In response to the potential shortcomin s of sin le technique strategies in the investigation oferosion and sedimentation, a of Howden Reservoir, Derbyshire. By combining these techniques, some assessment of sediment sources and the erosion status of the catchment has been achieved. Alone, each approach would have been unable to determine unequivocally sediment provenance. Furthermore, the parallel use of these measurements has highlighted limitations and/or uncertainties in both the magnetic and I3'Cs techniques. These problems reflect the particular soil characteristics and drainage conditions of this upland catchment. Despite the documented severity of peat erosion in the region, Howden Reservoir has a mixture of sediment sources and a relatively moderate rate of sedimentation. Sediment yields (total 127.7 t km-* yr-' including organic fraction 31.3 t km-2 yr-') are, however, higher than in other British upland areas. combined magnetic and radiometric ( 1 8 Cs and*"Pb) approach has been undertaken in the upland, watershed-lake system