| Revegetation Efforts Build on Discovery of Original Floodplain Surfaces |
| Restoration - Clark Fork River Restoration |
| Written by Tom Parker |
During spring and early summer 2008, the Clark Fork River scoured away portions of its floodplain upstream from Duck Bridge, leaving acres of exposed gravel and cobble at an elevation that is very close to the final design elevation for floodplain restoration. This past winter, the State’s restoration design team re-evaluated the floodplain grading and planting plans to see whether we could incorporate this work accomplished by natural river processes.
Natural changes allow more wetland features Comparing the post run-off floodplain surface with the design floodplain surface, we found that many areas will now only require minimal grading and shaping to reach target floodplain elevations. For the revegetation plan, this means we will be able to leave some exposed depositional surfaces as they are, ready to recruit cottonwood seedlings and other native vegetation that begin their life cycles on gravel bars. These natural changes also allowed us to design in more wetland features to take advantage of areas that are now low relative to the river’s future stage through this reach. Old floodplain surface still intact after 100 years The discovery of the old floodplain surfaces, also near the design surface elevation, provides another opportunity to use soil that is already in place. While this verifies that the designed floodplain is at the correct elevation, it also reduces our need to import soil for floodplain revegetation. The old floodplain surface still has intact soil structure, coarse woody debris and roots within the soil profile that have been preserved by one hundred years of constant saturation when the reservoir was in place. We will watch this area closely this summer to see if any pre-dam era seeds remained viable in the soil. Volunteers learn about river processes on weed pulls
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