A felt heart with "get well soon" embroided on the front, sewn to the wire fencing in front of in front of Bill Hammond's house in Lyttelton. The heart offers a bit of beauty and hope to an otherwise depressing scene.
The Christchurch suburb of New Brighton was hit hard by the Christchurch earthquakes, with roads that still haven't been fixed and many families on struggle street. One local is hoping a fridge offering free food, will help.
Photograph captioned by Fairfax, "Christchurch CBD was 'yarn-bombed' during the weekend using yarn and fabric pieces to brighten public areas and earthquake-affected spaces. Hope sign at Hereford and Manchester Streets".
Photograph captioned by Fairfax, "Christchurch CBD was 'yarn-bombed' during the weekend using yarn and fabric pieces to brighten public areas and earthquake-affected spaces. Hope sign at Hereford and Manchester Streets".
A car park on the corner of Tuam and Colombo Streets replaces the building that was demolished there. On the wall of an adjoining building, a chalkboard mural encourages people to leave their thoughts, with the prompt "I hope Christchurch will...".
Nikki Ross is still waiting on an insurance settlement almost seven years after her family home was damaged in the February, 2011 Christchurch earthquake. Trish Keith from EQC says they're hoping to offer the family a settlement in the next three weeks.
At least five companies are busy working in and around Christchurch blasting rock on unstable slopes in the hope of reducing danger since the earthquakes. Spectrum's Deborah Nation joins backcountry construction company Solutions 2 Access, as the team blasts rock on the Port Hills above Lyttelton.
Photograph captioned, "I'll have mixed feelings when I leave. I'll be sad to go - and sad to see my house go. But I hope it'll be a good feeling once it's over. I'll be pleased to get to that stage and feel like I'm finally moving on".
Detail of the fence around the 'Ark of Hope' by Wongi Wilson in Sydenham Square, corner of Brougham and Colombo Streets. A sign reading "In the end it will be alright - if it is not alright, it is not the end." has been attached to the fence.
The road cordon on Hereford Street just outside the T & G Building (formerly known as Kenton Chambers). On the fence is a banner that reads 'Hope' and behind it is a street sign that reads 'Road closed'. A digger and building rubble can be seen in the background.
The road cordon on Hereford Street just outside the T & G Building (formerly known as Kenton Chambers). On the fence is a banner that reads 'Hope' and behind it is a street sign that reads 'Road closed'. A digger and building rubble can be seen in the background.
Documenting earthquake-induced ground deformation is significant to assess the characteristics of past and contemporary earthquakes and provide insight into seismic hazard. This study uses airborne light detection and ranging (LiDAR) and conducts multi-disciplinary field techniques to document the surface rupture morphology and evaluate the paleoseismicity and seismic hazard parameters of the Hurunui segment of the Hope Fault in the northern South Island of New Zealand. It also documents and evaluates seismically induced features and ground motion characteristics of the 2010 Darfield and 2011 Christchurch earthquakes in the Port Hills, south of Christchurch. These two studies are linked in that they investigate the near-field coseismic features of large (Mw ~7.1) earthquakes in New Zealand and produce data for evaluating seismic hazards of future earthquakes. In the northern South Island of New Zealand, the Australian-Pacific plate boundary is characterised by strike-slip deformation across the Marlborough Fault System (MFS). The ENE-striking Hope Fault (length: ~230 km) is the youngest and southernmost fault in the MFS, and the second fastest slipping fault in New Zealand. The Hope Fault is a major source of seismic hazard in New Zealand and has ruptured (in-part) historically in the Mw 7.1 1888 Amuri earthquake. In the west, the Hurunui segment of the Hope Fault is covered by beech forest. Hence, its seismic hazard parameters and paleoearthquake chronology were poorly constrained and it was unknown whether the 1888 earthquake ruptured this segment or not and if so, to what extent. Utilising LiDAR and field data, a 29 km-long section of the Hurunui segment of the Hope Fault is mapped. LiDAR-mapping clearly reveals the principal slip zone (PSZ) of the fault and a suite of previously unrecognised structures that form the fault deformation zone (FDZ). FDZ width measurements from 415 locations reveal a spatially-variable, active FDZ up to ~500 m wide with an average width of 200 m. Kinematic analysis of the fault structures shows that the Hurunui segment strikes between 070° and 075° and is optimally oriented for dextral strike-slip within the regional stress field. This implies that the wide FDZ observed is unlikely to result from large-scale fault mis-orientation with respect to regional stresses. The analysis of