| PublicID | 1544154 |
| UTC Time | 1951-05-04T21:15:46Z |
| Latitude | -38.73 (± 0.4 km) |
| Longitude | 175.57 (± 0.4 km) |
| Depth | 166 km (± 43 km) |
| Depth Type | free |
| Earth Model | nz1d |
| Used Phase Count | 6 |
| Used Station Count | 5 |
| Standard Error | 0.80 (s) |
| Azimuthal Gap | 232.00 (degrees) |
| Minimum Distance | 1.24 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (ML) | 4.3 (± 0.3) | |
| ML | 4.3 (± 0.3) | 2 |
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.
