A flood-incised chute or floodplain channel that evolves into the dominant conveyor of river discharge (Constantine et al. 2010).
A type of meander cutoff.
A new channel section along a swale between point bars (Stolum 1996).
- Ahnert F (1998) Introduction into geomorphology. Routledge, LondonGoogle Scholar
- Kargel JS (1994) An alluvial depositional analog for some volcanic plains on Venus. 25th Lunar Planet Sci Conf, 667–668, HoustonGoogle Scholar
- Lagasse PF, Spitz WJ, Zevenbergen LW, Zachimann DW et al (2004) Handbook for predicting stream meander migration. NCHRP report 533. Transportation Research Board, Washington, DCGoogle Scholar