DEBRIS FLOWS AFFECTING HIGHWAYS: THE WYOMING EXPERIENCE
To mitigate the effects of the debris flows, the existing concrete box culvert was removed, the roadway grade was raised, the channel was steepened as much as possible and a single span bridge was installed. Since the installation of the bridge, all subsequent debris flows have passed under the bridge and not affected the roadway.
The other major debris flow occurred on May 18, 1997 in the Snake River Canyon 18 miles southwest of Jackson, Wyoming. This debris flow was a result of a large landslide which occurred on a steep slope 1500' above the roadway. It is estimated that 100,000 cubic yards of rocks, mud and trees flowed down the slope, covered the highway with 15'-20' of material and created a delta 250' out into the Snake River. It took two weeks for the debris flow to stabilize enough to begin removal of material from the roadway. It took another month before full time traffic was restored.
To provide protection for the road from disturbed material in the existing channel, a large triangular catchment basin was cut into the slope above the roadway. This basin was designed to hold 8000 cubic yards of material. The next spring, during a period of rapid snow melt, a debris flow completely filled the basin within a 12-hour period. Maintenance forces were able clean out the culvert which drained the basin and allowed the slide debris to flow into the river without closing the road. In subsequent years, the amount of material flowing into the basin has decreased and a large concrete box culvert has been installed to allow material to pass under the road.