PublicID | 2025p285783 |
UTC Time | 2025-04-16T17:44:39Z |
Latitude | -34.07 (± 5.3 km) |
Longitude | -178.84 (± 8.2 km) |
Depth | 33 km (± 0 km) |
Depth Type | operator assigned |
Earth Model | iasp91 |
Used Phase Count | 31 |
Used Station Count | 28 |
Standard Error | 1.06 (s) |
Azimuthal Gap | 140.24 (degrees) |
Minimum Distance | 4.19 (degrees) |
Type | Magnitude | Station Count |
Preferred (Mw(mB)) | 5.4 (± 0.4) | |
mB | 5.8 (± 0.2) | 48 |
Mw(mB) | 5.4 (± 0.4) | 48 |
ML | 5.5 (± 0.3) | 18 |
MLv | 5.6 (± 0.2) | 19 |
M | 5.4 | 48 |
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.