| |
| | Monitoring Channel Morphology and Bluff Erosion at Two Installations of Flow-Deflecting Vanes, North Fish Creek, ... |
 | | Erosion of the streambed by these tip vortexes moves the thalweg away from the outside of the bend (cut bank) and toward the point bar, causing the channel radius to increase (flattening the bend) and channel cross sections to become more symmetrical (fig. |
 | | From 2000 to 2003, erosion was measured on the inside of the bend and deposition was measured on the toe of the eroding bluff at cross-sections 1, 3, 4, 5, and 8. |
 | | Channel morphology, bluff erosion, and streamflow on North Fish Creek could continue to be monitored to further evaluate the positive and negative effects from large floods, the longevity of the vanes, and the possible need for maintenance and replacement of the vanes. |
| pubs.usgs.gov /sir/2004/5272 (10933 words) |
|