20130827_2645_1D3-24 Colombo and Armagh corner What was one of the busier intersection pre earthquakes! #4150
20130827_2621_1D3-47 Looking towards Cathedral Square Where once were buildings! From the corner of Armagh Street and Oxford Terrace. #4147
The seismic survey truck T-Rex (from University of Texas) was in Bexley and Pacific Park a few days ago and may have left this calling card on the front lawn of my old "red zone" house. Obviously the geotechs will know what it means.
A red-zone house just a few down the road from where we used to live in Velsheda Street, with bricks (brick veneer?) off and lifted prior to transporting away.
20130911_8095_EOS M-33 Another one ready to leave Another salvaged house from the Bexley (Pacific Park) red zone is on the truck and may start it's journey to a new location overnight. #4204
A house, one of the few still remaining in the Dallington Red Zone (Avonside Drive, Dallington). The area is "red zoned" due to land damage from earthquakes (mainly the February 22nd 2011 6.4 magnitude quake).
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Earthquake damage. As a result of the September 2010 earthquake, with further damage from the February 2011 event.
Canterbury Provincial Council Buildings after the 6.3 magnitude quake hit Christchurch 22 Feburary 2011. This small cluster of historic buildings in central Christchurch are treasured by the city, both for their historical importance and their beauty. Canterbury Provincial Council Buildings (1858 to 1865) were designed by Benjamin Mountfort, C...
The unforgettable beauty of lavender Occurs in both the earth As well as part of the many changing Shades of the daily heavens on high. Is quickly there, and then is gone. Light violet, lavender, How unique is its special glow, Colored in nature in light lilac, Amethyst, and airy, purple indigo. From a poem by Gil Saenz
This statue of the Virgin Mary stood in the south tower of The Cathedral of the Blessed Sacrament and had been facing inside from when she was placed there and through the September 2010 earthquake. That changed on February 22 2010 at 12.51pm when Christchurch was rocked by a 6.3 magnitude earthquake. During the violent shaking motion Mary was t...
20100918_3500_1D3-60 Porritt Park - Christchurch earthquake The bridge at the north end of Porritt Park, Avondale. #402
Manchester Courts, a seven-storey building on the corner of Hereford and Manchester Streets, is a category one historic place built in 1905-1906 that up until the 7.1 earthquake, housed offices. News of the scheduled demolition provoked an emotional response from the people of Christchurch. UPDATE 14 October 2010: A group of residents is campaig...
My house (bought in March 2004) till the government procured it in October 2012, is finally being demolished. It will be an empty section in a couple of days, once they rip up the concrete base. Note the rainbow on right.
20161018_9063_7D2-70 Restricted Area (292/366) In the suburban red zone on Avonside Drive. #7826
The objective of this study is to examine the influence of near-fault motions on liquefaction triggering in Christchurch and neighboring towns during the 2010-2011 Canterbury earthquake sequence (CES). The CES began with the 4 September 2010, Mw7.1 Darfield earthquake and included up to ten events that triggered liquefaction. However, most notably, widespread liquefaction was induced by the Darfield earthquake and the Mw6.2, 22 February 2011 Christchurch earthquake. Of particular relevance to this study is the forward directivity effects that were prevalent in the motions recorded during the Darfield earthquake, and to a much lesser extent, during the Christchurch earthquake. A 2D variant of the Richart-Newmark fatigue theory was used to compute the equivalent number of cycles (neq) for the ground motions, where volumetric strain was used as the damage metric. This study is unique because it considers the contribution and phasing of both the fault-normal and fault-parallel components of motion on neq and the magnitude scaling factor (MSF). It was found that when the fault-normal and fault-parallel motions were treated individually, the former yielded a lower neq than the latter. Additionally, when the combined effects of fault-normal and fault-parallel components were considered, it was found that the MSF were higher than those commonly used. This implies that motions containing near-fault effects are less demanding on the soil than motions that do not. This may be one of several factors that resulted in less severe liquefaction occurring during the Darfield earthquake than the Christchurch earthquake.
