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Line 21: [[Braided river]]s, which form in (tectonically active) areas that have a larger sedimentary load than the discharge of the river and a high gradient. [[Meandering river]]s, which form a [[sinuous]] path in a usually low-gradient plain toward the end of a fluvial system. [[Anastomosis#Geography and hydrology\|Anastomosed river]] is a rare case of a relatively straight, complicated vertical sequence of river deposits with banks held together by dense [[vegetation]]. == See also == {{annotated link\|Channel types}} {{annotated link\|Depositional environment}} {{annotated link\|~~Sedimentary~~Drainage ~~structures~~system (geomorphology)}} {{annotated link\|Fluvial landforms}} {{annotated link\|Fluvial processes}} {{annotated link\|~~List~~Sedimentary ~~of landforms#Fluvial landforms\|Fluvial landforms~~structures}} == References == {{~~Reflist~~reflist}} == Further reading== Prothero, D. R. and Schwab, F., 1996, Sedimentary Geology, pg. 137-167, {{ISBN\|0-7167-2726-9}} {{River morphology}} {{Rivers, streams and springs}} [[Category:Geomorphology]]