The Physical Environment

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braided streams

Braided channel
Click to enlarge image

Braided river at junction of Gakona and Copper River, Alaska

(Photo credit: USGS Digital Data Series
DDS-21 Used with permission)

Braided channel, Nelchina River
Click to enlarge image

Nelchina River, Copper River region, Alaska

(Photo credit: USGS Digital Data Series
DDS-21. Used with permission)

Braided streams are created when the discharge of water cannot transport its load. When there is a decrease in stream velocity sediment is deposited on the floor of the channel creating bars. The bars separate the channel into several smaller channels creating a braided appearance. Braided channels are common in glaciated or recently glaciated landscapes where streams are  fed by debris-choked melt water..

 

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© 2003 - 2015 Michael Ritter (tpeauthor@mac.com)
Last Revised September 26, 2006