Hydrologists use records of past river discharge levels over long periods to predict future flood likelihoods and return periods. They rank discharge levels and calculate recurrence intervals using a formula, which allows them to plot interval against discharge on a graph. This graph's line of best fit can then predict when the next flood of a particular magnitude might occur, known as its return period. The document asks the reader to use this process and graph to determine return periods for example discharges from the East Fork of the Carson River based on recordings from 1997 and 1955 over a 200 year period.