USGS · October 12, 2026
Magnitude 4.2 earthquake near Masterton, New Zealand
A magnitude 4.2 earthquake was recorded near 25 km SSE of Pahiatua, New Zealand on Oct 12, 2026, 07:52 PM (local time at the epicentre — UTC+13), at a depth of about 32.3 km, according to USGS.
USGSShallow (0–70 km)Reviewed by a seismologist
Updated 2026-10-12 17:38 UTC
The full record
- Magnitude
- M 4.2 · body-wave magnitude
- Location
- 25 km SSE of Pahiatua, New Zealand
- Local time at the epicentre
- Oct 12, 2026, 07:52 PM — UTC+13
- Time (UTC)
- 2026-10-12 06:52 UTC
- Depth
- 32.3 km · Shallow (0–70 km)
- Coordinates
- -40.677, 175.900
- Felt reports
- No “Did You Feel It?” reports submitted
- Tsunami
- No tsunami evaluation was flagged for this earthquake.
- Significance
- 271 / 1000 · routine event
- Solution quality
- 33 seismic stations used · 58° azimuthal gap (well-constrained epicentre)
- Review status
- Reviewed by a seismologist
- Catalog
- USGS
Epicentre and nearby recent earthquakes
The highlighted circle is this earthquake. Smaller circles are other events recorded nearby in the last 30 days.
What the shaking was like
Shallow earthquakes release their energy close to the surface, so they are felt more strongly nearby than a deeper earthquake of the same magnitude.
No intensity estimate was published for this event, which is usual for small earthquakes far from populated areas.
Felt it yourself? USGS collects first-hand reports through “Did You Feel It?”, and those reports are what produce the community intensity above.
Who lives nearby
About 3,990 people live in towns within 30 km of the epicentre, and 463,130 within 100 km. Distances are from the epicentre to the town centre.
| Place | Distance | Population |
|---|---|---|
| Pahiatua | 25.4 km NNW | 2,860 |
| Kopuaranga | 26.3 km SW | 1,130 |
| Castlepoint | 36.4 km SE | 1,686 |
| Masterton | 37.5 km SSW | 28,900 |
| Woodville | 37.9 km N | 1,680 |
| Solway | 39.7 km SW | 7,430 |
| Fitzherbert | 40.3 km NW | 4,370 |
| Hokowhitu | 41.6 km NNW | 11,730 |
| Awapuni | 42.8 km NW | 9,050 |
| Shannon | 43.0 km WNW | 1,610 |
Earthquake history in this area
12 earthquakes of magnitude 4.5+ have been recorded within 200 km of this epicentre since 1960, in New Zealand.
Other earthquakes near this epicentre
7 other events within 100 km in the last 30 days.
M 3.2 52 km W of Dannevirke, New Zealand
M 3.5 NORTH ISLAND OF NEW ZEALAND
M 4.2 4 km NNE of Mangatainoka, New ZealandFelt · 1
M 4.0 9 km WNW of Solway, New ZealandFelt · 4
M 3.2 22 km SE of Raumati Beach, New Zealand
M 3.1 7 km ESE of Paekakariki, New Zealand
Be first to know about the next earthquake near 25 km SSE of Pahiatua, New Zealand
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Frequently asked questions
How strong was the 25 km SSE of Pahiatua, New Zealand earthquake?
Magnitude 4.2 (body-wave magnitude), at a depth of 32.3 km. Shallow earthquakes release their energy close to the surface, so they are felt more strongly nearby than a deeper earthquake of the same magnitude.
Exactly when did it happen?
Oct 12, 2026, 07:52 PM (local time at the epicentre — UTC+13). In universal time: 2026-10-12 06:52 UTC.
Was it felt?
No “Did You Feel It?” reports were submitted for this event. Small earthquakes usually pass unnoticed except very close to the epicentre.
Was there a tsunami warning?
No tsunami evaluation was flagged for this earthquake.
Which towns are closest to the epicentre?
The closest is Pahiatua, 25.4 km NNW (population 2,860).
Are earthquakes normal in this area?
Yes. The largest earthquake recorded within 200 km since 1960 was magnitude 6.5 (29 km SE of Blenheim, New Zealand, 2013), and 7 further events were recorded within 100 km in the last 30 days.
How do I get alerts for the next earthquake here?
Install the free SeismoWatch Android app, draw a box over this area, set a minimum magnitude, and turn alerts on.
About this page
Event data: U.S. Geological Survey (USGS), the European-Mediterranean Seismological Centre (EMSC), in Venezuela FUNVISIS and in Brazil the RSBR through the Centro de Sismologia da USP. Populated places and time zones: GeoNames (CC BY 4.0). Preliminary solutions are revised as more observations arrive.