Channel pattern

Fluvial sediment transport (rivers, etc.) form several channel patterns, including:

• Straight, which are found in the most tectonically incised/active areas. This is more of a hypothetical end-member, and are not often found in nature. Straight-type channels can be found at alluvial fans.

• Braided rivers, which form in (tectonically active) areas that have a larger sedimentary load than the discharge of the river and a high gradient.

• Meandering rivers, which form a sinuous path in a usually low-gradient plain toward the end of a fluvial system.

• 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

• River
• River channel
• Sedimentary depositional environment
• Sedimentary structures
• Fluvial
• Fluvial landforms

References

• Prothero, D. R. and Schwab, F., 1996, Sedimentary Geology, pg. 137-167, ISBN 0-7167-2726-9