Debris flow frequency and magnitude were determined for 33 basins in southw
est British Columbia. Basins were first classified as either weathering-lim
ited or transport-limited using a discriminant function based on debris-con
tributing area, an area-weighted terrain stability number, and drainage den
sity. Multiple regression was used to predict magnitude, peak discharge, fr
equency and activity (frequency times magnitude) within each group of basin
s. Model performance was improved by stratifying the total sample of debris
flow basins into weathering-and transport-limited groups. Explained varian
ce increased by an average of 15 per cent in the transport-limited sample,
indicating that sediment supply conditions in the more active basins are fu
ndamental in predicting debris flow activity. An independent test of the re
gression models with 11 basins yielded generally good results for debris fl
ow magnitude and peak discharge. Prediction of debris flow frequency proved
problematical in weathering-limited basins. The methods developed here pro
vide estimates of debris flow attributes in basins for which few data on pa
st events are available. Copyright (C) 1999 John Wiley & Sons, Ltd.