Steel bracing on the Moorhouse Avenue overpass. The photographer comments, "Standing underneath I did hear a clump as if a part of the road overhead was pivoting as a car passed over it".
An earthquake memories story from Mike Ardagh, Medical Specialist, Emergency Department, Christchurch Hospital, titled, "Clear heads on strong shoulders".
A video about the discovery of a historic tramline on North Avon Road. The video includes an interview with Brent Leersynder, a site engineer for SCIRT, and Steve Timpson, site foreman for SCIRT. The SCIRT team found the tramline while repairing the damaged wastewater system under North Avon Road in May.
A video of the removal of the earthquake-damaged Medway Street bridge from the banks of the Avon River. The video shows members of the Stronger Christchurch Infrastructure Rebuild Team removing the bridge and preparing it for transport to the Ferrymead Heritage Park. It will remain at the park until a permanent home can be found for it as an earthquake memorial.
Object Overview of 'General distribution and characteristics of active faults and folds in the Ashburton District, mid-Canterbury (Barrell and Strong, 2009).'
Object Overview of 'General distribution and characteristics of active faults and folds in the Mackenzie District, South Canterbury (Barrell and Strong, 2010).'
A heart has been tied to a silhouetted figure on a fence. Written on the heart is "Dear Christchurch, I know it is a hard time for us right now but we have to be strong and put up with it. Love from Connie".
A video capturing an aftershock from the Canterbury earthquake on 13 June 2011, 2:20 pm. A strong shake after lunch time caused Ben Post to set up his camera in his workplace, capturing this aftershock. The camera is mounted on a small sturdy tripod on top of a table with wheels.
Digitally manipulated image of the damaged Cathedral of the Blessed Sacrament, superimposed with a seismograph trace. The photographer comments, "What we want to forget, but must remember".
Photograph captioned by Fairfax, "The 800-strong student army helps residents of Rebecca Avenue, Burwood clean up several feet of liquefaction after Tuesday's massive earthquake. Pictures to accompany story by reporter Blair Ensor. Christchurch Earthquake aftermath - day four."
Photograph captioned by Fairfax, "The 800-strong student army helps residents of Rebecca Avenue, Burwood clean up several feet of liquefaction after Tuesday's massive earthquake. Pictures to accompany story by reporter Blair Ensor. Christchurch Earthquake aftermath - day four."
Dried liquefaction silt in North New Brighton. The photographer comments, "This is the the top layer of liquefaction that has dried up in the hot sun. A broken eggshell is around 5 times stronger than these, but a fallen leaf is just not enough to break one. You can see underneath that the heavier sandy layer of liquefaction has dried and has cracked as well".
This report provides information on the locations and character of active geological faults and folds in Ashburton District. The faults are mapped at a district scale and the information is intended to highlight areas where there is a risk of permanent fault movement at the ground surface, and where more detailed investigations should be done if development is proposed in that area (depending on the potential activity of the fault and the type of development proposed). See Object Overview for background and usage information. Most of the faults and folds identified at the ground surface in Ashburton District are in rural or very sparsely populated areas. In addition, most of the faults have relatively long recurrence intervals (long-term average time between fault movements) in the order of several thousand years. Following the Ministry for the Environment Active Fault Guidelines, normal residential development would be allowed on or near faults with recurrence intervals this long. There are no recommendations associated with this report. The information in the report will be reviewed as required, after the remaining district reports are completed in the region.
This report provides information on the locations and character of active geological faults and folds in Mackenzie District. The faults are mapped at a district scale and the information is intended to highlight areas where there is a risk of fault movement, and where more detailed investigations should be done if development is proposed in that area(depending on the potential activity of the fault and the type of development proposed). Most of the faults and folds identified at the ground surface in Mackenzie District are in rural or very sparsely populated areas. In addition, most of the faults have relatively long recurrence intervals (long-term average time between fault movements) in the order of several thousand years. Following the Ministry for the Environment Active Fault Guidelines, normal residential development would be allowed on or near faults with recurrence intervals this long. There are no recommendations associated with this report. The information in the report will be reviewed as required, after the remaining district reports are completed in the region. See Object Overview for background and usage information.