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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 about what happens when liquefaction happens and starts to form.
When an earthquake hits the cement turns to water underneath and then makes the concrete ground collapse.
Sediment is water/liquid filled which is under the ground and it turns to liquid when an earthquake hits.

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The Richter scale rates the size of an earthquake by

measuring the energy the earthquake released. Every whole number on the scale is ten times the previous number, so a level 7 earthquake is ten

times stronger than a level 6 and one hundred times stronger than a level 5. We don’t usually feel

earthquakes less than 3 on the Richter scale.

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There were two earthquakes that were big on the township. The first one was in September 2010 which was a magnitude of 7.1 and was close to Darfield.   This was done along the fault lines west of the city beneath the Canterbury Plains.

Liquefaction: Liquefaction and ground deformation resulted in a great deal of damage. It causes damage because the liquid cement turn back and then make it collapses inwards.

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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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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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Read text

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I think it's about when the Christchurch Earthquakes happen and how they now live from the Earthquakes

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Reading Response Activity week 3-4 T3 Group 4 Answer all questions on your Padlet.  Label each box with the question number and complete your answers in full sentences, with punctuation!  WALT:  To summarise an article's main points/ideas To skim and scan the text for specific information To loc...

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Learning from the Christchurch Earthquakes