Figure 6. Coulomb stress (left) and dilatation (right) caused by the same simplified source, the 1989 magnitude 6.9 Loma Prieta earthquake. These comparisons can help assess which is better correlated with subsequent seismicity or fault creep. Credit: Temblor, CC BY-NC-ND 4.0

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Figure 6. Coulomb stress (left) and dilatation (right) caused by the same simplified source, the 1989 magnitude 6.9 Loma Prieta earthquake. These comparisons can help assess which is better correlated with subsequent seismicity or fault creep. Credit: Temblor, CC BY-NC-ND 4.0

Figure 6. Coulomb stress (left) and dilatation (right) caused by the same simplified source, the 1989 magnitude 6.9 Loma Prieta earthquake. These comparisons can help assess which is better correlated with subsequent seismicity or fault creep. Credit: Temblor, CC BY-NC-ND 4.0

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