Table 1. Summary of approximate surface lengths (kilometers), maximum potential moment magnitudes (Mw), and historical earthquakes along the different segments of the Philippine Fault in eastern Mindanao. The maximum potential magnitude of earthquakes is determined by applying the empirical scaling relationship based on fault length (Wells and Coppersmith, 1994). Adapted from Perez et al., 2015.

Posted on by

Table 1. Summary of approximate surface lengths (kilometers), maximum potential moment magnitudes (Mw), and historical earthquakes along the different segments of the Philippine Fault in eastern Mindanao. The maximum potential magnitude of earthquakes is determined by applying the empirical scaling relationship based on fault length (Wells and Coppersmith, 1994). Adapted from Perez et al., 2015.

Table 1. Summary of approximate surface lengths (kilometers), maximum potential moment magnitudes (Mw), and historical earthquakes along the different segments of the Philippine Fault in eastern Mindanao. The maximum potential magnitude of earthquakes is determined by applying the empirical scaling relationship based on fault length (Wells and Coppersmith, 1994). Adapted from Perez et al., 2015.

Latest posts by Rachel Crowell (see all)