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Correlation between Rainfall and Mass Movements in North Coast Region of Sao Paulo State, Brazil for 2014 2018

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Figure

Figure 1. Map of the study area with geographic position of the CEMADEN rain gauge network and the evaluated mass movement events
Table 1. An example for elaboration of mass movement events database for Baixada Santista and Litoral Norte regions for a 2014 to 2018 period (source: SIDEC)
Figure 3. Graphic showing the relation between accumulated 6 h × 72 hrainfall from the local time of the mass movement events divided by the type of the slope and the talus rupture
Figure 5. Graphic showing the relation between accumulated rainfall 6 h × 72 h from the local time of the mass movement events divided by the impact level: affected houses
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