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Field-by-field comparison
Initial edition
Christchurch Earthquake
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At 12:51 p.m. on 22 February 2011, a shallow magnitude 6.2 earthquake struck close to central Christchurch during a working day. Exceptionally strong ground motion, liquefaction, rockfall, falling masonry, and major building collapses killed 185 people. The Canterbury Television building collapse caused 115 deaths. The earthquake was part of the sequence that began in September 2010, but its proximity, depth, timing, and direction made this shock far more deadly.
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22 February 2011
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Former Canterbury Television building site
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A magnitude 7.1 earthquake near Darfield on 4 September 2010 had damaged buildings and infrastructure across Canterbury without causing direct deaths. Thousands of aftershocks followed, and assessments, repairs, reoccupation decisions, and everyday life continued under uncertainty. Central Christchurch contained unreinforced masonry and modern reinforced-concrete buildings with different vulnerabilities. The February fault had not been identified at the surface before the sequence.
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A shallow fault rupture occurred within about 10 kilometers of the city. Strong shaking reached extreme accelerations in parts of the urban area and interacted with soft ground, slopes, and existing damage. Masonry fell into streets, hillsides released rock, and water-saturated soils lost strength. The CTV and PGC buildings collapsed, while failures across utilities and transport complicated movement and rescue.
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Urban search and rescue teams, emergency services, construction workers, medical staff, residents, and international teams worked through unstable debris and repeated aftershocks. A central-city cordon remained for an extended period. Liquefaction buried streets and damaged services across eastern suburbs. Families awaited identification and recovery. Decisions about demolition, land zoning, insurance, temporary housing, heritage, and business relocation shaped a recovery lasting far beyond the emergency.
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A Royal Commission examined building failures, especially the CTV collapse, and recommended changes in engineering, design review, permitting, construction oversight, assessment, and professional practice. The central city was substantially rebuilt, while some residential red zones became open land. The sequence advanced liquefaction, strong-motion, geotechnical, and structural research and exposed the social costs of long insurance and governance processes.
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Christchurch shows why earthquake magnitude alone is a poor guide to urban harm. A smaller but shallow and nearby event during daytime caused far greater loss than the earlier larger shock. Building history, ground conditions, occupancy, prior damage, inspection, and rescue access all mattered.
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The CTV memorial site, Canterbury Earthquake National Memorial, Quake City museum, rebuilt streets, stabilized or lost heritage buildings, and open red-zone land preserve different layers of the sequence. Monitoring, engineering records, and continuing community projects make the earthquake visible beyond individual monuments.
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GeoNet headlines the event as magnitude 6.2 while some technical text and catalogs use local magnitude 6.3; the difference reflects scale and revision, not two earthquakes. Many buildings had complex histories of earlier damage and inspection. The mapped CTV site represents one critical failure within a citywide disaster.
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Chaos Tourist editorial
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M 6.2 Christchurch, Tuesday 22 February 2011
Canterbury Earthquakes Royal Commission Final Report: summary and recommendations
Collapse of the Canterbury Television Building
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At 12:51 p.m.
A shallow fault rupture occurred within about 10 kilometers of the city.
GeoNet headlines the event as magnitude 6.2 while some technical text and catalogs use local magnitude 6.3; the difference reflects scale and revision, not two earthquakes.
Christchurch shows why earthquake magnitude alone is a poor guide to urban harm.