Abstract
Abstract Deposits from 46 Holocene rock avalanches, with volumes ranging from 1 000 000 m3 to 500 000 000 m3 , have been identified from aerial photographs of the Southern Alps between Arthur's Pass and Mt Cook. The rock avalanches occur mainly in the eastern Southern Alps, in Torlesse Supergroup rocks. Rock avalanches are rare in schist terrain. Rock avalanching is a significant slope process in the Southern Alps. In the last 2000 years, 19 large rock avalanches have moved about 1 000 000 000 m3 of material; equivalent to an areally averaged erosion rate of 100 t/km2 per year, although the material is seldom moved far from its source. Rock avalanche deposits may be a significant sediment source for major rivers in the Southern Alps. The average annual yield of 36 000 t from a rock avalanche in the Jollie River is more than the measured annual sediment yield of the river.
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