What causes pools below waterfalls to periodically fill with sediment?

Reporting in the journal Geology today, Joel Scheingross of the University of Nevada Reno, and Michael Lamb of the California Institute of Technology, provided a new theoretical framework to predict when plunge pools fill with sediment, and when they subsequently evacuate that sediment exposing the rock walls of the pool to erosion. They showed that waterfall plunge pools tend to fill with sediment during modest river floods when sediment is transported in the reach upstream of the waterfall, but the waterfall jet is too weak to move all the sediment it receives from upstream. In contrast, during large floods, a strong waterfall jet can more efficiently move sediment up and out of the pool, outpacing the delivery of sediment from upstream, and exposing bedrock to erosion.

Scheingross and Lamb showed that waterfall plunge pools are most likely to fill with sediment following landscape disturbances -- such as wildfire or landslides -- that cause large influxes of sediment to rivers, or during prolonged droughts when river floods are rare. This information is useful to scientists and land managers interested in maintaining habitat and mitigating natural hazards. They also showed that bedrock erosion in plunge pools likely occurs only during large, infrequent floods, which tend to happen every 10 years or even less frequently. Therefore, the slow march of waterfalls upstream over geologic time likely occurs by fits and starts at a cadence set by extreme flood events.