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:
15 Jun 2019 22:55:04
Depth:
46.0
M 7.0+:
There are 11 swarms found nearby.
2003
PS20030930.1(78.0km)
29 Sep
1 day 16 hours
7 earthquakes
PS20031002.1(75.7km)
2 Oct
23 hours
6 earthquakes
2005
PS20051208.1(88.6km)
7 Dec
5 hours
5 earthquakes
2008
PS20080929.1(79.8km)
29 Sep
8 hours
5 earthquakes
PS20081005.1(93.8km)
4 Oct
1 day 11 hours
7 earthquakes
2014
PS20140623.1(82.7km)
23 Jun
1 day 0 hours
27 earthquakes
S20140624.1(96.7km)
23 Jun
1 day 11 hours
41 earthquakes
2016
PS20160204.1(76.5km)
4 Feb
8 hours
5 earthquakes
2019
PS20190616.1(38.7km)
15 Jun
3 days 8 hours
21 earthquakes
PS20190621.1(59.4km)
20 Jun
1 day 1 hours
7 earthquakes
2023
PS20230424.1(91.3km)
23 Apr
1 day 12 hours
7 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Events in the Kermadec Islands Region

The Kermadec Islands form a remote volcanic arc in the South Pacific Ocean, approximately 800–1,000 km northeast of New Zealand’s North Island. They sit directly above the Kermadec-Tonga subduction zone, where the Pacific Plate descends beneath the Australian Plate at rates exceeding 6 cm per year. This tectonic setting produces frequent large earthquakes, many at intermediate depths between 30 and 100 km.

On 15 June 2019 at 22:55 UTC, a magnitude 7.3 earthquake struck the Kermadec Islands at a focal depth of 46 km. The event occurred within the subducting slab and was felt across the northern North Island of New Zealand, though no significant damage or tsunami resulted owing to the offshore location and depth. Four years later, on 24 April 2023, another strong earthquake of magnitude 7.1 occurred roughly 80 km from the 2019 epicenter, again at intermediate depth and without reported casualties.

Both events exemplify the persistent seismic hazard of the region. Since 2000, the Kermadec segment has hosted multiple earthquakes above magnitude 7.0, reflecting ongoing plate convergence and occasional intraslab rupture. Historical records document even larger events, including great earthquakes capable of generating regional tsunamis, underscoring the long-term activity of this subduction interface.

Geologically, the Kermadec arc is composed of basaltic to andesitic volcanoes built on oceanic crust. The trench itself reaches depths greater than 8 km, and the Wadati-Benioff zone extends to more than 600 km, illustrating active subduction. Crustal deformation is accommodated by both thrust faulting near the trench and normal faulting within the downgoing slab, consistent with the mechanisms of the 2019 and 2023 events.

Ongoing monitoring by GeoNet and international agencies continues to track aftershock sequences and background seismicity. While the remote setting limits direct impact on populated areas, the potential for larger interface earthquakes remains a key focus for regional hazard assessment.

References

USGS Earthquake Catalog
GeoNet New Zealand Seismic Database