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Large earthquakes in mountainous regions may trigger thousands of landslides,some active for years. We analysed the changes in landslide activity near theepicentre of the 2008 Wenchuan earthquake by generating five landslideinventories for different years through stereoscopic digital visual imageinterpretation. From May 2008 to April 2015, 660 new landslides occurredoutside the co-seismic landslide areas. In April 2015, the number of activelandslides had gone down to 66, less than 1 % of the co-seismic landslides,but still much higher than the pre-earthquake levels. We expect that thelandslide activity will continue to decay, but may be halted if extremerainfall events occur

Analysing post-earthquake landslide activity using multi-temporal landslide inventories near the epicentral area of the 2008 Wenchuan earthquake