Photograph captioned by Fairfax, "Earthquake damage".
Photograph captioned by Fairfax, "Aerial pics of the fault line which ruptured causing Saturday's 7.1 earthquake".
Photograph captioned by Fairfax, "Jennifer Graham found $3000 in her bathroom, which fell out from behind the mirror after the last large aftershock recently".
Photograph captioned by Fairfax, "Aerial pics of the fault line which ruptured causing Saturday's 7.1 earthquake".
Photograph captioned by Fairfax, "Businesswoman Angel Wu, president of North South Business Incorporated, says members of the mainly Chinese group of businesses and store operators have been rallying around to try to help members hardest hit by the earthquake. She talks of serious suffering for those worst-affected".
Liquefaction of sandy soil has been observed to cause significant damage to infrastructure during major earthquakes. Historical cases of liquefaction have typically occurred in sands containing some portion of fines particles, which are defined as 75μm or smaller in diameter. The effects of fines on the undrained behaviour of sand are not however fully understood, and this study therefore attempts to quantify these effects through the undrained testing of sand mixed with non-plastic fines sourced from Christchurch, New Zealand. The experimental program carried out during this study consisted of undrained monotonic and cyclic triaxial tests performed on three different mixtures of sand and fines: the Fitzgerald Bridge mixture (FBM), and two Pinnacles Sand mixtures (PSM1 and PSM2). The fines content of each host sand was systematically varied up to a maximum of 30%, with all test specimens being reconstituted using moist tamping deposition. The undrained test results from the FBM soils were interpreted using a range of different measures of initial state. When using void ratio and relative density, the addition of fines to the FBM sand caused more contractive behaviour for both monotonic and cyclic loadings. This resulted in lower strengths at the steady state of deformation, and lower liquefaction resistances. When the intergranular void ratio was used for the interpretation, the effect of additional fines was to cause less contractive response in the sand. The state parameter and state index were also used to interpret the undrained cyclic test results – these measures suggested that additional fines caused less contractive sand behaviour, the opposite to that observed when using the void ratio. This highlighted the dependency on the parameter chosen as a basis for the response comparison when determining the effects of fines, and pointed out a need to identify a measure that normalizes such effects. Based on the FBM undrained test results and interpretations, the equivalent granular void ratio, e*, was identified from the literature as a measure of initial state that normalizes the effects of fines on the undrained behaviour of sand up to a fines content of 30%. This is done through a parameter within the e* definition termed the fines influence factor, b, which quantifies the effects of fines from a value of zero (no effect) to one (same effect as sand particles). The value of b was also determined to be different when interpreting the steady state lines (bSSL) and cyclic resistance curves (bCR) respectively for a given mixture of sand and fines. The steady state lines and cyclic resistance curves of the FBM soils and a number of other sand-fines mixtures sourced from the literature were subsequently interpreted using the equivalent granular void ratio concept, with bSSL and bCR values being back-calculated from the respective test data sets. Based on these interpretations, it was concluded that e* was conceptually a useful parameter for characterizing and quantifying the effects of fines on the undrained behaviour of sand, assuming the fines influence factor value could be derived. To allow prediction of the fines influence factor values, bSSL and bCR were correlated with material and depositional properties of the presented sand-fines mixtures. It was found that as the size of the fines particles relative to the sand particles became smaller, the values of bSSL and bCR reduced, indicating lower effect of fines. The same trend was also observed as the angularity of the sand particles increased. The depositional method was found to influence the value of bCR, due to the sensitivity of cyclic loading to initial soil fabric. This led to bSSL being used as a reference for the effect of fines, with specimens prepared by moist tamping having bCR > bSSL, and specimens prepared by slurry deposition having bCR < bSSL. Finally the correlations of the fines influence factor values with material and depositional properties were used to define the simplified estimation method – a procedure capable of predicting the approximate steady state lines and cyclic resistance curves of a sand as the non-plastic fines content is increased up to 30%. The method was critically reviewed based on the undrained test results of the PSM1 and PSM2 soils. This review suggested the method could accurately predict undrained response curves as the fines content was raised, based on the PSM1 test results. It also however identified some key issues with the method, such as the inability to accurately predict the responses of highly non-uniform soils, a lack of consideration for the entire particle size distribution of a soil, and the fact the errors in the prediction of bSSL carry through into the prediction of bCR. Lastly some areas of further investigation relating to the method were highlighted, including the need to verify the method through testing of sandy soils sourced from outside the Christchurch area, and the need to correlate the value of bCR with additional soil fabrics / depositional methods.
