| PublicID | 2022p449945 |
| UTC Time | 2022-06-16T11:29:23Z |
| Latitude | -29.59 (± 8.8 km) |
| Longitude | 179.99 (± 19.3 km) |
| Depth | 200 km (± 0 km) |
| Depth Type | operator assigned |
| Earth Model | iasp91 |
| Used Phase Count | 30 |
| Used Station Count | 20 |
| Standard Error | 0.95 (s) |
| Azimuthal Gap | 238.68 (degrees) |
| Minimum Distance | 1.86 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (mB) | 4.5 (± 0.1) | |
| M | 4.0 | 6 |
| MLv | 4.2 (± 0.7) | 2 |
| ML | 4.7 (± 0.1) | 5 |
| Mw(mB) | 3.7 (± 0.4) | 6 |
| mB | 4.5 (± 0.1) | 9 |
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.