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(Article of periodic en Anglais - 1987)

Document title

Channel pattern changes along the lower Oconee River, Georgia, 1805/7 to 1949

Authors(s) and Affiliation(s)

BROOK G. A. ; LUFT E. R. ;

Abstract

The channel pattern changes may have been a response to changing river discharge and sediment transport characteristics brought about in part by land use changes in the basin. Higher peak and annual discharges in the late 1800 s and early 1900 s together with higher concentrations of suspended sediment because of intense soil erosion caused the river to become more sinuous between 1805/7 and 1910. Sinuosity decreased slightly in the period 1910-49 as discharge and suspended sediment concentrations dropped

Source

Article of periodic

published at : Physical geography

Editor :

Millesime : 1987, vol. 8, no3 [pp. 191-209]

Bibliographic references : 21 réf.

Language

Anglais

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