Abstract
The form and structure of a tributary confluence bar in a regulated channel are analysed and related to channel adjustment to the imposed flow regime. The bar is characterized by a tripartite structure with two facies, and by marked lateral coarsening, characteristics which relate to the changing hydraulic conditions within the narrowing channel form.
| Original language | English |
|---|---|
| Pages (from-to) | 433-440 |
| Journal | Earth Surface Processes and Landforms |
| Volume | 12 |
| Issue number | 4 |
| DOIs | |
| Publication status | Published - 31 Jul 1987 |
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