This paper presents insights from recent advanced laboratory testing of undisturbed and reconstituted specimens of Christchurch silty-sands. The purpose of the testing was to establish the cyclic strength of silty-sands from sites in the Central Business District (CBD), where liquefaction was observed in 4 September 2010, 22 February 2011, and 13 June 2011. Similar overall strengths were obtained from undisturbed and reconstituted tests prepared at similar densities, albeit with higher variability for the reconstituted specimens. Reconstituted specimens exhibited distinctly different response in terms of lower compressibility during initial loading cycles, and exhibited a more brittle response when large strains were mobilised, particularly for samples with high fines content. Given the lower variability in natural sample response and the possibility of age-related strength to be significant for sites not subjected to earthquakes, high quality undisturbed samples are recommended over the use of reconstituted specimens to establish the cyclic strength of natural sands.
In recent years, significant research has been undertaken into the development of lead-extrusion damping technology. The high force-to-volume (HF2V) devices developed at the University of Canterbury have been the subject of much of this research. However, while these devices have undergone a limited range of velocity testing, limitations in test equipment has meant that they have never been tested at representative earthquake velocities. Such testing is important as the peak resistive force provided by the dampers under large velocity spikes is an important design input that must be known for structural applications. This manuscript presents the high-speed testing of HF2V devices with quasi-static force capacities of 250-300kN. These devices have been subjected to peak input velocities of approximately 200mm/s, producing peak resistive forces of approximately 350kN. The devices show stable hysteretic performance, with slight force reduction during high-speed testing due to heat build-up and softening of the lead working material. This force reduction is recovered following cyclic loading as heat is dissipated and the lead hardens again. The devices are shown to be only weakly velocity dependent, an advantage in that they do not deliver large forces to the connecting elements and surrounding structure if larger than expected response velocities occur. This high-speed testing is an important step towards uptake as it provides important information to designers.
In recent years, significant research has been undertaken into the development of lead-extrusion damping technology. The high force-to-volume (HF2V) devices developed at the University of Canterbury have been the subject of much of this research. However, while these devices have undergone a limited range of velocity testing, limitations in test equipment has meant that they have never been tested at representative earthquake velocities. Such testing is important as the peak resistive force provided by the dampers under large velocity spikes is an important design input that must be known for structural applications. This manuscript presents the high-speed testing of HF2V devices with quasi-static force capacities of 250-300kN. These devices have been subjected to peak input velocities of approximately 200mm/s, producing peak resistive forces of approximately 350kN. The devices show stable hysteretic performance, with slight force reduction during high-speed testing due to heat build-up and softening of the lead working material. This force reduction is recovered following cyclic loading as heat is dissipated and the lead hardens again. The devices are shown to be only weakly velocity dependent, an advantage in that they do not deliver large forces to the connecting elements and surrounding structure if larger than expected response velocities occur. This high-speed testing is an important step towards uptake as it provides important information to designers.
20130827_2654_1D3-24 Corner Colombo/Hereford Street, Christchurch The same view as the previous photo. Building demolished after the earthquake of 2011! #4156
A local inspecting the damage to St Lukes Church after the 6.3 quake hit. For whom the bell tolls Time marches on For whom the bell tolls Take a look to the sky just before you die It's the last time you will Blackened roar, massive roar, fills the crumbling sky Shattered goal fills his soul with a ruthless cry Stranger now are his eyes to this...
The Christchurch Cathedral Square showing the Anglican Cathedral after loosing its tower and spire after the 6.3 quake hit Christchurch 22 February 2011. This image also shows the remains of the very heavy snow fall we had on Monday 25 July 2011. The centre of the city is still cordoned off. This image was taken from a helicopter flight over the...
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This winter-eve is warm, Humid the air! leafless, yet soft as spring, The tender purple spray on copse and briers! And that sweet city with her dreaming spires, She needs not June for beauty's heightening, Lovely all times she lies, lovely to-night!— From "Thyrsis: A Monody" by Matthew Arnold 1822–1888
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Sadly the Chapel has been badly damaged in the magnitude 6.3 earthquake that hit Christchurch 22 February 2011. See below. The Rose Historic Chapel formerly St Mary’s Convent Chapel is the sole survivor of a group of heritage buildings in Christchurch that once comprised the St Mary’s Convent complex for the Sisters of Mercy in North Colombo St...
Earthquake damage. As a result of the September 2010 earthquake, with further damage from the February 2011 event.
Worcester Blvd. Lawrence Roberts works for Photo & Video in Christchurch, suppliers of much of my photo gear in exchange for cash!
At least two broken pieces from the Scott statue rest in the Canterbury Museum. The statue toppled in the 22nd February 2011 earthquake.