪmənt ɪz kˈæɹid ɪn səspˈɛnʃən, ænd bɪkˈʌz ɪɾ ɪz kˈæɹid aʊtsˈaɪd ʌvðə mˈeɪn tʃˈænəl, ɐwˈeɪ fɹʌm fˈæstɚ flˈoʊ, ðə sˈɛdɪmənt ɪz tˈɪpɪkli fˈaɪŋɡɹˈeɪnd.
The sediment is carried in suspension, and because it is carried outside of the main channel, away from faster flow, the sediment is typically fine-grained.