The occurrence of obtuse junction angles and changes in channel width below tributaries along the Mekong River, South-East Asia
Classic descriptions of drainage patterns suggest that confluence angle is determined by the shape of the drainage basin unless constraining factors, such as the geological structure, affect stream flow. Downstream changes in channel width below tributary junctions have long been associated with tri...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
2011-09-30.
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| Subjects: | |
| Online Access: | Get fulltext |