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A method is presented for quantifying erosion in mountainous catchments. Historical aerial photographs were used to measure elevation changes on all potential areas of erosion and deposition within a catchment. Total catchment erosion volume and the ensuing sediment supply rate were then calculated. The upper basin of the Waipawa River. Ruahine Range, New Zealand, is used as a case study area to demonstrate the method. There, the average annual specific sediment yield was 7,200 (± 2.000) m3/km2/year. The accuracies of measured elevations from common aerial survey scales are of the order of ± 1 m. Thus, the method can be applied successfully only in mountainous catchments that include areas prone to high erosion rates.
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Dymond et al. (1986) studied this question.
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