Christchurch earthquake 2011 Flashcards
Causes and characteristics
September 2010- Greendale fault ruptured a M7.1 magnitude
22nd Feb 2011- M6.3 triggered quake, major aftershock
Although weaker, the 2011 earthquake caused more damage as it struck closer to the main built up area of Christchurch
Physical factors that increased the risk of damage
Epicentre close to Christchurch (10km SE)
5km deep focus
Christchurch is built on alluvial sediment which is unstable during earthquake and enabled liquefaction
Struck at lunch time
Human factors that increased the risk of damage
Densely population
GDP per capita $41,000- wealthy, building codes in place, all buildings checked for compliance with codes
Effects
185 people died
About 10,000 buildings needed to be demolished
50% central city buildings severely damaged
Water pipes, bridges, powelines damaged
Significant liquefaction
Population decline
80% of the water and sewerage system severely damaged
Damage to roads made it difficult for emergency services
Estimated to take New Zealand economy 50 to 100 years to completely recover
Responses
The government immediately activated its national crisis management centre
Rescue teams from all over the world came to help
Electricity was restless to 75% of the city within 3 days
Australia gave $5 million in aid
Government provided temporary housing p
CBD corned off for more than 2 years
Tectonic Setting
New Zealand is a highly tectonically active country
Conservative boundary- fault line between the Indo Australian and Pacific plates