April 13, 1882 Tsunami: Glenburn, Wairarapa, New Zealand
A tsunami caused by an earthquake began at Glenburn, Wairarapa, New Zealand on April 13, 1882. The water rose as high as 1.2 meters. Its effects were recorded at 1 place.
Where the waves reached
The source (white) and every runup with a place, colored by the water height recorded there. A ring is a runup NCEI marks doubtful.
- Under 1 m
- 1 to 3 m
- 3 to 10 m
- 10 to 30 m
- 30 m and more
- Height not recorded
The tsunami
- Date
- April 13, 1882
- Source
- Glenburn, Wairarapa, New Zealand
- Cause
- Earthquake
- Maximum water height
- 1.2 m (3.9 ft)
- Runups recorded
- 1
- Waters
- Ocean
- How certain
- Questionable tsunami
- Source location
- 41.320° S, 175.840° E
The toll
The record gives no deaths, injuries or damage for this tsunami.
What the record says
NCEI’s account, from the sources it cites.
Reference #5324:
1882, April 13th.
According to a correspondent from Glenburn, Wairarapa, "two smart earthquakes were felt here on Thursday last the 13th inst. [April] about 4 pm. The first accompanied by an unusual rise in the tide, it being about low water at the time, the sea came in beyond the usual high water mark" (Wairarapa Daily 17 April 1882)
The Wairarapa Daily was searched without success for any further information until 19 Apr 1882. No other location reported feeling an earthquake nor experiencing a tsunami on this date. However, there was a strong earthquake causing some chimney damage in Taranaki seven days previous, on 6 April, at the same time (note that this event is not yet in NZ National Earthquake Information Catalogue), and there may be some confusion. Being on the west coast of the North Island, it would not have caused a tsunami at Glenburn on the East Coast. Further, the earthquake does not appear to have been large enough to initiate seiching, nor strong enough locally to trigger a submarine landslide.
According to NIWA tide forecaster, high tide would have been about 1830 on 13 Apr 1882, ie it was mid-tide, or mean sea-level, at 4 pm rather than low water as indicated in the account. However, it is possible that the water had receded prior to the observer's noticing it. From mean sea level to over high tide is about 1-1.2 m. Spring tides occurred 5-8 days later, ie this is unlikely to cause confusion re the proper level of the tides.
An 6 April, when the Taranaki earthquake occurred, the time of low tide at Glenburn does not coincide with the observation either.
This event may be a tsunami, locally induced by a submarine or coastal landslide, which in turn may have been by a mild local earthquake. However, it is very doubtful.
Every runup
Nearest the source first. Heights are above sea level at the time; a tide gauge reads half the wave’s full height.
| Where | Country | Km from source | Water height, m | Inland, m | Measured by | First wave, UTC | Deaths |
|---|---|---|---|---|---|---|---|
| Glenburn, Wairarapa | New Zealand | 0 | 1.2 | Eyewitness observation of water height |
More
Every tsunami in 1882The 1800sTsunamis of New ZealandThis day in weather historyAlerts in force
Sources
Tsunami events and runups from NOAA’s National Centers for Environmental Information, Global Historical Hazard Database, cited as NCEI/WDS, doi:10.7289/V5PN93H7. Public domain. Read 2026-09-24. NCEI tsunami event 5528.