An entry from Deb Robertson's blog for 18 November 2011 entitled, "It must be November cause the Works in Progress pile has gone CRAZY...".
A photograph of the Avon River, showing the high water level caused by the earthquake displacing the land.
A photograph of the Avon River, showing the high water level caused by the earthquake displacing the land.
A photograph of the Avon River, showing the high water level caused by the earthquake displacing the land.
The courtyard inside the Peterborough Apartments. The ground has subsided under a section of the lawn, causing it to drop.
The courtyard inside the Peterborough Apartments. The ground has subsided under a section of the footpath, causing it to drop.
A photograph captioned by BeckerFraserPhotos, "Wall crushing caused this window in the Hotel Grand Chancellor to buckle".
The courtyard inside the Peterborough Apartments. The ground has subsided under a section of the lawn, causing it to drop.
Photograph captioned by BeckerFraserPhotos, "Typical damage caused to the Peterborough Apartments when the underground car park rose 40 cm".
A photograph of a volunteer from the Wellington Emergency Management Office standing next to a crack in a footpath caused by liquefaction.
Damage to a house in Richmond. Bricks have fallen from the walls onto the driveway. The photographer comments, "More movement caused the brick cladding to fall off the building".
At 12.51 p.m. on Tuesday 22 February 2011, a magnitude 6.3 earthquake caused severe damage in Christchurch and Lyttelton, killing 185 people and injuring several thousand.
The foundations of the historic Kaiapoi Railway Station building, which were damaged in the 4 September 2010 earthquake causing the building to lean towards the river.
Sand volcanoes" in the Heathcote Estuary. The volcanoes were caused by liquefaction, where the soil lost its strength and water erupted out of the hole, taking silt with it.
Sand volcanoes" in the Heathcote Estuary. The volcanoes were caused by liquefaction, where the soil lost its strength and water erupted out of the hole, taking silt with it.
Sand volcanoes" in the Heathcote Estuary. The volcanoes were caused by liquefaction, where the soil lost its strength and water erupted out of the hole, taking silt with it.
Sand volcanoes" in the Heathcote Estuary. The volcanoes were caused by liquefaction, where the soil lost its strength and water erupted out of the hole, taking silt with it.
A "sand volcano" in the Heathcote Estuary. The volcano was caused by liquefaction, where the soil lost its strength and water erupted out of the hole, taking silt with it.
Sand volcanoes" in the Heathcote Estuary. The volcanoes were caused by liquefaction, where the soil lost its strength and water erupted out of the hole, taking silt with it.
Sandbags placed along the river bank to prevent flooding onto the road. The earthquake caused the ground in this area to subside, making it susceptible to flooding.
Sandbags placed along the river bank to prevent flooding onto the road. The earthquake caused the ground in this area to subside , making it susceptible to flooding.
Paradise ducks search for food among 'sand volcanoes' in the Heathcote Estuary. The volcanoes were caused by liquefaction where the soil lost its strength and water erupted out of the hole, taking silt with it.
A photograph of a member of the New Zealand Army on the roof of an earthquake-damaged property in Christchurch. A tarpaulin has been placed over a hole in the roof caused by the collapsed chimney.
A sign erected on Retreat Road in Avonside by the Christchurch City Council reading, "Non-residents are asked not to enter this area. Traffic may cause further damage to roads and properties. Please respect the needs of local residents".
A view down a New Brighton Road next to the river. On the left sandbags have been placed on the banks of the river to prevent flooding onto the road. The earthquake caused the ground to subside and sink, making this area susceptible to flooding.
A view down a New Brighton Road next to the river. On the left sandbags have been placed on the banks of the river to prevent flooding onto the road. The earthquake caused the ground in this area to subside, making it susceptible to flooding.
A view down Cashel Street from the Bridge of Remembrance, showing earthquake damage to several buildings along Cashel Mall. In the background the Hotel Grand Chancellor can be seen, a Christchurch hotel that was badly damaged in the February 2011 earthquake. The collapse of a key supporting shear wall caused the building to visibly lean to one side.
A photograph of the earthquake damage to the Avonmore House on the corner of Hereford Street and Latimer Square. Large cracks have formed in the building, causing sections of the masonry to crumble. The windows on the Hereford Street side of the building have bent out of shape and many of the glass panes have shattered. USAR codes have been spray painted on the column next to the door. In the distance wire fencing has been placed across the street as a cordon.
Tree mortality is a fundamental process governing forest dynamics, but understanding tree mortality patterns is challenging because large, long-term datasets are required. Describing size-specific mortality patterns can be especially difficult, due to few trees in larger size classes. We used permanent plot data from Nothofagus solandri var. cliffortioides (mountain beech) forest on the eastern slopes of the Southern Alps, New Zealand, where the fates of trees on 250 plots of 0.04 ha were followed, to examine: (1) patterns of size-specific mortality over three consecutive periods spanning 30 years, each characterised by different disturbance, and (2) the strength and direction of neighbourhood crowding effects on sizespecific mortality rates. We found that the size-specific mortality function was U-shaped over the 30-year period as well as within two shorter periods characterised by small-scale pinhole beetle and windthrow disturbance. During a third period, characterised by earthquake disturbance, tree mortality was less size dependent. Small trees (,20 cm in diameter) were more likely to die, in all three periods, if surrounded by a high basal area of larger neighbours, suggesting that sizeasymmetric competition for light was a major cause of mortality. In contrast, large trees ($20 cm in diameter) were more likely to die in the first period if they had few neighbours, indicating that positive crowding effects were sometimes important for survival of large trees. Overall our results suggest that temporal variability in size-specific mortality patterns, and positive interactions between large trees, may sometimes need to be incorporated into models of forest dynamics.