PublicID | 2024p363250 |
UTC Time | 2024-05-14T09:38:08Z |
Latitude | -30.54 (± 4.2 km) |
Longitude | -176.86 (± 15.9 km) |
Depth | 33 km (± 0 km) |
Depth Type | operator assigned |
Earth Model | iasp91 |
Used Phase Count | 21 |
Used Station Count | 17 |
Standard Error | 3.60 (s) |
Azimuthal Gap | 241.94 (degrees) |
Minimum Distance | 1.57 (degrees) |
Type | Magnitude | Station Count |
Preferred (Mw(mB)) | 4.1 (± 0.4) | |
MLv | 5.2 (± 0.2) | 2 |
ML | 4.9 (± 0.3) | 3 |
mB | 4.8 (± 0.2) | 6 |
Mw(mB) | 4.1 (± 0.4) | 3 |
M | 5.1 | 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.