The Darfield earthquake caused severe building damage in mid-Canterbury, particularly to the city of Christchurch. It revealed the existence of a hidden west-east fault under the gravels of the Canterbury Plains.
| PublicID | 3366146 |
| UTC Time | 2010-09-03T16:35:41Z |
| Latitude | -43.53 (± 0.0 km) |
| Longitude | 172.17 (± 0.0 km) |
| Depth | 11 km (± 1 km) |
| Depth Type | free |
| Earth Model | nz1dr |
| Used Phase Count | 21 |
| Used Station Count | 16 |
| Standard Error | 0.14 (s) |
| Azimuthal Gap | 82.00 (degrees) |
| Minimum Distance | 0.06 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (Mw) | 7.2 | |
| ML | 7.1 | 0 |
| Mw | 7.2 | 0 |
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.