The earthquake which struck the Fiordland region in the evening of Wednesday 15 July was the biggest since the Buller and Hawke's Bay earthquakes of 1929 and 1931.
| PublicID | 3124785 |
| UTC Time | 2009-07-15T09:22:29Z |
| Latitude | -45.77 (± 0.0 km) |
| Longitude | 166.59 (± 0.0 km) |
| Depth | 12 km (± 0 km) |
| Depth Type | operator assigned |
| Earth Model | nz1dr |
| Used Phase Count | 19 |
| Used Station Count | 17 |
| Standard Error | 0.16 (s) |
| Azimuthal Gap | 230.00 (degrees) |
| Minimum Distance | 0.40 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (Mw) | 7.8 | |
| Mw | 7.8 | 0 |
GeoNet combines magnitudes into a summary magnitude, M, which consists of a weighted average of the individual magnitudes and attempts to be a best possible compromise between all magnitudes for a range of earthquake sizes.
Summary magnitude for GeoNet is then defined as:
M = (2 * MLv + (0.4 * number_of stations(Mw(mB)) - 1) * Mw(mB)) / (2 + (0.4 * number_of_stations(Mw(mB)) - 1))
Where MLv is local magnitude calculated on the vertical component and Mw(mB) is a Mw estimation based of mB by Bormann and Saul (2008).
Map showing stations with picks used to locate the earthquake. Stations with picks that have a zero weight in the solution are shown as small grey circles. Those with a higher weight are shown as larger circles. The quake is shown by the largest circle.