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Aftershocks Following the Fiordland Earthquake

Aftershocks in Fiordland up until mid-August, following the mainshock on 15 July 2009. The aftershocks, concentrated at either end of the main faulting area, are a mix of faulting mechanisms, reflecting the complexity of tectonics in the area.

Read the full article for more information about the work LINZ and GNS Science are doing to understand the July 2009 Fiordland earthquake.

Aftershocks in Fiordland up until mid-August, following the mainshock on 15 July 2009. The aftershocks, concentrated at either end of the main faulting area, are a mix of faulting mechanisms, reflecting the complexity of tectonics in the area. (Image courtesy of GNS Science).

Image courtesy of GNS Science.
 
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