| PublicID | 2025p430044 |
| UTC Time | 2025-06-09T02:46:13Z |
| Latitude | -30.31 (± 4.5 km) |
| Longitude | -179.02 (± 11.3 km) |
| Depth | 276 km (± 12 km) |
| Depth Type | free |
| Earth Model | iasp91 |
| Used Phase Count | 26 |
| Used Station Count | 25 |
| Standard Error | 3.36 (s) |
| Azimuthal Gap | 130.00 (degrees) |
| Minimum Distance | 1.42 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (Mw(mB)) | 4.4 (± 0.4) | |
| MLv | 5.5 (± 0.6) | 8 |
| mB | 5.1 (± 0.2) | 37 |
| Mw(mB) | 4.4 (± 0.4) | 37 |
| M | 4.6 | 37 |
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.
