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A meander is one of a series of regular sinuous curves in the channel of a river or other watercourse. It is produced as a watercourse erodes the sediments of an outer, concave bank and deposits sediments on an inner, convex bank which is typically a point bar. The result of this coupled erosion and sedimentation is the formation of a sinuous course as the channel migrates back and forth across the axis of a floodplain.
In a flowing stream, a riffle-pool sequence develops as a stream's hydrological flow structure alternates from areas of relatively shallow to deeper water. This sequence is present only in streams carrying gravel or coarser sediments. Riffles are formed in shallow areas by coarser materials, such as gravel deposits, over which water flows. Pools are deeper, calmer areas whose bed load is made up of finer material such as silt. Streams with only sand or silt laden beds do not develop the feature. The sequence within a stream bed commonly occurs at intervals of from 5 to 7 stream widths. Meandering streams with relatively coarse bed load tend to develop a riffle-pool sequence with pools in the outsides of the bends and riffles in the crossovers between one meander to the next on the opposite margin of the stream. The pools are areas of active erosion and the material eroded tends to be deposited in the riffle areas between them.
A riffle is a shallow landform in a flowing channel. Colloquially, it is a shallow place in a river where water flows quickly past rocks. However, in geology a riffle has specific characteristics.
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References
- 1 2 "Professor Nick Clifford". Loughborough University . Archived from the original on 22 July 2019. Retrieved 22 July 2019.
- ↑ "The formation, nature and maintenance of riffle-pool sequences in gravel-bedded rivers", EThOS (British Library). Retrieved 22 July 2019.
- ↑ "Dean of Social, Political and Geographical Sciences appointed". Loughborough University . 10 March 2016. Retrieved 9 July 2024.
- ↑ Clifford, N. J., & Malanson, G. P. (2019). Retrospect and prospect reconsidered: The progress of Progress in Physical Geography. Progress in Physical Geography: Earth and Environment, 43(3), 315-318.
- ↑ Editorial Board (2009) Note from the Editorial Board, Progress in Physical Geography 33(1) pp. 3–4
- ↑ https://journals.sagepub.com/editorial-board/PPG
- ↑ http://riverscience.wikidot.com/nick-clifford
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