FDZ width indicates that it increases with increased hanging wall topography and increased topographic relief suggesting that along-strike topographic perturbations to fault geometry and stress states increase fault zone complexity and width. FDZ width also increases where the tips of adjacent PSZ strands locally vary in strike, and where the thickness of alluvial deposits overlying bedrock increases. LiDAR- and photogrammetrically-derived topographic mapping indicates that the boundary between the Hurunui and Hope River segments is characterised by a ~850-m-wide right stepover and a 9º-14° fault bend. Paleoseismic trenching at Hope Shelter site reveals that 6 earthquakes occurred at A.D. 1888, 1740-1840, 1479-1623, 819-1092, 439-551, and 373- 419. These rupture events have a mean recurrence interval of ~298 ± 88 yr and inter-event times ranging from 98 to 595 yrs. The variation in the inter-event times is explained by (1) coalescing rupture overlap from the adjacent Hope River segment on to the Hurunui segment at the study site, (2) temporal clustering of large earthquakes on the Hurunui segment, and/or (3) ‘missing’ rupture events. It appears that the first two options are more plausible to explain the earthquake chronologies and rupture behaviour on the Hurunui segment, given the detailed nature of the geologic and chronologic investigations. This study provides first evidence for coseismic multi-segment ruptures on the Hope Fault by identifying a rupture length of 44-70 km for the 1888 earthquake, which was not confined to the Hope River segment (primary source for the 1888 earthquake). LiDAR data is also used to identify and measure dextral displacements and scarp heights from the PSZ and structures within the FDZ along the Hurunui segment. Reconstruction of large dextrally-offset geomorphic features shows that the vertical component of slip accounts for only ~1% of the horizontal displacements and confirms that the fault is predominantly strike-slip. A strong correlation exists between the dextral displacements and elevations of geomorphic features suggesting the possibility of age correlation between the geomorphic features. A mean single event displacement (SED) of 3.6 ± 0.7 m is determined from interpretation of sets of dextral displacements of ≤ 25 m. Using the available surface age data and the cumulative dextral displacements from Matagouri Flat, McKenzie Fan, Macs Knob and Hope River sites, and the mean SED, a mean slip rate of 12.2 ± 2.4 mm/yr, and a mean recurrence interval of ~320 ± 120 yr, and a potential earthquake magnitude of Mw 7.2 are determined for the Hurunui segment. This study suggests that the fault slip rate has been constant over the last ~15000 yr. Strong ground motions from the 2010 Darfield (Canterbury) earthquake displaced boulders and caused ground damage on some ridge crests in the Port Hills. However, the 2011 Christchurch earthquake neither displaced boulders nor caused ground damage at the same ridge crests. Documentation of locations (~400 m a.s.l.), lateral displacements (8-970 cm), displacement direction (250° ± 20°) of displaced boulders, in addition to their hosting socket geometries (< 1 cm to 50 cm depth), the orientation of the ridges (000°-015°) indicate that boulders have been displaced in the direction of instrumentally recorded transient peak ground horizontal displacements nearby and that the seismic waves have been amplified at the study sites. The co-existence of displaced and non-displaced boulders at proximal sites suggests small-scale ground motion variability and/or varying boulder-ground dynamic interactions relating to shallow phenomena such as variability in soil depth, bedrock fracture density and/or microtopography on the bedrock-soil interface. Shorter shaking duration of the 2011 Christchurch event, differing frequency contents and different source characteristics were all factors that may have contributed to generating circumstances less favourable to boulder displacement in this earthquake. Investigating seismically induced features, fault behaviour, site effects on the rupture behaviour, and site response to the seismic waves provides insights into fault rupture hazards.
Photograph captioned by Fairfax, "Christchurch Airport opened at 8am this morning to domestic flights. Robby and Rolly Alden were booked to leave to go back to the UK yesterday (Feb 22 2010) and are hoping to get out of Christchurch today".
A decision on the future of Christchurch's red zoned land could be made within a year. That's the hope of the man at the helm of Regenerate Christchurch, one of two organisations charged with taking over the city's rebuild from the Earthquake Recovery Authority, which shuts its doors in just three days.
A felt heart sewn to the wire fence in front of the Lyttelton Borough Council Chambers Building, a pile of bricks fallen from which are visible on the street. The heart provides a bit of beauty and hope to an otherwise depressing scene, the words "say yes often" embroided on the felt.
