Reviewed by USGSNew Zealand15y ago
M4.0 earthquake 26 km SSE of Lincoln, New Zealand
Tuesday, June 21, 2011, 15:52:10 UTC · 43.852°S, 172.666°E
A magnitude 4.0 earthquake struck 26 km SSE of Lincoln, New Zealand on Tuesday, June 21, 2011, 15:52:10 UTC, at a depth of 5.0 km (shallow).
- Magnitude
- 4.0
- Light · ml
- Depth
- 5 km
- Shallow
- Felt reports
- 0
- Did You Feel It?
- Est. shaking
- —
- No ShakeMap
- PAGER alert
- None
- Not issued
- Tsunami
- No flag
- USGS feed
Outlined circle: this earthquakeDashed circle: 50 km aftershock search area
In context
How big was it, and why here?
Energy released
15 tons of TNT
That is about 1/998 of the Hiroshima bomb. A magnitude 5.0 releases about 32 times more energy.
Tectonic setting
148 km
from the nearest mapped plate boundary, between the Australian and Pacific plates. Earthquakes this far from a boundary happen on faults inside a plate, often less frequently but sometimes strongly.
Depth: shallow
5 km
Shallow earthquakes (under 70 km) produce the strongest surface shaking for their size, so they are the ones most likely to cause damage near the epicenter.
Did You Feel It?
Where it was felt
No “Did You Feel It?” reports have been published for this event yet. If you felt it, you can add your report on the USGS website.
I felt it — report to USGS ↗USGS PAGER estimate
Who was exposed to shaking
USGS publishes PAGER impact estimates for significant earthquakes, usually within an hour. No PAGER estimate is available for this event.
After the main event
Aftershocks within 50 km
USGS lists 11 M2.5+ earthquakes within 50 km in the following 30 days; the largest was M4.4 on July 11, 2011. Most nearby activity right after a large earthquake is aftershocks, which usually become less frequent over days and weeks.
- 4.2South Island of New Zealand15y ago · 28 km N of this epicenter
- 4.08 km NNW of Burnham, New Zealand15y ago · 47 km NW of this epicenter
- 4.311 km ESE of Christchurch, New Zealand15y ago · 34 km N of this epicenter
- 4.47 km SSE of Christchurch, New Zealand15y ago · 29 km N of this epicenter
- 3.91 km SW of Prebbleton, New Zealand15y ago · 31 km NW of this epicenter
- 4.113 km ESE of Christchurch, New Zealand15y ago · 29 km N of this epicenter
- 4.413 km E of Christchurch, New Zealand15y ago · 39 km N of this epicenter
- 3.86 km W of Lincoln, New Zealand15y ago · 31 km NW of this epicenter
Regional history
Past M5+ earthquakes within 300 km
USGS lists 69 M5.0+ earthquakes within 300 km before this one (catalog from 1900; older records are less complete). The strongest:
- 7.368 km S of Wakefield, New ZealandJune 16, 1929 · 210 km N of this epicenter
- 7.138 km E of Westport, New ZealandMay 23, 1968 · 241 km N of this epicenter
- 7.030 km NW of Amberley, New ZealandMarch 9, 1929 · 98 km N of this epicenter
- 7.019 km NE of Methven, New ZealandSeptember 3, 2010 · 77 km NW of this epicenter
- 6.856 km NW of Oxford, New ZealandJune 18, 1994 · 128 km NW of this epicenter
- 6.535 km NNW of Methven, New ZealandJune 26, 1946 · 113 km NW of this epicenter
- 6.558 km SW of Wakefield, New ZealandJune 22, 1929 · 226 km N of this epicenter
- 6.471 km NNE of Amberley, New ZealandMay 22, 1948 · 148 km N of this epicenter
History · NOAA
Deadliest earthquakes in this area
NOAA’s significant-earthquake database lists 15 damaging, deadly or tsunami-generating earthquakes within 300 km of this epicenter since 1700, which together caused about 209 recorded deaths. The most severe:
- 2011M6.1
Christchurch, Lyttelton
21 Feb 2011 · 30 km away
185 deaths$15 billion damagetsunami
- 1929M7.5
South Island
16 Jun 1929 · 236 km away
17 deathsModerate damage ($1–5M)tsunami
- 1968M7.1
South Island: Nw Coast
23 May 1968 · 245 km away
3 deaths$3 million damage
- 1848M6.0
Awatere River, Marlborough
18 Oct 1848 · 266 km away
3 deathstsunami
- 2011M6.0
South Island: Canterbury
13 Jun 2011 · 33 km away
1 death$3.0 billion damage
- 2010M7.0
Christchurch
3 Sep 2010 · 77 km away · intensity IX
$6.5 billion damage
NOAA NCEI Global Significant Earthquake Database. Historical figures are estimates; older records are incomplete.