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Fig. 2 | Geoenvironmental Disasters

Fig. 2

From: Adapting sudden landslide identification product (SLIP) and detecting real-time increased precipitation (DRIP) algorithms to map rainfall-triggered landslides in Western Cameroon highlands (Central-Africa)

Fig. 2

Unscaled partial views of the scarps leaved by landslides of Foumban (in 2018) and Bafoussam (in 2019) – Both events were sudden with transitional to rotational movements, but the one in Foumban happened in one step, while the one in Bafoussam happened in three steps (yellow dashed), justifying three main blocks/stairs. Based on the soil horizontal surface, the sliding depths (arrows) are 5 m in Foumban, and 1 to 5 m in Bafoussam. The affected area was ≈30,100 m2 in Foumban (IGMR-Penaye et al., 2018) and ≈ 15,051 m2 in Bafoussam (IGMR-Kankeu & Ntchantcho, 2019)

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