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. 2011 Aug 10;41(2):206–210. doi: 10.1007/s13280-011-0178-9

Fig. 1.

Fig. 1

Schematic graph showing decline in sediment yield over time during the period of paraglacial readjustment, and the role of episodic high-magnitude events such as landslides, rainstorms or periods of enhanced erosion in temporarily increasing he sediment yield (after Church and Ryder 1972; Ballantyne 2002)