This shock was centered near Cape Campbell, but was felt as far away as Hokitika and Taranaki.
| PublicID | 1549063 |
| UTC Time | 1966-04-23T06:49:39Z |
| Latitude | -41.64 (± 0.1 km) |
| Longitude | 174.54 (± 0.1 km) |
| Depth | 12 km (± 0 km) |
| Depth Type | operator assigned |
| Earth Model | nz1d |
| Used Phase Count | 11 |
| Used Station Count | 6 |
| Standard Error | 0.80 (s) |
| Azimuthal Gap | 179.00 (degrees) |
| Minimum Distance | 0.40 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (Mw) | 5.8 | |
| ML | 5.8 (± 0.1) | 8 |
| MS | 5.6 | 0 |
| Mw | 5.8 | 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.