A photograph of SPCA Field Officer Vanessa Hampton releasing a pigeon at SPCA Canterbury as a symbol of love, hope and renewal. The pigeon was named Barney Rubble due to the fact that it was found amongst the rubble and debris of the ChristChurch Cathedral.
A photograph captioned by BeckerFraserPhotos, "Jenni and Keith Hague with Lillian and Elaine outside their home at 7 Ching Gardens. They have found somewhere else suitable to live and hope to complete the sale of this house to CERA soon".
Shows a Christmas card from the cartoonist to the 'sick, bereaved, and the people of Christchurch, Pike River & Nelson'. Refers to the Canterbury earthquakes that have caused death, misery and uncertainty for many in the region, the Pike River mining tragedy and floods in the Nelson region. Quantity: 1 digital cartoon(s).
A PDF copy of pages 164-165 of the book Christchurch: The Transitional City Pt IV. The pages document the transitional project 'CPIT Design/Build'. Photos: Gap Filler
An edited video of Betty and Michael's second earthquake story, captured by the UC QuakeBox Take 2 project. Please note that the final 3 minutes, 49 seconds of the original video are corrupted and have thus been edited out of this video. Interviewer: Samuel Hope.
It's hoped a new art installation in Ōtautahi Christchurch can help people talk their worries away through a series of telephones by the riverside. Twelve telephones have popped up across sites commemorating the city's devastating 2011 earthquakes. The group behind the project is Flourish Kia Puawai. Its associate director Sharon Torstonson spoke to Corin Dann.
A video of an interview with Joe Bennett, columnist and Lyttelton resident, about his experiences during the 22 February 2011 earthquake, and his hopes for post-quake Christchurch. This video was part of The Press's 'Christchurch, one year after February 22, 2011' series.
Flowers blooming in a vacant site left by the demolition of a building at the corner of Worcester Street and Stanmore Road. A sign on the ground says 'Commemorative service here Wed 22nd Feb. Bring flowers, seedheads and symbols of memory and hope". In the background, on the wall it says 'Do not demo!'.
The government has announced hundreds of new carparks it hopes will solve the ongoing issues at Christchurch Hospital. Parking was significantly reduced after the earthquakes - forcing patients, visitors and staff to park far away and walk, or catch a shuttle to the hospital. The government's pledging a new building and extension of staff car-parking. Sally Murphy reports.
Two people crawl across a desert littered with animal bones and skulls towards the words 'Land reports' in the distance. The woman says 'Don't get your hopes up! It's probably a mirage!' Context - On Thursday 23 June Prime Minister John Key, Canterbury Earthquake Recovery Minister Gerry Brownlee and representatives from engineering consultants Tonkin & Taylor announced the first part of the Government's long-awaited land report that revealed the fate of up to 5000 quake-damaged homes. Quantity: 1 digital cartoon(s).
A video about the restoration of New Regent Street. The restoration is hoped to be completed in time for the Christmas shopping season. The project is being led by Edward Leeson of Naylor Love, who is also managing the restoration of the Isaac Theatre Royal next door.
In the living room of a house half-ruined by the Christchurch earthquake a decrepit and useless-looking man in a grubby white singlet doses in his armchair with a glass of beer in his hand; his wife whispers to a friend 'Just between you and me, I'm hoping to have him red-stickered!' Context - The two Christchurch earthquakes of 4 September 2010 and 22 February 2011 and the technique of using different coloured stickers to designate the degree of damage to buildings - 'red' indicates that it needs to be demolished. Colour and black and white versions available Quantity: 2 digital cartoon(s).
This report describes the earthquake hazard in Kaikoura district and gives details of historic earthquakes. It includes district-scale (1:250,000) active fault, ground shaking zone, liquefaction and landslide susceptibility maps. The report describes an earthquake scenario for a magnitude 7.0-7.3 Hope Fault earthquake near Kaikoura, and a subsequent local tsunami.
A video of Principal Tony Simpson announcing to staff and parents at Phillipstown School that the Ministry of Education has decided to merge the school with Woolston School. The video also includes an interview with Tony Simpson about the merger, and his hopes for education in Christchurch in the future.
A sign on the door of a shop reading, "I have been reclosed again by the Council due to buckled retaining wall in basement. My landlord is getting wall braced for all our safety. I hope to reopen in 2/3 weeks. I will try and keep you informed by note on shop glass. Ross".