Seismic Hazards - (Christchurch Liquefaction 2011) Flashcards
(8 cards)
What is liquefaction?
Liquefaction is when saturated, loose soil loses strength and behaves like a liquid during intense ground shaking, usually during an earthquake.
This phenomenon can lead to significant structural damage during seismic events.
When did the Christchurch earthquake occur that caused major liquefaction?
On 22 February 2011.
This earthquake was one of the most devastating in New Zealand’s history.
What magnitude was the Christchurch earthquake in 2011?
Magnitude 6.3.
This magnitude is considered extremely strong and capable of causing severe damage.
Why was liquefaction such a big issue in Christchurch?
Christchurch is built on soft, waterlogged alluvial soils which are highly susceptible to liquefaction.
The geological composition of the area contributed significantly to the effects of the earthquake.
What were the effects of liquefaction in Christchurch?
Roads cracked, buildings tilted or sank, and sand and silt erupted from the ground, covering streets and properties.
These effects severely disrupted daily life and infrastructure.
How many tonnes of silt were estimated to have been ejected during the liquefaction in Christchurch?
Over 400,000 tonnes of silt.
This large volume of material significantly altered the landscape and posed cleanup challenges.
What areas of Christchurch were most affected by liquefaction?
Eastern suburbs like Bexley and Avonside.
These areas experienced some of the most severe ground instability.
How did liquefaction impact the economy of Christchurch?
It caused billions in damage, especially to infrastructure and housing, and led to the red-zoning of certain areas for future development.
The economic repercussions were felt for years following the earthquake.