River meanders and vorticity theorem
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Abstract
The serpentine windings of rivers, which in certain reaches attain a remarkable symmetry and are then called meanders, must represent one aspect of the tendency for establishment of quasi-equilibrium in natural streams. With the increase in knowledge of the interaction of forces operating in rivers, this tendency toward equilibrium has assumed a greater significance.
Publication type | Article |
---|---|
Publication Subtype | Journal Article |
Title | River meanders and vorticity theorem |
Series title | Eos, Earth and Space Science News |
DOI | 10.1029/TR034i006p00955 |
Volume | 34 |
Issue | 6 |
Year Published | 1953 |
Language | English |
Publisher | AGU Publications |
Description | 5 p. |
First page | 955 |
Last page | 959 |
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