Channel patterns are found in rivers, streams, and other bodies of water that transport water from one place to another. Systems of branching river channels dissect most of the sub-aerial landscape, each in a valley proportioned to its size. Whether formed by chance or necessity, by headward erosion or downslope convergence, whether inherited or newly formed.[1] Depending on different geological factors such as weathering, erosion, depositional environment, and sediment type, different types of channel patterns can form.

Bedrock vs. alluvial channels

There are two main types of channels, bedrock and alluvial, which are present no matter the sub-classification. Bedrock channels are composed entirely of compacted rock, with only patches of alluvium scattered throughout. Because the bedrock is constantly exposed it takes much less stream power to carve the channel. The hydraulic force of flowing water can push and pull detached joint blocks out of their initial position and roll or drag them downstream. Plucking is common in jointed rocks, where this occurs.[2]

Alluvial channels are much more common and can be large or small. All large rivers, and most small ones, have channels that are usually lined with alluvium, sediment that was carried to that channel reach by the river and that eventually will be carried farther downstream.[3] This lining of alluvium creates a protective shield over the bedrock, which means it takes a much greater stream power to carve the channel.

Braided channels

There are a few distinctly different channel types based on their geological structure and depositional environment. Braided rivers carry fairly coarse-grained sediment down a fairly steep gradient. They typically exhibit numerous channels that split off and rejoin each other to give a braided appearance. Additionally, the water discharge tends to be highly variable. Consequently, braided rivers usually exist near mountainous regions, especially those with glaciers.[4] These braided channels usually occur in tectonically active environments and have a larger sediment load due to varying water flow and discharge.

Anastomosed channels

Often confused with braided channels, anastomosing is reserved for a type of river with multiple, interconnected, coexisting channel belts on alluvial plains. Based on its geomorphology, saucer-shaped islands called flood-basins characterize anastomosing rivers.[5] These channels are classified as a composite form of which the individual channel belts may have braided, meandering or straight channels. Although similar to, and even encompass other channel types, anastomosed rivers are their own entity and have just begun to be studied by geologists, revealing that much is still unknown.

Fluvial processes form several channel patterns, including:

See also


  1. ^ "The Stages of a River". Retrieved 2017-05-16.
  2. ^ Leroy., Bloom, Arthur (1998). Geomorphology : a systematic analysis of late Cenozoic landforms. Prentice-Hall. ISBN 0135054966. OCLC 299847567.((cite book)): CS1 maint: multiple names: authors list (link)
  3. ^ Diplas, Panayiotis (1990). "Characteristics of Self‐Formed Straight Channels". Journal of Hydraulic Engineering. 116 (5): 707–728. doi:10.1061/(asce)0733-9429(1990)116:5(707).
  4. ^ Stanley, Chernicoff; L., Whitney, Donna (2007). Geology : an introduction to physical geology. Pearson Prentice Hall. ISBN 978-0131474642. OCLC 489065099.((cite book)): CS1 maint: multiple names: authors list (link)
  5. ^ Makaske, Bart (2001). "Anastomosing rivers: a review of their classification, origin and sedimentary products" (PDF). Earth-Science Reviews. 53 (3–4): 149–196. Bibcode:2001ESRv...53..149M. doi:10.1016/S0012-8252(00)00038-6. Archived from the original (PDF) on 2016-10-11. Retrieved 2017-05-16.

Further reading