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The image is when the 2011 Christchurch earthquake struck and quite a few of the building collapsed and made a big rumble.

Here is some evidence:
Christchurch, seconds after the

2011 earthquake struck.

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The diagrams show what the trampoline affect is and how it happens.

The first factor was that the fault lines were very solid. The second factor is the earthquake rupture was also thought to be faster than most earthquakes of this magnitude.The third factor is the trampoline affect which is what happens when a big earthquake strikes and damages things.

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The second earthquake was much stronger than the first because the ground was still weak and then it made the second one more damaging.

The first was 7.1 and struck bad. The second was 6.3 but the ground was still weak and it collapsed buildings and damaged many roads and killed  185 people. This was because the ground still was very weak from the previous earthquake.

The Richter Scale colors are different because on how big and deep it was. So a level 7 one is 10 times stronger that the level 6 one and 100 times stronger than the level 5 one. We don't normally feel ones lees than level 3 on the Richter Scale.

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The images are showing how liquefaction works. Sediment is soil

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the Richter is something that assigns a magnitude number to quantify the size of an earthquake.

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The two main earthquakes where caused by movement along fault lines west of the city beneath the Canterbury plains.

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The main aim of the scientists is that if they do heaps of research on the faults they may soon know when an earthquake will happen.

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Learning from the Christchurch Earthquakes

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What is stated is that some of the 2010 and 2011 earthquakes in Christchurch had a big impact.

By studying the causes and impact of the earthquakes, scientists now understand more about the processes involved.

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I think this text will be about big earthquakes that happened in Christchurch.