Note:This page contains AI-generated content for informational and entertainment purposes only. It may contain inaccuracies. Raw event data is from USGS and EMSC. All statistics, lists, and derived information are generated by this site. Full disclaimerFound an error?
Location:
Magnitude:
7.3
Time:
4 Mar 2021 13:27:34
Depth:
10.0
M 7.0+:
There are 5 swarms found nearby.
2011
PS20111118.1(25.0km)
18 Nov
5 hours
6 earthquakes
2016
PS20160901.1(44.0km)
31 Aug
1 day 4 hours
21 earthquakes
2021
PS20210304.1(45.6km)
4 Mar
3 days 9 hours
34 earthquakes
S20210304.1(43.0km)
4 Mar
6 days 0 hours
188 earthquakes
PS20210311.1(44.2km)
11 Mar
1 day 6 hours
6 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Activity Offshore Gisborne: The 2021 M7.3 Earthquake and Regional Tectonics

The M7.3 earthquake that struck 182 km northeast of Gisborne, New Zealand, on 4 March 2021 at 13:27 local time originated at a shallow depth of 10 km. This event highlights the persistent seismic hazard along New Zealand’s northeastern margin. A comparable M7.0 earthquake occurred only 30 km away on 1 September 2016, underscoring the repeated release of strain in the same offshore segment. Gisborne lies adjacent to the Hikurangi subduction zone, where the Pacific plate subducts westward beneath the Australian plate at rates of 4–6 cm per year. The shallow depth of the 2021 rupture is consistent with seismicity occurring near the plate interface or within the overriding Australian plate. The region experiences frequent moderate-to-large earthquakes because of this oblique convergence, which also drives slow-slip events and volcanic activity farther west in the Taupo Volcanic Zone. Historically, the Hikurangi margin has generated several events exceeding M7 since European settlement, including damaging shocks in 1947 and 1966 that produced localized tsunami. Paleoseismic records indicate recurrence intervals of several hundred years for great (M8+) interface earthquakes, although the 2021 and 2016 events appear to have occurred on crustal faults or the shallower part of the interface. Both recent quakes were felt widely across the North Island, prompting tsunami advisories, yet neither produced significant damage or casualties owing to their offshore locations. Ongoing GPS and seafloor geodetic monitoring show that the subduction interface is locked in some patches and freely slipping in others, creating heterogeneous stress accumulation. The proximity of the two M7-class events suggests that stress transfer or shared structural controls may influence rupture patterns in this segment. Continued seismic and geodetic surveillance remains essential for refining hazard models and improving early-warning capabilities for coastal communities.

References

USGS Earthquake Catalog (events of 4 March 2021 and 1 September 2016)
GNS Science, Hikurangi Subduction Zone Overview (2023 update)