Here is an example of the dazzling detail of the relocated seismicity (colored by depth) in the new catalog, which I annotated. Because most of the seismicity at depth lies to the northeast of the fault at the ground surface, the faults must be inclined 8-9° to the northeast, consistent with earlier studies (Fattaruso et al, 2014).

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Here is an example of the dazzling detail of the relocated seismicity (colored by depth) in the new catalog, which I annotated. Because most of the seismicity at depth lies to the northeast of the fault at the ground surface, the faults must be inclined 8-9° to the northeast, consistent with earlier studies (Fattaruso et al, 2014).

Here is an example of the dazzling detail of the relocated seismicity (colored by depth) in the new catalog, which I annotated. Because most of the seismicity at depth lies to the northeast of the fault at the ground surface, the faults must be inclined 8-9° to the northeast, consistent with earlier studies (Fattaruso et al, 2014).

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