High sediment-transport rates were generated by lahars, lake "breakouts," and other sudden flows from the eroding debris-avalanche deposit. These flows were considered rare and transient, so they were amply documented to serve unforeseen research needs. Observations and measurements of these unique sediment-laden flows were made whenever possible. Examples of unique sediment-laden flows include:
Personnel collected sediment data at gaging stations along the route of sediment transport for the period of interest. Basic data were recorded as sediment concentrations and daily sediment-discharge records, and were used in detailed descriptions of some sediment-laden flows (see references in "Chronology of Data Collection and Analysis").