FAILURE OF THE HOLOCENE-AGE LAKE KSNEA DAM
Results indicate that a combination of factors caused the destruction of the dam. The presence of steep valley walls and low-permeability tephra both acted to deter normal water flow; including groundwater flow. Numerous tectonic events also acted to destabilize the extremely sturdy dam, which was composed of angular schist and relatively stable sediments and tree logs. Results indicate that a large earthquake just west of the dam occurred 6,400 years ago during a very wet spring snowmelt, resulting in a landslide that deposited into Lake Ksnea. The resulting wave of water topped the dam, causing internal erosion, and eventual failure. Additionally, due to the massive amounts of low-permeability tephra on the bottom of Lake Ksnea, it was calculated that the tephra only discharged 1% of incoming water from the lake, even though the tephra accounted for 11% of total post-landslide lake volume. It is therefore believed that the tephra deposits caused the dam to fail because of reduced lake holding capacity, low permeability, as well as the shear volume of the tephra on the lake floor. Springtime slope saturation, natural weakening of the dam, and the continuous barrage of water resulting from the aforementioned landslide into the lake all interacted to cause the destruction of the dam 6,400 years ago.