| PublicID | 2025p924021 |
| UTC Time | 2025-12-08T21:16:26Z |
| Latitude | -23.78 (± 24.6 km) |
| Longitude | -179.65 (± 28.3 km) |
| Depth | 600 km (± 0 km) |
| Depth Type | operator assigned |
| Earth Model | iasp91 |
| Used Phase Count | 8 |
| Used Station Count | 6 |
| Standard Error | 0.96 (s) |
| Azimuthal Gap | 233.33 (degrees) |
| Minimum Distance | 10.19 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (mB) | 3.8 (± 0.1) | |
| mB | 3.8 (± 0.1) | 3 |
| Mw(mB) | 2.8 (± 0.4) | 3 |
| M | 2.8 | 3 |
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.