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Earthquakes in Christchurch

Christchurch experienced one of the world's most damaging earthquake sequences in 2010-2011, when a M7.1 and subsequent M6.3 earthquake killed 185 people and destroyed much of the city center. The city of 380,000 spent a decade rebuilding and is now a global case study in post-earthquake urban regeneration.

~2,000+ aftershocks recorded (2010-2020)
Largest recent: M7.1 (2010), M6.3 (2011)
Population: 380,000

Why Does Christchurch Face Earthquake Risk?

Christchurch sits on the Canterbury Plains, which despite being far from the Alpine Fault, contains numerous previously unknown reverse and strike-slip faults. The 2010 earthquake revealed hidden seismic hazards in areas previously considered lower-risk. The Alpine Fault 150 km to the west is also capable of a M8+ earthquake.

Active Fault Systems

  • Greendale Fault
  • Porters Pass-Amberley Fault Zone
  • Alpine Fault (regional)

Safety Advice

GNS Science monitors seismicity in New Zealand. Christchurch has implemented a "rebuild green" policy for the former CBD, with extensive open space buffers replacing some damaged building blocks. The city's liquefaction hazard maps are publicly available from Christchurch City Council.

Historical Earthquake Context

Before 2010, Christchurch had not experienced a significant earthquake in recorded history. The September 4, 2010 M7.1 earthquake caused no deaths but significant damage. The February 22, 2011 M6.3 aftershock at 5 km depth destroyed the CBD, killing 185 people including 115 in the CTV building collapse.

Significant Earthquakes Near Christchurch

Year Magnitude Event
2011 M6.3 New Zealand
2010 M7.1 New Zealand

Fault Maps & Tectonic Setting

Tectonic and seismic hazard maps from Wikimedia Commons, USGS, and NASA — open licenses (CC / Public Domain)

Maps sourced from Wikimedia Commons, USGS, and NASA under open licenses. Attribution required where specified. Click any map to enlarge.

FAQ

Frequently Asked Questions

Is Christchurch safe to live in now after the 2011 earthquake?

Christchurch has been extensively rebuilt with improved seismic standards and detailed hazard mapping. The city removed or demolished over 12,000 buildings after the earthquakes. New construction in Christchurch meets modern seismic codes. The ongoing Alpine Fault threat remains, but Christchurch is now far better prepared than before 2010.

How seismically active is Christchurch?

Christchurch sits on the Canterbury Plains near the Alpine Fault and multiple local faults that were not well understood before 2010. The city experiences moderate seismicity — multiple felt earthquakes per year — and remains in an extended aftershock sequence from the 2010-2011 earthquake series that is gradually declining.

What earthquake faults affect Christchurch?

The Greendale Fault caused the 2010 M7.1 earthquake and was previously unmapped. The Alpine Fault, 200 km to the west, is considered overdue for a M8.0+ rupture. The Port Hills Fault contributed to the 2011 M6.3 event. Canterbury's complex fault network means additional significant earthquakes remain possible.

Is Christchurch safe now after the earthquakes?

Christchurch has been extensively rebuilt with modern seismic-resistant construction after the 2010-2011 earthquake sequence. The Red Zone — land deemed too dangerous to rebuild — was cleared. The rebuilt central city uses modern engineering. However, the Alpine Fault and other regional faults continue to pose future earthquake risk.

Where can I see live earthquake data for Christchurch?

Track earthquakes near Christchurch on the Earthquake Globe app or at earthquakes.site/map?country=new-zealand. GeoNet (geonet.org.nz) operated by GNS Science provides real-time New Zealand earthquake data. The Canterbury seismic sequence is among the most thoroughly documented in seismological history.

Get Earthquake Alerts for Christchurch

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