Channel pattern: Difference between revisions

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*[[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 ==