Photograph captioned by BeckerFraserPhotos, "Rock fall damaged this house".
A photograph captioned by BeckerFraserPhotos, "The Cave House, well known for its bright colour, on Main Road in Redcliffs. The house was further demolished by the most recent rock fall in the 23 December 2011 earthquake".
A photograph captioned by BeckerFraserPhotos, "A recent rock fall at Main Road in Redcliffs".
A photograph captioned by BeckerFraserPhotos, "The Cave House garage on Main Road in Redcliffs".
A photograph of fallen rocks behind a row of shipping containers on Main Road in Redcliffs.
A photograph captioned by BeckerFraserPhotos, "A recent rock fall at Main Road in Redcliffs".
A photograph captioned by BeckerFraserPhotos, "A recent rock fall at Main Road in Redcliffs".
A cliff in Redcliffs showing signs of recent collapse. The grass at the foot of the cliff is scattered with fallen rocks. Two workers can be seen running wires down the side of the cliff.
A cliff above Redcliffs showing signs of recent collapse. A hole in the cliff indicates where a huge boulder dislodged during the 22 February 2011 earthquake.
Photograph captioned by BeckerFraserPhotos, "Big rock brought down by rock fall".
Photograph captioned by BeckerFraserPhotos, "Huge rocks on Heberden Avenue, Sumner".
A cliff above Redcliffs. Above it is a breeze-block building with broken windows and cracks in its masonry.
A cliff in Redcliffs showing signs of recent collapse. The grass at the foot of the cliff is scattered with fallen rocks. Two workers can be seen running wires down the side of the cliff.
Photograph captioned by BeckerFraserPhotos, "These rocks fell onto Heberden Avenue in Sumner".
A crushed trailer on a property in Redcliffs. A large rock from cliff above fell onto the trailer during the 22 February 2011 earthquake.
A photograph of a line of shipping containers protecting Main Road from rockfall. Several of the containers have covers printed with artworks.
A photograph of a line of shipping containers protecting Main Road from rockfall. Several of the containers have covers printed with artworks.
A photograph of a line of shipping containers protecting Main Road from rockfall. Several of the containers have covers printed with artworks.
Rockfall in Peacock's Gallop, seen through cordon fencing.
Rockfall in Peacock's Gallop, seen through cordon fencing.
Rockfall in Peacock's Gallop, seen through cordon fencing.
Rockfall in Peacock's Gallop, seen through cordon fencing.
The Canterbury Earthquake Sequence (CES) of 2010-2011 produced large seismic moments up to Mw 7.1. These large, near-to-surface (<15 km) ruptures triggered >6,000 rockfall boulders on the Port Hills of Christchurch, many of which impacted houses and affected the livelihoods of people within the impacted area. From these disastrous and unpredicted natural events a need arose to be able to assess the areas affected by rockfall events in the future, where it is known that a rockfall is possible from a specific source outcrop but the potential boulder runout and dynamics are not understood. The distribution of rockfall deposits is largely constrained by the physical properties and processes of the boulder and its motion such as block density, shape and size, block velocity, bounce height, impact and rebound angle, as well as the properties of the substrate. Numerical rockfall models go some way to accounting for all the complex factors in an algorithm, commonly parameterised in a user interface where site-specific effects can be calibrated. Calibration of these algorithms requires thorough field checks and often experimental practises. The purpose of this project, which began immediately following the most destructive rupture of the CES (February 22, 2011), is to collate data to characterise boulder falls, and to use this information, supplemented by a set of anthropogenic boulder fall data, to perform an in-depth calibration of the three-dimensional numerical rockfall model RAMMS::Rockfall. The thesis covers the following topics: • Use of field data to calibrate RAMMS. Boulder impact trails in the loess-colluvium soils at Rapaki Bay have been used to estimate ranges of boulder velocities and bounce heights. RAMMS results replicate field data closely; it is concluded that the model is appropriate for analysing the earthquake-triggered boulder trails at Rapaki Bay, and that it can be usefully applied to rockfall trajectory and hazard assessment at this and similar sites elsewhere. • Detailed analysis of dynamic rockfall processes, interpreted from recorded boulder rolling experiments, and compared to RAMMS simulated results at the same site. Recorded rotational and translational velocities of a particular boulder show that the boulder behaves logically and dynamically on impact with different substrate types. Simulations show that seasonal changes in soil moisture alter rockfall dynamics and runout predictions within RAMMS, and adjustments are made to the calibration to reflect this; suggesting that in hazard analysis a rockfall model should be calibrated to dry rather than wet soil conditions to anticipate the most serious outcome. • Verifying the model calibration for a separate site on the Port Hills. The results of the RAMMS simulations show the effectiveness of calibration against a real data set, as well as the effectiveness of vegetation as a rockfall barrier/retardant. The results of simulations are compared using hazard maps, where the maximum runouts match well the mapped CES fallen boulder maximum runouts. The results of the simulations in terms of frequency distribution of deposit locations on the slope are also compared with those of the CES data, using the shadow angle tool to apportion slope zones. These results also replicate real field data well. Results show that a maximum runout envelope can be mapped, as well as frequency distribution of deposited boulders for hazard (and thus risk) analysis purposes. The accuracy of the rockfall runout envelope and frequency distribution can be improved by comprehensive vegetation and substrate mapping. The topics above define the scope of the project, limiting the focus to rockfall processes on the Port Hills, and implications for model calibration for the wider scientific community. The results provide a useful rockfall analysis methodology with a defensible and replicable calibration process, that has the potential to be applied to other lithologies and substrates. Its applications include a method of analysis for the selection and positioning of rockfall countermeasure design; site safety assessment for scaling and demolition works; and risk analysis and land planning for future construction in Christchurch.
A photograph of recent rockfall in the Port Hills.
A photograph of recent rockfall in the Port Hills.
A photograph of recent rockfall in the Port Hills.
A photograph of recent rockfall in the Port Hills.
An infographic showing a simulation of rockfall risk in Sumner.
Rockfall from the cliffs in Sumner littering a bowling green.
Photograph captioned by BeckerFraserPhotos, "Rock falls on Sumner Road".