Two of the large boulders (larger than a house or two) that came down from Castle Rock (see the fence in front of the boulders).
Nearly two weeks after the 7.1 earthquake, and a week after demolition started, this is the end of The Valley Inn in Heathcote.
Strong aftershocks felt in Canterbury, Quake firms to seek government wage subsidy, More services, access to buildings being restored in Christchurch, Minister for Earthquake Recovery discusses plans, Heavy rain causes flooding and road closures in Lower North Island, Building codes minimised quake's injuries and damage, Glass supply freezes as Christchurch companies clean up.
Photograph captioned by Fairfax, "Major earthquake hits Christchurch. Maling Street in Avonside. From left: Charlie Tarawa, Tamatea Briggs (12) and Ngarita Briggs (8) outside their make shift shelter. They are too scared to go in the house so are sleeping on the lawn".
A photograph of a sign on the door of the Botanic Gardens Cafe. The sign indicates that the premises have been assessed by the Christchurch City Council after the 4 September 2010 earthquake and no apparent food safety issues were found.
Photograph captioned by Fairfax, "Major earthquake hits Christchurch. Maling Street in Avonside. From left:Charlie Tarawa, Tamatea Briggs (12), Ngarita Briggs (8) and Walton Briggs sit under a make shift shelter while they wait for a wood fire to boil water".
The historic Provincial Hotel at the Barbadoes Street / Cashel Street corner has been cordoned off for fear of collapse; aftermath of the magnitude 7.1 earthquake that struck Christchurch on Saturday 4 September 2010.
This building at the corner of Barbadoes Street / St Asaph Street was so badly damaged in the magnitude 7.1 earthquake that struck Christchurch on Saturday 4 September 2010 that it had to be demolished
Demolition of Robertson's Bakery building, Victoria Street, Christchurch. The Chandelier rescue ... Walking into work I saw the building I always wanted to buy (and run as a bookshop, perfumery, shoe shop) - the old Robertson's Bakery getting demolished. But the bigass digger gently reached into the wreckage and saved this chandelier, bringing...
A pile of bricks on the roof of The Christchurch Club, the remains of its collapsed chimney.
Photograph captioned by Fairfax, "Christchurch begins the slow recovery process after last weeks devastating 7.1 earthquake".
Many of New Zealand's companies are fronting up with large donations to help with rebuilding in Christchurch.
The police in Christchurch say reports of domestic violence have jumped by half since Saturday's destructive earthquake.
How Christchurch museums, galleries and libraries which store many of NZ's treasures have fared after the earthquake.
Photograph captioned by Fairfax, "Christchurch begins the slow recovery process after last weeks devastating 7.1 earthquake".
Photograph captioned by Fairfax, "Christchurch begins the slow recovery process after last weeks devastating 7.1 earthquake".
Photograph captioned by Fairfax, "Christchurch begins the slow recovery process after last weeks devastating 7.1 earthquake".
Photograph captioned by Fairfax, "Christchurch begins the slow recovery process after last weeks devastating 7.1 earthquake".
Photograph captioned by Fairfax, "Christchurch begins the slow recovery process after last weeks devastating 7.1 earthquake".
Photograph captioned by Fairfax, "Christchurch begins the slow recovery process after last weeks devastating 7.1 earthquake".
Photograph captioned by Fairfax, "Christchurch begins the slow recovery process after last weeks devastating 7.1 earthquake".
Photograph captioned by Fairfax, "Christchurch begins the slow recovery process after last weeks devastating 7.1 earthquake".
Photograph captioned by Fairfax, "Christchurch begins the slow recovery process after last weeks devastating 7.1 earthquake".
A damaged section of road is cordoned off with road cones on a residential street in Christchurch.